CAS: 7440-17-7
Description: Soft, silver-white metal
Classification: Alkali Metal
Date of Discovery: 1861
Discoverer: R. Bunsen
Name Origin: Latin rubidus, "deepest red"
Atomic Number: 37
Number of Neutrons: 48
Atomic Mass: 85.4678(3) amu
Melting Point: 39.31 °C
Boiling Point: 688 °C
Density @ 20 °C: 1.532 g/cm3 (solid)
1.475 g/cm3 (liquid, 39 °C)
Atomic volume: 55.9 cm3/mol
Electrical resistivity: 0.0779 10-6/cm Thermal conductivity: 0.582 W/cmK
Enthalpy of atomization: 82.0 kJ/mol
Enthalpy of vaporization: 72.216 kJ/mol
Enthalpy of fusion: 2.192 kJ/mol
Specific heat capacity: 0.363 J/gK
Energy levels: 2-8-18-8-1
Electron configuration: [Kr]5s1 Crystal Structure: Cubic body centered
Atomic radius: 2.98 Å
Covalent radius: 2.16 Å
Oxidation States: +1, +2, +3, +4
Electronegativity, Pauling: 0.82
Electron affinity: 0.48592 eV
First ionization energy: 4.177 eV
2nd ionization energy: 27.28 eV
3rd ionization energy: 40.0 eV
Polarizability: 47.3 10-24cm3
Isotope
Natural Abundance
Atomic Mass
Half-life
Decay Mode
Spin
74Rb
73.9445
65 ms
+
75Rb
74.93857
19 s
+
76Rb
75.93508
39 s
+
1-
77Rb
76.93041
3.8
+
3/2-
78mRb
5.7 m
IT; +; EC
4-
78Rb
77.92814
17.7 m
+; EC
0+
79Rb
78.92400
23 m
+; EC
5/2+
80Rb
79.92252
34 s
+
1+
81mRb
30.5 m
IT; +
9/2+
81Rb
80.91900
4.57 h
+; EC
3/2-
82mRb
6.47 h
+; EC
5-
82Rb
81.91821
1.258 m
+; EC
1+
83Rb
82.91511
86.2
EC
5/2-
84mRb
20.3 m
IT
6-
84Rb
83.914387
32.9 d
+; EC; -
2-
85Rb
72.165(20)
84.911792
Stable
5/2-
86mRb
1.018 m
IT
6-
86Rb
85.911170
18.65 d
-
2-
87Rb
27.835(20)
86.909186
4.88 x 1010
-
3/2-
88Rb
87.911323
17.7 m
-
2-
89Rb
88.91229
15.4 m
-
3/2-
90mRb
4.3 m
-
4-
90Rb
89.91481
2.6 m
-
1-
91Rb
90.91649
58.0 s
-
3/2-
92Rb
91.91968
4.48 s
-
1-
93Rb
92.92195
5.85
-; n
5/2
94Rb
93.92643
2.71 s
-; n
3
95Rb
94.92929
0.377 s
-; n
5/2
96Rb
95.93427
0.199 s
-; n
2+
97Rb
96.93733
0.169 s
-; n
3/2
98Rb
97.94174
0.107 s
-; n
99Rb
98.9453
59 ms
-
100Rb
99.9499
53 ms
-
101Rb
100.9532
0.03 s
-
102Rb
0.09 s
-
Discovered in 1861 by Bunsen and Kirchoff in the mineral lepidolite by use of the spectroscope. The element is much more abundant than was thought several years ago. It is now considered to be the 16th most abundant element in the earth's crust. Rubidium occurs in pollucite, leucite, and zinnwaldite, which contains traces up to 1%, in the form of the oxide. It is found in lepidolite to the extent of about 1.5%, and is recovered commercially from this source. Potassium minerals, such as those found at Searles Lake, California, and potassium chloride recovered from the brines in Michigan also contain the element and are commercial sources. It is also found along with cesium in the extensive deposits of pollucite at Bernic Lake, Manitoba. Rubidium can be liquid at room temperature. It is a soft, silvery-white metallic element of the alkali group and is the second most electropositive and alkaline element. It ignites spontaneously in air and reacts violently in water, setting fire to the liberated hydrogen. As with other alkali metals, it forms amalgams with mercury and it alloys with gold, cesium, sodium, and
potassium. It colors a flame yellowish violet. Rubidium metal can be prepared by
reducing rubidium chloride with calcium, and by a number of other methods. It must
be kept under a dry mineral oil or in a vacuum or inert atmosphere. Thirty-five isotopes of rubidium are known. Naturally occurring rubidium is made of two isotopes, 85Rb and 87Rb. Rubidium-87 is present to the extent of 27.83% in natural rubidium and is a beta emitter with a half-life of 4.9 x 1010 years. Ordinary rubidium is sufficiently radioactive to expose a photographic film in about 30 to 60 days. Rubidium forms four oxides: Rb2O, Rb2O2, Rb2O3, Rb2O4. Because rubidium can be easily ionized, it has been considered for use in "ion engines" for space vehicles; however, cesium is somewhat more efficient for this purpose. It is also proposed for use as a working fluid for vapor turbines and for use in a thermoelectric generator using the magnetohydrodynamic principle where rubidium ions are formed by heat at high temperature and passed through a magnetic field. These conduct electricity and act like an armature of a generator thereby generating an electric current. Rubidium is used as a getter in vacuum tubes and as a photocell component. It has been used in making special glasses. RbAg4I5 is important, as it has the highest room conductivity of any known ionic crystal. At 20 °C its conductivity is about the same as dilute sulfuric acid. This suggests use in thin film batteries and other applications.
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