CAS: 7440-64-4
Description: Soft, silvery metal
Classification: Rare Earth (Lanthanide)
Date of Discovery: 1878
Discoverer: Jena de Marignac
Name Origin:Ytterby, a village in Sweden
Atomic Number: 70
Number of Neutrons: 103
Atomic Mass: 173.04(3) amu
Melting Point: 819 °C
Boiling Point: 1196 °C
Density (293 K): - 6.903 g/cm3 - 6.966 g/cm3 Atomic volume: 24.79 cm3/mol
Electrical resistivity: 0.0351 10-6/cm Thermal conductivity: 0.349 W/cmK
Enthalpy of atomization: 180 kJ/mol (est.)
Enthalpy of vaporization: 128.90 kJ/mol
Enthalpy of fusion: 7.660 kJ/mol
Specific heat capacity: 0.15 J/gK
Energy levels: 2-8-18-32-8-2
Electron configuration: [Xe]4f 146s2 Crystal Structure: Cubic face centered
Atomic radius: 2.40 Å
Covalent radius: 1.74 Å
Oxidation States: +2, +3
Electronegativity, Pauling: 1.27
Electron affinity: First ionization energy: 6.254 eV
2nd ionization energy: 12.188 eV
3rd ionization energy: 25.03 eV
Polarizability: 21.0 10-24cm3
Isotope
Natural Abundance
Atomic Mass
Half-life
Decay Mode
Spin
151Yb
150.9545
1.6 s
+
152Yb
151.9502
3.2 s
+, EC
153Yb
152.9492
4 s
+, EC
154Yb
153.9455
0.40 s
+, EC;
155Yb
154.9456
1.7 s
+, EC;
156Yb
155.94277
26 s
+, EC;
0+
157Yb
156.9427
39 s
+, EC;
158Yb
157.93986
1.5 m
+, EC
0+
159Yb
158.9402
1.4 m
EC, +
160Yb
159.9376
4.8 m
+, EC
0+
161Yb
160.9375
4.2 m
+, EC
3/2-
162Yb
161.9358
18.9 m
+, EC
0+
163Yb
162.9363
11.1 m
+
3/2-
164Yb
163.9345
1.26 h
EC
0+
165Yb
164.93540
9.9 m
+; EC
(5/2-)
166Yb
165.93388
2.363 d
EC
0+
167Yb
166.934947
17.5 m
+; EC
5/2-
168Yb
0.13(1)
167.933895
Stable
0+
169mYb
46 s
IT
1/2-
169Yb
168.935187
32.03 d
EC
7/2+
170Yb
3.05(6)
169.934759
Stable
0+
171Yb
14.3(2)
170.936323
Stable
1/2-
172Yb
21.9(3)
171.936378
Stable
0+
173Yb
16.12(21)
172.938207
Stable
5/2-
174Yb
31.8(4)
173.938858
Stable
0+
175Yb
174.941273
4.19 d
-
7/2-
176mYb
11.4 s
IT
(8-)
176Yb
12.7(2)
175.942569
Stable
0+
177mYb
6.41 s
IT
1/2-
177Yb
176.945257
1.9 h
-
9/2+
178Yb
177.94664
1.23 h
-
0+
179Yb
178.9499
8 m
-
180Yb
2 m
-
Marignac in 1878 discovered a new component, which he called ytterbia, in the earth then known as erbia. In 1907, Urbain separated ytterbia into two components, which he called neoytterbia and lutecia. The elements in these
earths are now known as ytterbium and lutetium, respectively. These elements are identical with aldebaranium and cassiopeium, discovered independently and at about the same time by von Welsbach. Ytterbium occurs along with other rare earths in a number of rare minerals. It is commercially recovered principally from monazite sand, which contains about 0.03%. Ion-exchange and solvent extraction techniques developed in recent years have greatly simplified the separation of the rare earths from one another. The element was first prepared by Klemm and Bonner in 1937 by reducing ytterbium trichloride with potassium. Their metal was mixed, however, with KCl. Daane, Dennison, and Spedding prepared a much purer form in 1953 from which the chemical and physical properties of the element could be determined. Ytterbium has a bright silvery luster, is soft, malleable, and quite ductile. While the element is fairly stable, it should be kept in closed containers to protect it from air and moisture. Ytterbium is readily attacked and dissolved by dilute and concentrated mineral acids and reacts slowly with water.
Ytterbium has three allotropic forms with transformation points at -13 °C and 795 °C. The beta form is a room-temperature, face-centered, cubic modification, while the high-temperature gamma form is a body-centered cubic form. Another body-centered cubic phase has recently been found to be stable at high pressures at room temperatures. The beta form ordinarily has metallic-type conductivity, but becomes a semiconductor when the pressure is increased above 16,000 atm. The electrical resistance increases tenfold as the pressure is increased to 39,000 atm and drops to about 80% of its standard
temperature-pressure resistivity at a pressure of 40,000 atm. Natural ytterbium is a mixture of seven stable isotopes. Twenty-six other unstable isotopes and isomers are known. Ytterbium metal has possible use in improving the grain refinement, strength, and other mechanical properties of stainless steel. One isotope is reported to have been used as a radiation source as a substitute for a portable X-ray machine where electricity is
unavailable. Few other uses have been found. Ytterbium has a low acute toxic rating, but may present a carcinogenic hazard.
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