CAS: 7440-52-0
Description: Grayish-silver metal
Classification: Rare Earth (Lanthanide)
Date of Discovery: 1843
Discoverer: Carl Mosander
Name Origin:Ytterby, a town in Sweden
Atomic Number: 68
Number of Neutrons: 99
Atomic Mass: 167.26(3) amu
Melting Point: 1529 °C
Boiling Point: 2868 °C
Density (25 °C): 9.066 g/cm3 Atomic volume: 18.4 cm3/mol
Electrical resistivity: 0.0117 10-6/cm Thermal conductivity: 0.143 W/cmK
Enthalpy of atomization: 314 kJ/mol (est.)
Enthalpy of vaporization: 261.0 kJ/mol
Enthalpy of fusion: 19.90 kJ/mol
Specific heat capacity: 0.17 J/gK
Energy levels: 2-8-18-30-8-2
Electron configuration: [Xe]4f 126s2 Crystal Structure: Hexagonal
Atomic radius: 2.45 Å
Covalent radius: 1.57 Å
Oxidation States: +3
Electronegativity, Pauling: 1.24
Electron affinity: First ionization energy: 6.101 eV
2nd ionization energy: 11.929 eV
3rd ionization energy: 22.739 eV
Polarizability: 22.7 10-24cm3
Isotope
Natural Abundance
Atomic Mass
Half-life
Decay Mode
Spin
147Er
146.9494
2.5 s
EC, +
148Er
147.9444
4.5 s
+, EC
149mEr
10 s
IT
11/2-
149Er
148.9425
10.7 s
EC, +
1/2+
150Er
149.9370
18 s
+; EC
0+
151Er
150.9373
23 s
+, EC
7/2-
152Er
151.93500
10.2 s
+;
0+
153Er
152.93509
37.1 s
; +, EC
154Er
153.93278
3.7 m
+, EC;
0+
155Er
154.93321
5.3 m
+, EC; EC
(7/2-)
156Er
155.9308
20 m
+, EC
0+
157Er
156.9319
25 m
+, EC
3/2-
158Er
157.93087
2.2 h
EC; +
0+
159Er
158.930681
36 m
+; EC
3/2-
160Er
159.92908
1.191 d
EC
0+
161Er
160.9300
3.21 h
EC
3/2-
162Er
0.14(1)
161.928775
Stable
0+
163Er
162.93003
1.25 h
EC
5/2-
164Er
1.61(2)
163.929197
Stable
0+
165Er
164.930723
10.36 h
EC
5/2-
166Er
33.6(2)
165.930290
Stable
0+
167mEr
2.27 s
-
1/2-
167Er
22.95(15)
166.932046
Stable
7/2+
168Er
26.8(2)
167.932368
Stable
0+
169Er
168.934588
9.40 d
-
1/2-
170Er
14.9(2)
169.935461
Stable
0+
171Er
170.938026
7.52 h
-
5/2-
172Er
171.939352
2.05 d
-
173Er
172.9424
1.4 m
-
(7/2-)
174Er
173.9441
3.1 m
-
Erbium one of the so-called rare-earth elements of the lanthanide series, is found in the minerals mentioned under dysprosium above. in 1842 Mosander separated "yttria," found
in the mineral gadolinite, into three fractions which he called yttria, erbia, and terbia. The names erbia and terbia became confused in this early period. After 1860, Mosander's terbia was known as erbia, and after 1877, the earlier known erbia became terbia. The erbia of this period was later shown to consist of five oxides, now known as erbia, scandia, holmia, thulia and ytterbia. By 1905 Urbain and James independently succeeded in isolating fairly pure Er2O3. Klemm and Bommer first produced reasonably pure erbium metal in 1934 by reducing the anhydrous chloride with potassium vapor. The pure metal is soft and malleable and has a bright, silvery, metallic luster. As with other rare-earth metals, its properties depend to a certain extent on the impurities present. The metal is fairly stable in air and does not oxidize as rapidly as some of the other rare-earth metals. Naturally occurring erbium is a mixture of six isotopes, all of which are stable. Twenty-four radioactive isotopes of erbium are also recognized. Recent production techniques, using ion-exchange reactions, have resulted in much lower prices of the rare-earth metals and their compounds in recent years. Erbium is finding nuclear and metallurgical uses. Added to vanadium, for example, erbium lowers the hardness and improves workability. Most of the rare-earth oxides have sharp absorption bands in the visible, ultraviolet, and near infrared. This property, associated with the electronic structure, serves beautiful pastel colors to many of the rare-earth salts. Erbium oxide gives a pink color and has been used as a colorant in glasses and porcelain enamel glazes.
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