俄罗斯平原北部森林草原区当代沟壑侵蚀趋势:以俄罗斯欧洲部分鞑靼斯坦共和国为例

Q3 Earth and Planetary Sciences
A. Sharifullin, A. Gafurov, R. Medvedeva, V. Golosov, Aleksandr Dvinskih, A. Gusarov, B. Essuman-Quainoo
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引用次数: 2

摘要

摘要本文介绍了基于监测(1984-1994年和2015-2018年)和高分辨率卫星图像(2004-2014年)解译的前卡马地区(俄罗斯鞑靼斯坦共和国)沟头削减后退率(GHRR)的结果。结果表明,平均线性GHRR减少了约5倍,从每年1.6 m(1983-1994)减少到每年0.4 m(2015-2018)。沟壑侵蚀显著减少的主要原因是冬春气温的升高,导致土壤冻结深度和地表径流的减少。在20世纪80年代末和90年代初在研究区域实施的土地利用和侵蚀控制措施的影响被发现不那么重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Contemporary gully erosion trend in the northern part of the forest-steppe zone of the Russian Plain: a case study from the Republic of Tatarstan, European Russia
Abstract. This article presents results for gully head cut retreat rates (GHRR) in the Pre-Kama region (Republic of Tatarstan, Russia) based on monitoring (1984–1994 and 2015–2018) and the interpretation of high-resolution satellite images (2004–2014). The results suggested that the mean linear GHRR have reduced by about five times, from 1.6 m per year (1983–1994) to 0.4 m per year (2015–2018). The main reason for the significant decrease in gully erosion was the increase in winter-spring air temperatures, which resulted in a reduction in the depth of soil freezing and surface runoff. The impact of land use, as well as erosion control measures, which were implemented in the study area during the late 1980s and early 1990s, was found to be less important.
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来源期刊
Proceedings of the International Association of Hydrological Sciences
Proceedings of the International Association of Hydrological Sciences Earth and Planetary Sciences-Earth and Planetary Sciences (all)
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