Under
standard conditions, germanium is a brittle, silvery-white, At pressures above 120
kbar, germanium becomes the metallic allotrope
β-germanium with the same structure as β-
tin. making it one of the purest materials ever obtained. The first semi-metallic material discovered (in 2005) to become a
superconductor in the presence of an extremely strong
electromagnetic field was an
alloy of germanium, uranium, and rhodium. Pure germanium is known to spontaneously extrude very long
screw dislocations, referred to as
germanium whiskers. The growth of these whiskers is one of the primary reasons for the failure of older diodes and transistors made from germanium, as, depending on what they eventually touch, they may lead to an
electrical short.
Chemistry Elemental germanium starts to oxidize slowly in air at around 250 °C, forming
GeO2 . Germanium is insoluble in dilute
acids and
alkalis but dissolves slowly in hot concentrated sulfuric and nitric acids and reacts violently with molten alkalis to produce
germanates (). Germanium occurs mostly in the
oxidation state +4 although many +2 compounds are known. Other oxidation states are rare: +3 is found in compounds such as Ge2Cl6, and +3 and +1 are found on the surface of oxides, or negative oxidation states in
germanides, such as −4 in . Germanium cluster anions (
Zintl ions) such as , , , have been prepared by the extraction from alloys containing alkali metals and germanium in liquid ammonia in the presence of
ethylenediamine or a
cryptand. The oxidation states of the element in these ions are not integers—similar to the
ozonides O3−. Two
oxides of germanium are known:
germanium dioxide (, germania) and
germanium monoxide, (). The dioxide, GeO2, can be obtained by roasting
germanium disulfide (), and is a white powder that is only slightly soluble in water but reacts with alkalis to form
germanates.
Bismuth germanate, Bi4Ge3O12 (BGO), is used as a
scintillator.
Binary compounds with other
chalcogens are also known, such as the
disulfide () and
diselenide (), and the
monosulfide (GeS),
monoselenide (GeSe), and
monotelluride (GeTe). By heating the disulfide in a current of
hydrogen, the monosulfide (GeS) is formed, which sublimes in thin plates of a dark color and metallic luster, and is soluble in solutions of the caustic alkalis. .|alt=Skeletal chemical structure of a tetrahedral molecule with germanium atom in its center bonded to four hydrogen atoms. The Ge–H distance is 152.51 picometers. Four tetra
halides are known. Under normal conditions
germanium tetraiodide (GeI4) is a solid,
germanium tetrafluoride (GeF4) a gas and the others volatile liquids. For example,
germanium tetrachloride, GeCl4, is obtained as a colorless fuming liquid boiling at 83.1 °C by heating the metal with chlorine.
Germane (GeH4) is a compound similar in structure to
methane. Polygermanes—compounds that are similar to
alkanes—with formula Ge
nH2
n+2 containing up to five germanium atoms are known. The organogermanium compound
2-carboxyethylgermasesquioxane was first reported in the 1970s, and for a while was used as a dietary supplement and thought to possibly have anti-tumor qualities.
Isotopes Germanium occurs in five natural
isotopes: , , , , and . Of these, is very slightly radioactive, undergoing
double beta decay with a
half-life of . Apart from , at least 27 other
radioisotopes have been synthesized, ranging in atomic mass from 58 to 89. The most stable of these is , decaying by
electron capture with a half-life of . This is followed by , also decaying by electron capture with half-life , Germanium has been detected in some of the most distant stars and in the atmosphere of Jupiter. Germanium's abundance
in the Earth's crust is approximately 1.6
ppm. Only a few minerals like
argyrodite,
briartite,
germanite,
renierite and
sphalerite contain appreciable amounts of germanium. Only few of them (especially germanite) are, very rarely, found in mineable amounts. Some zinc–copper–lead ore bodies contain enough germanium to justify extraction from the final ore concentrate. The highest concentration ever found was in
Hartley coal ash with as much as 1.6% germanium. The coal deposits near
Xilinhaote,
Inner Mongolia, contain an estimated 1600
tonnes of germanium. == Production ==