Abstract

Roselite from the Aghbar Mine, Morocco, [Ca2(Co2+,Mg)(AsO4)2 2H2O], was investigated by X-ray Photoelectron and Raman spectroscopy. X-ray Photoelectron Spectroscopy revealed a cobalt to magnesium ratio of 3:1. Magnesium, cobalt and calcium showed single bands associated with unique crystallographic positions. The oxygen 1s spectrum displayed two bands associated with the arsenate group and crystal water. Arsenic 3d exhibited bands with a ratio close to that of the cobalt to magnesium ratio, indicative of the local arsenic environment being sensitive to the substitution of magnesium for cobalt. The Raman arsenate symmetric and antisymmetric modes were all split with the antisymmetric modes observed around 865 and 818 cm−1, while the symmetric modes were found around 980 and 709 cm−1. An overlapping water-libration mode was observed at 709 cm−1. The region at 400–500 cm−1 showed splitting of the arsenate antisymmetric mode with bands at 499, 475, 450 and 425 cm−1. The 300–400 cm−1 region showed the corresponding symmetric bending modes at 377, 353, 336 and 304 cm−1. The bands below 300 cm−1 were assigned to lattice modes.

Highlights

  • Asan part of an ongoing study arsenate minerals this study aims to better understand the

  • X-ray photoelectron on arsenate minerals [16,17,18,19,20,21,22,23,24,25] this study aims to better understand the X-ray photoelectron spectroscopy (XPS)

  • XPS normally probes to a depth of 10 nm and involves the detection of photoelectrons emitted from a sample as a result of irradiation of the sample by single-energy X-ray photons, mostly Al Kα as in this study

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Summary

Introduction

Roselite is a rare secondary arsenate mineral in cobalt-bearing hydrothermal mineral deposits forming a solid solution with wendwilsonite with Mg substituting for Co2+. Since both minerals are very similar in appearance, it is almost impossible to distinguish between the two minerals without proper chemical analysis. Roselite is often associated with related arsenates such as wendwilsonite, talmessite and erythrite, as can be observed at Bou Azzer, Morocco [2,3,4,5]. Minerals of the roselite group can by characterized by the general formula X2 M(TO4 )2 .2H2 O with X = Ca, Na; M = Mg, Mn2+ , Co2+ , Cu2+ , Zn and T = As5+ , S6+. The roselite group consists of the end-member minerals: roselite Ca2 Co(AsO4 )2 .2H2 O, wendwilsonite Ca2 Mg(AsO4 )2 .2H2 O, brandtite

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