Difference between revisions of "Potassium" - New World Encyclopedia

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'''Potassium''' (chemical symbol '''K''', [[atomic number]] 19) is a silvery white metal.
+
'''Potassium''' (chemical symbol '''K''', [[atomic number]] 19) is a member of a group of chemical elements known as alkali metals.
 +
 
 +
*silvery white metal.
  
 
*is the [[chemical element]] in the [[periodic table]].
 
*is the [[chemical element]] in the [[periodic table]].
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Potassium minerals such as [[carnallite]]*, [[langbeinite]]*, [[polyhalite]]*, and [[sylvite]]* form extensive deposits in the beds of ancient [[lake]]s and [[sea]]s. The principal source of potassium, potash (impure form of potassium carbonate), is mined in California, New Mexico, Utah, [[Germany]], and in other places around the world. Large deposits of potash have been found about 3,000 feet below the surface of [[Saskatchewan]]*, and several large mines have been in operation since the 1960s. Saskatchewan pioneered the method of freezing wet sands (the Blairmore formation) as a way to drive mine shafts through them. The [[ocean]]s are another source of potassium, but the quantity present in a given volume of [[seawater]]* is relatively low, compared to the concentration of [[sodium]].
 
Potassium minerals such as [[carnallite]]*, [[langbeinite]]*, [[polyhalite]]*, and [[sylvite]]* form extensive deposits in the beds of ancient [[lake]]s and [[sea]]s. The principal source of potassium, potash (impure form of potassium carbonate), is mined in California, New Mexico, Utah, [[Germany]], and in other places around the world. Large deposits of potash have been found about 3,000 feet below the surface of [[Saskatchewan]]*, and several large mines have been in operation since the 1960s. Saskatchewan pioneered the method of freezing wet sands (the Blairmore formation) as a way to drive mine shafts through them. The [[ocean]]s are another source of potassium, but the quantity present in a given volume of [[seawater]]* is relatively low, compared to the concentration of [[sodium]].
  
Potassium can be isolated through the [[electrolysis]] of its hydroxide, by a process that has changed little since the time of Davy. Thermal methods are also employed in potassium production from potassium chloride.
+
Potassium can be isolated through the [[electrolysis]] of its hydroxide, by a process that has changed little since the time of Davy. Thermal methods are also employed to obtain potassium from potassium chloride.
  
 
== Notable characteristics ==
 
== Notable characteristics ==
With a density less than that of water, potassium is the second least dense metal after [[lithium]]. It is a soft, low-melting solid that can easily be cut with a knife.  Freshly cut potassium is silvery in appearance but it quickly tarnishes.  It [[redox|oxidizes]] in [[Earth's atmosphere|air]] rapidly and thus should be protected for storage.  Often samples are maintained under an inert medium such as kerosene.
 
  
Similar to other alkali metals but more so than Li and Na, potassium reacts violently with [[water]] producing [[hydrogen]]. The reaction is sufficiently exothermic that the evolved hydrogen gas ignites. Potassium and its compounds emit a [[violet (color)|violet]] [[color]] in a flame. This fact is the basis of the [[flame test]] for the presence of potassium in a sample.
+
As an alkali metal, potassium is part of group 1 of the [[periodic table]], between [[sodium]] and [[rubidium]], and it lies in period 4, just before [[calcium]]. It is a soft, low-melting solid that can be easily cut with a knife. With a density less than that of water, potassium is the second least dense metal after [[lithium]].
 +
 
 +
Like other alkali metals, potassium has a single electron in its outermost shell, and it can readily lose this electron to become a positive ion. For this reason, although freshly cut potassium is silvery in appearance, it [[redox|oxidizes]] and tarnishes rapidly when exposed to the [[Earth's atmosphere|air]]. In addition, it reacts violently with [[water]], even more so than [[lithium]] or [[sodium]], producing [[hydrogen]]. The reaction produces so much heat that the evolved hydrogen gas ignites. To prevent this from happening, samples of potassium are stored in an inert medium such as kerosene.
 +
 
 +
Potassium and its compounds emit a violet [[color]] in a flame. This fact is the basis of the [[flame test]]* for the presence of potassium in a sample.
 +
 
