Каков порядковый номер калия

Potassium, ₁₉K

Potassium pearls (in paraffin oil, ~5 mm each)
Potassium
Pronunciation	​(pə-TASS-ee-əm)
Appearance	silvery white, faint bluish-purple hue when exposed to air
Standard atomic weight Ar°(K)
	39.0983±0.0001 39.098±0.001 (abridged)[1]
Potassium in the periodic table
Hydrogen Helium Lithium Beryllium Boron Carbon Nitrogen Oxygen Fluorine Neon Sodium Magnesium Aluminium Silicon Phosphorus Sulfur Chlorine Argon Potassium Calcium Scandium Titanium Vanadium Chromium Manganese Iron Cobalt Nickel Copper Zinc Gallium Germanium Arsenic Selenium Bromine Krypton Rubidium Strontium Yttrium Zirconium Niobium Molybdenum Technetium Ruthenium Rhodium Palladium Silver Cadmium Indium Tin Antimony Tellurium Iodine Xenon Caesium Barium Lanthanum Cerium Praseodymium Neodymium Promethium Samarium Europium Gadolinium Terbium Dysprosium Holmium Erbium Thulium Ytterbium Lutetium Hafnium Tantalum Tungsten Rhenium Osmium Iridium Platinum Gold Mercury (element) Thallium Lead Bismuth Polonium Astatine Radon Francium Radium Actinium Thorium Protactinium Uranium Neptunium Plutonium Americium Curium Berkelium Californium Einsteinium Fermium Mendelevium Nobelium Lawrencium Rutherfordium Dubnium Seaborgium Bohrium Hassium Meitnerium Darmstadtium Roentgenium Copernicium Nihonium Flerovium Moscovium Livermorium Tennessine Oganesson Na ↑ K ↓ Rb argon ← potassium → calcium
Atomic number (Z)	19
Group	group 1: hydrogen and alkali metals
Period	period 4
Block	s-block
Electron configuration	[Ar] 4s1
Electrons per shell	2, 8, 8, 1
Physical properties
Phase at STP	solid
Melting point	336.7 K ​(63.5 °C, ​146.3 °F)
Boiling point	1030.793 K ​(757.643 °C, ​1395.757 °F)[2]
Density (near r.t.)	0.89 g/cm3
when liquid (at m.p.)	0.82948 g/cm3[2]
Critical point	2223 K, 16 MPa[3]
Heat of fusion	2.33 kJ/mol
Heat of vaporization	76.9 kJ/mol
Molar heat capacity	29.6 J/(mol·K)
Atomic properties
Oxidation states	−1, +1 (a strongly basic oxide)
Electronegativity	Pauling scale: 0.82
Ionization energies	1st: 418.8 kJ/mol 2nd: 3052 kJ/mol 3rd: 4420 kJ/mol (more)
Atomic radius	empirical: 227 pm
Covalent radius	203±12 pm
Van der Waals radius	275 pm
Spectral lines of potassium
Other properties
Natural occurrence	primordial
Crystal structure	​body-centered cubic (bcc)
Speed of sound thin rod	2000 m/s (at 20 °C)
Thermal expansion	83.3 µm/(m⋅K) (at 25 °C)
Thermal conductivity	102.5 W/(m⋅K)
Electrical resistivity	72 nΩ⋅m (at 20 °C)
Magnetic ordering	paramagnetic[4]
Molar magnetic susceptibility	+20.8×10−6 cm3/mol (298 K)[5]
Young’s modulus	3.53 GPa
Shear modulus	1.3 GPa
Bulk modulus	3.1 GPa
Mohs hardness	0.4
Brinell hardness	0.363 MPa
CAS Number	7440-09-7
History
Discovery and first isolation	Humphry Davy (1807)
Symbol	«K»: from New Latin kalium
Main isotopes of potassium v e
Iso­tope Decay abun­dance half-life (t1/2) mode pro­duct 39K 93.258% stable 40K 0.012% 1.248×109 y β− 40Ca ε 40Ar β+ 40Ar 41K 6.730% stable
Category: Potassium view talk edit | references

Potassium is the chemical element with the symbol K (from Neo-Latin kalium) and atomic number 19. It is a silvery-white metal that is soft enough to easily cut with a knife.^[6] Potassium metal reacts rapidly with atmospheric oxygen to form flaky white potassium peroxide in only seconds of exposure. It was first isolated from potash, the ashes of plants, from which its name derives. In the periodic table, potassium is one of the alkali metals, all of which have a single valence electron in the outer electron shell, which is easily removed to create an ion with a positive charge (which combines with anions to form salts). In nature, potassium occurs only in ionic salts. Elemental potassium reacts vigorously with water, generating sufficient heat to ignite hydrogen emitted in the reaction, and burning with a lilac-colored flame. It is found dissolved in seawater (which is 0.04% potassium by weight),^[7][8] and occurs in many minerals such as orthoclase, a common constituent of granites and other igneous rocks.^[9]

Potassium is chemically very similar to sodium, the previous element in group 1 of the periodic table. They have a similar first ionization energy, which allows for each atom to give up its sole outer electron. It was suspected in 1702 that they were distinct elements that combine with the same anions to make similar salts,^[10] and this was proven in 1807 through using electrolysis. Naturally occurring potassium is composed of three isotopes, of which ⁴⁰
K is radioactive. Traces of ⁴⁰
K are found in all potassium, and it is the most common radioisotope in the human body.

Potassium ions are vital for the functioning of all living cells. The transfer of potassium ions across nerve cell membranes is necessary for normal nerve transmission; potassium deficiency and excess can each result in numerous signs and symptoms, including an abnormal heart rhythm and various electrocardiographic abnormalities. Fresh fruits and vegetables are good dietary sources of potassium. The body responds to the influx of dietary potassium, which raises serum potassium levels, by shifting potassium from outside to inside cells and increasing potassium excretion by the kidneys.

Most industrial applications of potassium exploit the high solubility of its compounds in water, such as saltwater soap. Heavy crop production rapidly depletes the soil of potassium, and this can be remedied with agricultural fertilizers containing potassium, accounting for 95% of global potassium chemical production.^[11]

Etymology

The English name for the element potassium comes from the word potash,^[12] which refers to an early method of extracting various potassium salts: placing in a pot the ash of burnt wood or tree leaves, adding water, heating, and evaporating the solution. When Humphry Davy first isolated the pure element using electrolysis in 1807, he named it potassium, which he derived from the word potash.

The symbol K stems from kali, itself from the root word alkali, which in turn comes from Arabic: القَلْيَه al-qalyah ‘plant ashes’. In 1797, the German chemist Martin Klaproth discovered «potash» in the minerals leucite and lepidolite, and realized that «potash» was not a product of plant growth but actually contained a new element, which he proposed calling kali.^[13] In 1807, Humphry Davy produced the element via electrolysis: in 1809, Ludwig Wilhelm Gilbert proposed the name Kalium for Davy’s «potassium».^[14] In 1814, the Swedish chemist Berzelius advocated the name kalium for potassium, with the chemical symbol K.^[15]

The English and French-speaking countries adopted Davy and Gay-Lussac/Thénard’s name Potassium, whereas the Germanic countries adopted Gilbert/Klaproth’s name Kalium.^[16] The «Gold Book» of the International Union of Pure and Applied Chemistry has designated the official chemical symbol as K.^[17]

Properties

Physical

Potassium is the second least dense metal after lithium. It is a soft solid with a low melting point, and can be easily cut with a knife. Freshly cut potassium is silvery in appearance, but it begins to tarnish toward gray immediately on exposure to air.^[18] In a flame test, potassium and its compounds emit a lilac color with a peak emission wavelength of 766.5 nanometers.^[19]

Neutral potassium atoms have 19 electrons, one more than the configuration of the noble gas argon. Because of its low first ionization energy of 418.8 kJ/mol, the potassium atom is much more likely to lose the last electron and acquire a positive charge, although negatively charged alkalide K⁻ ions are not impossible.^[20] In contrast, the second ionization energy is very high (3052 kJ/mol).

Chemical

Potassium reacts with oxygen, water, and carbon dioxide components in air. With oxygen it forms potassium peroxide. With water potassium forms potassium hydroxide (KOH). The reaction of potassium with water can be violently exothermic, especially since the coproduced hydrogen gas can ignite. Because of this, potassium and the liquid sodium-potassium (NaK) alloy are potent desiccants, although they are no longer used as such.^[21]

Compounds

Four oxides of potassium are well studied: potassium oxide (K₂O), potassium peroxide (K₂O₂), potassium superoxide (KO₂)^[22] and potassium ozonide (KO₃). The binary potassium-oxygen compounds react with water forming KOH.

KOH is a strong base. Illustrating its hydrophilic character, as much as 1.21 kg of KOH can dissolve in a single liter of water.^[23][24] Anhydrous KOH is rarely encountered. KOH reacts readily with carbon dioxide (CO₂) to produce potassium carbonate (K₂CO₃), and in principle could be used to remove traces of the gas from air. Like the closely related sodium hydroxide, KOH reacts with fats to produce soaps.

In general, potassium compounds are ionic and, owing to the high hydration energy of the K⁺ ion, have excellent water solubility. The main species in water solution are the aquo complexes [K(H₂O)_n]⁺ where n = 6 and 7.^[25]

Potassium heptafluorotantalate (K₂[TaF₇]) is an intermediate in the purification of tantalum from the otherwise persistent contaminant of niobium.^[26]

Organopotassium compounds illustrate nonionic compounds of potassium. They feature highly polar covalent K–C bonds. Examples include benzyl potassium KCH₂C₆H₅. Potassium intercalates into graphite to give a variety of graphite intercalation compounds, including KC₈.

Isotopes

There are 25 known isotopes of potassium, three of which occur naturally: ³⁹
K (93.3%), ⁴⁰
K (0.0117%), and ⁴¹
K (6.7%) (by mole fraction). Naturally occurring ⁴⁰
K has a half-life of 1.250×10⁹ years. It decays to stable ⁴⁰
Ar by electron capture or positron emission (11.2%) or to stable ⁴⁰
Ca by beta decay (88.8%).^[27] The decay of ⁴⁰
K to ⁴⁰
Ar is the basis of a common method for dating rocks. The conventional K-Ar dating method depends on the assumption that the rocks contained no argon at the time of formation and that all the subsequent radiogenic argon (⁴⁰
Ar) was quantitatively retained. Minerals are dated by measurement of the concentration of potassium and the amount of radiogenic ⁴⁰
Ar that has accumulated. The minerals best suited for dating include biotite, muscovite, metamorphic hornblende, and volcanic feldspar; whole rock samples from volcanic flows and shallow instrusives can also be dated if they are unaltered.^[27][28] Apart from dating, potassium isotopes have been used as tracers in studies of weathering and for nutrient cycling studies because potassium is a macronutrient required for life^[29] on Earth.

⁴⁰
K occurs in natural potassium (and thus in some commercial salt substitutes) in sufficient quantity that large bags of those substitutes can be used as a radioactive source for classroom demonstrations. ⁴⁰
K is the radioisotope with the largest abundance in the human body. In healthy animals and people, ⁴⁰
K represents the largest source of radioactivity, greater even than ¹⁴
C. In a human body of 70 kg, about 4,400 nuclei of ⁴⁰
K decay per second.^[30] The activity of natural potassium is 31 Bq/g.^[31]

Cosmic formation and distribution

Potassium is formed in supernovae by nucleosynthesis from lighter atoms. Potassium is principally created in Type II supernovae via an explosive oxygen-burning process.^[32] (These are fusion reactions; do not confuse with chemical burning between potassium and oxygen.) ⁴⁰
K is also formed in s-process nucleosynthesis and the neon burning process.^[33]

Potassium is the 20th most abundant element in the solar system and the 17th most abundant element by weight in the Earth. It makes up about 2.6% of the weight of the Earth’s crust and is the seventh most abundant element in the crust.^[34] The potassium concentration in seawater is 0.39 g/L^[7] (0.039 wt/v%), about one twenty-seventh the concentration of sodium.^[35][36]

Potash

Potash is primarily a mixture of potassium salts because plants have little or no sodium content, and the rest of a plant’s major mineral content consists of calcium salts of relatively low solubility in water. While potash has been used since ancient times, its composition was not understood. Georg Ernst Stahl obtained experimental evidence that led him to suggest the fundamental difference of sodium and potassium salts in 1702,^[10] and Henri Louis Duhamel du Monceau was able to prove this difference in 1736.^[37] The exact chemical composition of potassium and sodium compounds, and the status as chemical element of potassium and sodium, was not known then, and thus Antoine Lavoisier did not include the alkali in his list of chemical elements in 1789.^[38][39] For a long time the only significant applications for potash were the production of glass, bleach, soap and gunpowder as potassium nitrate.^[40] Potassium soaps from animal fats and vegetable oils were especially prized because they tend to be more water-soluble and of softer texture, and are therefore known as soft soaps.^[11] The discovery by Justus Liebig in 1840 that potassium is a necessary element for plants and that most types of soil lack potassium^[41] caused a steep rise in demand for potassium salts. Wood-ash from fir trees was initially used as a potassium salt source for fertilizer, but, with the discovery in 1868 of mineral deposits containing potassium chloride near Staßfurt, Germany, the production of potassium-containing fertilizers began at an industrial scale.^[42][43][44] Other potash deposits were discovered, and by the 1960s Canada became the dominant producer.^[45][46]

Metal

Potassium metal was first isolated in 1807 by Humphry Davy, who derived it by electrolysis of molten KOH with the newly discovered voltaic pile. Potassium was the first metal that was isolated by electrolysis.^[47] Later in the same year, Davy reported extraction of the metal sodium from a mineral derivative (caustic soda, NaOH, or lye) rather than a plant salt, by a similar technique, demonstrating that the elements, and thus the salts, are different.^{[38][39][48][49]} Although the production of potassium and sodium metal should have shown that both are elements, it took some time before this view was universally accepted.^[39]

