剥蚀过程对Zbójn地区(Dobrzyńskie湖区)冰下水域侵蚀形成的填充竖井之间凹坑的沉积物特性的影响

M. Karasiewicz, P. Hulisz, M. Świtoniak
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引用次数: 7

摘要

这项研究是在dobrzyz Lakeland东南部Zbójno附近一个1平方公里的试验田内进行的。研究的目的是分析自然剥蚀和人为剥蚀对冰川曲线间洼地沉积物性质的影响。在研究的坳陷中发现了五种类型的矿床。这些洼地充满了与自然过程和长期粗放耕作密切相关的沉积物层序。沉积和凹陷的转化程度和范围在很大程度上取决于这些凹陷的形态特征。与形成冰川曲线脊的沉积物相比,所分析的洼地沉积物具有明显不同的化学成分特征,这清楚地表明它们具有沉积物圈闭的功能。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Wpływ procesów denudacji na właściwości osadów wypełniających zagłębienia między krętymi wałami z erozji wód subglacjalnych w okolicy Zbójna (Pojezierze Dobrzyńskie)
The research was conducted within a test field of 1 km2 located near Zbójno, that lies in the south-eastern part of the Dobrzyń Lakeland. The objective of the research was to analyze the effect of natural and anthropogenic denudation on the properties of sediments in depressions between glacial curvilineations. Five types of deposits were identified in the studied depressions. These depressions are filled with sediments sequences which are closely associated with natural processes and long-term extensive farming. The degree and the range of transformations of deposits and depressions depend largely on their morphometric characteristics of these depressions. Compared with sediments building the ridge of a glacial curvilineation, the deposits of the analysed depressions were characterised by significantly different chemical composition, which clearly indicates their function as sediment traps.
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