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1)  conductivity and TDS
电导率和TDS
1.
Analyses of conductivity and TDS in runoff samples collected from May to August in the three hydrological stations at the headwaters of the rümqi River during 2003-2006 are presented in this paper.
利用2003—2006年冰川消融期(5-8月)对乌鲁木齐河源1号冰川、空冰斗和总控3个水文点逐日定时(14:00时)的径流及电导率和TDS监测资料,分析河源区不同下垫面流域径流电导率和TDS的差异特征及各影响因素的控制作用。
2)  pH and conductivity
pH和电导率
3)  pH level and conductivity
pH值和电导率
4)  conductivity-saturation model
电导率-饱和度模型
5)  Wiedemann-Franz ratio
威德曼-弗朗芝比(热导率和电导率之比)
6)  Soil saturated hydraulic conductivity
饱和导水率
1.
Effect of spatial variability of surface soil saturated hydraulic conductivity on water drainage at field scale;
表层土壤饱和导水率的空间变异对农田水分渗漏的影响
2.
In addition the infection factors of the soil saturated hydraulic conductivities have been studied,which includes bulk density,soil saturated hydraulic conductivity,soil texture,soil structure coefficient,soil aggregation,soil porosities and the organic matter capacity.
主要研究了太湖地区3种主要水稻土(白土、黄泥土和乌栅土)的原状土和扰动土的饱和导水率,并分析了土壤的有机质含量、土壤质地、土壤容重、土壤团聚度、土壤结构系数等土壤基本性质对土壤饱和导水率的影响。
3.
The soil saturated hydraulic conductivity in different vegetation degeneration type and its influential factors in southwest karst region of China were studied.
通过对西南喀斯特地区典型土壤的饱和导水率的分析,研究了喀斯特地区不同植被退化类型下土壤的饱和导水率及其影响因素。
补充资料:电导率(见电阻率)


电导率(见电阻率)
conductivity

d!日nd日O}已电导率(eonduetivity)见电阻率。
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