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1)  erratic subsoil
不均一土壤
2)  nonuniform soil
不均匀土壤
3)  spatial soil evaporation variability
土壤蒸发空间不均匀性
4)  Uniform Soil
均匀土壤
1.
From the basic concept of grounding grid resistance, a full analysis of the measures and effect of decreasing the grounding grid resistance is performed in non uniform soils condition.
该文从地网接地电阻的物理本质出发 ,考虑不均匀土壤情况 ,对地网接地电阻降低措施及效果进行了分析和讨论。
2.
Reference resistance and assistant resistance in the formula are ground resistances of grids in uniform soil.
计算式中包含的参考电阻和辅助电阻都是均匀土壤中地网接地电阻,这两个接地电阻可用IEEE标准或中国电力行业标准的推荐公式代替。
5)  homogeneous soil
均质土壤
1.
Based on solutes transport and diffusion equation, and with taking the liquid saturation state in impermeable stratum in homogeneous soil and lots of saturated solutes (e.
从溶质扩散方程出发 ,针对不透水层上均质土壤的液体饱和状态 ,在顶层含有大量饱和溶质 (如养分等 )维持着扩散的条件下 ,进行严密的数学推证 ,给出均质土壤中溶质浓度分布的解析解 ,并分析了解的合理性 ,讨论了解的正确性。
2.
In this article, starting from solute′s transport and diffusion equation, aiming at the saturation state of liquid in homogeneous soil of impermeable stratum and on the condition that lots of saturated solute (e.
从溶质输移扩散方程出发 ,针对强透水层上均质土壤的液体饱和状态 ,在顶层含有大量饱和溶质 (如养分等 )维持着渗透扩散的条件下 ,进行严密的数学推证 ,给出均质土壤中溶质浓度分布的解析解。
3.
This paper was supported by Project about Colleges and Universities Key Laboratory Visited Scholar Plan in shannxi province,Which focus on the infiltration law with homogeneous soil and layered structure soil of the three typical soils (Xifeng soil of Gansu province,Yulin soil of Shannxi province and Xinjiang sand soil )in the area of Northwestern China.
本文结合陕西省重点实验室访问学者专项计划项目,针对西北地区三种典型土壤(甘肃西峰土、陕西榆林土、新疆沙土)的特点开展有关均质土壤和层状结构土壤入渗规律的研究。
6)  general soil
一般土壤
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。
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