1) agriconcentration
土壤渗透浓度
2) soil permeability
土壤渗透
1.
The soil permeability characteristics of waste rock hill is studied.
结果表明:相同排矸年限不同坡向土壤渗透速率差异较大,不同排矸年限间相同坡向土壤渗透速率的差异也十分显著。
2.
Four main vegetation types, which are Picea crassifolia,Sabina przewalskii,bushes and pastureland ,whose soil permeability function was analyzed from angle of its physics,capacity of water, storing water in it .
从土壤物理性质、蓄水量、贮水量等角度对祁连山苔藓云杉林、祁连圆柏林、亚高山灌丛林、牧坡草地 4种主要植被类型的土壤渗透功能进行分析 ,结果表明 :土壤的渗透功能主要由土壤非毛管孔隙度的质和量决定的 ,苔藓云杉林土壤非毛管孔隙度的质和量最好 ,它的渗透功能也最好 ;虽然亚高山灌丛林的渗透功能次之 ,但由于它自身的特点 ,蓄水性能最好 ,又加之面最大 ,因此 ,贮水量也最大。
3.
The soil permeability characteristics of shelter forest in silting coastal area is studied.
探讨了淤泥质海岸防护林土壤的渗透特性 ,指出同一林分土壤渗透速率差异较大 ,不同样地间土壤渗透速率的差异也十分显著。
3) soil infiltration
土壤渗透
1.
Experimental study on the soil infiltration characteristics at the area of the Three Gorges reservoir;
三峡库区土壤渗透特性实验研究
2.
Soil infiltration of stormwater runoff in residential quarter;
建筑小区雨水径流的土壤渗透净化
3.
In this paper a soil infiltration and recovery simulation model of bioretention trough was constructed by using evaporation,transpiration and gravity flow as the soil recovery mechanisms.
以蒸发蒸腾和重力流作为土壤渗透恢复机制,建立了生物滞留槽土壤渗透与恢复过程模拟模型。
4) Osmotic concentration
渗透浓度
1.
The change of salinity made osmotic concentration extremely significant difference,sodium and chloride concentrations significant difference, and potassium concentration no significant difference in hemolymph of Fenneropenaeus chinensis.
本文检验了环境因子和生物自身因子对中国明对虾渗透浓度和离子浓度的影响。
5) Osmolarity
[ɔzmə'læriti]
渗透浓度
1.
Calculation of Osmolarity and Tensility of Clinic Solutions;
临床常用溶液渗透浓度和张力的计算
6) Osmolality
[,ɔsmə'læliti]
渗透浓度
1.
Osmolality in the hemolyph of P.
试验观察了中国对虾脱壳活动，并探讨了脱壳和盐度突变对中国对虾血淋巴渗透浓度和离子浓度的影响。
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