Because of the sensitivity of potassium to water and air, air-free techniques are normally employed for handling the element. It is unreactive toward nitrogen and saturated hydrocarbons such as mineral oil or kerosene.^[50] It readily dissolves in liquid ammonia, up to 480 g per 1000 g of ammonia at 0 °C. Depending on the concentration, the ammonia solutions are blue to yellow, and their electrical conductivity is similar to that of liquid metals. Potassium slowly reacts with ammonia to form KNH
₂, but this reaction is accelerated by minute amounts of transition metal salts.^[51] Because it can reduce the salts to the metal, potassium is often used as the reductant in the preparation of finely divided metals from their salts by the Rieke method.^[52] Illustrative is the preparation of magnesium:

MgCl₂ + 2 K → Mg + 2 KCl

Geology

Elemental potassium does not occur in nature because of its high reactivity. It reacts violently with water (see section Precautions below)^[50] and also reacts with oxygen. Orthoclase (potassium feldspar) is a common rock-forming mineral. Granite for example contains 5% potassium, which is well above the average in the Earth’s crust. Sylvite (KCl), carnallite (KCl·MgCl₂·6H₂O), kainite (MgSO₄·KCl·3H₂O) and langbeinite (MgSO₄·K₂SO₄) are the minerals found in large evaporite deposits worldwide. The deposits often show layers starting with the least soluble at the bottom and the most soluble on top.^[36] Deposits of niter (potassium nitrate) are formed by decomposition of organic material in contact with atmosphere, mostly in caves; because of the good water solubility of niter the formation of larger deposits requires special environmental conditions.^[53]

Biological role

Potassium is the eighth or ninth most common element by mass (0.2%) in the human body, so that a 60 kg adult contains a total of about 120 g of potassium.^[54] The body has about as much potassium as sulfur and chlorine, and only calcium and phosphorus are more abundant (with the exception of the ubiquitous CHON elements).^[55] Potassium ions are present in a wide variety of proteins and enzymes.^[56]

Biochemical function

Potassium levels influence multiple physiological processes, including^[57][58][59]

• resting cellular-membrane potential and the propagation of action potentials in neuronal, muscular, and cardiac tissue. Due to the electrostatic and chemical properties, K⁺ ions are larger than Na⁺ ions, and ion channels and pumps in cell membranes can differentiate between the two ions, actively pumping or passively passing one of the two ions while blocking the other.^[60]
• hormone secretion and action
• vascular tone
• systemic blood pressure control
• gastrointestinal motility
• acid–base homeostasis
• glucose and insulin metabolism
• mineralocorticoid action
• renal concentrating ability
• fluid and electrolyte balance

Homeostasis

Potassium homeostasis denotes the maintenance of the total body potassium content, plasma potassium level, and the ratio of the intracellular to extracellular potassium concentrations within narrow limits, in the face of pulsatile intake (meals), obligatory renal excretion, and shifts between intracellular and extracellular compartments.

Plasma levels

Plasma potassium is normally kept at 3.5 to 5.5 millimoles (mmol) [or milliequivalents (mEq)] per liter by multiple mechanisms.^[61] Levels outside this range are associated with an increasing rate of death from multiple causes,^[62] and some cardiac, kidney,^[63] and lung diseases progress more rapidly if serum potassium levels are not maintained within the normal range.

An average meal of 40–50 mmol presents the body with more potassium than is present in all plasma (20–25 mmol). However, this surge causes the plasma potassium to rise only 10% at most as a result of prompt and efficient clearance by both renal and extra-renal mechanisms.^[64]

Hypokalemia, a deficiency of potassium in the plasma, can be fatal if severe. Common causes are increased gastrointestinal loss (vomiting, diarrhea), and increased renal loss (diuresis).^[65] Deficiency symptoms include muscle weakness, paralytic ileus, ECG abnormalities, decreased reflex response; and in severe cases, respiratory paralysis, alkalosis, and cardiac arrhythmia.^[66]

Control mechanisms

Potassium content in the plasma is tightly controlled by four basic mechanisms, which have various names and classifications. The four are 1) a reactive negative-feedback system, 2) a reactive feed-forward system, 3) a predictive or circadian system, and 4) an internal or cell membrane transport system. Collectively, the first three are sometimes termed the «external potassium homeostasis system»;^[67] and the first two, the «reactive potassium homeostasis system».

• The reactive negative-feedback system refers to the system that induces renal secretion of potassium in response to a rise in the plasma potassium (potassium ingestion, shift out of cells, or intravenous infusion.)
• The reactive feed-forward system refers to an incompletely understood system that induces renal potassium secretion in response to potassium ingestion prior to any rise in the plasma potassium. This is probably initiated by gut cell potassium receptors that detect ingested potassium and trigger vagal afferent signals to the pituitary gland.
• The predictive or circadian system increases renal secretion of potassium during mealtime hours (e.g. daytime for humans, nighttime for rodents) independent of the presence, amount, or absence of potassium ingestion. It is mediated by a circadian oscillator in the suprachiasmatic nucleus of the brain (central clock), which causes the kidney (peripheral clock) to secrete potassium in this rhythmic circadian fashion.

  

  The action of the sodium-potassium pump is an example of primary active transport. The two carrier proteins embedded in the cell membrane on the left are using ATP to move sodium out of the cell against the concentration gradient; The two proteins on the right are using secondary active transport to move potassium into the cell. This process results in reconstitution of ATP.

• The ion transport system moves potassium across the cell membrane using two mechanisms. One is active and pumps sodium out of, and potassium into, the cell. The other is passive and allows potassium to leak out of the cell. Potassium and sodium cations influence fluid distribution between intracellular and extracellular compartments by osmotic forces. The movement of potassium and sodium through the cell membrane is mediated by the Na⁺/K⁺-ATPase pump.^[68] This ion pump uses ATP to pump three sodium ions out of the cell and two potassium ions into the cell, creating an electrochemical gradient and electromotive force across the cell membrane. The highly selective potassium ion channels (which are tetramers) are crucial for hyperpolarization inside neurons after an action potential is triggered, to cite one example. The most recently discovered potassium ion channel is KirBac3.1, which makes a total of five potassium ion channels (KcsA, KirBac1.1, KirBac3.1, KvAP, and MthK) with a determined structure. All five are from prokaryotic species.^[69]

Renal filtration, reabsorption, and excretion

Renal handling of potassium is closely connected to sodium handling. Potassium is the major cation (positive ion) inside animal cells [150 mmol/L, (4.8 g)], while sodium is the major cation of extracellular fluid [150 mmol/L, (3.345 g)]. In the kidneys, about 180 liters of plasma is filtered through the glomeruli and into the renal tubules per day.^[70] This filtering involves about 600 g of sodium and 33 g of potassium. Since only 1–10 g of sodium and 1–4 g of potassium are likely to be replaced by diet, renal filtering must efficiently reabsorb the remainder from the plasma.

Sodium is reabsorbed to maintain extracellular volume, osmotic pressure, and serum sodium concentration within narrow limits. Potassium is reabsorbed to maintain serum potassium concentration within narrow limits.^[71] Sodium pumps in the renal tubules operate to reabsorb sodium. Potassium must be conserved, but because the amount of potassium in the blood plasma is very small and the pool of potassium in the cells is about 30 times as large, the situation is not so critical for potassium. Since potassium is moved passively^[72][73] in counter flow to sodium in response to an apparent (but not actual) Donnan equilibrium,^[74] the urine can never sink below the concentration of potassium in serum except sometimes by actively excreting water at the end of the processing. Potassium is excreted twice and reabsorbed three times before the urine reaches the collecting tubules.^[75] At that point, urine usually has about the same potassium concentration as plasma. At the end of the processing, potassium is secreted one more time if the serum levels are too high.^{[citation needed]}

With no potassium intake, it is excreted at about 200 mg per day until, in about a week, potassium in the serum declines to a mildly deficient level of 3.0–3.5 mmol/L.^[76] If potassium is still withheld, the concentration continues to fall until a severe deficiency causes eventual death.^[77]

The potassium moves passively through pores in the cell membrane. When ions move through Ion transporters (pumps) there is a gate in the pumps on both sides of the cell membrane and only one gate can be open at once. As a result, approximately 100 ions are forced through per second. Ion channel have only one gate, and there only one kind of ion can stream through, at 10 million to 100 million ions per second.^[78] Calcium is required to open the pores,^[79] although calcium may work in reverse by blocking at least one of the pores.^[80] Carbonyl groups inside the pore on the amino acids mimic the water hydration that takes place in water solution^[81] by the nature of the electrostatic charges on four carbonyl groups inside the pore.^[82]

Nutrition

Dietary recommendations

The U.S. National Academy of Medicine (NAM), on behalf of both the U.S. and Canada, sets Dietary Reference Intakes, including Estimated Average Requirements (EARs) and Recommended Dietary Allowances (RDAs), or Adequate Intakes (AIs) for when there is not sufficient information to set EARs and RDAs.

For both males and females under 9 years of age, the AIs for potassium are: 400 mg of potassium for 0-6-month-old infants, 860 mg of potassium for 7-12-month-old infants, 2,000 mg of potassium for 1-3-year-old children, and 2,300 mg of potassium for 4-8-year-old children.

For males 9 years of age and older, the AIs for potassium are: 2,500 mg of potassium for 9-13-year-old males, 3,000 mg of potassium for 14-18-year-old males, and 3,400 mg for males that are 19 years of age and older.

For females 9 years of age and older, the AIs for potassium are: 2,300 mg of potassium for 9-18-year-old females, and 2,600 mg of potassium for females that are 19 years of age and older.

For pregnant and lactating females, the AIs for potassium are: 2,600 mg of potassium for 14-18-year-old pregnant females, 2,900 mg for pregnant females that are 19 years of age and older; furthermore, 2,500 mg of potassium for 14-18-year-old lactating females, and 2,800 mg for lactating females that are 19 years of age and older. As for safety, the NAM also sets tolerable upper intake levels (ULs) for vitamins and minerals, but for potassium the evidence was insufficient, so no UL was established.^[83][84]

As of 2004, most Americans adults consume less than 3,000 mg.^[85]

Likewise, in the European Union, in particular in Germany, and Italy, insufficient potassium intake is somewhat common.^[86] The British National Health Service recommends a similar intake, saying that adults need 3,500 mg per day and that excess amounts may cause health problems such as stomach pain and diarrhea.^[87]

In 2019, the National Academies of Sciences, Engineering, and Medicine revised the Adequate Intake for potassium to 2,600 mg/day for females 19 years of age and older who are not pregnant or lactating, and 3,400 mg/day for males 19 years of age and older.^[88][89]

Food sources

Potassium is present in all fruits, vegetables, meat and fish. Foods with high potassium concentrations include yam, parsley, dried apricots, milk, chocolate, all nuts (especially almonds and pistachios), potatoes, bamboo shoots, bananas, avocados, coconut water, soybeans, and bran.^[90]

The United States Department of Agriculture lists tomato paste, orange juice, beet greens, white beans, potatoes, plantains, bananas, apricots, and many other dietary sources of potassium, ranked in descending order according to potassium content. A day’s worth of potassium is in 5 plantains or 11 bananas.^[91]

Deficient intake

Diets low in potassium can lead to hypertension^[92] and hypokalemia.

Supplementation

Supplements of potassium are most widely used in conjunction with diuretics that block reabsorption of sodium and water upstream from the distal tubule (thiazides and loop diuretics), because this promotes increased distal tubular potassium secretion, with resultant increased potassium excretion.^{[medical citation needed]} A variety of prescription and over-the counter supplements are available.^{[citation needed]} Potassium chloride may be dissolved in water, but the salty/bitter taste makes liquid supplements unpalatable.^[93] Typical doses range from 10 mmol (400 mg), to 20 mmol (800 mg).^{[medical citation needed]} Potassium is also available in tablets or capsules, which are formulated to allow potassium to leach slowly out of a matrix, since very high concentrations of potassium ion that occur adjacent to a solid tablet can injure the gastric or intestinal mucosa.^{[medical citation needed]} For this reason, non-prescription potassium pills are limited by law in the US to a maximum of 99 mg of potassium.^{[citation needed]}

A meta-analysis concluded that a 1640 mg increase in the daily intake of potassium was associated with a 21% lower risk of stroke.^[94] Potassium chloride and potassium bicarbonate may be useful to control mild hypertension.^[95] In 2020, potassium was the 33rd most commonly prescribed medication in the U.S., with more than 17 million prescriptions.^[96][97]

Detection by taste buds

Potassium can be detected by taste because it triggers three of the five types of taste sensations, according to concentration. Dilute solutions of potassium ions taste sweet, allowing moderate concentrations in milk and juices, while higher concentrations become increasingly bitter/alkaline, and finally also salty to the taste. The combined bitterness and saltiness of high-potassium solutions makes high-dose potassium supplementation by liquid drinks a palatability challenge.^[93][98]

Commercial production

Mining

Potassium salts such as carnallite, langbeinite, polyhalite, and sylvite form extensive evaporite deposits in ancient lake bottoms and seabeds,^[35] making extraction of potassium salts in these environments commercially viable. The principal source of potassium – potash – is mined in Canada, Russia, Belarus, Kazakhstan, Germany, Israel, the U.S., Jordan, and other places around the world.^{[99][100][101]} The first mined deposits were located near Staßfurt, Germany, but the deposits span from Great Britain over Germany into Poland. They are located in the Zechstein and were deposited in the Middle to Late Permian. The largest deposits ever found lie 1,000 meters (3,300 feet) below the surface of the Canadian province of Saskatchewan. The deposits are located in the Elk Point Group produced in the Middle Devonian. Saskatchewan, where several large mines have operated since the 1960s pioneered the technique of freezing of wet sands (the Blairmore formation) to drive mine shafts through them. The main potash mining company in Saskatchewan until its merge was the Potash Corporation of Saskatchewan, now Nutrien.^[102] The water of the Dead Sea is used by Israel and Jordan as a source of potash, while the concentration in normal oceans is too low for commercial production at current prices.^[100][101]

Several methods are used to separate potassium salts from sodium and magnesium compounds. The most-used method is fractional precipitation using the solubility differences of the salts. Electrostatic separation of the ground salt mixture is also used in some mines. The resulting sodium and magnesium waste is either stored underground or piled up in slag heaps. Most of the mined potassium mineral ends up as potassium chloride after processing. The mineral industry refers to potassium chloride either as potash, muriate of potash, or simply MOP.^[36]

Pure potassium metal can be isolated by electrolysis of its hydroxide in a process that has changed little since it was first used by Humphry Davy in 1807. Although the electrolysis process was developed and used in industrial scale in the 1920s, the thermal method by reacting sodium with potassium chloride in a chemical equilibrium reaction became the dominant method in the 1950s.

