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容重对土壤饱和水分运动参数的影响
引用本文:吕殿青,邵明安,刘春平.容重对土壤饱和水分运动参数的影响[J].水土保持学报,2006,20(3):154-157.
作者姓名:吕殿青  邵明安  刘春平
作者单位:1. 湖南师范大学,资源与环境科学学院,湖南,长沙,410081;中国科学院,水利部水土保持研究所,黄土高原土壤侵蚀与旱地农业国家重点实验室,陕西,杨陵,712100
2. 中国科学院地理科学与资源研究所,北京,100101;中国科学院,水利部水土保持研究所,黄土高原土壤侵蚀与旱地农业国家重点实验室,陕西,杨陵,712100
基金项目:中国科学院资助项目;中国科学院"百人计划"
摘    要:通过石蜡固定容重方法测定了4种土壤不同容重下的饱和重量含水量与饱和导水率,分析了容重对这两个土壤饱和水分运动参数的影响。结果表明:饱和重量含水量随容重的增加而减小,与容重成反比关系.饱和导水率随着容重的增加呈现幂函数形式递减。这些结果将为构建变容重土壤水分运动创新性理论体系提供适当的定量关系,有利于实现土壤水资源的合理利用。

关 键 词:容重  饱和含水量  饱和导水率
文章编号:1009-2242(2006)03-0154-04
收稿时间:2005-08-14
修稿时间:2005-08-14

Effect of Bulk Density on Soil Saturated Water Movement Parameters
LU Dian-qing,SHAO Ming-an,LIU Chun-ping.Effect of Bulk Density on Soil Saturated Water Movement Parameters[J].Journal of Soil and Water Conservation,2006,20(3):154-157.
Authors:LU Dian-qing  SHAO Ming-an  LIU Chun-ping
Institution:1. College of Resources and Environment Science, Hunan Normal University, Changsha 4100811; 2. Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101; 3. State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences, Yangling, Shaanxi 712100
Abstract:In the paper, saturated mass water content and saturated hydraulic conductivity for different hulk densities were measured by the method of fixing bulk density of olefin. Effects of bulk density on the two parameters were analyzed. The results showed that saturated mass water content decreased with the increment of bulk density and was inverse to bulk density. Saturated hydraulic conductivity tended to diminish in power function when bulk density increased. The researches will provide appropriate function quantificetionally to build innovative frame on water movement theory for the soil with changing bulk density. It is helpful to utilize soil water resource reasonably.
Keywords:bulk density  saturated water content  saturated hydraulic conductivity
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