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大理河流域土壤侵蚀时空分布及控制程度研究

Research on the spatiotemporal distribution and control degree of soil erosion in Dali River Basin.

作者信息

Liu Jiayi, Gao Kailin, Zhao Hao, Pan Shaoqi, Zhang Xiwang, Yu Shiqi, Chen Mengwei, Cheng Yuhui, Zhang Chengqiang

机构信息

Key Laboratory of Geospatial Technology for the Middle and Lower Yellow River Regions (Henan University), Ministry of Education, Kaifeng, 475004, China.

College of Geography and Environmental Science, Henan University, Kaifeng, 475004, China.

出版信息

Sci Rep. 2024 Nov 2;14(1):26379. doi: 10.1038/s41598-024-77828-2.

Abstract

The Dali River basin as the representative areas of the middle reaches of the Yellow River. Accurately evaluating the degree of soil erosion control is very important for soil erosion control. In response to the problems existing in the current research on soil erosion control degree (SECD) methods, the maximum possible soil erosion modulus is introduced into the evaluation model. Thereby eliminating the uncertainty of the assumed state of the original model. This paper calculates the SECD for 2020 based on this method. The results show: (1) From the soil erosion modulus spatial distribution, it can be seen that the soil erosion intensity is stronger in the eastern and southwestern parts. (2) Based on the SECD spatial distribution, it was found that eastern and southwestern regions were well controlled. This is consistent with the actual situation. (3) As the slope increases, the area proportion of SECD within the 0.2-0.3 range in each slope zone shows an increasing trend, while that of SECD within the 0.5-1 range gradually decreases; (4) In the case of vegetation coverage greater than 80%, SECD is still concentrated between 0.3-0.5, which indicates that vegetation coverage is not the only factor affecting soil erosion control. This research provided a new perspective for the evaluation of SECD.

摘要

大理河流域作为黄河中游的代表性区域,准确评估土壤侵蚀控制程度对于土壤侵蚀防治至关重要。针对当前土壤侵蚀控制程度(SECD)方法研究中存在的问题,将最大可能土壤侵蚀模数引入评价模型,从而消除了原模型假设状态的不确定性。本文基于该方法计算了2020年的SECD。结果表明:(1)从土壤侵蚀模数空间分布来看,东部和西南部地区土壤侵蚀强度较强。(2)基于SECD空间分布发现,东部和西南部地区得到了较好的控制,这与实际情况相符。(3)随着坡度增加,各坡度带内SECD在0.2 - 0.3范围内的面积比例呈增加趋势,而在0.5 - 1范围内的SECD面积比例逐渐减小;(4)在植被覆盖度大于80%的情况下,SECD仍集中在0.3 - 0.5之间,这表明植被覆盖度不是影响土壤侵蚀控制的唯一因素。该研究为SECD评价提供了新的视角。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5609/11530430/1a5d2dfac435/41598_2024_77828_Fig1_HTML.jpg

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