Na + KCl → NaCl + K

The production of sodium potassium alloys is accomplished by changing the reaction time and the amount of sodium used in the reaction. The Griesheimer process employing the reaction of potassium fluoride with calcium carbide was also used to produce potassium.^[36][103]

2 KF + CaC₂ → 2 K + CaF₂ + 2 C

Reagent-grade potassium metal costs about $10.00/pound ($22/kg) in 2010 when purchased by the tonne. Lower purity metal is considerably cheaper. The market is volatile because long-term storage of the metal is difficult. It must be stored in a dry inert gas atmosphere or anhydrous mineral oil to prevent the formation of a surface layer of potassium superoxide, a pressure-sensitive explosive that detonates when scratched. The resulting explosion often starts a fire difficult to extinguish.^[104][105]

Cation identification

Potassium is now quantified by ionization techniques, but at one time it was quantitated by gravimetric analysis.

Reagents used to precipitate potassium salts include sodium tetraphenylborate, hexachloroplatinic acid, and sodium cobaltinitrite into respectively potassium tetraphenylborate, potassium hexachloroplatinate, and potassium cobaltinitrite.^[50]
The reaction with sodium cobaltinitrite is illustrative:

3 K⁺ + Na₃[Co(NO₂)₆] → K₃[Co(NO₂)₆] + 3 Na⁺

The potassium cobaltinitrite is obtained as a yellow solid.

Commercial uses

Fertilizer

Potassium ions are an essential component of plant nutrition and are found in most soil types.^[11] They are used as a fertilizer in agriculture, horticulture, and hydroponic culture in the form of chloride (KCl), sulfate (K₂SO₄), or nitrate (KNO₃), representing the ‘K’ in ‘NPK’. Agricultural fertilizers consume 95% of global potassium chemical production, and about 90% of this potassium is supplied as KCl.^[11] The potassium content of most plants ranges from 0.5% to 2% of the harvested weight of crops, conventionally expressed as amount of K₂O. Modern high-yield agriculture depends upon fertilizers to replace the potassium lost at harvest. Most agricultural fertilizers contain potassium chloride, while potassium sulfate is used for chloride-sensitive crops or crops needing higher sulfur content. The sulfate is produced mostly by decomposition of the complex minerals kainite (MgSO₄·KCl·3H₂O) and langbeinite (MgSO₄·K₂SO₄). Only a very few fertilizers contain potassium nitrate.^[106] In 2005, about 93% of world potassium production was consumed by the fertilizer industry.^[101] Furthermore, potassium can play a key role in nutrient cycling by controlling litter composition.^[107]

Medical use

Potassium citrate

Potassium citrate is used to treat a kidney stone condition called renal tubular acidosis.^[108]

Potassium chloride

Potassium, in the form of potassium chloride is used as a medication to treat and prevent low blood potassium.^[109] Low blood potassium may occur due to vomiting, diarrhea, or certain medications.^[110] It is given by slow injection into a vein or by mouth.^[111]

Food additives

Potassium sodium tartrate (KNaC₄H₄O₆, Rochelle salt) is a main constituent of some varieties of baking powder; it is also used in the silvering of mirrors. Potassium bromate (KBrO₃) is a strong oxidizer (E924), used to improve dough strength and rise height. Potassium bisulfite (KHSO₃) is used as a food preservative, for example in wine and beer-making (but not in meats). It is also used to bleach textiles and straw, and in the tanning of leathers.^[112][113]

Industrial

Major potassium chemicals are potassium hydroxide, potassium carbonate, potassium sulfate, and potassium chloride. Megatons of these compounds are produced annually.^[114]

KOH is a strong base, which is used in industry to neutralize strong and weak acids, to control pH and to manufacture potassium salts. It is also used to saponify fats and oils, in industrial cleaners, and in hydrolysis reactions, for example of esters.^[115][116]

Potassium nitrate (KNO₃) or saltpeter is obtained from natural sources such as guano and evaporites or manufactured via the Haber process; it is the oxidant in gunpowder (black powder) and an important agricultural fertilizer. Potassium cyanide (KCN) is used industrially to dissolve copper and precious metals, in particular silver and gold, by forming complexes. Its applications include gold mining, electroplating, and electroforming of these metals; it is also used in organic synthesis to make nitriles. Potassium carbonate (K₂CO₃ or potash) is used in the manufacture of glass, soap, color TV tubes, fluorescent lamps, textile dyes and pigments.^[117] Potassium permanganate (KMnO₄) is an oxidizing, bleaching and purification substance and is used for production of saccharin. Potassium chlorate (KClO₃) is added to matches and explosives. Potassium bromide (KBr) was formerly used as a sedative and in photography.^[11]

While potassium chromate (K₂CrO₄) is used in the manufacture of a host of different commercial products such as inks, dyes, wood stains (by reacting with the tannic acid in wood), explosives, fireworks, fly paper, and safety matches,^[118] as well as in the tanning of leather, all of these uses are due to the chemistry of the chromate ion rather than to that of the potassium ion.^[119]

Niche uses

There are thousands of uses of various potassium compounds. One example is potassium superoxide, KO₂, an orange solid that acts as a portable source of oxygen and a carbon dioxide absorber. It is widely used in respiration systems in mines, submarines and spacecraft as it takes less volume than the gaseous oxygen.^[120][121]

4 KO₂ + 2 CO₂ → 2 K₂CO₃ + 3 O₂

Another example is potassium cobaltinitrite, K₃[Co(NO₂)₆], which is used as artist’s pigment under the name of Aureolin or Cobalt Yellow.^[122]

The stable isotopes of potassium can be laser cooled and used to probe fundamental and technological problems in quantum physics. The two bosonic isotopes possess convenient Feshbach resonances to enable studies requiring tunable interactions, while ⁴⁰
K is one of only two stable fermions amongst the alkali metals.^[123]

Laboratory uses

An alloy of sodium and potassium, NaK is a liquid used as a heat-transfer medium and a desiccant for producing dry and air-free solvents. It can also be used in reactive distillation.^[124] The ternary alloy of 12% Na, 47% K and 41% Cs has the lowest melting point of −78 °C of any metallic compound.^[18]

Metallic potassium is used in several types of magnetometers.^[125]

Precautions

Potassium

Hazards
GHS labelling:
Pictograms
Signal word	Danger
Hazard statements	H260, H314
Precautionary statements	P223, P231+P232, P280, P305+P351+P338, P370+P378, P422[126]
NFPA 704 (fire diamond)	3 3 2 W

Potassium metal can react violently with water producing KOH and hydrogen gas.

2 K(s) + 2 H₂O(l) → 2 KOH(aq) + H₂(g)↑

This reaction is exothermic and releases sufficient heat to ignite the resulting hydrogen in the presence of oxygen. Finely powdered potassium ignites in air at room temperature. The bulk metal ignites in air if heated. Because its density is 0.89 g/cm³, burning potassium floats in water that exposes it to atmospheric oxygen. Many common fire extinguishing agents, including water, either are ineffective or make a potassium fire worse. Nitrogen, argon, sodium chloride (table salt), sodium carbonate (soda ash), and silicon dioxide (sand) are effective if they are dry. Some Class D dry powder extinguishers designed for metal fires are also effective. These agents deprive the fire of oxygen and cool the potassium metal.^[127]

During storage, potassium forms peroxides and superoxides. These peroxides may react violently with organic compounds such as oils. Both peroxides and superoxides may react explosively with metallic potassium.^[128]

Because potassium reacts with water vapor in the air, it is usually stored under anhydrous mineral oil or kerosene. Unlike lithium and sodium, however, potassium should not be stored under oil for longer than six months, unless in an inert (oxygen free) atmosphere, or under vacuum. After prolonged storage in air dangerous shock-sensitive peroxides can form on the metal and under the lid of the container, and can detonate upon opening.^[129]

Ingestion of large amounts of potassium compounds can lead to hyperkalemia, strongly influencing the cardiovascular system.^[130][131] Potassium chloride is used in the U.S. for lethal injection executions.^[130]

See also

References

Bibliography

• Burkhardt, Elizabeth R. (2006). «Potassium and Potassium Alloys». Ullmann’s Encyclopedia of Industrial Chemistry. Vol. A22. pp. 31–38. doi:10.1002/14356007.a22_031.pub2. ISBN 978-3-527-30673-2.
• Greenwood, Norman N.; Earnshaw, Alan (1997). Chemistry of the Elements (2nd ed.). Butterworth-Heinemann. ISBN 978-0-08-037941-8.
• Holleman, Arnold F.; Wiberg, Egon; Wiberg, Nils (2007). «Potassium». Lehrbuch der Anorganischen Chemie (in German) (91–100 ed.). Walter de Gruyter. ISBN 978-3110177701.
• Schultz, H.; et al. (2006). «Potassium compounds». Ullmann’s Encyclopedia of Industrial Chemistry. Vol. A22. pp. 39–103. doi:10.1002/14356007.a22_031.pub2. ISBN 978-3-527-30673-2.
• National Nutrient Database Archived 2014-08-10 at the Wayback Machine at USDA Website

External links

• «Potassium». Drug Information Portal. U.S. National Library of Medicine.

Potassium, ₁₉K

Potassium pearls (in paraffin oil, ~5 mm each)
Potassium
Pronunciation	​(pə-TASS-ee-əm)
Appearance	silvery white, faint bluish-purple hue when exposed to air
Standard atomic weight Ar°(K)
	39.0983±0.0001 39.098±0.001 (abridged)[1]
Potassium in the periodic table
Hydrogen Helium Lithium Beryllium Boron Carbon Nitrogen Oxygen Fluorine Neon Sodium Magnesium Aluminium Silicon Phosphorus Sulfur Chlorine Argon Potassium Calcium Scandium Titanium Vanadium Chromium Manganese Iron Cobalt Nickel Copper Zinc Gallium Germanium Arsenic Selenium Bromine Krypton Rubidium Strontium Yttrium Zirconium Niobium Molybdenum Technetium Ruthenium Rhodium Palladium Silver Cadmium Indium Tin Antimony Tellurium Iodine Xenon Caesium Barium Lanthanum Cerium Praseodymium Neodymium Promethium Samarium Europium Gadolinium Terbium Dysprosium Holmium Erbium Thulium Ytterbium Lutetium Hafnium Tantalum Tungsten Rhenium Osmium Iridium Platinum Gold Mercury (element) Thallium Lead Bismuth Polonium Astatine Radon Francium Radium Actinium Thorium Protactinium Uranium Neptunium Plutonium Americium Curium Berkelium Californium Einsteinium Fermium Mendelevium Nobelium Lawrencium Rutherfordium Dubnium Seaborgium Bohrium Hassium Meitnerium Darmstadtium Roentgenium Copernicium Nihonium Flerovium Moscovium Livermorium Tennessine Oganesson Na ↑ K ↓ Rb argon ← potassium → calcium
Atomic number (Z)	19
Group	group 1: hydrogen and alkali metals
Period	period 4
Block	s-block
Electron configuration	[Ar] 4s1
Electrons per shell	2, 8, 8, 1
Physical properties
Phase at STP	solid
Melting point	336.7 K ​(63.5 °C, ​146.3 °F)
Boiling point	1030.793 K ​(757.643 °C, ​1395.757 °F)[2]
Density (near r.t.)	0.89 g/cm3
when liquid (at m.p.)	0.82948 g/cm3[2]
Critical point	2223 K, 16 MPa[3]
Heat of fusion	2.33 kJ/mol
Heat of vaporization	76.9 kJ/mol
Molar heat capacity	29.6 J/(mol·K)
Atomic properties
Oxidation states	−1, +1 (a strongly basic oxide)
Electronegativity	Pauling scale: 0.82
Ionization energies	1st: 418.8 kJ/mol 2nd: 3052 kJ/mol 3rd: 4420 kJ/mol (more)
Atomic radius	empirical: 227 pm
Covalent radius	203±12 pm
Van der Waals radius	275 pm
Spectral lines of potassium
Other properties
Natural occurrence	primordial
Crystal structure	​body-centered cubic (bcc)
Speed of sound thin rod	2000 m/s (at 20 °C)
Thermal expansion	83.3 µm/(m⋅K) (at 25 °C)
Thermal conductivity	102.5 W/(m⋅K)
Electrical resistivity	72 nΩ⋅m (at 20 °C)
Magnetic ordering	paramagnetic[4]
Molar magnetic susceptibility	+20.8×10−6 cm3/mol (298 K)[5]
Young’s modulus	3.53 GPa
Shear modulus	1.3 GPa
Bulk modulus	3.1 GPa
Mohs hardness	0.4
Brinell hardness	0.363 MPa
CAS Number	7440-09-7
History
Discovery and first isolation	Humphry Davy (1807)
Symbol	«K»: from New Latin kalium
Main isotopes of potassium v e
Iso­tope Decay abun­dance half-life (t1/2) mode pro­duct 39K 93.258% stable 40K 0.012% 1.248×109 y β− 40Ca ε 40Ar β+ 40Ar 41K 6.730% stable
Category: Potassium view talk edit | references

Potassium is the chemical element with the symbol K (from Neo-Latin kalium) and atomic number 19. It is a silvery-white metal that is soft enough to easily cut with a knife.^[6] Potassium metal reacts rapidly with atmospheric oxygen to form flaky white potassium peroxide in only seconds of exposure. It was first isolated from potash, the ashes of plants, from which its name derives. In the periodic table, potassium is one of the alkali metals, all of which have a single valence electron in the outer electron shell, which is easily removed to create an ion with a positive charge (which combines with anions to form salts). In nature, potassium occurs only in ionic salts. Elemental potassium reacts vigorously with water, generating sufficient heat to ignite hydrogen emitted in the reaction, and burning with a lilac-colored flame. It is found dissolved in seawater (which is 0.04% potassium by weight),^[7][8] and occurs in many minerals such as orthoclase, a common constituent of granites and other igneous rocks.^[9]

Potassium is chemically very similar to sodium, the previous element in group 1 of the periodic table. They have a similar first ionization energy, which allows for each atom to give up its sole outer electron. It was suspected in 1702 that they were distinct elements that combine with the same anions to make similar salts,^[10] and this was proven in 1807 through using electrolysis. Naturally occurring potassium is composed of three isotopes, of which ⁴⁰
K is radioactive. Traces of ⁴⁰
K are found in all potassium, and it is the most common radioisotope in the human body.

