32
Ge
Germanium
Atomic Mass 72.630
Electron Configuration [Ar]4s23d104p2
Oxidation States +4, +2
Year Discovered 1886

Identifiers

Element Name Germanium
Element Symbol Ge
InChI InChI=1S/Ge
InChIKey GNPVGFCGXDBREM-UHFFFAOYSA-N

Properties

Atomic Weight

72.630(8)

72.630

72.64

72.630(8)

Electron Configuration

[Ar]4s23d104p2

Atomic Radius

Van der Waals Atomic Radius : 211 pm (Van der Waals)

Empirical Atomic Radius : 125pm (Empirical)

Covalent Atomic Radius : 120(4) pm (Covalent)

Oxidation States

+4, +2

4, 3, 2, 1, 0, -1, -2, -3, -4 ​(an amphoteric oxide)

Ground Level

3P0

Ionization Energy

7.900 eV

7.899435 ± 0.000012 eV

Electronegativity

Pauling Scale Electronegativity : 2.01(Pauling Scale)

Allen Scale Electronegativity : 1.994(Allen Scale)

Electron Affinity

1.35eV

1.44eV

Atomic Spectra

Lines Holdings

Levels Holdings

Physical Description

Solid

Element Classification

Semi-metal

Element Period Number

4

Element Group Number

14

Density

5.323 grams per cubic centimeter

Melting Point

1211.40 K (938.25°C or 1720.85°F)

938.25°C

Boiling Point

3106 K (2833°C or 5131°F)

2833°C

Estimated Crustal Abundance

1.5 milligrams per kilogram

Estimated Oceanic Abundance

5×10-5 milligrams per liter

History

The name derives from the Latin germania for Germany. It was discovered and isolated by the German chemist Clemens-Alexander Winkler in 1886 in the mineral argyrodite (GeS2×4Ag2S).

First proposed to exist by Dmitri Mendeleyev in 1871 based on gaps in his newly created Periodic Table of Elements, germanium was discovered by the German chemist Clemens Winkler in the mineral argyrodite (Ag8GeS6) in 1886. Today, germanium is primarily obtained from the smelting of zinc ores and from the byproducts of burning certain types of coal.

From the Latin word Germania, Germany. Mendeleev predicted the existence of Germanium in 1871 as ekasilicon, and the element was discovered by Winkler in 1886.

Historical Atomic Weights

Year Atomic Weight (uncertainty) [u] Reference
2011 72.630(8) https://doi.org/10.1351/PAC-REP-13-03-02
2009 72.63(1) https://doi.org/10.1351/PAC-REP-10-09-14
1999 72.64(1) https://doi.org/10.1351/pac200173040667
1985 72.61(2) https://doi.org/10.1351/pac198658121677
1969 72.59(3) https://doi.org/10.1351/pac197021010091
1961 72.59 https://doi.org/10.1021/ja00881a001
1925 72.60 https://doi.org/10.1039/CT9252700913
1903 72.5 https://doi.org/10.1021/ja02003a001
1902 72 https://doi.org/10.1007/BF01370337

Historical Isotopic Abundances

Year Isotope Abundance (uncertainty) Reference
2013 70Ge 0.2052(19) https://doi.org/10.1515/pac-2015-0503
2013 72Ge 0.2745(15) https://doi.org/10.1515/pac-2015-0503
2013 73Ge 0.0776(8) https://doi.org/10.1515/pac-2015-0503
2013 74Ge 0.3652(12) https://doi.org/10.1515/pac-2015-0503
2013 76Ge 0.0775(12) https://doi.org/10.1515/pac-2015-0503
2009 70Ge 0.2057(27) https://doi.org/10.1351/PAC-REP-10-06-02
2009 72Ge 0.2745(32) https://doi.org/10.1351/PAC-REP-10-06-02
2009 73Ge 0.0775(12) https://doi.org/10.1351/PAC-REP-10-06-02
2009 74Ge 0.3650(20) https://doi.org/10.1351/PAC-REP-10-06-02
2009 76Ge 0.077 30(43) https://doi.org/10.1351/PAC-REP-10-06-02
2001 70Ge 0.2038(18) https://doi.org/10.1063/1.1836764
2001 72Ge 0.2731(26) https://doi.org/10.1063/1.1836764
2001 73Ge 0.0776(8) https://doi.org/10.1063/1.1836764
2001 74Ge 0.3672(15) https://doi.org/10.1063/1.1836764
2001 76Ge 0.0783(7) https://doi.org/10.1063/1.1836764
1997 70Ge 0.2084(87) https://doi.org/10.1351/pac199870010217
1997 72Ge 0.2754(34) https://doi.org/10.1351/pac199870010217
1997 73Ge 0.0773(5) https://doi.org/10.1351/pac199870010217
1997 74Ge 0.3628(73) https://doi.org/10.1351/pac199870010217
1997 76Ge 0.0761(38) https://doi.org/10.1351/pac199870010217
1989 70Ge 0.2123(4) https://doi.org/10.1351/pac199163070991
1989 72Ge 0.2766(3) https://doi.org/10.1351/pac199163070991
1989 73Ge 0.0773(1) https://doi.org/10.1351/pac199163070991
1989 74Ge 0.3594(2) https://doi.org/10.1351/pac199163070991
1989 76Ge 0.0744(2) https://doi.org/10.1351/pac199163070991
1975 70Ge 0.205 https://doi.org/10.1351/pac197647010075
1975 72Ge 0.274 https://doi.org/10.1351/pac197647010075
1975 73Ge 0.078 https://doi.org/10.1351/pac197647010075
1975 74Ge 0.365 https://doi.org/10.1351/pac197647010075
1975 76Ge 0.078 https://doi.org/10.1351/pac197647010075

