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黄土高塬沟壑区植被恢复对土壤入渗及产流的影响

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[目的]研究植被恢复对降雨入渗及产流的影响,对流域水资源合理利用和生态环境建设具有重要理论意义和应用价值.[方法]以黄土高塬沟壑区南小河沟流域为研究区域,采用双环入渗试验和坡面模拟降雨试验方法,分析探究植被恢复对坡面水分入渗产流过程及特征的影响.[结果](1)植被恢复显著提高土壤入渗特征值与入渗能力,具体表现为人工林地>自然草地>玉米农田.(2)草地较裸地增加降雨量向土壤蓄量的转化,减少地表径流,出现多层壤中流.(3)草地较裸地土壤含水量变化更迅速,径流成分更丰富,产流量更少.(4)裸地降雨强度远大于土地下渗能力时,快速形成地表径流,下渗量较小,自然恢复草地则存在浅层相对不透水层,上下土层入渗能力差异大,形成壤中流.[结论]植被恢复通过改变土壤水文物理性质而使坡面产流机制发生变化,从多是超渗地表径流转变为超渗地表径流和壤中流同时出现.
Effects of Vegetation Restoration on Soil Infiltration and Runoff in the Gully Regions on the Loess Plateau
[Objective]To study the effects of vegetation restoration on rainfall infiltration and runoff is of great theoretical and practical value for rational utilization of watershed water resources and ecological construction.[Methods]Taking the Nanxiaohegou Watershed in the Gully Region on the Loess Plateau as the research area,the double-ring infiltration experiments and slope surface simulated rainfall experiments were conducted to analyze the effects of vegetation restoration on infiltration and runoff processes and characteristics on slopes.[Results](1)Vegetation restoration significantly increased the values of soil infiltration characteristics and capacity,with the order of artificial forest>natural grassland>corn farmland.(2)Compared to bare ground,grassland increased the transformation of rainfall into soil storage,reduced surface runoff,and led to the appearance of multiple layers of interflow.(3)Compared to bare ground,grassland showed more rapid changes in soil moisture content,richer runoff components,and less runoff volume.(4)When the intensity of rainfall on bare ground was much greater than the infiltration capacity of the land,surface runoff would be formed rapidly,and the amount of infiltration would be small,and there was a shallow and relatively impermeable layer in naturally restored grassland,and there was a big difference between the infiltration capacity of the upper and lower soil layers,so as to form a loamy mid-stream.[Conclusion]Vegetation restoration alters the hydrological properties of the soil,changing the runoff mechanism on slopes from predominantly overland flow to a combination of overland flow and interflow.

vegetation restorationsoil infiltrationrainfall runoffthe Loess Plateau

马雪燕、穆兴民、王双银、白云岗、牛芳鹏

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新疆水利水电科学研究院,乌鲁木齐 830049

西北农林科技大学土壤侵蚀与旱地农业国家重点实验室,陕西杨凌 712100

中国科学院水利部水土保持研究所土壤侵蚀与旱地农业国家重点实验室,陕西杨凌 712100

西北农林科技大学水利与建筑工程学院,陕西杨凌 712100

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植被恢复 土壤入渗 降雨产流 黄土高原

2024

水土保持学报
中国土壤学会 中国科学院水利部水土保持研究所

水土保持学报

CSTPCD北大核心
影响因子:1.226
ISSN:1009-2242
年,卷(期):2024.38(6)