 +
=== Isotopes ===
 +
[[Image:PotassiumFeldsparUSGOV.jpg|thumb|left|Potassium in [[feldspar]]]]
 +
 
 +
There are 17 known [[isotope]]s of potassium, three of which occur naturally: <sup>39</sup>K (93.3%), <sup>40</sup>K (0.012%), and <sup>41</sup>K (6.7%). The isotope <sup>40</sup>K is radioactive and decays to stable <sup>40</sup>Ar ([[argon]]-40) (11.2%) by [[electron capture]]* and [[positron emission]]*, and it decays to stable <sup>40</sup>Ca ([[calcium]]-40) (88.8%) by [[beta decay]]*. The [[half-life]]* of <sup>40</sup>K is 1.250&times;10<sup>9</sup> years.
 +
 
 +
The decay of <sup>40</sup>K to <sup>40</sup>Ar is the basis for a commonly used method for dating rocks. The conventional potassium-argon dating method depends on the assumption that the rocks contained no argon at the time of formation and that all the subsequent <sup>40</sup>Ar was quantitatively retained. [[Mineral]]s are dated by measurement of the concentration of potassium and the amount of radiogenic (radioactively produced) <sup>40</sup>Ar that has accumulated. Minerals that are best suited for dating include [[biotite]]*, [[muscovite]]*, plutonic/high grade metamorphic [[hornblende]]*, and volcanic [[feldspar]]*. Whole rock samples from volcanic flows and shallow instrusives can also be dated if they are unaltered.
 +
 
 +
Besides their use for dating, potassium isotopes have been used extensively as [[radioactive tracer]]*s in studies of [[weathering]]*. They have also been used for [[nutrient cycling]]* studies because potassium is a [[macronutrient]]* required for living organisms.
 +
 
 +
Given that radioactive <sup>40</sup>K occurs in nature, it becomes part of some commercially available salt substitutes in sufficient quantity for large bags of those substitutes to be used as a radioactive source for classroom demonstrations. In healthy animals and people, <sup>40</sup>K represents the largest source of radioactivity, greater even then <sup>14</sup>C (carbon-14). In a person who weighs 70 kilograms (kg), about 4,000 nuclei of <sup>40</sup>K decay per second. [http://www.fas.harvard.edu/~scdiroff/lds/QuantumRelativity/RadioactiveHumanBody/RadioactiveHumanBody.html]
  
 
== Applications ==
 
== Applications ==
 +
 
*It is primarily used in [[fertilizer]] as either the [[Potassium chloride|chloride]], [[Potassium sulfate|sulfate]] or [[Potassium carbonate|carbonate]] - not as the [[Potassium oxide|oxide]].
 
*It is primarily used in [[fertilizer]] as either the [[Potassium chloride|chloride]], [[Potassium sulfate|sulfate]] or [[Potassium carbonate|carbonate]] - not as the [[Potassium oxide|oxide]].
 
*[[Potassium hydroxide]] is an important industrial chemical used as a strong base.
 
*[[Potassium hydroxide]] is an important industrial chemical used as a strong base.
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Many potassium salts are very important, and include: [[potassium bromide]], [[potassium carbonate]], [[potassium chlorate]], [[potassium chloride]], [[potassium chromate]], [[potassium cyanide]], [[potassium dichromate]], [[potassium iodide]], [[potassium nitrate]], [[potassium sulfate]].
 
Many potassium salts are very important, and include: [[potassium bromide]], [[potassium carbonate]], [[potassium chlorate]], [[potassium chloride]], [[potassium chromate]], [[potassium cyanide]], [[potassium dichromate]], [[potassium iodide]], [[potassium nitrate]], [[potassium sulfate]].
  
 +
== Precautions ==
  
 
 
 
== Isotopes ==
 
[[Image:PotassiumFeldsparUSGOV.jpg|thumb|left|Potassium in [[feldspar]]]]
 
There are seventeen known [[isotope]]s of potassium. Three isotopes occur naturally: <sup>39</sup>K (93.3%), <sup>40</sup>K (0.012%) and <sup>41</sup>K (6.7%). Naturally occurring <sup>40</sup>K decays to stable [[Argon|<sup>40</sup>Ar]] (11.2%) by [[electron capture]] and by [[positron emission]], and decays to stable [[Calcium|<sup>40</sup>Ca]] (88.8%) by [[beta decay]]; <sup>40</sup>K has a [[half-life]] of 1.250&times;10<sup>9</sup> years.
 