Description

The element is a gray-white metalloid. In pure state, the element is crystalline and brittle, retaining its luster in air at room temperature. It is a very important semiconductor. Zone-refining techniques have led to production of crystalline germanium for semiconductor use with an impurity of only one part in 1010.

Users

The largest use of germanium is in the semiconductor industry. When doped with small amounts of arsenic, gallium, indium, antimony or phosphorus, germanium is used to make transistors for use in electronic devices. Germanium is also used to create alloys and as a phosphor in fluorescent lamps. Both germanium and germanium oxide (GeO) are transparent to infrared radiation and are used in infrared optical instruments and infrared detectors. Some germanium compounds seem to be effective in killing some types of bacteria and are currently being studied for use in chemotherapy.

When germanium is doped with arsenic, gallium, or other elements, it is used as a transistor element in thousands of electronic applications. The most common use of germanium is as a semiconductor. 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.

The high index of refraction and dispersion properties of its oxide's have made germanium useful as a component of wide-angle camera lenses and microscope objectives.

The field of organo-germanium chemistry is becoming increasingly important. Certain germanium compounds have a low mammalian toxicity, but a marked activity against certain bacteria, which makes them useful as chemotherapeutic agents.

Sources

The metal is found in

▸ argyrodite, a sulfide of germanium and silver;

▸ germanite, which contains 8 percent of the element;

▸ zinc ores;

▸ coal; and

▸ other minerals

The element is commercially obtained from the dust from smelters that process zinc ores. It is also recovered from combustion by-products of certain coals.

Germanium can be separated from other metals by fractional distillation of its volatile tetrachloride. These techniques permit the production of germanium of ultra-high purity.

Compounds

See more information at the Germanium compound page.

Element Forms

CID Name Formula SMILES Molecular Weight
6326954 germanium Ge [Ge] 72.63
73608878 germanium(4+) Ge+4 [Ge+4] 72.63
6337084 germanium-68 Ge [68Ge] 67.92810
6337566 germanium-69 Ge [69Ge] 68.92796
6337568 germanium-73 Ge [73Ge] 72.9234590
6337045 germanium-71 Ge [71Ge] 70.924952
6337052 germanium-75 Ge [75Ge] 74.9228584
6337053 germanium-77 Ge [77Ge] 76.9235498
6337083 germanium-67 Ge [67Ge] 66.93272
6337085 germanium-78 Ge [78Ge] 77.92285
6337086 germanium-66 Ge [66Ge] 65.93386
6337569 germanium-74 Ge [74Ge] 73.9211778
44152739 germanium-72 Ge [72Ge] 71.9220758
131708370 germanium-70 Ge [70Ge] 69.924249
131708371 germanium-76 Ge [76Ge] 75.9214027

Isotopes

Stable Isotope Count 5

Isotopes in Earth/Planetary Science

Because molecules, atoms, and ions of the stable isotopes of germanium possess slightly different physical and chemical properties, they commonly will be fractionated during physical, chemical, and biological processes, giving rise to variations in isotopic abundances and in atomic weights. There are measureable variations in the isotopic abundances of germanium in terrestrial materials (Fig. IUPAC.32.1).

Fig. IUPAC.32.1: Variation in the isotope-amount ratio n(⁷⁴Ge)/n(⁷⁰Ge) of selected geranium-bearing rocks and marine precipitates (modified from [266]), assuming a measured n(⁷⁴Ge)/n(⁷⁰Ge) isotope-amount ratio of 1.7794 [267].

