Dynamic Changes of Soil and Water Loss in Rich and Coarse Sediment Areas of Middle Yellow River Basin From 1985 to 2020

Yin Baoku; Su Pengfei; Zhang Jianguo; Cao Xiayu

doi:10.13961/j.cnki.stbctb.2021.05.017

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Dynamic Changes of Soil and Water Loss in Rich and Coarse Sediment Areas of Middle Yellow River Basin From 1985 to 2020

- Dynamic Changes of Soil and Water Loss in Rich and Coarse Sediment Areas of Middle Yellow River Basin From 1985 to 2020
- Bulletin of Soiland Water Conservation Vol. 41, Issue 5, Pages: 123-126(2021)
- 作者机构：
  
  黄河水利委员会黄河上中游管理局,陕西,西安,710021
- 作者简介：
- 基金信息：
- DOI：10.13961/j.cnki.stbctb.2021.05.017
  CLC： S157.1
- Published：2021
- 稿件说明：
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Yin Baoku, Su Pengfei, Zhang Jianguo, et al. Dynamic Changes of Soil and Water Loss in Rich and Coarse Sediment Areas of Middle Yellow River Basin From 1985 to 2020[J]. Bulletin of Soiland Water Conservation, 2021, 41(5): 123-126.
DOI：

Yin Baoku, Su Pengfei, Zhang Jianguo, et al. Dynamic Changes of Soil and Water Loss in Rich and Coarse Sediment Areas of Middle Yellow River Basin From 1985 to 2020[J]. Bulletin of Soiland Water Conservation, 2021, 41(5): 123-126. DOI： 10.13961/j.cnki.stbctb.2021.05.017.

摘要

[目的] 掌握黄河中游多沙粗沙区水土流失空间分布状况，为黄河流域水土流失治理、生态环境保护和高质量发展提供数据支撑和科学建议。[方法] 利用2020年水土流失动态监测和1985，1999年全国水土流失遥感普查成果，开展黄河中游多沙粗沙区水土流失动态变化分析。[结果] ①研究区域水土流失面积减少43.22%，高强度水土流失面积减少90.80%，水土流失状况明显改善；1985—1999年和1999—2020年两个时段，前时段变化相对较小，后时段变化较大。②两个时段内水土流失强度均降低，1999—2020年降低幅度明显大于1985—1999年且高强度水土流失面积大幅减少。1985—1999年以剧烈侵蚀面积减少为主，1999—2020年强烈、极强烈、剧烈侵蚀等高强度侵蚀面积下降明显。[结论] 研究区生态环境状况改善的主要驱动力是区域水土保持监督管理工作的加强，预防保护与水土保持综合治理的协同推进，经济社会的发展，保护环境和生态政策的引导等。虽然研究区水土流失日趋严重的态势得到了遏制，但其依然是黄土高原乃至中国水土流失最严重的地区，后续仍需持续采取适宜措施保护好生态环境。

Abstract

[Objective] The spatial distribution of soil erosion in the rich and coarse sediment areas of the Yellow River basin was studied in order to provide data support and scientific suggestions for soil erosion control

ecological environmental protection

and high-quality development in the Yellow River basin.[Methods] Dynamic changes of soil and water loss in rich and coarse sediment areas of the middle reaches of the Yellow River basin were analyzed based on dynamic monitoring of soil erosion in 2020 and the results of the national remote sensing surveys of soil erosion in China in 1985 and 1999.[Results] ① The area of regional soil and water loss decreased by 43.22%

the area of high-intensity soil and water loss decreased by 90.80%

and the status of soil erosion has been improved significantly over time. The changes in 1985-1999 were relatively small

while the changes in 1999-2020 were relatively large. ② The intensity of soil and water loss decreased in both periods. The decrease in 1999-2020 was significantly greater than in 1985-1999

and high-intensity soil erosion decreased significantly. In 1985-1999

the area of severe erosion mainly decreased

while in 1999-2020

the areas classified as intensive

extremely intensive

and severe erosion decreased significantly.[Conclusion] The main driving forces for the improvement of the ecological environment in the study area were the strengthening of the supervision and management of regional soil and water conservation

coordinated promotion of preventive protection and comprehensive management of soil and water conservation

economic and social development

environmental protection

and ecological policy guidance. Although the increasingly serious conditions resulting in soil and water loss in the Loess Plateau have been controlled

the region is still considered to be under the most severe soil erosion threat in China. It is still necessary to continue to take appropriate measures for the protection of the ecological environment.

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references

李敏, 王白春, 许林军.多沙粗沙区综合治理规划与减沙作用[J].人民黄河, 2013, 35(10):124-126.

张含玉.黄河中游多沙粗沙区侵蚀产沙变化特征及影响因子分析[D].陕西杨凌:中国科学院教育部水土保持与生态环境研究中心, 2016.

赵辉, 黎家作, 李晶晶.中国水土流失动态监测与评价的现状与对策[J].水土保持通报, 2016, 36(1):115-119.

王光谦, 张长春, 刘家宏, 等.黄河流域多沙粗沙区植被覆盖变化与减水减沙效益分析[J].泥沙研究, 2006(2):10-16.

陈劭锋, 刘全友, 陆中臣, 等.黄土高原多沙粗沙区侵蚀产沙的多维临界[J].生态学报, 2007, 27(8):3277-3285.

杨胜天, 周旭, 刘晓燕, 等.黄河中游多沙粗沙区(渭河段)土地利用对植被盖度的影响[J].地理学报, 2014, 69(1):31-41.

王正兴, 李芳.中国分省土壤侵蚀变化数据集(1985-2011)[J].全球变化数据学报(中英文), 2018, 2(1):51-58.

刘宝元, 谢云, 张科利.土壤侵蚀预报模型[M].中国科学技术出版社, 2001.

水利部水土保持监测中心.区域水土流失动态监测技术规程[S].2018.

中华人民共和国水利部.SL190-2007土壤侵蚀分类分级标准[S].北京:中国水利水电出版社, 2008.

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