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1)  soil hydrology
土壤水文
1.
<Abstrcat>The soil hydrology-physical properties of the soils adret and ubac of the forest was studied, through two-year observation(2003~2004) and comparision in the artificial forest of Cinnamomum camphora(L.
 对樟树人工林林地不同坡向阳坡和阴坡的土壤水文-物理性质进行为期两年的观测和对比分析。
2.
The diversity structure character and soil hydrology function of plant communities after conversion of cropland to forest project in loess and bedrock area ecotone was researched by using restoration ecology,forest hydrology,forest management principles and method.
2、植物群落演替过程中林地土壤水文特征(1)植物群落顺向演替过程中,土壤容重逐渐减小随着植物群落的顺向演替,植物群落的土壤容重逐渐减小,各个演替阶段植物群落的土壤容重均小于演替的初始阶段(退耕地阶段)。
2)  hydropedology
水文土壤学
1.
Advances in theory of hydropedology and its applications;
水文土壤学理论及其应用研究进展
3)  vadose zone hydrology
土壤水文学
1.
Recent advances in pore-scale network modeling in vadose zone hydrology;
孔隙网络模型在土壤水文学中的应用研究进展
4)  soil hydrology effect
土壤水文效应
1.
The result shows:(1)The water holding capacity of sub-alpine shrub meadow soil is best and aerate well and then forest gray-brown soil with best aeration, chestnut soil has little water holding capacity and bad aeration;(2)The index of soil hydrology effect changes with s.
通过测定国家重点野外科学观测试验站———祁连山森林生态站排露沟流域土壤水分物理性质,研究其水文效应表明:(1)亚高山灌丛草甸土持水能力最强、通气状况良好,山地森林灰褐土持水能力次之、通气状况最好,山地栗钙土持水能力较差、通气不良;(2)土壤水文效应随深度而变化,变化幅度亚高山灌丛草甸土>山地森林灰褐土>山地栗钙土;(3)单位土壤水文效应亚高山灌丛草甸土>山地森林灰褐土>山地栗钙土;(4)土壤水文效应大小除受本身的性质决定外,还受其厚度影响,亚高山灌丛草甸土各项指标均高于其它土壤类型,由于其处于较高海拔土层薄,总的水文效应指标除自然贮水量外反而比山地森林灰褐土和山地栗钙土低。
5)  soil hydrological processes
土壤水文过程
1.
This paper synthetically analyzed the regulation effect of MC on soil hydrological processes such as precipitation penetration, soil water redistribution and surface evaporation, through a series of field ecological investigation on MC, experimental analysis on MC s hydrological properties and soil hydrodynamics experiment under simulated precipitation, as well as dynamic monitoring.
生物结皮的土壤水文过程一直是学术界比较关注的争议性问题。
6)  soil hydrophysics
土壤水文物理学
补充资料:土壤水分运动基本方程(见土壤水运动)


土壤水分运动基本方程(见土壤水运动)


turang shuifen yundong iiben土壤水分运动基本方程fangeheng见土壤水运动。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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