칼륨 (K)

발견 과정

발견: 1807 · Humphry Davy

Potassium metal was first isolated in 1807 by Humphry Davy, who derived it by electrolysis of molten caustic potash (KOH) with the newly discovered voltaic pile. Potassium was the first metal that was isolated by electrolysis. 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. 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.

용도와 활용

Reflecting its low first ionization energy of 418.8 kJ/mol, potassium is a strong reducing agent, i.e., it readily releases an electron upon contact with other materials. With graphite, potassium metal forms graphite intercalation compounds. One such compound has the formula KC8, a gold colored solid that is described as a K+ salt of negatively charged graphite. Potassium can reduce many salts to the metal as illustrated by the Rieke method for making magnesium powder from magnesium chloride:

동위원소

There are 25 known isotopes of potassium, three of which occur naturally: 39K (93.3%), 40K (0.0117%), and 41K (6.7%) (by mole fraction). Naturally occurring 40K has a half-life of 1.250×109 years. It decays to stable 40Ar by electron capture or positron emission (11.2%) or to stable 40Ca by beta decay (88.8%). This decay results in a relatively higher concentration of Argon in the atmosphere. The decay of 40K to 40Ar is the basis of a common 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 radiogenic argon (40Ar) was quantitatively retained. Minerals are dated by measurement of the concentration of potassium and the amount of radiogenic 40Ar that has accumulated. The minerals best suited for dating include biotite, muscovite, metamorphic hornblende, and