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1.西北农林科技大学水利与建筑工程学院, 陕西 杨凌 712100
2.西北农林科技大学水土保持与;荒漠化整治全国重点实验室, 陕西 杨凌 712100
3.中国科学院地理科学与资源研究所, 北京 100101
4.中国科学院大学资源与环境学院, 北京 100101
5.青海大学土木水利学院,西宁 810016
Received:22 January 2026,
Revised:2026-03-18,
Accepted:25 March 2026,
Online First:14 April 2026,
Published:28 August 2026
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张彪,王治英,宋法通,等.生态恢复背景下黄河源区复合土壤侵蚀强度评估及其对气候变化的响应[J].水土保持学报,2026,40(4):331-344.
Zhang Biao, Wang Zhiying, Song Fatong, et al. Intensity assessment of compound soil erosion in source region of Yellow River and its response to climate change under background of ecological restoration[J]. Journal of Soil and Water Conservation, 2026, 40(4):331-344.
张彪,王治英,宋法通,等.生态恢复背景下黄河源区复合土壤侵蚀强度评估及其对气候变化的响应[J].水土保持学报,2026,40(4):331-344. DOI: 10.13870/j.cnki.stbcxb.2026.04.018. CSTR: 32310.14.stbcxb.2026.04.018.
Zhang Biao, Wang Zhiying, Song Fatong, et al. Intensity assessment of compound soil erosion in source region of Yellow River and its response to climate change under background of ecological restoration[J]. Journal of Soil and Water Conservation, 2026, 40(4):331-344. DOI: 10.13870/j.cnki.stbcxb.2026.04.018. CSTR: 32310.14.stbcxb.2026.04.018.
目的
2
为阐明生态恢复背景下黄河源区复合土壤侵蚀时空演变特征及其对气候变化的响应机制。
方法
2
基于1980—2020年气象观测、遥感植被指数及地形数据,耦合RUSLE、RWEQ与冻融侵蚀模型,定量评估3类营力侵蚀强度;结合转移矩阵分析时空演变路径,并采用逐栅格偏相关分析揭示复合侵蚀对年降水量、年平均气温和年平均风速的独立响应关系。
结果
2
1980—2020年黄河源区气候呈“暖湿化”趋势(降水显著增加,气温上升1.5 ℃,风速下降0.3~0.6 m/s),植被覆盖度提升超40.0%。水蚀、风蚀与冻融侵蚀强度均显著降低。不同气候变量与复合侵蚀营力的偏相关分析表明,1980—2020年降水对侵蚀的正向驱动持续增强(正相关区占比由27.4%提升至56.0%),气温影响由促进转为抑制(正相关区占比从46.0%下降至12.8%),风速驱动作用明显弱化(正相关区占比下降至19.8%)。黄河源区复合侵蚀营力的交替和协同作用,导致特定时空条件中气候变量与侵蚀强度变化的异常响应。
结论
2
生态恢复工程有效改善黄河源区复合土壤侵蚀环境特征,抑制黄河源区复合土壤侵蚀;复合营力侵蚀交替和协同作用导致气候变量与侵蚀强度变化异常响应的时空关系。研究结果为复合土壤侵蚀强度评估及其与环境变化之间的响应研究提供理论参考。
Objective
2
This study aims to clarify the spatiotemporal evolution characteristics of compound soil erosion in the source region of the Yellow River under the background of ecological restoration and reveal its response mechanisms to climate change.
Methods
2
Based on meteorological observations, remote sensing-derived vegetation index, and topographic data from 1980 to 2020, the RUSLE, RWEQ, and freeze-thaw erosion models were coupled to quantitatively assess the intensity of three types of soil erosion driving forces. Transition matrices were employed to analyze the spatiotemporal evolution pathways, while pixel-based partial correlation analysis was conducted to reveal the independent responses of compound erosion to annual precipitation, annual average temperature, and annual average wind speed.
Results
2
From 1980 to 2020, the climate in the source region of the Yellow River exhibited a warming and wetting trend, characterized by a significant increase in precipitation, a temperature rise of 1.5 ℃, and a wind speed reduction of 0.3-0
.6 m/s, while vegetation coverage increased by more than 40.0%. The intensities of water, wind, and freeze-thaw erosion all decreased significantly. Partial correlation analysis between different climate variables and compound erosion driving forces revealed that, during the study period (1980-2020), the positive driving effect of precipitation on erosion continuously strengthened (the proportion of positively correlated area increased from 27.4% to 56.0%), the influence of temperature shifted from promoting to suppressing erosion (the proportion of positively correlated area decreased from 46.0% to 12.8%), and the driving effect of wind speed markedly weakened (the proportion of positively correlated area decreased to 19.8%)
.
The alternating and synergistic effects of compound erosion driving forces in the source region of the Yellow River resulted in abnormal responses of climate variables and erosion intensity changes under specific spatiotemporal conditions.
Conclusion
2
The ecological restoration project effectively improves the compound soil erosion environmental characteristics in the source region of the Yellow River, thereby suppressing the compound soil erosion in this region. The alternating and synergistic effects of compound erosion driving forces lead to abnormal spatiotemporal responses of climate variables and erosion intensity changes. The research findings provide theoretical references for the intensity assessment of compound soil erosion and its response to environmental changes.
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