Potassium ions are vital for the functioning of all living cells. The transfer of potassium ions across nerve cell membranes is necessary for normal nerve transmission; potassium deficiency and excess can each result in numerous signs and symptoms, including an abnormal heart rhythm and various electrocardiographic abnormalities. Fresh fruits and vegetables are good dietary sources of potassium. The body responds to the influx of dietary potassium, which raises serum potassium levels, by shifting potassium from outside to inside cells and increasing potassium excretion by the kidneys.

Most industrial applications of potassium exploit the high solubility of its compounds in water, such as saltwater soap. Heavy crop production rapidly depletes the soil of potassium, and this can be remedied with agricultural fertilizers containing potassium, accounting for 95% of global potassium chemical production.^[11]

Etymology

The English name for the element potassium comes from the word potash,^[12] which refers to an early method of extracting various potassium salts: placing in a pot the ash of burnt wood or tree leaves, adding water, heating, and evaporating the solution. When Humphry Davy first isolated the pure element using electrolysis in 1807, he named it potassium, which he derived from the word potash.

The symbol K stems from kali, itself from the root word alkali, which in turn comes from Arabic: القَلْيَه al-qalyah ‘plant ashes’. In 1797, the German chemist Martin Klaproth discovered «potash» in the minerals leucite and lepidolite, and realized that «potash» was not a product of plant growth but actually contained a new element, which he proposed calling kali.^[13] In 1807, Humphry Davy produced the element via electrolysis: in 1809, Ludwig Wilhelm Gilbert proposed the name Kalium for Davy’s «potassium».^[14] In 1814, the Swedish chemist Berzelius advocated the name kalium for potassium, with the chemical symbol K.^[15]

The English and French-speaking countries adopted Davy and Gay-Lussac/Thénard’s name Potassium, whereas the Germanic countries adopted Gilbert/Klaproth’s name Kalium.^[16] The «Gold Book» of the International Union of Pure and Applied Chemistry has designated the official chemical symbol as K.^[17]

Properties

Physical

Potassium is the second least dense metal after lithium. It is a soft solid with a low melting point, and can be easily cut with a knife. Freshly cut potassium is silvery in appearance, but it begins to tarnish toward gray immediately on exposure to air.^[18] In a flame test, potassium and its compounds emit a lilac color with a peak emission wavelength of 766.5 nanometers.^[19]

Neutral potassium atoms have 19 electrons, one more than the configuration of the noble gas argon. Because of its low first ionization energy of 418.8 kJ/mol, the potassium atom is much more likely to lose the last electron and acquire a positive charge, although negatively charged alkalide K⁻ ions are not impossible.^[20] In contrast, the second ionization energy is very high (3052 kJ/mol).

Chemical

Potassium reacts with oxygen, water, and carbon dioxide components in air. With oxygen it forms potassium peroxide. With water potassium forms potassium hydroxide (KOH). The reaction of potassium with water can be violently exothermic, especially since the coproduced hydrogen gas can ignite. Because of this, potassium and the liquid sodium-potassium (NaK) alloy are potent desiccants, although they are no longer used as such.^[21]

Compounds

Four oxides of potassium are well studied: potassium oxide (K₂O), potassium peroxide (K₂O₂), potassium superoxide (KO₂)^[22] and potassium ozonide (KO₃). The binary potassium-oxygen compounds react with water forming KOH.

KOH is a strong base. Illustrating its hydrophilic character, as much as 1.21 kg of KOH can dissolve in a single liter of water.^[23][24] Anhydrous KOH is rarely encountered. KOH reacts readily with carbon dioxide (CO₂) to produce potassium carbonate (K₂CO₃), and in principle could be used to remove traces of the gas from air. Like the closely related sodium hydroxide, KOH reacts with fats to produce soaps.

In general, potassium compounds are ionic and, owing to the high hydration energy of the K⁺ ion, have excellent water solubility. The main species in water solution are the aquo complexes [K(H₂O)_n]⁺ where n = 6 and 7.^[25]

Potassium heptafluorotantalate (K₂[TaF₇]) is an intermediate in the purification of tantalum from the otherwise persistent contaminant of niobium.^[26]

Organopotassium compounds illustrate nonionic compounds of potassium. They feature highly polar covalent K–C bonds. Examples include benzyl potassium KCH₂C₆H₅. Potassium intercalates into graphite to give a variety of graphite intercalation compounds, including KC₈.

Isotopes

There are 25 known isotopes of potassium, three of which occur naturally: ³⁹
K (93.3%), ⁴⁰
K (0.0117%), and ⁴¹
K (6.7%) (by mole fraction). Naturally occurring ⁴⁰
K has a half-life of 1.250×10⁹ years. It decays to stable ⁴⁰
Ar by electron capture or positron emission (11.2%) or to stable ⁴⁰
Ca by beta decay (88.8%).^[27] The decay of ⁴⁰
K to ⁴⁰
Ar is the basis of a common method for dating rocks. The conventional K-Ar dating method depends on the assumption that the rocks contained no argon at the time of formation and that all the subsequent radiogenic argon (⁴⁰
Ar) was quantitatively retained. Minerals are dated by measurement of the concentration of potassium and the amount of radiogenic ⁴⁰
Ar that has accumulated. The minerals best suited for dating include biotite, muscovite, metamorphic hornblende, and volcanic feldspar; whole rock samples from volcanic flows and shallow instrusives can also be dated if they are unaltered.^[27][28] Apart from dating, potassium isotopes have been used as tracers in studies of weathering and for nutrient cycling studies because potassium is a macronutrient required for life^[29] on Earth.

⁴⁰
K occurs in natural potassium (and thus in some commercial salt substitutes) in sufficient quantity that large bags of those substitutes can be used as a radioactive source for classroom demonstrations. ⁴⁰
K is the radioisotope with the largest abundance in the human body. In healthy animals and people, ⁴⁰
K represents the largest source of radioactivity, greater even than ¹⁴
C. In a human body of 70 kg, about 4,400 nuclei of ⁴⁰
K decay per second.^[30] The activity of natural potassium is 31 Bq/g.^[31]

Cosmic formation and distribution

Potassium is formed in supernovae by nucleosynthesis from lighter atoms. Potassium is principally created in Type II supernovae via an explosive oxygen-burning process.^[32] (These are fusion reactions; do not confuse with chemical burning between potassium and oxygen.) ⁴⁰
K is also formed in s-process nucleosynthesis and the neon burning process.^[33]

Potassium is the 20th most abundant element in the solar system and the 17th most abundant element by weight in the Earth. It makes up about 2.6% of the weight of the Earth’s crust and is the seventh most abundant element in the crust.^[34] The potassium concentration in seawater is 0.39 g/L^[7] (0.039 wt/v%), about one twenty-seventh the concentration of sodium.^[35][36]

Potash

Potash is primarily a mixture of potassium salts because plants have little or no sodium content, and the rest of a plant’s major mineral content consists of calcium salts of relatively low solubility in water. While potash has been used since ancient times, its composition was not understood. Georg Ernst Stahl obtained experimental evidence that led him to suggest the fundamental difference of sodium and potassium salts in 1702,^[10] and Henri Louis Duhamel du Monceau was able to prove this difference in 1736.^[37] The exact chemical composition of potassium and sodium compounds, and the status as chemical element of potassium and sodium, was not known then, and thus Antoine Lavoisier did not include the alkali in his list of chemical elements in 1789.^[38][39] For a long time the only significant applications for potash were the production of glass, bleach, soap and gunpowder as potassium nitrate.^[40] Potassium soaps from animal fats and vegetable oils were especially prized because they tend to be more water-soluble and of softer texture, and are therefore known as soft soaps.^[11] The discovery by Justus Liebig in 1840 that potassium is a necessary element for plants and that most types of soil lack potassium^[41] caused a steep rise in demand for potassium salts. Wood-ash from fir trees was initially used as a potassium salt source for fertilizer, but, with the discovery in 1868 of mineral deposits containing potassium chloride near Staßfurt, Germany, the production of potassium-containing fertilizers began at an industrial scale.^[42][43][44] Other potash deposits were discovered, and by the 1960s Canada became the dominant producer.^[45][46]

Metal

Potassium metal was first isolated in 1807 by Humphry Davy, who derived it by electrolysis of molten KOH with the newly discovered voltaic pile. Potassium was the first metal that was isolated by electrolysis.^[47] Later in the same year, Davy reported extraction of the metal sodium from a mineral derivative (caustic soda, NaOH, or lye) rather than a plant salt, by a similar technique, demonstrating that the elements, and thus the salts, are different.^{[38][39][48][49]} Although the production of potassium and sodium metal should have shown that both are elements, it took some time before this view was universally accepted.^[39]

Because of the sensitivity of potassium to water and air, air-free techniques are normally employed for handling the element. It is unreactive toward nitrogen and saturated hydrocarbons such as mineral oil or kerosene.^[50] It readily dissolves in liquid ammonia, up to 480 g per 1000 g of ammonia at 0 °C. Depending on the concentration, the ammonia solutions are blue to yellow, and their electrical conductivity is similar to that of liquid metals. Potassium slowly reacts with ammonia to form KNH
₂, but this reaction is accelerated by minute amounts of transition metal salts.^[51] Because it can reduce the salts to the metal, potassium is often used as the reductant in the preparation of finely divided metals from their salts by the Rieke method.^[52] Illustrative is the preparation of magnesium:

MgCl₂ + 2 K → Mg + 2 KCl

Geology

Elemental potassium does not occur in nature because of its high reactivity. It reacts violently with water (see section Precautions below)^[50] and also reacts with oxygen. Orthoclase (potassium feldspar) is a common rock-forming mineral. Granite for example contains 5% potassium, which is well above the average in the Earth’s crust. Sylvite (KCl), carnallite (KCl·MgCl₂·6H₂O), kainite (MgSO₄·KCl·3H₂O) and langbeinite (MgSO₄·K₂SO₄) are the minerals found in large evaporite deposits worldwide. The deposits often show layers starting with the least soluble at the bottom and the most soluble on top.^[36] Deposits of niter (potassium nitrate) are formed by decomposition of organic material in contact with atmosphere, mostly in caves; because of the good water solubility of niter the formation of larger deposits requires special environmental conditions.^[53]

Biological role

Potassium is the eighth or ninth most common element by mass (0.2%) in the human body, so that a 60 kg adult contains a total of about 120 g of potassium.^[54] The body has about as much potassium as sulfur and chlorine, and only calcium and phosphorus are more abundant (with the exception of the ubiquitous CHON elements).^[55] Potassium ions are present in a wide variety of proteins and enzymes.^[56]

Biochemical function

Potassium levels influence multiple physiological processes, including^[57][58][59]

• resting cellular-membrane potential and the propagation of action potentials in neuronal, muscular, and cardiac tissue. Due to the electrostatic and chemical properties, K⁺ ions are larger than Na⁺ ions, and ion channels and pumps in cell membranes can differentiate between the two ions, actively pumping or passively passing one of the two ions while blocking the other.^[60]
• hormone secretion and action
• vascular tone
• systemic blood pressure control
• gastrointestinal motility
• acid–base homeostasis
• glucose and insulin metabolism
• mineralocorticoid action
• renal concentrating ability
• fluid and electrolyte balance

Homeostasis

Potassium homeostasis denotes the maintenance of the total body potassium content, plasma potassium level, and the ratio of the intracellular to extracellular potassium concentrations within narrow limits, in the face of pulsatile intake (meals), obligatory renal excretion, and shifts between intracellular and extracellular compartments.

Plasma levels

Plasma potassium is normally kept at 3.5 to 5.5 millimoles (mmol) [or milliequivalents (mEq)] per liter by multiple mechanisms.^[61] Levels outside this range are associated with an increasing rate of death from multiple causes,^[62] and some cardiac, kidney,^[63] and lung diseases progress more rapidly if serum potassium levels are not maintained within the normal range.

An average meal of 40–50 mmol presents the body with more potassium than is present in all plasma (20–25 mmol). However, this surge causes the plasma potassium to rise only 10% at most as a result of prompt and efficient clearance by both renal and extra-renal mechanisms.^[64]

Hypokalemia, a deficiency of potassium in the plasma, can be fatal if severe. Common causes are increased gastrointestinal loss (vomiting, diarrhea), and increased renal loss (diuresis).^[65] Deficiency symptoms include muscle weakness, paralytic ileus, ECG abnormalities, decreased reflex response; and in severe cases, respiratory paralysis, alkalosis, and cardiac arrhythmia.^[66]

Control mechanisms

Potassium content in the plasma is tightly controlled by four basic mechanisms, which have various names and classifications. The four are 1) a reactive negative-feedback system, 2) a reactive feed-forward system, 3) a predictive or circadian system, and 4) an internal or cell membrane transport system. Collectively, the first three are sometimes termed the «external potassium homeostasis system»;^[67] and the first two, the «reactive potassium homeostasis system».

