CAS: 7429-91-6
Description: Soft, metallic, with a bright silver luster
Classification: Rare Earth (Lanthanide)
Date of Discovery: 1886
Discoverer: Paul Emile Lecoq de Boisbaudran
Name Origin: Greek word dysprositos "hard to get at"
Atomic Number: 66
Number of Neutrons: 97
Atomic Mass: 162.50(3) amu
Melting Point: 1412 °C
Boiling Point: 2567 °C
Density (25 °C): 8.551 g/cm3 Atomic volume: 19.0 cm3/mol
Electrical resistivity: 0.0108 10-6/cm Thermal conductivity: 0.107 W/cm/K
Enthalpy of atomization: 301 kJ/mol (est.)
Enthalpy of vaporization: 230.0 kJ/mol
Enthalpy of fusion: 11.05 kJ/mol
Specific heat capacity: 0.17 J/gK
Energy levels: 2-8-18-28-8-2
Electron configuration: [Xe]4f 106s2 Crystal Structure: Hexagonal
Atomic radius: 2.49 Å
Covalent radius: 1.59 Å
Oxidation States: +3
Electronegativity, Pauling: 1.23
Electron affinity: First ionization energy: 5.94 eV
2nd ionization energy: 11.67 eV
3rd ionization energy: 22.802 eV
Polarizability: 24.5 10-24cm3
Isotope
Natural Abundance
Atomic Mass
Half-life
Decay Mode
Spin
141Dy
140.951
0.9 s
EC, +
142Dy
141.946
2.3 s
EC, +
143Dy
142.9440
3.9 s
EC, +
144Dy
143.9391
9.1 s
EC, +
145Dy
144.9365
14 s
EC, +
11/2-
146mDy
0.15 s
IT
10+
146Dy
145.9325
30 s
EC, +
147mDy
56 s
IT; +, EC
(11/2-)
147Dy
146.9309
75 s
EC, +
1/2+
148Dy
147.92710
3.1 m
+; EC
0+
149Dy
148.92734
4.2 m
+, EC
(7/2-)
150Dy
149.92558
7.18 m
-;
0+
151Dy
150.926181
17 m
+; EC;
7/2-
152Dy
151.92472
2.37 h
EC;
0+
153Dy
152.925763
6.3 h
+; EC;
(7/2-)
154Dy
153.92442
3 x 106 y
0+
155Dy
154.92575
9.9 h
+; EC
3/2-
156Dy
0.06(1)
155.92428
Stable
0+
157Dy
156.92546
8.1 h
EC
3/2-
158Dy
0.10(1)
157.924405
Stable
0+
159Dy
158.925736
144 d
EC
3/2-
160Dy
2.34(6)
159.925194
Stable
0+
161Dy
18.9(2)
160.926930
Stable
5/2+
162Dy
25.5(2)
161.926795
Stable
0+
163Dy
24.9(2)
162.928728
Stable
5/2-
164Dy
28.2(2)
163.929171
Stable
0+
165mDy
1.26 m
IT; -
1/2-
165Dy
164.931700
2.33 h
-
7/2+
166Dy
165.932803
3.400 d
-
0+
167Dy
166.9357
6.2 m
-
(1/2-)
168Dy
167.9372
8.5 m
-
0+
169Dy
168.9403
39 s
-
Dysprosium was discovered in 1886 by Lecoq de Boisbaudran, but not isolated. Neither the oxide nor the metal was available in relatively pure form until the development of ion-exchange separation and metallographic reduction techniques by Spedding and associates about 1950. Dysprosium occurs along with other so-called rare-earth or lanthanide elements in a variety of minerals such as xenotime, fergusonite, gadolinite, euxenite, polycrase, and blomstrandine (aeschynite). The most important sources, however, are from monazite and bastnasite. Dysprosium can be prepared by reduction of the trifluoride with calcium. The element has a metallic, bright silver luster. It is relatively stable in air at room temperature, and is readily attacked and dissolved, with the evolution of hydrogen, by dilute and concentrated mineral acids. The metal is soft enough to be cut with a knife and can be machined without sparking if overheating is avoided. Small amounts of impurities can greatly affect its physical properties. While dysprosium has not yet found many applications, its thermal neutron absorption cross-section and high melting point suggest metallurgical uses in nuclear control applications and for alloying with special stainless steels. A dysprosium oxide-nickel cermet has found use in cooling nuclear reactor rods. This cermet absorbs neutrons readily without swelling or contracting under prolonged neutron bombardment. In combination with vanadium and other rare earths, dysprosium has been used in making laser materials. Dysprosium-cadmium chalcogenides, as sources of infrared radiation, have been used for studying chemical reactions. The cost of dysprosium metal has dropped in recent years since the development of ion-exchange and solvent extraction techniques, and the discovery of large ore bodies. Thirty-two isotopes and isomers are now known.
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