Nb; at. wt 92.90638; at. no. 41; valence 2, 3, 4, 5; usually pentavalent. Group VB (5). One naturally occurring isotope: 93Nb; artificial, radioactive isotopes: 88-92; 94-101. Approximately as abundant as nickel. Occurs in nature together with tantalum in the minerals columbite [(Fe,Mn)(Nb,Ta)2O6], pyrochlore (NaCaNb2O6F) and tantalite [(Fe,Mn)(Ta,Nb)2O6]. Discovered by Hatchett in 1801, isolated by Blomstrand in 1866, named after Niobe, daughter of Tantalos. Extracted from columbite which is mined largely in Nigeria and Zaire. Less than 10% of niobium-bearing ores come from the US, Canada, and Norway. Reviews of niobium and its compds: Technology of Columbium (Niobium) B. W. Gonser, E. M. Sherwood, Eds. (Wiley, New York, 1958); G. L. Miller, Tantalum and Niobium (Academic Press, New York, 1959) 767 pp; Brown, “The Chemistry of Niobium and Tantalum” in Comprehensive Inorganic Chemistry Vol. 3, J. C. Bailar, Jr. et al., Eds. (Pergamon Press, Oxford, 1973) pp 553-622; P. H. Payton in Kirk-Othmer Encyclopedia of Chemical Technology vol. 15 (Wiley-Interscience, New York, 3rd ed., 1981) pp 820-840.