 
The decay of <sup>40</sup>K to <sup>40</sup>Ar enables a commonly used method for dating rocks. The conventional [[Potassium-argon dating|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 (i.e., <sup>40</sup>Ar) was quantitatively retained. [[Mineral]]s are dated by measurement of the concentration of potassium and the amount of radiogenic <sup>40</sup>Ar that has accumulated. The minerals that are best suited for dating include [[biotite]], [[muscovite]], plutonic/high grade metamorphic [[hornblende]], and volcanic [[feldspar]]; whole rock samples from volcanic flows and shallow instrusives can also be dated if they are unaltered.
 
 
Outside of dating, potassium isotopes have been used extensively as [[radioactive tracer|tracer]]s in studies of [[weathering]]. They have also be used for [[nutrient cycling]] studies because potassium is a [[macro-nutrient]] required for [[life]].
 
 
<sup>40</sup>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.  In healthy animals and people, <sup>40</sup>K represents the largest source of radioactivity, greater even then <sup>14</sup>C. In a human body of 70 kg mass, about 4,000 nuclei of <sup>40</sup>K decay per second. [http://www.fas.harvard.edu/~scdiroff/lds/QuantumRelativity/RadioactiveHumanBody/RadioactiveHumanBody.html]
 
 
== Precautions ==
 
 
Solid potassium reacts violently with water, and should therefore be kept under a mineral oil such as [[kerosene]] and handled with care. Unlike lithium and sodium however, potassium cannot be stored under oil indefinitely.  If stored longer than 6 months to a year, dangerous shock-sensitive peroxides can form on the metal and under the lid of the container that can detonate upon opening. DO NOT store potassium, rubidium or cesium for longer than a year unless stored in an inert (argon) atmosphere or in a vacuum.
 
Solid potassium reacts violently with water, and should therefore be kept under a mineral oil such as [[kerosene]] and handled with care. Unlike lithium and sodium however, potassium cannot be stored under oil indefinitely.  If stored longer than 6 months to a year, dangerous shock-sensitive peroxides can form on the metal and under the lid of the container that can detonate upon opening. DO NOT store potassium, rubidium or cesium for longer than a year unless stored in an inert (argon) atmosphere or in a vacuum.
  
 
== Potassium in diet ==
 
== Potassium in diet ==
 +
 
Potassium is an [[essential]] mineral [[micronutrient]] in human nutrition; it assists in [[muscle]] contraction and in maintaining fluid and [[electrolyte]] balance in body cells. Potassium is also important in sending nerve impulses as well as releasing [[energy]] from [[protein]], [[fat]], and [[carbohydrate]]s during [[metabolism]].
 
Potassium is an [[essential]] mineral [[micronutrient]] in human nutrition; it assists in [[muscle]] contraction and in maintaining fluid and [[electrolyte]] balance in body cells. Potassium is also important in sending nerve impulses as well as releasing [[energy]] from [[protein]], [[fat]], and [[carbohydrate]]s during [[metabolism]].
  