[266] O. Rouxel, A. Galy, H. Elderfield. Geochim. Cosmochim. Acta70, 3387 (2006).
[267] L. Yang, J. Meija. Anal. Chem.82, 4188 (2010).

Isotopes in Medicine

68Ge is used to calibrate positron emission tomography (PET) scanners, which have been used for medical diagnostic procedures [268].

[268] Office of Science, Los Alamos National Laboratory. Isotope Production and Applications, Los Alamos National Laboratory (2017), Feb. 26; http://www.lanl.gov/science-innovation/science-programs/office-of-science-programs/nuclear-physics/isotopes/_assets/docs/isotope-program-brochure.pdf.

Isotopes Used as a Source of Radioactive Isotope(s)

72Ge and 74Ge are used to produce the radioactive isotopes 72As and 74As, with half-lives of 26 h and 17.8 days, respectively. The arsenic nuclei can attach to tumors and the decay of these isotopes is used to image the location of cancerous tumors in vivovia the 72Ge (n, p) 72As reaction and the 74Ge (n, p) 74As reaction [269]. 70Ge, 72Ge, and 74Ge have all been used to produce the medical radioisotope 73Se via the 70Ge (4He, n) 73Se reaction, via the 72Ge (4He, 3n) 73Se reaction and via the reaction 74Ge (4He, 5n) 73Se, respectively [269].

[269] M. Jennewein, M. A. Lewis, D. Zhao, E. Tsyganov, N. Slavine, J. He, L. Watkins, V. D. Kodibagkar, S. O’Kelly, P. Kulkarni, P. P. Antich, A. Hermanne, F. Rösch, R. P. Mason, P. E. Thorpe. Clin. Cancer Res.14, 1377 (2008).

Isotope Mass and Abundance

Isotope Atomic Mass (uncertainty) [u] Abundance (uncertainty)
70Ge 69.924 249(6) 0.2052(19)
72Ge 71.922 0758(5) 0.2745(15)
73Ge 72.923 4590(4) 0.0776(8)
74Ge 73.921 177 76(8) 0.3652(12)
76Ge 75.921 4027(1) 0.0775(12)
Isotope Atomic Mass (uncertainty) [u] Abundance (uncertainty)
70Ge 69.92424875(90) 0.2057(27)
72Ge 71.922075826(81) 0.2745(32)
73Ge 72.923458956(61) 0.0775(12)
74Ge 73.921177761(13) 0.3650(20)
76Ge 75.921402726(19) 0.0773(12)