• The reactive negative-feedback system refers to the system that induces renal secretion of potassium in response to a rise in the plasma potassium (potassium ingestion, shift out of cells, or intravenous infusion.)
• The reactive feed-forward system refers to an incompletely understood system that induces renal potassium secretion in response to potassium ingestion prior to any rise in the plasma potassium. This is probably initiated by gut cell potassium receptors that detect ingested potassium and trigger vagal afferent signals to the pituitary gland.
• The predictive or circadian system increases renal secretion of potassium during mealtime hours (e.g. daytime for humans, nighttime for rodents) independent of the presence, amount, or absence of potassium ingestion. It is mediated by a circadian oscillator in the suprachiasmatic nucleus of the brain (central clock), which causes the kidney (peripheral clock) to secrete potassium in this rhythmic circadian fashion.

  

  The action of the sodium-potassium pump is an example of primary active transport. The two carrier proteins embedded in the cell membrane on the left are using ATP to move sodium out of the cell against the concentration gradient; The two proteins on the right are using secondary active transport to move potassium into the cell. This process results in reconstitution of ATP.

• The ion transport system moves potassium across the cell membrane using two mechanisms. One is active and pumps sodium out of, and potassium into, the cell. The other is passive and allows potassium to leak out of the cell. Potassium and sodium cations influence fluid distribution between intracellular and extracellular compartments by osmotic forces. The movement of potassium and sodium through the cell membrane is mediated by the Na⁺/K⁺-ATPase pump.^[68] This ion pump uses ATP to pump three sodium ions out of the cell and two potassium ions into the cell, creating an electrochemical gradient and electromotive force across the cell membrane. The highly selective potassium ion channels (which are tetramers) are crucial for hyperpolarization inside neurons after an action potential is triggered, to cite one example. The most recently discovered potassium ion channel is KirBac3.1, which makes a total of five potassium ion channels (KcsA, KirBac1.1, KirBac3.1, KvAP, and MthK) with a determined structure. All five are from prokaryotic species.^[69]

Renal filtration, reabsorption, and excretion

Renal handling of potassium is closely connected to sodium handling. Potassium is the major cation (positive ion) inside animal cells [150 mmol/L, (4.8 g)], while sodium is the major cation of extracellular fluid [150 mmol/L, (3.345 g)]. In the kidneys, about 180 liters of plasma is filtered through the glomeruli and into the renal tubules per day.^[70] This filtering involves about 600 g of sodium and 33 g of potassium. Since only 1–10 g of sodium and 1–4 g of potassium are likely to be replaced by diet, renal filtering must efficiently reabsorb the remainder from the plasma.

Sodium is reabsorbed to maintain extracellular volume, osmotic pressure, and serum sodium concentration within narrow limits. Potassium is reabsorbed to maintain serum potassium concentration within narrow limits.^[71] Sodium pumps in the renal tubules operate to reabsorb sodium. Potassium must be conserved, but because the amount of potassium in the blood plasma is very small and the pool of potassium in the cells is about 30 times as large, the situation is not so critical for potassium. Since potassium is moved passively^[72][73] in counter flow to sodium in response to an apparent (but not actual) Donnan equilibrium,^[74] the urine can never sink below the concentration of potassium in serum except sometimes by actively excreting water at the end of the processing. Potassium is excreted twice and reabsorbed three times before the urine reaches the collecting tubules.^[75] At that point, urine usually has about the same potassium concentration as plasma. At the end of the processing, potassium is secreted one more time if the serum levels are too high.^{[citation needed]}

With no potassium intake, it is excreted at about 200 mg per day until, in about a week, potassium in the serum declines to a mildly deficient level of 3.0–3.5 mmol/L.^[76] If potassium is still withheld, the concentration continues to fall until a severe deficiency causes eventual death.^[77]

The potassium moves passively through pores in the cell membrane. When ions move through Ion transporters (pumps) there is a gate in the pumps on both sides of the cell membrane and only one gate can be open at once. As a result, approximately 100 ions are forced through per second. Ion channel have only one gate, and there only one kind of ion can stream through, at 10 million to 100 million ions per second.^[78] Calcium is required to open the pores,^[79] although calcium may work in reverse by blocking at least one of the pores.^[80] Carbonyl groups inside the pore on the amino acids mimic the water hydration that takes place in water solution^[81] by the nature of the electrostatic charges on four carbonyl groups inside the pore.^[82]

Nutrition

Dietary recommendations

The U.S. National Academy of Medicine (NAM), on behalf of both the U.S. and Canada, sets Dietary Reference Intakes, including Estimated Average Requirements (EARs) and Recommended Dietary Allowances (RDAs), or Adequate Intakes (AIs) for when there is not sufficient information to set EARs and RDAs.

For both males and females under 9 years of age, the AIs for potassium are: 400 mg of potassium for 0-6-month-old infants, 860 mg of potassium for 7-12-month-old infants, 2,000 mg of potassium for 1-3-year-old children, and 2,300 mg of potassium for 4-8-year-old children.

For males 9 years of age and older, the AIs for potassium are: 2,500 mg of potassium for 9-13-year-old males, 3,000 mg of potassium for 14-18-year-old males, and 3,400 mg for males that are 19 years of age and older.

For females 9 years of age and older, the AIs for potassium are: 2,300 mg of potassium for 9-18-year-old females, and 2,600 mg of potassium for females that are 19 years of age and older.

For pregnant and lactating females, the AIs for potassium are: 2,600 mg of potassium for 14-18-year-old pregnant females, 2,900 mg for pregnant females that are 19 years of age and older; furthermore, 2,500 mg of potassium for 14-18-year-old lactating females, and 2,800 mg for lactating females that are 19 years of age and older. As for safety, the NAM also sets tolerable upper intake levels (ULs) for vitamins and minerals, but for potassium the evidence was insufficient, so no UL was established.^[83][84]

As of 2004, most Americans adults consume less than 3,000 mg.^[85]

Likewise, in the European Union, in particular in Germany, and Italy, insufficient potassium intake is somewhat common.^[86] The British National Health Service recommends a similar intake, saying that adults need 3,500 mg per day and that excess amounts may cause health problems such as stomach pain and diarrhea.^[87]

In 2019, the National Academies of Sciences, Engineering, and Medicine revised the Adequate Intake for potassium to 2,600 mg/day for females 19 years of age and older who are not pregnant or lactating, and 3,400 mg/day for males 19 years of age and older.^[88][89]

Food sources

Potassium is present in all fruits, vegetables, meat and fish. Foods with high potassium concentrations include yam, parsley, dried apricots, milk, chocolate, all nuts (especially almonds and pistachios), potatoes, bamboo shoots, bananas, avocados, coconut water, soybeans, and bran.^[90]

The United States Department of Agriculture lists tomato paste, orange juice, beet greens, white beans, potatoes, plantains, bananas, apricots, and many other dietary sources of potassium, ranked in descending order according to potassium content. A day’s worth of potassium is in 5 plantains or 11 bananas.^[91]

Deficient intake

Diets low in potassium can lead to hypertension^[92] and hypokalemia.

Supplementation

Supplements of potassium are most widely used in conjunction with diuretics that block reabsorption of sodium and water upstream from the distal tubule (thiazides and loop diuretics), because this promotes increased distal tubular potassium secretion, with resultant increased potassium excretion.^{[medical citation needed]} A variety of prescription and over-the counter supplements are available.^{[citation needed]} Potassium chloride may be dissolved in water, but the salty/bitter taste makes liquid supplements unpalatable.^[93] Typical doses range from 10 mmol (400 mg), to 20 mmol (800 mg).^{[medical citation needed]} Potassium is also available in tablets or capsules, which are formulated to allow potassium to leach slowly out of a matrix, since very high concentrations of potassium ion that occur adjacent to a solid tablet can injure the gastric or intestinal mucosa.^{[medical citation needed]} For this reason, non-prescription potassium pills are limited by law in the US to a maximum of 99 mg of potassium.^{[citation needed]}

A meta-analysis concluded that a 1640 mg increase in the daily intake of potassium was associated with a 21% lower risk of stroke.^[94] Potassium chloride and potassium bicarbonate may be useful to control mild hypertension.^[95] In 2020, potassium was the 33rd most commonly prescribed medication in the U.S., with more than 17 million prescriptions.^[96][97]

Detection by taste buds

Potassium can be detected by taste because it triggers three of the five types of taste sensations, according to concentration. Dilute solutions of potassium ions taste sweet, allowing moderate concentrations in milk and juices, while higher concentrations become increasingly bitter/alkaline, and finally also salty to the taste. The combined bitterness and saltiness of high-potassium solutions makes high-dose potassium supplementation by liquid drinks a palatability challenge.^[93][98]

Commercial production

Mining

Potassium salts such as carnallite, langbeinite, polyhalite, and sylvite form extensive evaporite deposits in ancient lake bottoms and seabeds,^[35] making extraction of potassium salts in these environments commercially viable. The principal source of potassium – potash – is mined in Canada, Russia, Belarus, Kazakhstan, Germany, Israel, the U.S., Jordan, and other places around the world.^{[99][100][101]} The first mined deposits were located near Staßfurt, Germany, but the deposits span from Great Britain over Germany into Poland. They are located in the Zechstein and were deposited in the Middle to Late Permian. The largest deposits ever found lie 1,000 meters (3,300 feet) below the surface of the Canadian province of Saskatchewan. The deposits are located in the Elk Point Group produced in the Middle Devonian. Saskatchewan, where several large mines have operated since the 1960s pioneered the technique of freezing of wet sands (the Blairmore formation) to drive mine shafts through them. The main potash mining company in Saskatchewan until its merge was the Potash Corporation of Saskatchewan, now Nutrien.^[102] The water of the Dead Sea is used by Israel and Jordan as a source of potash, while the concentration in normal oceans is too low for commercial production at current prices.^[100][101]

Several methods are used to separate potassium salts from sodium and magnesium compounds. The most-used method is fractional precipitation using the solubility differences of the salts. Electrostatic separation of the ground salt mixture is also used in some mines. The resulting sodium and magnesium waste is either stored underground or piled up in slag heaps. Most of the mined potassium mineral ends up as potassium chloride after processing. The mineral industry refers to potassium chloride either as potash, muriate of potash, or simply MOP.^[36]

Pure potassium metal can be isolated by electrolysis of its hydroxide in a process that has changed little since it was first used by Humphry Davy in 1807. Although the electrolysis process was developed and used in industrial scale in the 1920s, the thermal method by reacting sodium with potassium chloride in a chemical equilibrium reaction became the dominant method in the 1950s.

Na + KCl → NaCl + K

The production of sodium potassium alloys is accomplished by changing the reaction time and the amount of sodium used in the reaction. The Griesheimer process employing the reaction of potassium fluoride with calcium carbide was also used to produce potassium.^[36][103]

2 KF + CaC₂ → 2 K + CaF₂ + 2 C

Reagent-grade potassium metal costs about $10.00/pound ($22/kg) in 2010 when purchased by the tonne. Lower purity metal is considerably cheaper. The market is volatile because long-term storage of the metal is difficult. It must be stored in a dry inert gas atmosphere or anhydrous mineral oil to prevent the formation of a surface layer of potassium superoxide, a pressure-sensitive explosive that detonates when scratched. The resulting explosion often starts a fire difficult to extinguish.^[104][105]

Cation identification

Potassium is now quantified by ionization techniques, but at one time it was quantitated by gravimetric analysis.

Reagents used to precipitate potassium salts include sodium tetraphenylborate, hexachloroplatinic acid, and sodium cobaltinitrite into respectively potassium tetraphenylborate, potassium hexachloroplatinate, and potassium cobaltinitrite.^[50]
The reaction with sodium cobaltinitrite is illustrative:

3 K⁺ + Na₃[Co(NO₂)₆] → K₃[Co(NO₂)₆] + 3 Na⁺

The potassium cobaltinitrite is obtained as a yellow solid.

