Soil erosion estimation in a catchment with implemented soil and water conservation measures

IF 2.8 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL
He Wang, Xiang Ji, Xiaopeng Wang, Yue Zhang, Fangshi Jiang, Yanhe Huang, Jinshi Lin
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Abstract

The variations in soil erosion significantly impact regional ecological security. Under rapid urbanisation, extensive ecological restoration and climate change, soil erosion development in the red soil region of southern China is ambiguous. Therefore, this study investigated the current (1980s–2020) and future (2050) erosion characteristics in a typical soil erosion control catchment (Changting section catchment) in this region by using the Cellular Automata Markov model and CMIP6 data to predict future scenarios and the Revised Universal Soil Loss Equation to estimate soil erosion. The results showed significant changes in the vegetation coverage of major land uses from 1980s to 2020, which was mainly caused by continuous soil and water conservation (SWC). The land use subtypes that were obtained by reclassifying land use based on the threshold of vegetation cover on soil erosion control, reflect a continuous transformation from those with poor SWC effectiveness to those with great SWC effectiveness. Therefore, the estimated soil erosion intensity continued to decrease from 1980s to 2020, and the contribution of land use/land cover (LULC) impacts ranged from 74%–195%. However, predictions of land use subtypes indicated that LULC may be stable after 2020; thus, soil erosion changed little when the climate was almost unchanged in 2050. Under climate change scenarios, soil erosion may increase by 111%–121%, and the contribution of precipitation impacts was 63%–66%. The major driving factor of soil erosion changes may shift from LULC to precipitation after 2020. Therefore, in the future, the potential for reducing soil erosion by vegetation restoration may be limited, and more engineering measures should be applied to address the erosion risk caused by climate changes. This study provides prospects for land use/land cover and soil erosion in the red soil region of southern China.

Abstract Image

对已实施水土保持措施的集水区进行水土流失估算
水土流失的变化极大地影响着区域生态安全。在快速城镇化、大面积生态修复和气候变化的背景下,中国南方红壤地区的水土流失发展不明确。因此,本研究利用细胞自动机马尔可夫模型和 CMIP6 数据预测未来情景,并利用修订的通用土壤流失方程估算土壤侵蚀量,研究了该地区典型水土流失控制流域(长汀段流域)当前(1980 年代-2020 年)和未来(2050 年)的水土流失特征。结果表明,从 20 世纪 80 年代到 2020 年,主要土地利用的植被覆盖率发生了显著变化,这主要是由持续的水土保持引起的。根据植被覆盖率对水土流失控制的临界值对土地利用进行重新分类后得到的土地利用亚类,反映了从水土保持效果差的土地利用向水土保持效果好的土地利用的持续转变。因此,从 20 世纪 80 年代到 2020 年,估计的土壤侵蚀强度持续下降,土地利用/土地覆被影响的贡献率在 74%-195% 之间。然而,对土地利用亚类的预测表明,2020 年后土地利用/土地覆被可能保持稳定;因此,在 2050 年气候几乎不变的情况下,土壤侵蚀变化不大。在气候变化情景下,土壤侵蚀可能增加 111%-121%,降水影响的贡献率为 63%-66%。2020 年后,土壤侵蚀变化的主要驱动因素可能会从 LULC 转向降水。因此,未来通过植被恢复来减少土壤侵蚀的潜力可能有限,应采用更多的工程措施来应对气候变化带来的水土流失风险。本研究为中国南方红壤地区的土地利用/土地覆被与水土流失提供了展望。
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来源期刊
Earth Surface Processes and Landforms
Earth Surface Processes and Landforms 地学-地球科学综合
CiteScore
6.40
自引率
12.10%
发文量
215
审稿时长
4 months
期刊介绍: Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with: the interactions between surface processes and landforms and landscapes; that lead to physical, chemical and biological changes; and which in turn create; current landscapes and the geological record of past landscapes. Its focus is core to both physical geographical and geological communities, and also the wider geosciences
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