Atomic Mass, Half Life, and Decay

Nuclide Atomic Mass and Uncertainty [u] Half Life and Uncertainty Discovery Year Decay Modes, Intensities and Uncertainties [%]
58Ge 57.991863 ± 0.000537 [Estimated] Not-specified 2p ?
59Ge 58.982426 ± 0.000429 [Estimated] 13.3 ms ± 1.7 2015 β+≈100%; β+p=93±0.7%; 2p<0.2%
60Ge 59.970445 ± 0.000322 [Estimated] 21 ms ± 6 2005 β+=100%; β+p≈100%; β+2p<14%
61Ge 60.963725 ± 0.000322 [Estimated] 40.7 ms ± 0.4 1987 β+=100%; β+p=87±0.3%
62Ge 61.954761 ± 0.00015 [Estimated] 82.5 ms ± 1.4 1991 β+=100%; β+p ?
63Ge 62.949628000 ± 0.00004 153.6 ms ± 1.1 1991 β+=100%; β+p ?
64Ge 63.941689912 ± 0.000004 63.7 s ± 2.5 1972 β+=100%
65Ge 64.939368136 ± 0.000002323 30.9 s ± 0.5 1972 β+=100%; β+p=0.011±0.3%
66Ge 65.933862124 ± 0.000002577 2.26 h ± 0.05 1950 β+=100%
67Ge 66.932716999 ± 0.000004636 18.9 m ± 0.3 1950 β+=100%
67Gem 66.932716999 ± 0.000004636 13.7 us ± 0.9 1978 IT=100%
67Gen 66.932716999 ± 0.000004636 109.1 ns ± 3.8 1973 IT=100%
68Ge 67.928095305 ± 0.000002014 271.05 d ± 0.08 1948 ε=100%
69Ge 68.927964467 ± 0.000001414 39.05 h ± 0.10 1938 β+=100%
69Gem 68.927964467 ± 0.000001414 5.1 us ± 0.2 1978 IT=100%
69Gen 68.927964467 ± 0.000001414 2.81 us ± 0.05 1978 IT=100%
70Ge 69.924248542 ± 0.00000088 Stable 1923 IS=20.52±1.9%
71Ge 70.924952120 ± 0.000000874 11.43 d ± 0.03 1941 ε=100%
71Gem 70.924952120 ± 0.000000874 20.41 ms ± 0.18 1959 IT=100%
72Ge 71.922075824 ± 0.000000081 Stable 1923 IS=27.45±1.5%
72Gem 71.922075824 ± 0.000000081 444.2 ns ± 0.8 1984 IT=100%
73Ge 72.923458954 ± 0.000000061 Stable 1933 IS=7.76±0.8%
73Gem 72.923458954 ± 0.000000061 2.91 us ± 0.03 1975 IT=100%
73Gen 72.923458954 ± 0.000000061 499 ms ± 11 1957 IT=100%
74Ge 73.921177760 ± 0.000000013 Stable 1923 IS=36.52±1.2%
75Ge 74.922858370 ± 0.000000055 82.78 m ± 0.04 1939 β-=100%
75Gem 74.922858370 ± 0.000000055 47.7 s ± 0.5 1952 IT≈100%; β-=0.030±0.6%
75Gen 74.922858370 ± 0.000000055 216 ns ± 5 1982 IT=100%
76Ge 75.921402725 ± 0.000000019 1.88 Zy ± 0.08 1933 IS=7.75±1.2%; 2β-=100%
77Ge 76.923549843 ± 0.000000056 11.211 h ± 0.003 1939 β-=100%
77Gem 76.923549843 ± 0.000000056 53.7 s ± 0.6 1947 β-=81±0.2%; IT=19±0.2%
78Ge 77.922852911 ± 0.000003795 88.0 m ± 1.0 1953 β-=100%
79Ge 78.925359506 ± 0.000039893 18.98 s ± 0.03 1970 β-=100%
79Gem 78.925359506 ± 0.000039893 39.0 s ± 1.0 1970 β-=96±0.1%; IT=4±0.1%
80Ge 79.925350773 ± 0.000002205 29.5 s ± 0.4 1972 β-=100%
81Ge 80.928832941 ± 0.000002205 9 s ± 2 1972 β-=100%
81Gem 80.928832941 ± 0.000002205 6 s ± 2 1981 β-≈100%; IT<1%
82Ge 81.929774031 ± 0.000002405 4.31 s ± 0.19 1972 β-=100%
83Ge 82.934539100 ± 0.000002604 1.85 s ± 0.06 1972 β-=100%; β-n ?
84Ge 83.937575090 ± 0.000003403 951 ms ± 9 1972 β-=100%; β-n=10.6±0.6%
85Ge 84.942969658 ± 0.000004003 495 ms ± 5 1991 β-=100%; β-n=17.2±1.8%; β-2n ?
86Ge 85.946967000 ± 0.00047 221.6 ms ± 11 1994 β-=100%; β-n=45±1.5%
87Ge 86.953204 ± 0.000322 [Estimated] 103 ms ± 4 1997 β-=100%; β-n ?; β-2n ?
88Ge 87.957574 ± 0.000429 [Estimated] 61 ms ± 6 1997 β-=100%; β-n ?; β-2n ?
89Ge 88.964530 ± 0.000429 [Estimated] 60 ms >300ns [Estimated] 1997 β- ?; β-n ?; β-2n ?
90Ge 89.969436 ± 0.000537 [Estimated] 30 ms >400ns [Estimated] 2010 β- ?; β-n ?; β-2n ?

Information Sources

  1. 1.  PubChem
  2. 2.  Atomic Mass Data Center (AMDC), International Atomic Energy Agency (IAEA)
  3. 3.  IUPAC Commission on Isotopic Abundances and Atomic Weights (CIAAW)
  4. 4.  Jefferson Lab, U.S. Department of Energy
    LICENSE
    Please see citation and linking information https https://www.jlab.org/privacy-and-security-notice
  5. 5.  Los Alamos National Laboratory, U.S. Department of Energy
  6. 6.  NIST Physical Measurement Laboratory
  7. 7.  IUPAC Periodic Table of the Elements and Isotopes (IPTEI)
    LICENSE
    Copyright (c) 2020 International Union of Pure and Applied Chemistry. The International Union of Pure and Applied Chemistry (IUPAC) contribution within Pubchem is provided under a CC-BY-NC-ND 4.0 license, unless otherwise stated.
    https://creativecommons.org/licenses/by-nc-nd/4.0/
  8. 8.  PubChem Elements
    Germanium

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