Commercial uses

Fertilizer

Potassium ions are an essential component of plant nutrition and are found in most soil types.^[11] They are used as a fertilizer in agriculture, horticulture, and hydroponic culture in the form of chloride (KCl), sulfate (K₂SO₄), or nitrate (KNO₃), representing the ‘K’ in ‘NPK’. Agricultural fertilizers consume 95% of global potassium chemical production, and about 90% of this potassium is supplied as KCl.^[11] The potassium content of most plants ranges from 0.5% to 2% of the harvested weight of crops, conventionally expressed as amount of K₂O. Modern high-yield agriculture depends upon fertilizers to replace the potassium lost at harvest. Most agricultural fertilizers contain potassium chloride, while potassium sulfate is used for chloride-sensitive crops or crops needing higher sulfur content. The sulfate is produced mostly by decomposition of the complex minerals kainite (MgSO₄·KCl·3H₂O) and langbeinite (MgSO₄·K₂SO₄). Only a very few fertilizers contain potassium nitrate.^[106] In 2005, about 93% of world potassium production was consumed by the fertilizer industry.^[101] Furthermore, potassium can play a key role in nutrient cycling by controlling litter composition.^[107]

Medical use

Potassium citrate

Potassium citrate is used to treat a kidney stone condition called renal tubular acidosis.^[108]

Potassium chloride

Potassium, in the form of potassium chloride is used as a medication to treat and prevent low blood potassium.^[109] Low blood potassium may occur due to vomiting, diarrhea, or certain medications.^[110] It is given by slow injection into a vein or by mouth.^[111]

Food additives

Potassium sodium tartrate (KNaC₄H₄O₆, Rochelle salt) is a main constituent of some varieties of baking powder; it is also used in the silvering of mirrors. Potassium bromate (KBrO₃) is a strong oxidizer (E924), used to improve dough strength and rise height. Potassium bisulfite (KHSO₃) is used as a food preservative, for example in wine and beer-making (but not in meats). It is also used to bleach textiles and straw, and in the tanning of leathers.^[112][113]

Industrial

Major potassium chemicals are potassium hydroxide, potassium carbonate, potassium sulfate, and potassium chloride. Megatons of these compounds are produced annually.^[114]

KOH is a strong base, which is used in industry to neutralize strong and weak acids, to control pH and to manufacture potassium salts. It is also used to saponify fats and oils, in industrial cleaners, and in hydrolysis reactions, for example of esters.^[115][116]

Potassium nitrate (KNO₃) or saltpeter is obtained from natural sources such as guano and evaporites or manufactured via the Haber process; it is the oxidant in gunpowder (black powder) and an important agricultural fertilizer. Potassium cyanide (KCN) is used industrially to dissolve copper and precious metals, in particular silver and gold, by forming complexes. Its applications include gold mining, electroplating, and electroforming of these metals; it is also used in organic synthesis to make nitriles. Potassium carbonate (K₂CO₃ or potash) is used in the manufacture of glass, soap, color TV tubes, fluorescent lamps, textile dyes and pigments.^[117] Potassium permanganate (KMnO₄) is an oxidizing, bleaching and purification substance and is used for production of saccharin. Potassium chlorate (KClO₃) is added to matches and explosives. Potassium bromide (KBr) was formerly used as a sedative and in photography.^[11]

While potassium chromate (K₂CrO₄) is used in the manufacture of a host of different commercial products such as inks, dyes, wood stains (by reacting with the tannic acid in wood), explosives, fireworks, fly paper, and safety matches,^[118] as well as in the tanning of leather, all of these uses are due to the chemistry of the chromate ion rather than to that of the potassium ion.^[119]

Niche uses

There are thousands of uses of various potassium compounds. One example is potassium superoxide, KO₂, an orange solid that acts as a portable source of oxygen and a carbon dioxide absorber. It is widely used in respiration systems in mines, submarines and spacecraft as it takes less volume than the gaseous oxygen.^[120][121]

4 KO₂ + 2 CO₂ → 2 K₂CO₃ + 3 O₂

Another example is potassium cobaltinitrite, K₃[Co(NO₂)₆], which is used as artist’s pigment under the name of Aureolin or Cobalt Yellow.^[122]

The stable isotopes of potassium can be laser cooled and used to probe fundamental and technological problems in quantum physics. The two bosonic isotopes possess convenient Feshbach resonances to enable studies requiring tunable interactions, while ⁴⁰
K is one of only two stable fermions amongst the alkali metals.^[123]

Laboratory uses

An alloy of sodium and potassium, NaK is a liquid used as a heat-transfer medium and a desiccant for producing dry and air-free solvents. It can also be used in reactive distillation.^[124] The ternary alloy of 12% Na, 47% K and 41% Cs has the lowest melting point of −78 °C of any metallic compound.^[18]

Metallic potassium is used in several types of magnetometers.^[125]

Precautions

Potassium

Hazards
GHS labelling:
Pictograms
Signal word	Danger
Hazard statements	H260, H314
Precautionary statements	P223, P231+P232, P280, P305+P351+P338, P370+P378, P422[126]
NFPA 704 (fire diamond)	3 3 2 W

Potassium metal can react violently with water producing KOH and hydrogen gas.

2 K(s) + 2 H₂O(l) → 2 KOH(aq) + H₂(g)↑

This reaction is exothermic and releases sufficient heat to ignite the resulting hydrogen in the presence of oxygen. Finely powdered potassium ignites in air at room temperature. The bulk metal ignites in air if heated. Because its density is 0.89 g/cm³, burning potassium floats in water that exposes it to atmospheric oxygen. Many common fire extinguishing agents, including water, either are ineffective or make a potassium fire worse. Nitrogen, argon, sodium chloride (table salt), sodium carbonate (soda ash), and silicon dioxide (sand) are effective if they are dry. Some Class D dry powder extinguishers designed for metal fires are also effective. These agents deprive the fire of oxygen and cool the potassium metal.^[127]

During storage, potassium forms peroxides and superoxides. These peroxides may react violently with organic compounds such as oils. Both peroxides and superoxides may react explosively with metallic potassium.^[128]

Because potassium reacts with water vapor in the air, it is usually stored under anhydrous mineral oil or kerosene. Unlike lithium and sodium, however, potassium should not be stored under oil for longer than six months, unless in an inert (oxygen free) atmosphere, or under vacuum. After prolonged storage in air dangerous shock-sensitive peroxides can form on the metal and under the lid of the container, and can detonate upon opening.^[129]

Ingestion of large amounts of potassium compounds can lead to hyperkalemia, strongly influencing the cardiovascular system.^[130][131] Potassium chloride is used in the U.S. for lethal injection executions.^[130]

See also

References

Bibliography

• Burkhardt, Elizabeth R. (2006). «Potassium and Potassium Alloys». Ullmann’s Encyclopedia of Industrial Chemistry. Vol. A22. pp. 31–38. doi:10.1002/14356007.a22_031.pub2. ISBN 978-3-527-30673-2.
• Greenwood, Norman N.; Earnshaw, Alan (1997). Chemistry of the Elements (2nd ed.). Butterworth-Heinemann. ISBN 978-0-08-037941-8.
• Holleman, Arnold F.; Wiberg, Egon; Wiberg, Nils (2007). «Potassium». Lehrbuch der Anorganischen Chemie (in German) (91–100 ed.). Walter de Gruyter. ISBN 978-3110177701.
• Schultz, H.; et al. (2006). «Potassium compounds». Ullmann’s Encyclopedia of Industrial Chemistry. Vol. A22. pp. 39–103. doi:10.1002/14356007.a22_031.pub2. ISBN 978-3-527-30673-2.
• National Nutrient Database Archived 2014-08-10 at the Wayback Machine at USDA Website

External links

• «Potassium». Drug Information Portal. U.S. National Library of Medicine.

19 Аргон ← Калий → Кальций 19K
Внешний вид простого вещества
Серебристо-белый мягкий металл
Свойства атома
Имя, символ, номер	Калий / Kalium (K), 19
Атомная масса (молярная масса)	39,0983[1] а. е. м. (г/моль)
Электронная конфигурация	[Ar] 4s1
Радиус атома	235 пм
Химические свойства
Ковалентный радиус	203 пм
Радиус иона	133 пм
Электроотрицательность	0,82 (шкала Полинга)
Электродный потенциал	−2,92 В
Степени окисления	1
Энергия ионизации (первый электрон)	418,5 (4,34) кДж/моль (эВ)
Термодинамические свойства простого вещества
Плотность (при н. у.)	0,856 г/см³
Температура плавления	63,51°С; 336,8 K
Температура кипения	1047 K
Теплота плавления	2,33 кДж/моль
Теплота испарения	76,9 кДж/моль
Молярная теплоёмкость	29,6[2] Дж/(K·моль)
Молярный объём	45,3 см³/моль
Кристаллическая решётка простого вещества
Структура решётки	кубическая объёмно-центрированная
Параметры решётки	5,332 Å
Температура Дебая	100 K
Прочие характеристики
Теплопроводность	(300 K) 79,0 Вт/(м·К)

Ка́лий — элемент главной подгруппы первой группы, четвёртого периода периодической системы химических элементов Д. И. Менделеева, с атомным номером 19. Обозначается символом K (лат. Kalium). Простое вещество калий (CAS-номер: 7440-09-7) — мягкий щелочной металл серебристо-белого цвета.

В природе калий встречается только в соединениях с другими элементами, например, в морской воде, а также во многих минералах. Очень быстро окисляется на воздухе и очень легко вступает в химические реакции, особенно с водой, образуя щёлочь. Во многих отношениях химические свойства калия очень близки к натрию, но с точки зрения биологической функции и использования их клетками живых организмов они всё же отличаются.

История и происхождение названия

Калий (точнее, его соединения) использовался с давних времён. Так, производство поташа (который применялся как моющее средство) существовало уже в XI веке. Золу, образующуюся при сжигании соломы или древесины, обрабатывали водой, а полученный раствор (щёлок) после фильтрования выпаривали. Сухой остаток, помимо карбоната калия, содержал сульфат калия K₂SO₄, соду и хлорид калия KCl.

В 1807 году английский химик Дэви электролизом расплава едкого кали (KOH) выделил калий и назвал его «потассий» (лат. potassium; это название до сих пор употребительно в английском, французском, испанском, португальском и польском языках). В 1809 году Л. В. Гильберт предложил название «калий» (лат. kalium, от араб. аль-кали — поташ). Это название вошло в немецкий язык, оттуда в большинство языков Северной и Восточной Европы (в том числе русский) и «победило» при выборе символа для этого элемента — K.

Нахождение в природе

В свободном состоянии не встречается. Породообразующий элемент, входит в состав слюд, полевых шпатов и т.д. Также калий входит в состав сильвина KCl, сильвинита KCl·NaCl, карналлита KCl·MgCl₂·6H₂O, каинита KCl·MgSO₄·6H₂O, а также присутствует в золе некоторых растений в виде карбоната K₂CO₃ (поташ). Калий входит в состав всех клеток (см. ниже раздел Биологическая роль). Кларк калия в земной коре составляет 2,4 % (5-й по распространённости металл, 7-й по содержанию в коре элемент). Концентрация в морской воде 380 мг/л^[3].

Месторождения

Крупнейшие месторождения калия находятся на территории Канады (производитель PotashCorp), России (ОАО «Уралкалий», г. Березники, ОАО «Сильвинит», г. Соликамск, Пермский край, Верхнекамское месторождение калийных руд^[4]), Белоруссии (ПО «Беларуськалий», г. Солигорск, Старобинское месторождение калийных руд^[5]).

Получение

Калий, как и другие щелочные металлы, получают электролизом расплавленных хлоридов или щелочей. Так как хлориды имеют более высокую температуру плавления (600—650 °C), то чаще проводят электролиз расплавленных щелочей с добавкой к ним соды или поташа (до 12 %). При электролизе расплавленных хлоридов на катоде выделяется расплавленный калий, а на аноде — хлор:

При электролизе щелочей на катоде также выделяется расплавленный калий, а на аноде — кислород:

Вода из расплава быстро испаряется. Чтобы калий не взаимодействовал с хлором или кислородом, катод изготовляют из меди и над ним помещают медный цилиндр. Образовавшийся калий в расплавленном виде собирается в цилиндре. Анод изготовляют также в виде цилиндра из никеля (при электролизе щелочей) либо из графита (при электролизе хлоридов).

Важное промышленное значение имеют и методы термохимического восстановления:

и восстановление из расплава хлорида калия карбидом кальция, алюминием или кремнием.^[6][7]

Физические свойства

Калий — серебристое вещество с характерным блеском на свежеобразованной поверхности. Очень лёгок и легкоплавок. Относительно хорошо растворяется в ртути, образуя амальгамы. Будучи внесённым в пламя горелки, калий (а также его соединения) окрашивает пламя в характерный розово-фиолетовый цвет^[8].

Калий образует кристаллы кубической сингонии, пространственная группа I m3m, параметры ячейки a = 0,5247 нм, Z = 2.

Химические свойства

Элементарный калий, как и другие щелочные металлы, проявляет типичные металлические свойства и очень химически активен, является сильным восстановителем. На воздухе свежий срез быстро тускнеет из-за образования плёнок соединений (оксиды и карбонат). При длительном контакте с атмосферой способен полностью разрушиться. С водой реагирует со взрывом. Хранить его необходимо под слоем бензина, керосина или силикона, дабы исключить контакт воздуха и воды с его поверхностью. С Na, Tl, Sn, Pb, Bi калий образует интерметаллиды.

Взаимодействие с простыми веществами

Калий при комнатной температуре реагирует с кислородом воздуха, галогенами; практически не реагирует с азотом (в отличие от лития и натрия). При умеренном нагревании реагирует с водородом с образованием гидрида (200—350 °C):

,

с халькогенами (100—200 °C, E = S, Se, Te):

.

При сгорании калия на воздухе образуется надпероксид калия KO₂ (с примесью K₂O₂):

В реакции с фосфором в инертной атмосфере образуется фосфид зелёного цвета (200 °C):

Взаимодействие со сложными веществами

Калий при комнатной температуре активно реагирует с водой, кислотами, растворяется в жидком аммиаке (−50 °C) с образованием тёмно-синего раствора.

Калий глубоко восстанавливает разбавленные серную и азотную кислоты:

При сплавлении металлического калия со щелочами он восстанавливает водород гидроксогруппы:

При умеренном нагревании реагирует с газообразным аммиаком с образованием амида (65—105 °C):

Металлический калий реагирует со спиртами с образованием алкоголятов:

Алкоголяты щелочных металлов (в данном случае, этаноат калия) являются очень сильными основаниями и широко используются в органическом синтезе.

Соединения с кислородом

При взаимодействии калия с кислородом воздуха образуется не оксид, а пероксид и супероксид:

Оксид калия может быть получен при нагревании металла до температуры не выше 180 °C в среде, содержащей очень мало кислорода, или при нагревании смеси супероксида калия с металлическим калием:

Оксиды калия обладают ярко выраженными основными свойствами, бурно реагируют с водой, кислотами и кислотными оксидами. Практического значения они не имеют. Пероксиды представляют собой желтовато-белые порошки, которые, хорошо растворяясь в воде, образуют щёлочи и пероксид водорода:

Свойство обменивать углекислый газ на кислород используется в изолирующих противогазах и на подводных лодках. В качестве поглотителя используют эквимолярную смесь супероксида калия и пероксида натрия. Если смесь не эквимолярна, то в случае избытка пероксида натрия поглотится больше газа, чем выделится (при поглощении двух объёмов CO₂ выделяется один объём O₂), и давление в замкнутом пространстве упадёт, а в случае избытка супероксида калия (при поглощении двух объёмов CO₂ выделяется три объёма O₂) выделяется больше газа, чем поглотится, и давление повысится.