Revision as of 19:16, 6 August 2006

19 argonpotassiumcalcium
Na

K

Rb
K-TableImage.png
periodic table
General
Name, Symbol, Number potassium, K, 19
Chemical series alkali metals
Group, Period, Block 1, 4, s
Appearance silvery white
K,19.jpg
Atomic mass 39.0983(1) g/mol
Electron configuration [Ar] 4s1
Electrons per shell 2, 8, 8, 1
Physical properties
Phase solid
Density (near r.t.) 0.89 g/cm³
Liquid density at m.p. 0.828 g/cm³
Melting point 336.53 K
(63.38 °C, 146.08 °F)
Boiling point 1032 K
(759 °C, 1398 °F)
Critical point (extrapolated)
2223 K, 16 MPa
Heat of fusion 2.321 kJ/mol
Heat of vaporization 76.90 kJ/mol
Heat capacity (25 °C) 29.600 J/(mol·K)
Vapor pressure
P/Pa 1 10 100 1 k 10 k 100 k
at T/K 473 530 601 697 832 1029
Atomic properties
Crystal structure cubic body centered
Oxidation states 1
(strongly basic oxide)
Electronegativity 0.82 (Pauling scale)
Ionization energies
(more)
1st: 418.8 kJ/mol
2nd: 3052 kJ/mol
3rd: 4420 kJ/mol
Atomic radius 220 pm
Atomic radius (calc.) 243 pm
Covalent radius 196 pm
Van der Waals radius 275 pm
Miscellaneous
Magnetic ordering ?
Electrical resistivity (20 °C) 72.0 nΩ·m
Thermal conductivity (300 K) 102.5 W/(m·K)
Thermal expansion (25 °C) 83.3 µm/(m·K)
Speed of sound (thin rod) (20 °C) 2000 m/s
Shear modulus 1.3 GPa
Bulk modulus 3.1 GPa
Mohs hardness 0.4
Brinell hardness 0.363 MPa
CAS registry number 7440-09-7
Notable isotopes
Main article: Isotopes of potassium
iso NA half-life DM DE (MeV) DP
39K 93.26% K is stable with 20 neutrons
40K 0.012% 1.277×109 y β- 1.311 40Ca
ε 1.505 40Ar
β+ 1.505 40Ar
41K 6.73% K is stable with 22 neutrons

Potassium (chemical symbol K, atomic number 19) is a member of a group of chemical elements known as alkali metals.

  • silvery white metal.

Discovery and etymology

Potassium was discovered in 1807 by Sir Humphry Davy, who derived it from caustic potash (potassium hydroxide, KOH). It was the first metal isolated by electrolysis.

Potassium was not known to the ancient Romans, and its names are neo-Latin, not Classical Latin. The Latin name kalium (from which potassium gets its symbol, K) was taken from the word "alkali", which came from Arabic al qalīy, meaning "the calcined ashes." The name potassium was made from the English word "potash," which originally meant an alkali extracted in water in a pot of ash of burnt wood or tree leaves.

Occurrence

Potassium makes up about 2.4% of the weight of the Earth's crust and is the seventh most abundant element in it. As it is very electropositive, potassium is never found as the free element in nature. Rather, it forms compounds from which it is difficult to separate.

Potassium minerals such as carnallite, langbeinite, polyhalite, and sylvite form extensive deposits in the beds of ancient lakes and seas. The principal source of potassium, potash (impure form of potassium carbonate), is mined in California, New Mexico, Utah, Germany, and in other places around the world. Large deposits of potash have been found about 3,000 feet below the surface of Saskatchewan, and several large mines have been in operation since the 1960s. Saskatchewan pioneered the method of freezing wet sands (the Blairmore formation) as a way to drive mine shafts through them. The oceans are another source of potassium, but the quantity present in a given volume of seawater is relatively low, compared to the concentration of sodium.

Potassium can be isolated through the electrolysis of its hydroxide, by a process that has changed little since the time of Davy. Thermal methods are also employed to obtain potassium from potassium chloride.

Notable characteristics

As an alkali metal, potassium is part of group 1 of the periodic table, between sodium and rubidium, and it lies in period 4, just before calcium. It is a soft, low-melting solid that can be easily cut with a knife. With a density less than that of water, potassium is the second least dense metal after lithium.

Like other alkali metals, potassium has a single electron in its outermost shell, and it can readily lose this electron to become a positive ion. For this reason, although freshly cut potassium is silvery in appearance, it oxidizes and tarnishes rapidly when exposed to the air. In addition, it reacts violently with water, even more so than lithium or sodium, producing hydrogen. The reaction produces so much heat that the evolved hydrogen gas ignites. To prevent this from happening, samples of potassium are stored in an inert medium such as kerosene.

Potassium and its compounds emit a violet color in a flame. This fact is the basis of the flame test for the presence of potassium in a sample.

Isotopes

Potassium in feldspar

There are 17 known isotopes of potassium, three of which occur naturally: 39K (93.3%), 40K (0.012%), and 41K (6.7%). The isotope 40K is radioactive and decays to stable 40Ar (argon-40) (11.2%) by electron capture and positron emission, and it decays to stable 40Ca (calcium-40) (88.8%) by beta decay. The half-life of 40K is 1.250×109 years.

