波兰西南部Stołowe山Rogowa Kopa山坑丘微地形的电阻率层析成像(ERT

Łukasz Pawlik, Marek Kasprzak
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引用次数: 5

摘要

本文介绍了在波兰西南部斯托洛山脉Rogowa Kopa山坡上发育的具有坑丘微地形的坡幔电成像的地球物理分析结果。利用二维电阻率层析成像(2D ERT)对山坡微地形进行非侵入性分析,完成了以前的地貌和土壤研究结果。获得的层析成像(反演结果)可以根据风化层厚度及其湿度进行解释,也可以根据在土丘中检测到的残树和新鲜树根等更小的特征进行解释。这些特征与在分析的山坡主截面测量的地电阻率的一般图像进行了比较。在层析图上观察到的坡面覆盖特征的差异证实了树木连根拔起过程在形成风化层和土壤的一些基本特征(包括它们在山坡上的不均匀再分布)中的重要作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Electrical resistivity tomography (ERT) of pit-and-mound microrelief, Mt Rogowa Kopa case study, the Stołowe Mountains, SW Poland
This article presents results of geophysical analyses based on electrical imaging of slope mantles with pit-and-mound microtopography developed on the Rogowa Kopa hillslope in the Stolowe Mountains, SW Poland. The use of two dimensional electrical resistivity tomography (2D ERT) to non-invasive analyses of the hillslope microrelief allowed completing previous results of geomorphological and soil studies. The tomograms (inversion results) acquired across individual forms of treethrow pits and mounds can be interpreted according to regolith thickness and its wetness, but also smaller features such as relict and fresh tree root systems detected in the mounds. These features were compared to a general picture of geoelectrical resistivity measured in the main cross-section of the analyzed hillslope. The differences in slope cover characteristics observed on the tomograms confirm important role of the tree uprooting process in formation of some basic features of the regolith and soils, including their uneven redistribution across the hillslope.
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