1) capillary water rise and distribution
毛管水分运动及分布
2) the behavior of capillary water movement
毛管水分运动特性
3) water movement
水分运动
1.
Numerical Simulation for 1-D Water Movement in Unsaturated Soil;
一维非饱和土壤水分运动的数值模拟
2.
Experimental study on water movement of latosol under drip irrigation;
滴灌条件下砖红壤水分运动试验研究
3.
Under different rainfall intensities,water movement in seashore saline soil was basically similar, and the whole process of water movement was divided into two phases,namely rapidly decreasing phase of water suction and slowly rising phase of water suction.
结果表明 :7,14和 2 8mm的雨量下 ,滨海盐渍土土壤剖面的水分运动规律基本相似 ,水分运动的整个过程可分为两个阶段 ,即入渗控制阶段和蒸发控制阶段。
4) water flow
水分运动
1.
The characteristic finite element method is applied to discretize the model of 1-Dwater flow in unsaturated soils with variable θ during infiltration and evaporation ,and the characteristic finte element model is obtained.
应用特征有限元法,对以含水率θ为因变量的一维非饱和土壤水分运动模型在入渗、蒸发条件下进行离散化,得到了该模型的特征有限元数值模型,所得数值模型形式简单、计算精度高、用时少,符合实际工作要求。
2.
Rock fragments in the soil may affect the soil structure and the tortuosity of water flow paths, which may further influence the hydrological process, soil water movement and its validity.
由于成土原因和人类活动,不同数量、不同种类的碎石覆盖表土和嵌入土壤以及碎石夹层经常存在,碎石的存在不仅会改变土壤的某些物理和化学性质,还会进而影响地表水文过程、土壤水分运动及有效性。
5) moisture movement
水分运动
1.
Hence,it is awfully necessitated to construct a hydrological model applicable to Hotan Oasis with which,the moisture movement mode can be easier to find and the precious water resour.
构建一个适用于和田绿洲的水文模型,借以搞清当地水分运动规律,合理配置有限的水资源--这已经成为绿洲可持续发展的迫切要求。
2.
In order to study the moisture movement in unsaturated zone,a improved finite element numerical method for solving Richard equation is built and compared with the results in presented literature.
为研究非饱和带土壤水分运动,对Richard方程的有限元求解方法进行了改进,改进后的算法可较为简便地处理边界条件,并与已有的求解方法进行对比验证;对V-G模型中的参数α和n对土壤重力释水和入渗过程的影响进行了敏感度分析。
补充资料：衡阳钢管厂φ108三辊轧管机轧制毛管
衡阳钢管厂φ108三辊轧管机轧制毛管
衡阳钢管厂事108三辊轧管机轧制毛管
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