The decay of 40K to 40Ar is the basis for a commonly used method for dating rocks. The conventional potassium-argon dating method depends on the assumption that the rocks contained no argon at the time of formation and that all the subsequent 40Ar was quantitatively retained. Minerals are dated by measurement of the concentration of potassium and the amount of radiogenic (radioactively produced) 40Ar that has accumulated. Minerals that are best suited for dating include biotite, muscovite, plutonic/high grade metamorphic hornblende, and volcanic feldspar. Whole rock samples from volcanic flows and shallow instrusives can also be dated if they are unaltered.

Besides their use for dating, potassium isotopes have been used extensively as radioactive tracers in studies of weathering. They have also been used for nutrient cycling studies because potassium is a macronutrient required for living organisms.

Given that radioactive 40K occurs in nature, it becomes part of some commercially available salt substitutes in sufficient quantity for large bags of those substitutes to be used as a radioactive source for classroom demonstrations. In healthy animals and people, 40K represents the largest source of radioactivity, greater even then 14C (carbon-14). In a person who weighs 70 kilograms (kg), about 4,000 nuclei of 40K decay per second. [1]

Applications

  • It is primarily used in fertilizer as either the chloride, sulfate or carbonate - not as the oxide.
  • Potassium hydroxide is an important industrial chemical used as a strong base.
  • Potassium nitrate is used in gunpowder (black powder). An older term for KNO3 is saltpeter.
  • Potassium carbonate, known as potash, is used in glass manufacture.
  • Glass treated with liquid potassium is much stronger than regular glass.
  • NaK, an alloy of sodium and potassium, is used as a heat-transfer medium.
  • Potassium is an essential component needed in plant growth and is found in most soil types.
  • In animal cells potassium ions are vital to keeping cells alive (see Na-K pump)
  • Potassium chloride is used as a substitute for table salt and is also used to stop the heart, e.g. in cardiac surgery and in executions by lethal injection in solution.
  • The superoxide KO2 is used as a portable source of oxygen and as a carbon dioxide absorber. It is useful in portable respiration systems.

Many potassium salts are very important, and include: potassium bromide, potassium carbonate, potassium chlorate, potassium chloride, potassium chromate, potassium cyanide, potassium dichromate, potassium iodide, potassium nitrate, potassium sulfate.

Precautions

Solid potassium reacts violently with water, and should therefore be kept under a mineral oil such as kerosene and handled with care. Unlike lithium and sodium however, potassium cannot be stored under oil indefinitely. If stored longer than 6 months to a year, dangerous shock-sensitive peroxides can form on the metal and under the lid of the container that can detonate upon opening. DO NOT store potassium, rubidium or cesium for longer than a year unless stored in an inert (argon) atmosphere or in a vacuum.

Potassium in diet

Potassium is an essential mineral micronutrient in human nutrition; it assists in muscle contraction and in maintaining fluid and electrolyte balance in body cells. Potassium is also important in sending nerve impulses as well as releasing energy from protein, fat, and carbohydrates during metabolism.

A shortage of potassium can cause a potentially fatal condition known as hypokalemia, typically resulting from diarrhea, increased diuresis and vomiting. Deficiency symptoms include, muscle weakness, paralytic ileus, ECG abnormalities, decreased reflex response, and in severe form respiratory paralysis and alkalosis and arrhythmia.

Eating a variety of foods that contain potassium is the best way to get an adequate amount. Healthy individuals who eat a balanced diet rarely need supplements. Foods with high sources of potassium include orange juice, avocados, celery, parsnips and turnips, although many other fruits, vegetables, and meats contain potassium. Research has indicated that diets high in potassium can reduce the risk of hypertension.

The 2004 guidelines of the Institute of Medicine specify an RDA of 4,700 mg of potassium. However, it is thought that most Americans consume only half that amount per day ([2]). Similarly, in the European Union, particularly in Germany and Italy, insufficient potassium intake is widespread ([3]).

Some people with kidney disease are advised to avoid large quantities of dietary potassium.

See also

  • Potassium compounds
  • Potassium in biology

References
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External links

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