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Isothermal remanence experiments at room and at liquid nitrogen temperature: Application to soil studies

机译:室温和液氮温度下的等温剩磁实验:在土壤研究中的应用

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摘要

A simple magnetic mineral identification technique is proposed which measures isothermal remanent magnetisation (IRM) acquired in different field strengths at 293 K and 77 K. Magnetic parameters are introduced that use these IRMs in order to distinguish concentration and type of ferromagnetic minerals in different magnetic states. The method determines easily contributions of superparamagnetic ferrimagnetic minerals in environmental magnetism studies. In addition, high coercivity goethite and possibly superparamagnetic hematite are identified. The analysis of the magnetic properties of a soil profile on a Late Pleistocene terrace from the Jarama river in central Spain is given as an example. [References: 15]
机译:提出了一种简单的磁性矿物识别技术,该技术可测量在293 K和77 K时在不同场强下获得的等温剩余磁化强度(IRM)。引入了使用这些IRM的磁性参数,以区分不同磁性状态下铁磁性矿物的浓度和类型。该方法可轻松确定超顺磁性亚铁磁性矿物在环境磁性研究中的贡献。另外,鉴定出高矫顽力针铁矿和可能的超顺磁性赤铁矿。以西班牙中部哈拉玛河晚更新世阶地土壤剖面的磁性分析为例。 [参考:15]

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