1) soil condensate
土壤凝结水
1.
An overview on soil condensate in North of China
中国北方土壤凝结水研究综述
2.
Through the analysis of the data of soil condensate and the synchronous meteorological element from Hengshui Experimental Station,this paper discussed the annual and intraanual change laws of soil condensate volume and congealment number of days,figured out the multi-annual mean volume of condensed water and discovered the elements related to the generation of soil condensate.
通过对衡水实验站土壤凝结水和同步气象要素资料进行综合分析,探讨了凝结水量和凝结天数的年际及年内变化规律,求算出多年平均凝结量,找出了与土壤凝结水生成有密切关系的相关要素。
3.
The micro-meteorological conditions are advantageous for forming soil condensate in arid and semiarid regions in north China.
中国北方干旱半干旱地区的气象条件有利于土壤凝结水的形成。
2) soil capillary condensation water
土壤毛管凝结水
4) soil coagulant
土壤凝结剂
1.
The erosion-deposition characteristic of soil coagulant sand-barrier with different concentration and size treatment was measured under wind tunnel test and field test.
对不同浓度和规格的土壤凝结剂沙障进行了风洞模拟实验和野外固结实验,实验结果表明:抗风蚀强度以40%浓度处理的固沙模型最强,20%最弱,但30%浓度防风蚀效果较为实用。
5) soil cohesion
土壤凝结性
6) soil coagulant sand barrier
土壤凝结剂沙障
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