初始含水量的英文

• initial moisture content

• "初始"英文翻译    initial
• "含水量"英文翻译    moisture content; water cont ...
• "原始含水量" 英文翻译 :    initial moisture content
• "含水量" 英文翻译 :    [力学] moisture content; water content; primage (例如蒸汽、雾、云中的)◇含水量测定计 drimeter
• "持水量；含水量；含水率" 英文翻译 :    humidity ratio
• "安全含水量" 英文翻译 :    safety water content
• "饱和含水量" 英文翻译 :    saturated water content; saturation capacity; saturation moisture content
• "采出含水量" 英文翻译 :    producing cut
• "产液含水量" 英文翻译 :    produced water cut; producing water cut; production water cut
• "单位含水量" 英文翻译 :    unit water content
• "等含水量线" 英文翻译 :    isohydron
• "地面含水量" 英文翻译 :    surface water cut
• "凋萎含水量" 英文翻译 :    wilting moisture content
• "废弃含水量" 英文翻译 :    abandonment water cut
• "分层含水量" 英文翻译 :    separated layer water cut
• "分子含水量" 英文翻译 :    molecular moisture capacity
• "工地含水量" 英文翻译 :    field moisture equivalent
• "含水层水量" 英文翻译 :    aquifer yield
• "含水量；湿度" 英文翻译 :    water content; watercontent
• "含水量不足" 英文翻译 :    moisture deficit
• "含水量测定" 英文翻译 :    moisture content determination; moisture determination
• "含水量测井" 英文翻译 :    hydro log
• "含水量测量" 英文翻译 :    moisture determination
• "含水量过多" 英文翻译 :    hyperhydration
• "含水量盒" 英文翻译 :    moisture can

• 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。
• If the soil water content is gradually added from very little value , the value of water content gradient resulted from temperature gradient first is lower , then bigger and finally lower . based on the test data , a linear regression equation about temperature and water content is got . after deciding the temperature and moisture distribution of the soil samples , the problem of coupled thermal and moisture is discussed , the temperature distributions show that the heat - conducting coefficient is related to the density and water content
  由温度场的分布可以得到：在温度梯度的作用下，导热系数是变化的，而导热系数沿长度方向的变化，使得稳态温度场沿长度方向成非线性分布；密实度对温度场分布的影响是干密度越大导热系数越大；初始含水量对温度场分布的影响是含水量增大，导热系数也增大，达到最大值后，含水量增加导热系数反而减少，含水量对温度场的分布有显著的影响。
• Under subsurface drip irrigation , soil wetted front movement when higher soil initial moisture content was quicker than that of when it is lower , so did the supplied water pressure and soil bulk density . the wetted front movement of clay loam was clearly slow than that of sandy soil , especially in the larger soil bulk density
  地下滴灌条件下，初始含水量较高的土柱，湿润锋运移速度快于含水量较低的；在较高的供水压力条件下，各个方向的湿润锋运移都比低水头情况下的快；容重越大的土柱湿润锋运移速度越缓慢。
• ( 3 ) when evaporation was stopped during the process of soil water redistribution , soil water would move downslope by gravity . when evaporation was in process , due to low initial water content , most infiltrated water from small intensity and amount of rainfall would be consumed by intensive evapotranspiration during rainy season , and lateral downslope unsaturated flow seldom took place . however , soil water would move downslope by gravitational and matric potential gradients after continuous rainfall
  ( 3 )在防止蒸发条件下，再分布过程中，土壤水分在重力的作用下有沿坡向下运移的趋势；在蒸发条件下，由于初始含水量一般较低，雨季量小且分散的降雨极易为强烈的蒸发蒸腾所消耗，侧向沿坡向下流难以发生，但在持续的降雨条件下，土壤水分在重力势和基质势梯度的作用下易沿坡向下运移。
• The rule about water flow in the unsaturated soil and the soil - water characteristic curve are described in this thesis in the first time step during the numerical simulation , the permeability coefficient is calculated according to the initial water content of the unsaturated soil , because of as shown in the soil - water characteristic curve has the hysteresis phenomenon
  阐述了非饱和土中水流动的基本规律和土水特征曲线。由于土水特征曲线具有滞后的特点，提出了根据初始含水量来确定数值模拟初始时步非饱和土的渗透系数。
• The main solutions in the paper are : 1 . the vaporization of soil water is suit to the dynamic equation as y = a + blnt , the coefficients in the equation are related to temperature and water content of soil , and the dynamic equation about vaporization including water and temperature and the is developed , which provide some new information for studying and applying dynamic including environmental factors
  土壤水分累积蒸发量符合elovich动力学方程y = a + blnt ，方程中系数与温度和土壤初始含水量有关， a 、 b值随土壤初始含水量和温度增高而增大，由此得到含温度因子或土壤湿度因子的土壤水分蒸发动力学方程，并建立了含水、热因子的土壤水分蒸发水热耦合效应动力学方程，为含环境影响因子动力学方程的研究和应用提供了新的信息。