1.
The Laboratorial Study and Academic Mathematics Model of a New Pore Water Pressure Instrument;
土壤孔隙水压力检测系统试验研究及关系模型建立
2.
Comparative Study on the Soil Water Retention Curve between Macroporous Soil and Homogeneous Soil
大孔隙土壤与均质土壤水分特征曲线比较研究
3.
The compression of the soil under the applied stresses would force some water out of the voids.
施加压力压缩土壤会使一些水从孔隙中排出。
4.
Study on mechanism of water and solute transport in soil with macropores;
水及溶质在有大孔隙的土壤中运移机制研究
5.
The Effect of the Infiltration Characteristics Under the Different Macropores' Depth in the soil
不同大孔隙深度对土壤水分入渗特性的影响
6.
A porous soil
多孔(透水)的土壤
7.
Computation and Observation of Pore Pressure in the Loam Core of Earth rockfili Dam at Bikou Hydropower Station
碧口水电站土石坝壤土心墙孔隙压力的计算与观测
8.
Ground water is the water that saturates the pores and cracks in soil and rock beneath the land surface.
地下水是充满在地面底下土壤与岩石的孔隙中的水。
9.
Research on Uncertainty of Macroporous Distribution and Characteristic Parameters of Soil Moisture of Paddy Field in Water-Saving Irrigation Condition;
节水灌溉稻田土壤大孔隙分布不确定性及持水特征参数研究
10.
soil lines of equal pore pressure
土内孔隙水压等同线
11.
"Some soils lack porosity, so that they' re hard to cultivate, slow to absorb water, and inclined to puddle. "
有的土壤孔隙少，所以耕作起来很费劲，吸收水分也慢，而且容易粘闭。
12.
Macropores Properties of Forest Soil and Its Influence on Water Infiltration in the upper Reaches of Minjiang River;
岷江上游森林土壤大孔隙特性与水分入渗性能研究
13.
Physical simulation experiments of effects of macropores on soil water infiltration characteristics
大孔隙对土壤水分入渗特性影响的物理模拟试验
14.
The total porosity and the aerate porosity decrease after the rain while the faster available porosity and the slow available porosity increase .
降雨后土壤的总孔隙度下降，通气孔隙下降较明显，同时速效孔隙和迟效孔隙增多。
15.
Gums and mucilages can reduce the size of some of the soli pores.
细菌胶和粘胶会使某些土壤的孔隙减
16.
Design and Realization for Network Model Reconstruction of Soil Pore
土壤孔隙网络模型的程序设计与实现
17.
We may have too large an internal surface area where the particles are too fine and the pore space may be filled up. Pore space depends on the size and arrangement of the particles.
如果土粒太小，土壤内表面积就会过大，致使土壤孔隙被阻塞。孔隙取决于土粒的大小与排列。
18.
Impacts of storativity and porosity on the head potential fluctuation are investigated in this paper.
本文也同时检查饱和土壤储水系数及孔隙率对地下水水头扰动的影响。