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土壤大孔隙对坡地产汇流和溶质运移影响研究

Analysis of Effect of Soil Macropore on Slope Runoff Yield and Concentration and Solute Transport

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【作者】 张小娜冯杰刘方贵张超

【Author】 ZHANG Xiaona1,2 FENG Jie2,3 LIU Fanggui4 ZHANG Chao1,2(1.Key Laboratory of Hydrology-water Resources and Hydraulic Engineering,Hohai University,Nanjing 210098,China;2.College of Water Resources and Hydrology,Hohai University,Nanjing 210098,China;3.Water Resources Research Institute,China Institute of Water Resources and Hydropower Research,Beijing 100044,China;4.School of Civil Engineering,Guangxi University,Nanning 530004,China)

【机构】 河海大学水文水资源与水利工程科学国家重点实验室河海大学水文水资源学院中国水利水电科学研究院水资源所广西大学土木建筑工程学院

【摘要】 以室内土槽为平台,采用人工模拟降雨实验探讨了有无大孔隙土槽中土壤含水量、地面径流、壤中流、地下径流及溶质运移的变化。结果表明,相对于无大孔隙土槽,含有大孔隙的土槽中各层土壤含水量增加较快、增幅较大、峰现时刻较早、地面径流量较小、壤中流和地下径流量较大、地面径流中溴离子浓度较低、铵根离子浓度较高、硝酸根离子浓度对比变化较复杂、地下径流中三种离子浓度较高,且变幅较大。

【Abstract】 Based on indoor soil tank experiment and the artificial rainfall simulation,the variations of soil moisture,surface runoff,interflow,underflow runoff and solute transport in macropore and nonmacropore soil tank are analyzed.The study shows that compared to non-macropore soil tank,the soil water content in each layer increases faster;the increasing extent is bigger;flow apex appears earlier;the runoff amount of surface is less;the runoff amount of interflow and underflow are bigger in macropore soil tank.The results also indicated that in macropore soil tank,the concentration of Br-in surface runoff is lower;the concentration NH+4 in the surface runoff is higher;and the change of the concentration of NO-3 is much more complex;and these three kinds of ion concentrations in underflow runoff are higher and the increasing extends are bigger.

【基金】 国家自然科学基金资助项目(50609005);教育部博士点专项科研基金资助项目(20050294002);霍英东青年教师基金资助项目(101075)
  • 【文献出处】 水电能源科学 ,Water Resources and Power , 编辑部邮箱 ,2009年01期
  • 【分类号】S153
  • 【被引频次】7
  • 【下载频次】361
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