基于实验研究的降雨强度对土壤侵蚀的影响

Mikołaj Majewski, Aleksandra Czuchaj, Marek Marciniak
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引用次数: 0

摘要

水对土壤的侵蚀受降水这一主要形态发生因素的影响。由降雨引发的地表径流在这一过程中起着关键作用。本文通过一系列不同强度和持续时间的降雨模拟,探讨了降雨强度和土壤湿度对土壤侵蚀的影响。在波兹南罗扎尼溪流集水区的一个研究站进行的测量使研究斜坡内的整个水平衡成为可能,包括降水、蒸发、地表径流和渗透。研究包括各种降雨强度,重点是反映当前气候变化和人类压力增加的极端事件。降雨模拟在干燥和潮湿的地面上进行。结果表明,降雨强度的增加导致地表径流和土壤流失增加。此外,土壤湿度被认为是影响土壤侵蚀的关键因素,较湿的条件会减少土壤流失,同时增加地表径流。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Impact of rainfall intensity on soil erosion based on experimental research
Soil erosion by water is influenced by a major morphogenetic factor – precipitation. Surface runoff, initiated by rainfall, plays a key role in this process. This article addresses the effects of rainfall intensity and soil moisture on soil erosion through a series of rainfall simulations of different intensity and duration. The implementation of measurements at a research station located in the Różany Stream catchment in Poznań made it possible to study the entire water balance within the slope, including precipitation, evaporation, surface runoff and infiltration. The study included various rainfall intensities, with a focus on extreme events reflecting ongoing climate change and increasing anthropopressure. Rainfall simulations were conducted on both dry and wet ground. The results showed that increasing rainfall intensity led to greater surface runoff and soil loss. Moreover, soil moisture was identified as a critical factor affecting soil erosion, with wetter conditions reducing soil loss while increasing surface runoff.
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