1) soil saturated hydraulic conductivity(Ks)
饱和导水率Ks
2) Soil saturated hydraulic conductivity
饱和导水率
1.
Effect of spatial variability of surface soil saturated hydraulic conductivity on water drainage at field scale;
表层土壤饱和导水率的空间变异对农田水分渗漏的影响
2.
In addition the infection factors of the soil saturated hydraulic conductivities have been studied,which includes bulk density,soil saturated hydraulic conductivity,soil texture,soil structure coefficient,soil aggregation,soil porosities and the organic matter capacity.
主要研究了太湖地区3种主要水稻土(白土、黄泥土和乌栅土)的原状土和扰动土的饱和导水率,并分析了土壤的有机质含量、土壤质地、土壤容重、土壤团聚度、土壤结构系数等土壤基本性质对土壤饱和导水率的影响。
3.
The soil saturated hydraulic conductivity in different vegetation degeneration type and its influential factors in southwest karst region of China were studied.
通过对西南喀斯特地区典型土壤的饱和导水率的分析,研究了喀斯特地区不同植被退化类型下土壤的饱和导水率及其影响因素。
3) saturated hydraulic conductivity
饱和导水率
1.
Preliminary study on the saturated hydraulic conductivity of brown forest soil in Yantai;
烟台棕壤土饱和导水率的初步研究
2.
Changes of topsoil bulk density and saturated hydraulic conductivity under infiltration condition of water storage pit
蓄水坑入渗表层土壤体积质量和饱和导水率的变化
3.
The results show that the range of the undisturbed soil saturated hydraulic conductivity was between 44.
研究了湖南祁阳红壤地区旱地、水田的原状土和扰动土的饱和导水率,并分析了土壤的有机质含量、土壤质地、土壤容重等土壤基本性质对土壤饱和导水率的影响状况。
4) unsaturated conductivity
非饱和导水率
1.
The fractal approach is employed in derivation of a power law equation consistent with the empirical Campbell's Law to predict unsaturated conductivity of porous media.
多孔介质非饱和导水率是地下水污染预测与评价的重要参数。
5) saturated hydraulic conductivity
土壤饱和导水率
1.
Bulk density,saturated soil moisture content,saturated hydraulic conductivity,and soil water characteristics are essential soil parameters related to infiltration,evaporation,soil erosion and pollutants movement.
土壤容重、土壤饱和含水率和土壤饱和导水率,以及土壤水分特征曲线是与土壤水分入渗、蒸发、土壤侵蚀及污染物运移有关的重要的土壤水分参数。
6) soil saturated hydraulic conductivity
土壤饱和导水率
1.
Effects of grassland vegetation restoration on soil saturated hydraulic conductivity in mountain area of southern Ningxia
宁南山区草地植被恢复方式对土壤饱和导水率的影响
2.
Effects of vegetation rehabilitation on soil saturated hydraulic conductivity in Ziwuling Forest Area
子午岭植被恢复对土壤饱和导水率的影响
3.
The soil saturated hydraulic conductivity Ks of BSC and three types of control(no any crust,physical crust and removed BSC) were measured by tension infiltrometer to explore the effects of BSC on soil water infiltration and conductivity.
结果表明:与无结皮土壤相比,两种类型生物结皮均可极显著降低土壤饱和导水率;与去除生物结皮土壤相比,两种类型生物结皮对土壤饱和导水率的降低均不显著;与有物理结皮发育的土壤相比,地表生物结皮对土壤饱和导水率的降低不显著,而地上生物结皮对土壤饱和导水率的降低显著。
补充资料：bis[O-(1-methylethyl) carbonodithioato-kS,kS']-, (T-4)-Zinc
CAS：1000-90-4
分子式：C8H14O2S4Zn
分子质量：335.86
中文名称：O,O'-二异丙基双二硫代碳酸酯锌盐
英文名称：bis[O-(1-methylethyl) carbonodithioato-kS,kS']-, (T-4)-Zinc
Zinc O,O'-diisopropyl bis(dithiocarbonate)
s']- bis[o-(1-methylethyl) carbonodithioato- (beta-4)-zinc
Bis(O-isopropyldithiocarbonato)zinc
分子式：C8H14O2S4Zn
分子质量：335.86
中文名称：O,O'-二异丙基双二硫代碳酸酯锌盐
英文名称：bis[O-(1-methylethyl) carbonodithioato-kS,kS']-, (T-4)-Zinc
Zinc O,O'-diisopropyl bis(dithiocarbonate)
s']- bis[o-(1-methylethyl) carbonodithioato- (beta-4)-zinc
Bis(O-isopropyldithiocarbonato)zinc
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