Abstract
A spectrometric study has been made over the range from 400 to 1500 nm on powdered specimens of saprolitic, nickel-bearing ore minerals from New Caledonia; analysis of the absorption spectra enables a distinction to be made between features due to Fe3+ and those due to Ni2+. Measurement of diffuse reflectance in the visible range makes it possible to estimate (to about 2% relative) the amount of nickel in the saprolites. The simplicity of the method and the fact that it is applied to powdered material enable these spectral characteristics of nickel to be used in prospecting for nickel or in the estimation of resources, eventually by remote-sensing.
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Maquet, M., Cervelle, B.D. & Gouet, G. Signatures of Ni2+ and Fe3+ in the optical spectra of limonitic ore from new caledonia: Application to the determination of the nickel content. Mineral. Deposita 16, 357–373 (1981). https://doi.org/10.1007/BF01798963
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DOI: https://doi.org/10.1007/BF01798963