Effects of Different Land Uses and Slope on Runoff and Soil Loss on the Loess Plateau of China

IF 3.6 2区 农林科学 Q2 ENVIRONMENTAL SCIENCES Land Degradation & Development Pub Date : 2024-10-15 DOI:10.1002/ldr.5337
Zhiwei Cui, Peng Li, Lei Zhang, Tian Wang, Jianye Ma, Lie Xiao, Binhua Zhao, Jianchun Han, Zixuan Yan, José A. Gómez
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Abstract

The Loess Plateau has one of the most serious areas of soil erosion in China; therefore, studying the effect of soil and water conservation measures on the erosion of loess soil slopes is important for land management and agricultural development. This study is based on 5 years of field runoff observations and rainfall data from 2015 to 2019. Correlation and regression analyses were used to study the runoff and sediment production of loess soil and its relationship with rainfall, slope and land use. The results show that > 80% of the erosive rainfall occurs mainly in July to August in the area. Runoff and soil loss from the plots differed substantially, depending on land use, soil conservation measures and slope degree. Bare plots experienced the highest soil loss rate of over 27 t/ha with higher runoff depth, followed by cultivated plots (4.55 t/ha), grass plots (0.43 t/ha), shrub plots (0.35 t/ha) and forest plots (0.13 t/ha). Among the four soil and water conservation measures, the runoff and sediment reduction benefits of forest and shrub plots were the highest. The runoff reduction benefit fluctuated at approximately 0.8, and the benefit of sediment reduction was ≈1. The overall performance was forest > shrubland > grassland > cultivated land > bare land, and the benefits of sediment reduction were greater than those of runoff reduction. Forests had the highest soil retention capacity on slopes from 5° to 25°, and forests on gentle slopes had the best water storage capacity. Shrub plots had the best water storage capacity when they were on steep slopes. Rainfall erosion forces were significantly and positively correlated (p < 0.01) with runoff depth and soil loss, making it the most significant rainfall indicator of sediment production. Under the same rainfall conditions, soil and water conservation measures are still required on bare slopes, land use is the main control factor for slope sediment production, and appropriate land use can greatly reduce the threat of slopes in terms of soil erosion. This study shows that soil and water conservation measures are imperative to prevent runoff and soil loss, especially for bare land without any measures; on steep slopes, a vegetation combination primarily featuring shrubs is expected to achieve greater benefits in reducing runoff and sediment. This study can provide a scientific basis for the management of vegetation measures and the implementation of soil and water conservation measures on loess soil slopes.
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不同土地利用方式和坡度对中国黄土高原径流和土壤流失的影响
黄土高原是中国水土流失最严重的地区之一,因此,研究水土保持措施对黄土坡面侵蚀的影响对土地管理和农业发展具有重要意义。本研究基于 2015 年至 2019 年 5 年的野外径流观测和降雨数据。采用相关分析和回归分析研究了黄土的径流量和泥沙产生量及其与降雨、坡度和土地利用的关系。结果表明,>80%的侵蚀性降雨主要发生在该地区的7月至8月。根据土地利用、土壤保持措施和坡度的不同,地块的径流和土壤流失量也大不相同。裸露地块的土壤流失率最高,超过 27 吨/公顷,径流深度也较大,其次是耕地(4.55 吨/公顷)、草地(0.43 吨/公顷)、灌木地(0.35 吨/公顷)和林地(0.13 吨/公顷)。在四种水土保持措施中,林地和灌木林地的径流和泥沙减少效益最高。径流减少效益在 0.8 左右波动,泥沙减少效益≈1。总体表现为森林>;灌木林>;草地>;耕地>;裸地,减少泥沙的效益大于减少径流的效益。在 5° 至 25° 的坡度上,森林的土壤保持能力最强,缓坡上的森林蓄水能力最好。灌木地在陡坡上的蓄水能力最强。降雨侵蚀力与径流深度和土壤流失量呈显著正相关(p < 0.01),是泥沙产生的最重要的降雨指标。在相同降雨条件下,裸露边坡仍需采取水土保持措施,土地利用是边坡泥沙产生的主要控制因素,合理的土地利用可大大减少边坡的水土流失威胁。本研究表明,水土保持措施是防止径流和土壤流失的必要措施,尤其是对于没有采取任何措施的裸露土地;在陡坡上,以灌木为主的植被组合有望在减少径流和泥沙方面取得更大的效益。这项研究可为黄土坡的植被措施管理和水土保持措施的实施提供科学依据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Land Degradation & Development
Land Degradation & Development 农林科学-环境科学
CiteScore
7.70
自引率
8.50%
发文量
379
审稿时长
5.5 months
期刊介绍: Land Degradation & Development is an international journal which seeks to promote rational study of the recognition, monitoring, control and rehabilitation of degradation in terrestrial environments. The journal focuses on: - what land degradation is; - what causes land degradation; - the impacts of land degradation - the scale of land degradation; - the history, current status or future trends of land degradation; - avoidance, mitigation and control of land degradation; - remedial actions to rehabilitate or restore degraded land; - sustainable land management.
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