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A NEW TOOL FOR IN SITU MEASUREMENTS OF THE VERTICAL DISTRIBUTION OF MAGNETIC SUSCEPTIBILITY IN SOILS AS BASIS FOR MAPPING DEPOSITED DUST

机译:基于原位测量土壤中磁化率分布的新工具

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In situ measurements of magnetic susceptibility of topsoils are commonly used for mapping the spatial distribution of atmospherically deposited ferrimagnetic particles. However, the surface measurements integrate signal from certain soil volume and, thus, it is not evident how deep is the magnetically enhanced layer, if there is such. This information is often required for detailed sampling. Furthermore, fast estimate of the significance of lithogenic contribution is needed for the proper interpretation of the surface data. This can be reliably done on the basis of vertical distribution of magnetic susceptibility of a soil column. Until now, there was practically no reliable, fast and sensitive enough tool to carry out these measurements in real time, directly in field. In this paper, we report on a new soil-profile kappameter SM400, which enables continuous real-time measurements, performed directly in the field. We describe its basic measurement principles. Performance parameters are discussed, showing that sensitivity is high enough to depict the soil layers with different susceptibility and a data density of 6 points per 1 mm of depth, which results in smooth curves of susceptibility, unlike field or laboratory probes used until now. Profiles acquired using different probes and instruments are compared in order to demonstrate advantages of the new approach.
机译:表土的磁化率的原位测量通常用于绘制大气沉积的亚铁磁性颗粒的空间分布。但是,表面测量结果会整合来自特定土壤体积的信号,因此,如果存在,那么磁增强层的深度尚不明显。经常需要此信息以进行详细采样。此外,为了正确解释表面数据,需要快速估算成岩作用的重要性。这可以根据土柱的磁化率的垂直分布可靠地完成。到目前为止,几乎没有可靠,快速和灵敏的工具可以直接在现场实时进行这些测量。在本文中,我们报告了一种新的土壤剖面kappaometer SM400,它可以在现场直接进行连续的实时测量。我们描述其基本的测量原理。讨论了性能参数,表明灵敏度足够高,可以描述具有不同敏感性的土壤层,每1毫米深度的数据密度为6点,这导致敏感性曲线平滑,这与迄今为止使用的野外或实验室探针不同。比较使用不同探针和仪器获得的配置文件,以证明新方法的优势。

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