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多维入渗理论在测量土壤水力特性参数中的应用

Application of Multi-Dimensional Infiltration Theory in the Measurement of Soil Hydraulic Property Parameters

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【作者】 张振华蔡焕杰杨润亚李庆志

【Author】 ZHANG Zhen-hua 1,2 ,CAI Huan-jie 1,YANG Run-ya 2,LI Qing-zhi 1,2 (1.College of Geography and Resources Management of Yantai Normal College,Yantai,Shandong 264025, China; 2.Key Lab of Arid agricultural Land and Water Engineering of Northwest Science and Technology University of Agriculture and Forestry,Yangling,Shaanxi,712100)

【机构】 烟台师范学院地理与资源管理学院教育部旱区农业水土工程重点实验室烟台师范学院地理与资源管理学院 山东烟台264025西北农林科技大学陕西杨凌712100山东烟台264025山东烟台264025

【摘要】 张力渗透仪是一种根据多维入渗原理进行土壤水分和溶质运移参数原位测量的仪器。介绍了张力渗透仪的测量原理和方法 ,并用盘源入渗试验得到人工填装土壤的饱和导水率 ,与土壤渗透仪测定的结果进行了比较 ,表明利用多维入渗理论所测数据与渗透仪测定结果接近 ,可用于土壤水分特性参数的测量。

【Abstract】 Tension infiltration meter is a kind of devices measuring soil moisture and solute movement parameters on the spot according to multi-dimensional infiltration theory. The measurement principle and methodology of tension infiltration meter are introduced,and the saturated conductivity of artificial-filled soil measured by the infiltration experiment in Panyuan is compared with that measured by soil infiltration meter. The result shows that the data obtained by multi-dimensional infiltration theory is very close to that measured by soil infiltration meter,thus the theory can be used in the measurement of soil hydraulic property parameters.

【基金】 国家高技术研究发展计划项目 (2 0 0 2AA2Z40 31 );烟台师范学院中青年自然科学基金项目的一部分
  • 【文献出处】 中国农村水利水电 ,China Rural Water and Hydropower , 编辑部邮箱 ,2004年05期
  • 【分类号】S152.7
  • 【被引频次】2
  • 【下载频次】154
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