1) Soil warming and drought
土壤暖干化
2) soil desiccation
土壤干化
1.
Approach to soil desiccation by vegetation and mechanism of its genesis;
植被作用下的土壤干化及其发生机制探讨
2.
Review of research on soil desiccation in the Loess Plateau;
黄土区土壤干化研究进展
3.
Owing to vegetation construction in the Loess Plateau,much attention has been paid to soil desiccation by vegetation for many years.
黄土高原普遍发生的植被作用下的土壤干化现象,从一个独特角度恰当反映了环境对植被的限制作用。
3) soil drying
土壤干化
1.
At present, soil drying is the sever problem in afforestation, which results in artificial forest not growing well and even withering.
当前植树造林面临的需要解决的重要问题是土壤干化。
4) soil drought
土壤干化
1.
The article synthetically expounds that soil drought of planted forest is found in drought,semi drought,arid and semi arid regions,The article emphatically presents different planted vegetations have different dynamics of soil water in different season and soil section.
该文综合阐述了不同的人工植被在干旱、半干旱、半湿润地区普遍存在着的土壤干化现象。
2.
The results show as follows:1) There is a possibility that the deep layer soil drought can be led by all kinds of artificial vegetation covers.
结果表明，各种人工植被均有导致深层土壤干化的可能。
5) soil desiccation
土壤干燥化
1.
Simulation of water productivity and soil desiccation effects of different planting density black locust forestlands on the Loess Plateau;
黄土高原不同密度刺槐(Robinia pseudoacia)林地水分生产力与土壤干燥化效应模拟
2.
Studies on soil desiccation of croplands in cinnamon soil region of Shanxi;
论山西褐土区农田土壤干燥化问题
3.
Effects of deep soil desiccation on artificial forestlands in different vegetation zones on the Loess Plateau of China;
黄土高原不同植被类型区人工林地深层土壤干燥化效应
6) the soil dry layer
土壤干化层
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