В случае эквимолярной смеси (Na₂O₂:K₂O₄ = 1:1) объёмы поглощаемого и выделяемого газов будут равны (при поглощении четырёх объёмов CO₂ выделяется четыре объёма O₂).

Пероксиды являются сильными окислителями, поэтому их применяют для отбеливания тканей в текстильной промышленности.

Получают пероксиды прокаливанием металлов на воздухе, освобождённом от углекислого газа.

Также известен озонид калия KO₃, оранжево-красного цвета. Получить его можно взаимодействием гидроксида калия с озоном при температуре не выше 20 °C:

Озонид калия является очень сильным окислителем, например, окисляет элементарную серу до сульфата и дисульфата уже при 50 °C:

Гидроксид

Гидроксид калия (или едкое кали) представляет собой твёрдые белые непрозрачные, очень гигроскопичные кристаллы, плавящиеся при температуре 360 °C. Гидроксид калия относится к щелочам. Он хорошо растворяется в воде с выделением большого количества тепла. Растворимость едкого кали при 20 °C в 100 г воды составляет 112 г.

Применение

• Жидкий при комнатной температуре сплав калия и натрия используется в качестве теплоносителя в замкнутых системах, например, в атомных силовых установках на быстрых нейтронах. Кроме того, широко применяются его жидкие сплавы с рубидием и цезием. Сплав состава: натрий 12 %, калий 47 %, цезий 41 % — обладает рекордно низкой температурой плавления −78 °C.
• Соединения калия — важнейший биогенный элемент и потому применяются в качестве удобрений.
• Соли калия широко используются в гальванотехнике, так как, несмотря на относительно высокую стоимость, они часто более растворимы, чем соответствующие соли натрия, и потому обеспечивают интенсивную работу электролитов при повышенной плотности тока.

Важные соединения

• Бромид калия применяется в медицине и как успокаивающее средство для нервной системы.
• Гидроксид калия (едкое кали) применяется в щелочных аккумуляторах и при сушке газов.
• Карбонат калия (поташ) используется как удобрение, при варке стекла.
• Хлорид калия (сильвин, «калийная соль») используется как удобрение.
• Нитрат калия (калийная селитра) — удобрение, компонент чёрного пороха.
• Перхлорат и хлорат калия (бертолетова соль) используются в производстве спичек, ракетных порохов, осветительных зарядов, взрывчатых веществ, в гальванотехнике.
• Дихромат калия (хромпик) — сильный окислитель, используется для приготовления «хромовой смеси» для мытья химической посуды и при обработке кожи (дубление). Также используется для очистки ацетилена на ацетиленовых заводах от аммиака, сероводорода и фосфина.

• Перманганат калия — сильный окислитель, используется как антисептическое средство в медицине и для лабораторного получения кислорода.
• Тартрат натрия-калия (сегнетова соль) в качестве пьезоэлектрика.
• Дигидрофосфат и дидейтерофосфат калия в виде монокристаллов в лазерной технике.
• Пероксид калия и супероксид калия используются для регенерации воздуха на подводных лодках и в изолирующих противогазах (поглощает углекислый газ с выделением кислорода).
• Фтороборат калия — важный флюс для пайки сталей и цветных металлов.
• Цианид калия применяется в гальванотехнике (серебрение, золочение), при добыче золота и при нитроцементации стали.
• Калий совместно с перекисью калия применяется при термохимическом разложении воды на водород и кислород (калиевый цикл «Газ де Франс», Франция).

Биологическая роль

Калий — важнейший биогенный элемент, особенно в растительном мире. При недостатке калия в почве растения развиваются очень плохо, уменьшается урожай, поэтому около 90 % добываемых солей калия используют в качестве удобрений.

Калий в организме человека

В этом разделе не хватает ссылок на источники информации. Информация должна быть проверяема, иначе она может быть поставлена под сомнение и удалена. Вы можете отредактировать эту статью, добавив ссылки на авторитетные источники. Эта отметка установлена 12 мая 2011.

Калий содержится большей частью в клетках, до 40 раз больше чем в межклеточном пространстве. В процессе функционирования клеток избыточный калий покидает цитоплазму, поэтому для сохранения концентрации он должен нагнетаться обратно при помощи натрий-калиевого насоса. Калий и натрий между собой функционально связаны и выполняют следующие функции:

• Создание условий для возникновения мембранного потенциала и мышечных сокращений.
• Поддержание осмотической концентрации крови.
• Поддержание кислотно-щелочного баланса.
• Нормализация водного баланса.

Рекомендуемая суточная доля калия составляет для детей от 600 до 1700 миллиграммов, для взрослых от 1800 до 5000 миллиграммов. Потребность в калии зависит от общего веса тела, физической активности, физиологического состояния, и климата места проживания. Рвота, продолжительные поносы, обильное потение, использование мочегонных повышают потребность организма в калии.

Основными пищевыми источниками являются сушёные абрикосы, дыня, бобы, киви, картофель, батат, авокадо, бананы, брокколи, печень, молоко, ореховое масло, цитрусовые, виноград. Калия достаточно много в рыбе и молочных продуктах.

Практически все сорта рыбы содержат более 200 мг калия в 100 г. Количество калия в разных видах рыбы различается. Овощи, грибы и травы также содержат много калия, однако в консервированных продуктах его уровень может быть гораздо меньше. Много калия содержится в шоколаде.

Всасывание происходит в тонком кишечнике. Усвоение калия облегчает витамин B6, затрудняет — алкоголь.

При недостатке калия развивается гипокалиемия. Возникают нарушения работы сердечной и скелетной мускулатуры. Продолжительный дефицит калия может быть причиной острой невралгии.

При переизбытке калия развивается гиперкалиемия, для которой основным симптомом является язва тонкого кишечника. Настоящая гиперкалиемия может вызвать остановку сердца.

Изотопы

Природный калий состоит из трёх изотопов. Два из них стабильны: ³⁹K (изотопная распространённость 93,258 %) и ⁴¹K (6,730 %). Третий изотоп ⁴⁰K (0,0117 %) является бета-активным с периодом полураспада 1,251·10⁹ лет. В каждом грамме природного калия в секунду распадается в среднем 32 ядра ⁴⁰K, благодаря чему, например, в организме человека массой 70 кг ежесекундно происходит около 4000 радиоактивных распадов. Поэтому легкодоступные в быту соединения калия (поташ, хлорид калия, калийная селитра и т. д.) можно использовать как пробные радиоактивные источники для проверки бытовых дозиметров. ⁴⁰K наряду с ураном и торием считается одним из основных источников геотермальной энергии, выделяемой в недрах Земли (полная скорость энерговыделения оценивается в 40—44 ТВт). В минералах, содержащих калий, постепенно накапливается калий-аргоновый метод является одним из основных методов ядерной геохронологии.

См. также

	Калий на Викискладе?

• Натрий
• Щелочные металлы
• Банановый эквивалент

Примечания

Литература

1. Пилипенко А. Т. Натрий и калий // Справочник по элементарной химии. — 2-е изд. — Киев: Наукова думка, 1978. — С. 316—319.
2. Дроздов А. Яростные металлы // Энциклопедия для детей. Химия. — М.: Аванта +, 2002. — С. 184—187. — ISBN 5-8483-0027-5
3. Ахметов Н. С. Общая и неорганическая химия. — М.: Высшая школа, 2001.
4. Некрасов Б. В. Основы общей химии. — М.: Химия, 1974.
5. Спицын В. И., Мартыненко Л. И. Неорганическая химия. — М.: МГУ, 1991, 1994.
6. Лидин Р. А. и др. Элементы IA-группы. Калий // Химические свойства неорганических веществ: Уч. пособие для вузов. — 4-е изд. — М.: КолосС, 2003. — С. 29—40. — ISBN 5-9532-0095-1

Ссылки

• Калий на Webelements
• Калий в Популярной библиотеке химических элементов

Периодическая система химических элементов Д. И. Менделеева
	1	2															3	4	5	6	7	8	9	10	11	12	13	14	15	16	17	18
1	H		He
2	Li	Be		B	C	N	O	F	Ne
3	Na	Mg		Al	Si	P	S	Cl	Ar
4	K	Ca		Sc	Ti	V	Cr	Mn	Fe	Co	Ni	Cu	Zn	Ga	Ge	As	Se	Br	Kr
5	Rb	Sr		Y	Zr	Nb	Mo	Tc	Ru	Rh	Pd	Ag	Cd	In	Sn	Sb	Te	I	Xe
6	Cs	Ba	La	Ce	Pr	Nd	Pm	Sm	Eu	Gd	Tb	Dy	Ho	Er	Tm	Yb	Lu	Hf	Ta	W	Re	Os	Ir	Pt	Au	Hg	Tl	Pb	Bi	Po	At	Rn
7	Fr	Ra	Ac	Th	Pa	U	Np	Pu	Am	Cm	Bk	Cf	Es	Fm	Md	No	Lr	Rf	Db	Sg	Bh	Hs	Mt	Ds	Rg	Cn	Uut	Fl	Uup	Lv	Uus	Uuo
Щелочные металлы  Щёлочноземельные металлы  Лантаноиды Актиноиды Переходные металлы Другие металлы Металлоиды Другие неметаллы Галогены Инертные газы

Электрохимический ряд активности металлов
Eu, Sm, Li, Cs, Rb, K, Ra, Ba, Sr, Ca, Na, Ac, La, Ce, Pr, Nd, Pm, Gd, Tb, Mg, Y, Dy, Am, Ho, Er, Tm, Lu, Sc, Pu, Th, Np, U, Hf, Be, Al, Ti, Zr, Yb, Mn, V, Nb, Pa, Cr, Zn, Ga, Fe, Cd, In, Tl, Co, Ni, Te, Mo, Sn, Pb, H2, W, Sb, Bi, Ge, Re, Cu, Tc, Te, Rh, Po, Hg, Ag, Pd, Os, Ir, Pt, Au Элементы расположены в порядке возрастания стандартного электродного потенциала.

Соединения калия

Азид калия (KN3) • Амид калия (KNH2) • Ацесульфам (C4H4KNO4S) • Ацетат калия (CH3COOK) • Ацетиленид калия (K2C2) • Бензоат тригидрат калия (Брутто-формула:C7H11KO5) • Бромат калия (KBrO3) • Бромид калия (KBr) • Гексагидроксоплатинат(IV) калия (K2[Pt(OH)6]) • Гексагидроксостибат калия (K[Sb(OH)6]) • Гексанитрокобальтат(III) калия (K3[Co(NO3)6]) • Гексаоксибензол калия (C6(OK)6) • Гексафторогерманат калия (K2[GeF6]) • Гексафторокупрат(III) калия (K3CuF6) • Гексафторомолибдат(III) калия (K3MoF6) • Гексафтороплатинат(V) калия (K[PtF6]) • Гексафторосиликат(IV) калия (K2[SiF6]) • Гексафторфосфат калия (KPF6) • Гексахлоропалладат(IV) калия (K2[PdCl6]) • Гексахлороплатинат(IV) калия (K2[PtCl6]) • Гексахлоростаннат(IV) калия (K2[SnCl6]) • Гексахлорплатинат калия (K2PtCl6) • Гексацианоферрат(II) калия (K4[Fe(CN)6]) • Гексацианоферрат(II) тригидрат калия (K4[Fe(CN)6]•3H2O) • Гексацианоферрат(III) калия (K3[Fe(CN)6]) • Гептафторониобат(V) калия (K2[NbF7]) • Гидрид калия (KH) • Гидрокарбонат калия (KHCO3) • Гидроксид калия (KOH) • Гидроортофосфат калия (K2HPO4) • Гидросульфат калия (KHSO4) • Гидросульфид калия (KHS) • Гидросульфит калия (KHSO3) • Гидрофторид калия (KHF2) • Дигидроарсенат калия (KH2AsO4) • Дигидроортофосфат калия (KH2PO4) • Динитрамид калия (KN(NO2)2) • Дисульфат калия (K2S2O7) • Дисульфит калия (K2S2O5) • Дисульфонатнитроксил калия ((KO3S)2NO) • Дитионат калия (K2S2O6) • Дихлородиамминпалладий ([Pd(NH3)2]Cl2) • Дихромат калия (K2Cr2O7) • Дицианоаргентат(I) калия (K[Ag(СN)2]) • Дицианоаурат(I) калия (K[Au(СN)2]) • Иодат калия (KIO3) • Иодид калия (KI) • Карбонат калия (K2CO3) • Манганат калия (K2MnO4) • Метаванадат калия (KVO3) • Метасиликат калия (K2SiO3) • Метафосфат калия (KPO3) • Надпероксид калия (KO2 или K2O4) • Нитрат калия (KNO3) • Нитрит калия (KNO2) • Озонид калия (KO3) • Оксалат калия (K2C2O4) • Оксалат моногидрат калия (K2C2O4•H2O) • Оксид калия (K2O) • Октахлоромолибдат калия (K4Mo2Cl8) • Ортофосфат калия (K3PO4) • Пербромат калия (KBrO4) • Периодат калия (KIO4) • Перманганат калия (KMnO4) • Пероксид калия (K2O2) • Пероксодикарбонат калия (К2С2О6) • Пероксомоносульфат калия (K2SO5) • Пероксодисульфат калия (K2S2O6(O2)) • Перренат калия (KReO4) • Перхлорат калия (KClO4) • Полисульфиды калия (K2Sn) • Политионаты калия (K2SnO6) • Сегнетова соль (NaKC4H4O6) • Соль Джонсона (K[I(I)2]•H2O) • Соль Цейзе (K[Pt(C2H4)Cl3]•H2O) • Сорбат калия (C6H7KO2) • Сульфат гидрат калия-гадолиния • Сульфат гидрат калия-кальция (K2Ca(SO4)2•H2O) • Сульфат калия (K2SO4) • Сульфат калия-кальция (K2Ca(SO4)2) • Сульфат хрома(III)-калия (KCr(SO4)2) Сульфид калия (K2S) • Сульфит дигидрат калия (K2SO3•2H2O) • Сульфит калия (K2SO3) • Тетрагидроалюминат калия (KAlH4) • Тетрагидроксодиоксоосмат(VI) калия (K2[OsO2(OH)4]) • Тетрагидроортотеллурат калия (K2H4TeO6) • Тетраиодомеркурат(II) калия (K2[HgI4]) • Тетранитроплатинат(II) калия (K2[Pt(NO2)4]) • Тетраоксорутенат(VI) калия (K2RuO4) • Тетрапероксохромат(V) калия (K3CrO8) • Тетрасиликат калия (K2Si4O9•H2O) • Тетрахлоромолибдат(III) калия (KMoCl4) • Тетрахлоропалладат(II) калия (K2[PdCl4]) • Тетрахлороплатинат(II) калия (K2[PtCl4]) • Тетрахлороферрат(III) калия (K[FeCl4]) • Тетрахлорплатинат калия (K2PtCl4) • Тетрацианоникколат(II) калия (K2[Ni(CN)4]) • Тетрацианоплатинат(II) калия (K2[Pt(CN)4]) • Тиосульфат калия (K2SO3S) • Тиоцианат калия (KSCN) • Феррат калия (K2FeO4) • Феррооксалат калия (K3[Fe(C2O4)3]) • Формиат калия (HCOOK) Фталимид калия • Фторид калия (KF) • Фторсульфит калия (KSO2F) • Хлорат калия (KClO3) • Хлорид калия (KCl) • Хлорид-триэтилалюминий калия ((C2H5)3Al•KCl) • Хромат калия (K2CrO4) • Хромит калия (KCrO2) • Цианат калия (KOCN) • Цианид калия (KCN) • Цианоаурат калия (K[Au(CN)2] • Этилксантогенат калия (C2H5OC(S)SK) •

Калий, свойства атома, химические и физические свойства.

