Quick Search:    advanced search

GSW Home   GeoRef Home   My GSW Alerts   Contact GSW   About GSW   Journals List   Help

This Article Figures Only Full Text Full Text (PDF) Alert me when this article is cited Alert me if a correction is posted Citation Map Services Email this article to a friend Similar articles in this journal Similar articles in Web of Science Alert me to new issues of the journal Download to citation manager Citing Articles Citing Articles via Google Scholar Google Scholar Articles by Schmidt, V. Articles by Günther, D. Search for Related Content GeoRef GeoRef Citation

Magnetic anisotropy of carbonate minerals at room temperature and 77 K

¹ Institute for Geophysics, ETH Zurich, HPP O.3, CH-8093 Zurich, Switzerland
² Laboratory for Inorganic Chemistry, ETH Zurich, HCI G.113, CH-8093 Zurich, Switzerland

Correspondence: ^* E-mail: schmidt{at}mag.ig.erdw.ethz.ch

The relationship between magnetic properties and chemical composition of 19 natural carbonate single crystals of the calcite, aragonite, and dolomite groups and of azurite were investigated. Magnetic susceptibility was determined in low fields, and magnetic anisotropy was measured at room temperature and at 77 K using a high-field torque magnetometer. The chemical composition was analyzed using LA-ICP MS. Planar arrangement of the CO₃-groups generates an oblate diamagnetic anisotropy with the minimum susceptibility k₃ along the crystallographic c-axis in all investigated anhydrous carbonate minerals. A prolate paramagnetic anisotropy with the maximum susceptibility k₁ along the c-axis is produced by Fe²⁺ in the trigonal carbonate lattice, which can lead to a transition from oblate to prolate shape of the total anisotropy. The transition occurs in the calcite structure above an Fe concentration of 400 ppm at room temperature and 150 ppm at 77 K. The susceptibility difference k₁ – k₃ for pure calcite is 4.06 x 10^–10 m³/kg and increases to 9.4 x 10^–9 m³/kg for 10 800 ppm Fe. In the hexagonal aragonite structure, no paramagnetic anisotropy due to Fe²⁺ was detected. Azurite shows a strong anisotropy with k₁ – k₃ = 1.5 x 10^–8 m³/kg, which is assigned to Cu²⁺. The paramagnetic anisotropy due to Fe²⁺ increases at 77 K in minerals of the calcite and dolomite group and in azurite, but not in minerals of the aragonite group. Upon cooling from room temperature to 77 K, k₁ – k₃ increases 13.3 times for 500 ppm to 100 000 ppm Fe²⁺ in the trigonal lattice and 7.2 times for siderite.

Key Words: Carbonate minerals • magnetic properties • anisotropy • calcite • siderite • rhodochrosite • LA ICP-MS