Low temperature magnetism and Mossbauer spectroscopy study from natural goethite

被引:22
作者
Berquo, T. S. [1 ]
Imbernon, R. A. L.
Blot, A.
Franco, D. R.
Toledo, M. C. M.
Partiti, C. S. M.
机构
[1] Univ Minnesota, Dept Geol & Geophys, Inst Rock Magnetism, Minneapolis, MN 55455 USA
[2] Univ Sao Paulo, Inst Fis, Lab Mat Magnet, Sao Paulo, Brazil
[3] Univ Sao Paulo, Inst Geociencias, Lab Hidrogeoquim, Sao Paulo, Brazil
[4] IRD Orstom, Ouagadougou, Burkina Faso
[5] Univ Sao Paulo, Inst Geociencias, Sao Paulo, Brazil
关键词
Goethite; Gossans; Magnetization; AC susceptibility; Mossbauer spectroscopy; FINE-PARTICLE GOETHITE; BURKINA-FASO; IRON-OXIDES; SYNTHETIC GOETHITE; NEEL TEMPERATURE; HYPERFINE FIELD; GRAIN-SIZE; BEHAVIOR; AL; DEMAGNETIZATION;
D O I
10.1007/s00269-007-0147-9
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
In this work a magnetic characterization was made of natural goethite from Burkina Faso, Africa, by using low temperature magnetization curves, hysteresis loops, Mossbauer spectroscopy at room temperature and 4.2 K, and AC susceptibility from 10 to 400 K. The samples are from two distinct geological sites that underwent different weathering processes. All measurements point to the occurrence of typical high coercivity goethite. Through Mossbauer spectroscopy sample BL44, from Gangaol, northeast Burkina Faso showed relaxation effects due to a wide distribution of grain size, including superparamagnetism threshold. AC susceptibility also supports this interpretation. The sample BL50 from Bonga in Burkina Faso is associated with lateritic Ni and in addition to goethite this sample also contained magnetite, as determined by Verwey transition in low temperature measurements as well as a small content of hematite identified by Mossbauer spectroscopy.
引用
收藏
页码:287 / 294
页数:8
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