History

(L. Holmia: Stockholm). The special absorption bands of holmium were noticed in 1878 by the Swiss chemists Delafontaine and Soret, who announced the existence of an "Element X." Cleve, of Sweden, later independently discovered the element while working on erbia earth. The element is named after Cleve's native city. Holmia, the yellow oxide, was prepared by Homberg in 1911. Holmium occurs in gadolinite, monazite, and in other rare-earth minerals. It is commercially obtained from monazite, occurring in that mineral to the extent of about 0.05%. It has been isolated by the reduction of its anhydrous chloride or fluoride with calcium metal.[1]

Properties

General
Name : holmium
Symbol : Ho
Atomic Number : 67
Chemical Series : Lanthanide
Block, Period : -, 6
Appearance : silvery white
Atomic Properties
Atomic Weight (amu) : 164.9303
Covalent Radius (pm) : 158
Physical Properties
Matter : solid (paramagnetic)
Density (kg/m^3) : 8800
Hardness : n/a
Melting Point (K) : 1743
Boiling Point (K) : 2968
Evaporation Heat (kJ/mol) : 241
Fusion Heat (kJ/mol) : 11.76
Specific Heat (J/(kg*K) ) : 160
Miscellaneous
Electrical Conductivity (MS/m) : 1.24
Thermal Conductivity (W/(m*K) ) : 16.2

Pure holmium has a metallic to bright silver luster. It is relatively soft and malleable, and is stable in dry air at room temperature, but rapidly oxidizes in moist air and at elevated temperatures. The metal has unusual magnetic properties. Few uses have yet been found for the element. The element, as with other rare earths, seems to have a low acute toxic rating.[1]

Notes

[1] From Los Alamos National Laboratory's Chemistry Division Website

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