初始含水量 meaning in Chinese
initial moisture content
Examples
- Taking the unsarurated loess soil sample , the water content distribution of the soil with various density and moisture content is tested in various thermal gradients
分别对不同温度梯度、不同密实度、不同初始含水量的土样进行试验，测定了各个土样中含水量的分布。 - The results indicate that the inial soil water conten t and the manner of water supply affect the dispersion - coefficient deeply , but the manner of fertilizer supply does not affect it
研究结果表明：土壤初始含水量、灌水方式对非饱和土壤水动力弥散系数影响大，而加肥方式对土壤水动力弥散系数影响小。 - Using the convective - dispersive equation and based on labo ratory exp eriment , the hydrodynamic dispersion coefficient of unsaturated soil is determi n ed under different inial soil water content , different manner of water infiltra t ion and fertilizer supply
用非饱和土壤水动力弥散方程及其解析解，在室内试验的基础上，研究了非饱和土壤在不同初始含水量、不同入渗方式及不同加肥方式下的水动力弥散系数。 - The results showed that the lower initial soil moisture content was , the less infiltration occurred and wetting front moved slowly , and soil salt were leached more efficiently . at the same time , salt reduced in the top soil and salt accumulated at the wetting front
通过对土壤初始含水量下土壤水盐运移规律室内模拟试验研究，发现随着土壤初始含水量的增加，相同入渗历时内的累积入渗量和湿润锋都在增加。 - Abstract : using the convective - dispersive equation and based on labo ratory exp eriment , the hydrodynamic dispersion coefficient of unsaturated soil is determi n ed under different inial soil water content , different manner of water infiltra t ion and fertilizer supply
文摘:用非饱和土壤水动力弥散方程及其解析解，在室内试验的基础上，研究了非饱和土壤在不同初始含水量、不同入渗方式及不同加肥方式下的水动力弥散系数。