CAS: 7440-65-5
Description: Silvery metal
Classification: Transition Metal
Date of Discovery: 1794
Discoverer: Johann Gadolin
Name Origin:Ytterby, village in Sweden near Vauxholm
Atomic Number: 39
Number of Neutrons: 50
Atomic Mass: 88.90585(2) amu
Melting Point: 1522 °C
Boiling Point: 3345 °C
Density (25 °C): 4.469 g/cm3 Atomic volume: 19.8 cm3/mol
Electrical resistivity: 0.0166 10-6/cm Thermal conductivity: 0.172 W/cmK
Enthalpy of atomization: 418 kJ/mol (est.)
Enthalpy of vaporization: 363.0 kJ/mol
Enthalpy of fusion: 11.40 kJ/mol
Specific heat capacity: 0.30 J/gK
Energy levels: 2-8-18-9-2
Electron configuration: [Kr]4d15s2 Crystal Structure: Hexagonal
Atomic radius: 2.27 Å
Covalent radius: 1.62 Å
Oxidation States: +3
Electronegativity, Pauling: 1.22
Electron affinity: 0.307 eV
First ionization energy: 6.38 eV
2nd ionization energy: 12.24 eV
3rd ionization energy: 20.52 eV
Polarizability: 22.7 10-24cm3
Isotope
Natural Abundance
Atomic Mass
Half-life
Decay Mode
Spin
78Y
77.9435
+
79Y
78.9374
15 s
+
80Y
79.9320
36 s
+
(4)
81Y
80.9291
1.21 m
+
82Y
81.9268
9.5 s
+
1+
83mY
2.85 m
+; EC
1/2-
83Y
82.92235
7.1 m
+; EC
84mY
4.6 s
+; EC
1+
84Y
83.9203
40 m
+; EC
5-
85mY
4.9 h
+; EC
9/2+
85Y
84.91643
2.6 h
+; EC
1/2-
86mY
48 m
IT; +; EC
86Y
85.91489
14.74 h
+; EC
4-
87mY
13 h
IT; +; EC
9/2+
87Y
86.910880
3.35 d
EC
1/2-
88Y
87.909506
106.6 d
EC; +
4-
89mY
15.7 s
IT
9/2+
89Y
100.
88.905849
Stable
1/2-
90mY
3.24 h
IT; -
7+
90Y
89.907152
2.67 d
-
2-
91mY
49.7 m
IT
9/2+
91Y
90.907301
58.5 d
-
1/2-
92Y
91.90893
3.54 h
-
2-
93mY
0.82 s
IT
9/2+
93Y
92.9056
10.2 h
-
1/2-
94Y
93.91160
18.7 m
-
2-
95Y
94.91279
10.3 m
-
1/2-
96mY
9.6 s
-
(3+)
96Y
95.91588
6.2 s
-
0-
97mY
1.21 s
-
9/2+
97Y
96.91813
3.76 s
-
1/2-
98mY
2.1 s
-
(4-)
98Y
97.92224
0.59 s
-
1+
99Y
98.92463
1.47 s
-
1/2-
100mY
0.94 s
-
3+
100Y
99.9278
0.73 s
-
1+
101Y
100.9303
0.43 s
-
(5/2)
102Y
101.9336
0.36 s
-
Yttria, which is an earth containing yttrium, was discovered by Gadolin in 1794. Ytterby is the site of a quarry which yielded many unusual minerals containing rare earths and other elements. This small town, near Stockholm, bears the honor of giving names to erbium, terbium, and ytterbium as well as yttrium. In 1843 Mosander showed that
yttria could be resolved into the oxides (or earths) of three elements. The name yttria was reserved for the most basic one; the others were named erbia and terbia. Yttrium occurs in nearly all of the rare-earth minerals. Analysis of lunar rock samples obtained during the Apollo missions show a relatively high yttrium content. It is recovered commercially from monazite sand, which contains about 3%, and from bastnasite [(Y,Ce)(CO3)F], which contains about 0.2%. Wohler obtained the impure element in 1828 by reduction of the anhydrous chloride with potassium. The metal is now produced commercially by reduction of the fluoride with calcium metal. It can also be prepared by other techniques. Yttrium has a silver-metallic luster and is relatively stable in air. Turnings of the metal, however, ignite in air if their temperature exceeds 400 °C, and finely divided yttrium is very unstable in air. Yttrium oxide is one of the most important compounds of yttrium and accounts for the largest use. It is widely used in making YVO4 europium, and Y203 europium phosphors to give the red color in color television tubes. Many hundreds of thousands of pounds are now used in this application. Yttrium oxide also is used to produce yttrium-iron-garnets, which are very effective microwave filters. Yttrium iron, aluminum, and gadolinium garnets, with formulas such as Y3Fe5O12 and Y3Al5O12, have interesting magnetic properties. Yttrium iron garnet is also exceptionally efficient as both a transmitter and transducer of acoustic energy. Yttrium aluminum garnet, with a hardness of 8.5, is also finding use as a gemstone (simulated diamond). Small amounts of yttrium (0.1 to 0.2%) can be used to reduce the grain size in chromium, molybdenum, zirconium, and titanium, and to increase strength of aluminum and magnesium alloys. Alloys with other useful properties can be obtained by using yttrium as an additive. The metal can be used as a deoxidizer for vanadium and other nonferrous metals. The metal has a low cross section for nuclear capture. 90Y, one of the isotopes of yttrium, exists in equilibrium with its parent 90Sr, a product of atomic explosions. Yttrium has been considered for use as a nodulizer for producing nodular cast iron, in which the graphite forms compact nodules instead of the usual flakes. Such iron has increased ductility. Yttrium is also finding application in laser systems and as a catalyst for ethylene polymerization. It has also potential use in ceramic and glass formulas, as the oxide has a high melting point and imparts shock resistance and low expansion characteristics to glass. Natural yttrium contains but one isotope, 89Y. Thirty-seven other unstable isotopes and isomers have been characterized.
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