1) soil solute
土壤溶质
1.
According to the research results for the interacting depth of rainfallrunoffsoil solute at home and abroad,the various methods for calculation of the interacting depth were compared based on the experimental data in laboratory.
在对国内外有关降雨-径流-土壤溶质相互作用深度研究成果综合分析的基础上,利用试验资料对各种模式进行比较分析。
2.
The physical processes of soil solute transfer with runoff and their features were analyzed based on the summation of research results at home and abroad.
土壤溶质随地表径流迁移是一个复杂的过程,受到多种因素的影响。
2) soil solute transport
土壤溶质运移
1.
Under certain soil texture, bulk density and water content of soil, moving time and distance of soil solute were regarded as the main parameters on soil solute transport.
在土壤质地、土壤容重和含水量一定的情况下 ,把土壤溶质运移时间和运移距离看作影响土壤溶质运移的主要参数 ,建立2个输入单元和 1个输出单元的三层BP网络 ,对一维垂直土柱Cd2 + 的穿透试验进行了模拟和预测。
2.
Nutrient migration and soil salinisation are the two major concerns in the research of soil solute transport.
土壤养分运移和土壤次生盐碱化都是土壤溶质运移领域研究的主要内容,而且土壤养分运移研究起源于土壤水盐运动的研究理论。
3.
Based on the review of national and international research results of soil solute transport and saline water use, both theoretical analysis and laboratory experiments were conducted to study infiltration of water and solute transport in layered soils, automatic measurement of soil water and solute transport parameters , and safe use of slightly saline water.
本文在结合国内外土壤溶质运移理论与微咸水利用试验研究成果的基础上,采取了理论分析与室内试验结合的方法,对层状土水分入渗和溶质运移特征、自动测定土壤水分、溶质运移参数的方法和微咸水安全利用进行了研究,取得了如下结论: 1。
4) loamy soil
壤质土壤
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。
参考词条