K 19  Калий

39,0983(1)      1s² 2s² 2p⁶ 3s² 3p⁶ 4s¹

Калий — элемент периодической системы химических элементов Д. И. Менделеева с атомным номером 19. Расположен в 1-й группе (по старой классификации — главной подгруппе первой группы), четвертом периоде периодической системы.

Атом и молекула калия. Формула калия. Строение калия

Изотопы и модификации калия

Свойства калия (таблица): температура, плотность, давление и пр.

Физические свойства калия

Химические свойства калия. Взаимодействие калия. Реакции с калием

Получение калия

Применение калия

Таблица химических элементов Д.И. Менделеева

Атом и молекула калия. Формула калия. Строение калия:

Калий (лат. Kalium, от араб. аль-кали – «поташ») – химический элемент периодической системы химических элементов Д. И. Менделеева с обозначением K и атомным номером 19. Расположен в 1-й группе (по старой классификации – главной подгруппе первой группы), четвертом периоде периодической системы.

Калий – металл. Относится к группе щелочных металлов, а также лёгких, цветных металлов.

Калий обозначается символом K.

Как простое вещество калий при нормальных условиях представляет собой мягкий металл серебристо-белого цвета.

Молекула калия одноатомна.

Химическая формула калия K.

Электронная конфигурация атома калия 1s² 2s² 2p⁶ 3s² 3p⁶ 4s¹. Потенциал ионизации (первый электрон) атома калия равен 418,81 кДж/моль (4,34066369(9) эВ).

Строение атома калия. Атом калия состоит из положительно заряженного ядра (+19), вокруг которого по четырем оболочкам движутся 19 электронов. При этом 18 электронов находятся на внутреннем уровне, а 1 электрон – на внешнем. Поскольку калий расположен в четвертом периоде, оболочек всего четыре. Первая – внутренняя оболочка представлена s-орбиталью. Вторая и третья – внутренние оболочки представлена s- и р-орбиталями. Четвертая – внешняя оболочка представлена s-орбиталью. На внешнем энергетическом уровне атома калия – на 4s-орбитали находится один неспаренный электрон. В свою очередь ядро атома калия состоит из 19 протонов и 20 нейтронов. Калий относится к элементам s-семейства.

Радиус атома калия (вычисленный) составляет 243 пм.

Атомная масса атома калия составляет 39,0983(1) а. е. м.

Калий – седьмой по распространённости элемент в земной коре. Содержание его в земной коре составляет 1,5 %, в океанах и морях – 0,042 %.

Калий очень легко вступает в химические реакции.

Изотопы и модификации калия:

Свойства калия (таблица): температура, плотность, давление и пр.:

Подробные сведения на сайте ChemicalStudy.ru

100	Общие сведения
101	Название	Калий
102	Прежнее название
103	Латинское название	Kalium
104	Английское название	Potassium
105	Символ	K
106	Атомный номер (номер в таблице)	19
107	Тип	Металл
108	Группа	Щелочной, лёгкий, цветной металл
109	Открыт	Хемфри Дэви, Великобритания, 1807 г.
110	Год открытия	1807 г.
111	Внешний вид и пр.	Мягкий, серебристо-белый металл
112	Происхождение	Природный материал
113	Модификации
114	Аллотропные модификации
115	Температура и иные условия перехода аллотропных модификаций друг в друга
116	Конденсат Бозе-Эйнштейна	39K, 41K
117	Двумерные материалы
118	Содержание в атмосфере и воздухе (по массе)	0 %
119	Содержание в земной коре (по массе)	1,5 %
120	Содержание в морях и океанах (по массе)	0,042 %
121	Содержание во Вселенной и космосе (по массе)	0,0003 %
122	Содержание в Солнце (по массе)	0,0004 %
123	Содержание в метеоритах (по массе)	0,07 %
124	Содержание в организме человека (по массе)	0,2 %
200	Свойства атома
201	Атомная масса (молярная масса)	39,0983(1) а. е. м. (г/моль)
202	Электронная конфигурация	1s2 2s2 2p6 3s2 3p6 4s1
203	Электронная оболочка	K2 L8 M8 N1 O0 P0 Q0 R0
204	Радиус атома (вычисленный)	243 пм
205	Эмпирический радиус атома*	220 пм
206	Ковалентный радиус*	203 пм
207	Радиус иона (кристаллический)	K+ 151 (4) пм, 152 (6) пм, 165 (8) пм, 178 (12) пм (в скобках указано координационное число – характеристика, которая определяет число ближайших частиц (ионов или атомов) в молекуле или кристалле)
208	Радиус Ван-дер-Ваальса	275 пм
209	Электроны, Протоны, Нейтроны	19 электронов, 19 протонов, 20 нейтронов
210	Семейство (блок)	элемент s-семейства
211	Период в периодической таблице	4
212	Группа в периодической таблице	1-ая группа (по старой классификации – главная подгруппа 1-ой группы)
213	Эмиссионный спектр излучения
300	Химические свойства
301	Степени окисления	0, +1
302	Валентность	I
303	Электроотрицательность	0,82 (шкала Полинга)
304	Энергия ионизации (первый электрон)	418,81 кДж/моль (4,34066369(9) эВ)
305	Электродный потенциал	K+ + e– → K, Eo = -2,924 В
306	Энергия сродства атома к электрону	48,383(2) кДж/моль (0,501459(13) эВ)
400	Физические свойства
401	Плотность*	0,862 г/см3 (при 20 °C и иных стандартных условиях, состояние вещества – твердое тело), 0,828  г/см3 (при температуре плавления 63,5 °C и иных стандартных условиях, состояние вещества – жидкость)
402	Температура плавления*	63,5 °C (336,7 K, 146,3 °F)
403	Температура кипения*	759 °C (1032 K, 1398 °F)
404	Температура сублимации
405	Температура разложения
406	Температура самовоспламенения смеси газа с воздухом
407	Удельная теплота плавления (энтальпия плавления ΔHпл)*	2,33 кДж/моль
408	Удельная теплота испарения (энтальпия кипения ΔHкип)*	76,9 кДж/моль
409	Удельная теплоемкость при постоянном давлении
410	Молярная теплоёмкость	29,6 Дж/(K·моль)
411	Молярный объём	45,675584 см³/моль
412	Теплопроводность	102,5 Вт/(м·К) (при стандартных условиях), 79,0 Вт/(м·К) (при 300 K)
500	Кристаллическая решётка
511	Кристаллическая решётка #1
512	Структура решётки	Кубическая объёмно-центрированная
513	Параметры решётки	5,332 Å
514	Отношение c/a
515	Температура Дебая	100 К
516	Название пространственной группы симметрии	Im_ 3m
517	Номер пространственной группы симметрии	229
900	Дополнительные сведения
901	Номер CAS	7440-09-7

Примечание:

205* Эмпирический радиус атома калия согласно [1] и [3] составляет 227 пм и 235 пм соответственно.

206* Ковалентный радиус калия согласно [1] составляет 203±12 пм.

401* Плотность калия согласно [3] составляет 0,856 г/см³ (при 0 °C и иных стандартных условиях, состояние вещества – твердое тело), согласно [4] 0,826  г/см³ (при 64 °C и иных стандартных условиях, состояние вещества – жидкость).

402* Температура плавления калия согласно [3] и [4] составляет 63,65 °C  (336,8 K, 146,57 °F) и 63,55 °C (336,7 K, 146,39 °F) соответственно.

403* Температура кипения калия согласно [3] и [4] составляет 773,85 °C (1047 K, 1424,93 °F) и 776 °C (1049,15 K, 1428,8 °F) соответственно.

407* Удельная теплота плавления (энтальпия плавления ΔH_пл) калия согласно [4] составляет 2,38 кДж/моль.

408* Удельная теплота испарения (энтальпия кипения ΔH_кип) калия согласно [4] составляет 79,2 кДж/моль.

Физические свойства калия:

Химические свойства калия. Взаимодействие калия. Реакции с калием:

Получение калия:

Применение калия:

Таблица химических элементов Д.И. Менделеева

1. 1. Водород
2. 2. Гелий
3. 3. Литий
4. 4. Бериллий
5. 5. Бор
6. 6. Углерод
7. 7. Азот
8. 8. Кислород
9. 9. Фтор
10. 10. Неон
11. 11. Натрий
12. 12. Магний
13. 13. Алюминий
14. 14. Кремний
15. 15. Фосфор
16. 16. Сера
17. 17. Хлор
18. 18. Аргон
19. 19. Калий
20. 20. Кальций
21. 21. Скандий
22. 22. Титан
23. 23. Ванадий
24. 24. Хром
25. 25. Марганец
26. 26. Железо
27. 27. Кобальт
28. 28. Никель
29. 29. Медь
30. 30. Цинк
31. 31. Галлий
32. 32. Германий
33. 33. Мышьяк
34. 34. Селен
35. 35. Бром
36. 36. Криптон
37. 37. Рубидий
38. 38. Стронций
39. 39. Иттрий
40. 40. Цирконий
41. 41. Ниобий
42. 42. Молибден
43. 43. Технеций
44. 44. Рутений
45. 45. Родий
46. 46. Палладий
47. 47. Серебро
48. 48. Кадмий
49. 49. Индий
50. 50. Олово
51. 51. Сурьма
52. 52. Теллур
53. 53. Йод
54. 54. Ксенон
55. 55. Цезий
56. 56. Барий
57. 57. Лантан
58. 58. Церий
59. 59. Празеодим
60. 60. Неодим
61. 61. Прометий
62. 62. Самарий
63. 63. Европий
64. 64. Гадолиний
65. 65. Тербий
66. 66. Диспрозий
67. 67. Гольмий
68. 68. Эрбий
69. 69. Тулий
70. 70. Иттербий
71. 71. Лютеций
72. 72. Гафний
73. 73. Тантал
74. 74. Вольфрам
75. 75. Рений
76. 76. Осмий
77. 77. Иридий
78. 78. Платина
79. 79. Золото
80. 80. Ртуть
81. 81. Таллий
82. 82. Свинец
83. 83. Висмут
84. 84. Полоний
85. 85. Астат
86. 86. Радон
87. 87. Франций
88. 88. Радий
89. 89. Актиний
90. 90. Торий
91. 91. Протактиний
92. 92. Уран
93. 93. Нептуний
94. 94. Плутоний
95. 95. Америций
96. 96. Кюрий
97. 97. Берклий
98. 98. Калифорний
99. 99. Эйнштейний
100. 100. Фермий
101. 101. Менделеевий
102. 102. Нобелий
103. 103. Лоуренсий
104. 104. Резерфордий
105. 105. Дубний
106. 106. Сиборгий
107. 107. Борий
108. 108. Хассий
109. 109. Мейтнерий
110. 110. Дармштадтий
111. 111. Рентгений
112. 112. Коперниций
113. 113. Нихоний
114. 114. Флеровий
115. 115. Московий
116. 116. Ливерморий
117. 117. Теннессин
118. 118. Оганесон

Таблица химических элементов Д.И. Менделеева

Источники:

1. https://en.wikipedia.org/wiki/Potassium
2. https://de.wikipedia.org/wiki/Kalium
3. https://ru.wikipedia.org/wiki/Калий
4. http://chemister.ru/Database/properties.php?dbid=1&id=229
5. https://chemicalstudy.ru/kaliy-svoystva-atoma-himicheskie-i-fizicheskie-svoystva/

Примечание: © Фото https://www.pexels.com, https://pixabay.com

калий атомная масса степень окисления валентность плотность температура кипения плавления физические химические свойства структура теплопроводность электропроводность кристаллическая решетка
атом нарисовать строение число протонов в ядре строение электронных оболочек электронная формула конфигурация схема строения электронной оболочки заряд ядра состав масса орбита уровни модель радиус энергия электрона переход скорость спектр длина волны молекулярная масса объем атома
электронные формулы сколько атомов в молекуле калия
сколько электронов в атоме свойства металлические неметаллические термодинамические 

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