晋西黄土区土地利用对降雨入渗产流模式和优先流分布的影响试验研究
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国家自然科学基金项目(42077059)


Experimental investigation to the effect of different land-use on rainfall infiltration runoff patterns and preferential flow distribution in the Loess area of western Shanxi Province
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    摘要:

    黄土高原退耕还林(草)工程显著改变了河川径流过程,但其作用机制尚不明晰。选取晋西黄土区4种典型下垫面(20年和30年刺槐人工林地、草地、休耕地)分别开展连续3场模拟降雨试验,观测坡面入渗产流过程,并结合染色示踪和图像处理软件技术,分析土地利用类型对坡面降雨入渗产流模式和优先流分布的影响。结果表明:(1)累积入渗量和优先流发育程度均表现为刺槐林地 > 草地 > 休耕地,刺槐林地优先流对总入渗的贡献是草地和休耕地的2.5-4.5倍,但优先流贡献均不超过10%,仍以基质流入渗为主。(2)4种用地类型降雨入渗主要补给地表60-70cm土层,前期降雨均匀增加表层土壤含水率,而后期降雨补给深层土壤水分的空间变异性显著增强。(3)刺槐林地产流量及径流系数均显著小于草地和休耕地,且前期含水量对20年刺槐林地的影响较小,而显著影响草地和休耕地径流系数。(4)直径d<1mm的细根显著促进降雨入渗和优先流发育,而d>5mm的粗根与入渗量和基质流量呈显著负相关。较高的土壤初始含水率、容重和粘粒含量会抑制入渗和优先流的发生。研究说明不同土地利用类型将改变降雨入渗产流过程及土壤水运动形式。

    Abstract:

    The Grain for Green Project has changed hydrological processes on the Loess Plateau, but there is little information on the infiltration and runoff mechanism. Four typical land-use types (20a and 30a Robinia pseudoacacia woodland (20 or 30 RW), grassland (GL), and fallow slopeland (FL)) in the Caijiachuan watershed of the Loess area of western Shanxi Province were selected to investigate the effects of land uses on rainfall-infiltration-runoff processes under field simulated rainfalls.The dyeing tracer and image processing software were used to analyze the spatial distribution of preferential flows. The results showed that:(1) both the cumulative infiltration amount and the preferential flow distribution ranked the order:RW > GL > FL. The contribution ratio of preferential flow to total infiltration in RW was 2.5-4.5 times those of GL and FL. However, the contribution of preferential flow was less than 10% for all land uses and matrix flow dominated the infiltration processes. (2) The threshold depth in soil water impacted by rainfall infiltration was 60-70cm for the 4 land-use types. For all plots, antecedent precipitation evenly increased the soil water content of topsoil, while late precipitation increased the infiltration depth and its spatial variability in the increased soil water content. (3) The RW had significantly smaller surface runoff ratios to rainfall than GL and FL. Antecedent soil water content had little effect on the runoff in 20 RW plots, and had great influence on those in GL and FL plots. (4) The fine roots of diameter d<1mm significantly strengthened water infiltration and preferential flow occurrence, while roots of d>5mm had negative effect on infiltration and matrix flow. Antecedent water content, bulk density and clay content were the key soil factors hindering soil infiltration and the formation of preferential flow. These results indicate that the land-use types can change the processes of rainfall infiltration and soil moisture movement on the hillslopes, which may help understand the runoff generation mechanism.

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牛凤娇,潘成忠,崔永生,邹春蕾,张国栋,马勇星.晋西黄土区土地利用对降雨入渗产流模式和优先流分布的影响试验研究.生态学报,2023,43(10):4154~4166

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