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Strongly magnetic soil developed on a non-magnetic rock basement: A case study from NW Bulgaria

机译:非磁性岩石基底上发育的强磁性土壤:以保加利亚西北地区为例

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摘要

The enhanced magnetic susceptibility of modern soils is assumed to have several reasons including, e.g., weathering of an iron-rich geological basement, natural fires, bacterial processes and atmospheric deposition of anthropogenic particles. We report on a case where none of the above sources of magnetic enhancement is evident: a modern soil with high magnetic susceptibility over the whole soil profile, developed on nonmagnetic limestones, in an area with no industrial activities. The surface magnetic susceptibility varies from 60 to 110×10−5 SI, while that of the rock basement is nearly zero. Moreover, significant frequency-dependent magnetic susceptibility (> 12%) suggests that superparamagnetic secondary magnetite/maghemite plays an important role. Possible mechanisms, responsible for this magnetic enhancement, are discussed.
机译:假定现代土壤的磁化率增强有几个原因,包括,例如富铁地质地下室的风化,自然火灾,细菌过程和人为颗粒的大气沉积。我们报道了一种上述磁场增强的来源均不明显的情况:在没有工业活动的地区,在非磁性石灰石上发育的,在整个土壤剖面中具有高磁化率的现代土壤。地表磁化率的变化范围从60到110×10−5 SI,而岩石地下室的磁化率几乎为零。此外,显着的频率相关磁化率(> 12%)表明超顺磁性次级磁铁矿/磁赤铁矿起着重要作用。讨论了造成这种磁性增强的可能机制。

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