CAS: 7440-56-4
Description: Hard brittle grayish-white metal
Classification: Metalloid
Date of Discovery: 1886
Discoverer: Clemens Winkler
Name Origin: Latin Germania, "Germany"
Atomic Number: 32
Number of Neutrons: 41
Atomic Mass: 72.61(2) amu
Melting Point: 938.25 °C
Boiling Point: 2833 °C
Density (293 K): 5.323 g/cm3 Atomic volume: 13.6 cm3/mol
Electrical resistivity: 1.45e-8 10-6/cm Thermal conductivity: 0.599 W/cmK
Enthalpy of atomization: 376.56 kJ/mol
Enthalpy of vaporization: 330.90 kJ/mol
Enthalpy of fusion: 36.940 kJ/mol
Specific heat capacity: 0.32 J/gK
Energy levels: 2-8-18-4
Electron configuration: [Ar]3d104s24p2 Crystal Structure: Cubic face centered
Atomic radius: 1.52 Å
Covalent radius: 1.22 Å
Oxidation States: +2, +4
Electronegativity, Pauling: 1.61
Electron affinity: 1.233 eV
First ionization energy: 7.899 eV
2nd ionization energy: 15.934 eV
3rd ionization energy: 34.22 eV
Polarizability: 6.07 10-24cm3
Isotope
Natural Abundance
Atomic Mass
Half-life
Decay Mode
Spin
61Ge
60.9638
0.04 s
+
63Ge
62.9496
0.10 s
-
64Ge
63.9416
1.06 m
+; EC
0+
65Ge
64.9394
31 s
+; EC
66Ge
65.93385
2.26 h
+; EC
0+
67Ge
66.932738
19.0 m
+; EC
1/2-
68Ge
67.92810
270.8 d
EC
0+
69Ge
68.927973
1.63 d
+; EC
5/2-
70Ge
21.23(4)
69.924250
Stable
0+
71mGe
20.4 ms
IT
9/2+
71Ge
70.924954
11.2 d
EC
1/2-
72Ge
27.66(3)
71.922076
Stable
0+
73Ge
7.73(1)
72.923460
Stable
9/2+
74Ge
35.94(2)
73.921178
Stable
0+
75mGe
48 s
IT
7/2+
75Ge
74.922860
1.380 h
-
1/2-
76Ge
7.44(2)
75.921403
Stable
0+
77mGe
53 s
IT; -
1/2-
77Ge
76.923549
11.30 h
-
7/2+
78Ge
77.922853
1.45 h
-
0+
79mGe
39 s
-; IT
7/2+
79Ge
78.9254
19.1
-
1/2-
80Ge
79.92545
29.5 s
-
0+
81mGe
7.6 s
-
1/2+
81Ge
80.9288
7.6 s
-
9/2+
82Ge
81.9296
4.6 s
-
0+
83Ge
82.9345
1.9 s
-
84Ge
83.9373
0.98 s
-
85Ge
83.943
0.54 s
-
Predicted by Mendeleev in 1871 as ekasilicon, and discovered by Winkler in 1886. The metal is found in argyrodite (Ag8GeS6); in germanite (Cu26Fe4Ge4S32), which containes 8% of the element; in zinc ores; in coal; and in other minerals. The element is frequently obtained commercially from the dusts of smelters procesing zinc ores, and has been recovered from the by-products of combustion of certain coals. Its presence in coal insures a large reserve of the element in the years to come. Germanium can be separated from other metals by fractional distillation of its volatile tetrachloride. The tetrachloride may then be hydrolyzed to give GeO2; the dioxide can then be reduced to give the metal. Recently developed zone-refining techniques permit the production of germanium of ultra-high purity. The
element is a gray-white metalloid, and in its pure state is crystalline and brittle,
retaining its luster in air at room temperature. It is a very important semiconductor
material. Zone-refining techniques have led to production of crystalline germanium
for semiconductor use with an impurity of only one part in 1010. Doped with arsenic, gallium, or other elements, it is used as a transistor element in thousands of electronic applications. Its applicaion as a semiconductor element now provides the largest use for germanium. Germanium is also finding many other applications including use as an alloying agent, as a phosphor in fluorescent lamps, and as a catalyst. Germanium and germanium oxide are transparent to the infrared and are used in infrared spectroscopes and other optical equipment, including extremely sensitive infrared detectors. Germanium oxide's high index of refraction and dispersion has made it useful as a component of glasses used in wide-angle camera lenses and microscope objectives. The field of organogermanium chemistry is
becoming increasingly important. Certain germanium compounds have a low mammalian toxicity, but a marked activity against certain bacteria, which makes them of interest as chemotherapeutic agents. Twenty-nine isotopes and isomers are known, five of which occur naturally.
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