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种植大豆条件下土壤结皮对坡耕地径流和侵蚀产沙的影响 被引量:11

Effects of soil crust onslope runoff and sediment yield under soybean cover
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摘要 研究作物生长覆盖条件下土壤结皮对坡耕地径流和侵蚀产沙的影响,可为坡耕地水土流失防治和水土资源合理利用提供科学依据。以种植大豆的坡耕地土壤结皮为研究对象,利用人工模拟降雨方法,观测前期土壤结皮和不同结皮厚度、覆盖度下的产流产沙,分析前期土壤结皮的存在和土壤结皮厚度、覆盖度对坡耕地土壤侵蚀的影响。结果表明:1)前期土壤结皮的存在对坡面的产流产沙量产生较大影响,使坡面径流量高于非结皮坡面,而坡面的土壤流失量又远低于非结皮坡面。2)裸地前期有土壤结皮的坡面径流量较非结皮坡面高5.27%,产沙量则较其降低了27.66%;种植大豆条件下,前期地表有土壤结皮坡面的径流量较非结皮坡面平均增加了24.81%,产沙量较非结皮坡面平均降低了14.26%。3)大豆作物的存在加大了土壤结皮与非结皮坡面之间径流量的差距,缩小了二者间产沙量的差异;坡耕地坡面土壤结皮厚度及其覆盖度的变化对坡面产流产沙的影响却不显著。 The soil crust on slope farmland is a sort of compact slab structure formed by rainfall on the soil surface,and it has the characteristics of being smooth,compact,and easy to become ramous.Previous researchers have done a multitude of experiments regarding development mechanism,process of formation and factors affecting them,and their findings indicated that the soil crust has effects in decreasing infiltration,improving soil surface runoff amount,influencing the process of sediment yield,and reducing the biomass and yield of crop and so forth. Protecting slope farmland against soil and water loss has become an important issue of constructing bio-environment and realizing sustainable development in China. It is evident that the soil crust is a special underlying surface and it has significant effect on runoff amount and sediment yield on the slope. Planting is the main activity on slope farmland,and it has certain influence on the soil crust. The objectives of this study were to investigate the effects of soil crust on runoff and sediment yield under soybean cover and to provide theoretical basis for soil and water conservation and rational utilization of slope lands. Our study was carried out in the southern fringe of the Loess Plateau in 2010. Soil in the study area is Eum-Orthic Anthrosols. The intensity of the precipitation in this research was 80 mm / h,with each rainfall lasting for 60 min. We took slopes planted with soybeanas object,and by using simulated rainfalls we investigated the existence of soil crust before rain and influences of its thickness and coverage on runoff and sediment yield. Soil crust before rain had considerable effects on runoff and sediment yield. Analysis of the effects of soil crust on runoff and sediment yield on slope land under soybean cover showed that,the volume of runoff was higher on soil crusted slopes and amount of soil loss was much lower compared to that on slopes without soil crust. The soil crust made the beginning time of runoff yield earlier. With the growth of the soybean,the beginning time of runoff yield on the slope without crust was postponed much. The runoff and sediment yield became lower on slope land with soybean growing,and the soil crust on slope made the surface smoother.Besides,the structure of the soil crust is compact,which speeds up the runoff,lower the infiltration of rainfall and runoff,and keeps the runoff amount on slope with prophase soil crust at a relatively high level. On bare soil,the runoff and sediment yield on soil crusted slopes was 5. 27% higher and 27. 66%lower than that on slopes without soil crust,respectively. On slopes with soybean cover,the runoff and sediment yield on soil crusted slopes was 24. 81% higher and 14. 26% lower than that on slopes without soil crust,respectively. The crust has great influence on the processes of the runoff and sediment yield,which have significant difference between the slope with prophase soil crust and without soil crust. On the whole,the fluctuation of the process of runoff and sediment yield was smooth on slope with prophase soil crust,while the volatility of slope without soil crust fluctuates greatly. The presence of soybean cover increased the difference in runoff yield between slopes with and without soil crust,but reduced the difference in sediment yield. The effect of soybean on the differences of runoff and sediment yield between slopes with and without soil crust became stronger with the growth of soybean plants. Effects of thickness and coverage of soil crust on runoff and sediment yield were not significant. The influence of soil crust on the soil erosion varied greatly due to different soil types,terrain,rainfall,crops and other factors,which makes the problem become more complex. The research on the principle of the influence of soil crust on soil erosion is helpful for illustrating the progress of such effects,which provides reference for agricultural sectors to weigh the pros and cons in the real production.
出处 《中国水土保持科学》 CSCD 北大核心 2015年第3期16-23,共8页 Science of Soil and Water Conservation
基金 国家"973"重点基础研究项目"中国主要水蚀区土壤侵蚀过程调控研究"(2007CB407201-5) 国家自然科学基金重点项目"黄土高原生态建设的生态-水文过程响应机理研究"(41330858)
关键词 作物 土壤结皮 土壤侵蚀 坡耕地 黄土高原 soybean soil crust soil erosion slope farmland Loess Plateau
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