土壤水流的英文

• soil water flow

• "非饱和区土壤水流量" 英文翻译 :    vadose-water discharge
• "土壤水" 英文翻译 :    holard; soil eater; soil moisture regime, soil water regime; soil moisture stress; soil moisture, soil water; soilwater; vadose water; water， soil
• "深层土壤水" 英文翻译 :    deep subsoil water
• "土壤水[分]蒸发" 英文翻译 :    soil water evaporation
• "土壤水带" 英文翻译 :    belt of soil moisture; belt of soil water; discrete film zone; discretefilm zone; soil water zone; soil-water belt; soilwaterzone; zone of soil water
• "土壤水动态" 英文翻译 :    soil water movement
• "土壤水分" 英文翻译 :    soil humidity; soil moisture content; soilmoisture
• "土壤水分带" 英文翻译 :    belt of soil water
• "土壤水观测" 英文翻译 :    soil－water observation
• "土壤水面" 英文翻译 :    soil water table
• "土壤水能态" 英文翻译 :    energy state of soil water
• "土壤水泥" 英文翻译 :    soil cement
• "土壤水平衡" 英文翻译 :    soil water balance
• "土壤水容量" 英文翻译 :    field (moisture) capacity
• "土壤水入渗" 英文翻译 :    soil water infiltration
• "土壤水渗漏" 英文翻译 :    percolation of soil water
• "土壤水生物" 英文翻译 :    edaphonekton
• "土壤水势" 英文翻译 :    soil water potential
• "土壤水文学" 英文翻译 :    pedohydrology
• "土壤水形态" 英文翻译 :    soil water form
• "土壤水质" 英文翻译 :    soil water quality
• "初始土壤水分" 英文翻译 :    initial soil moisture
• "土壤水[分]扩散率" 英文翻译 :    soil water diffusivity
• "土壤水[分]再分布" 英文翻译 :    soil water redistribution
• "土壤水量平衡" 英文翻译 :    soil moisture budget
• "土壤水扩散系数" 英文翻译 :    soil-water diffusivity

• Regard - ing the surface runoff mechanism , liang and xie 1 , 2 presented a new surface runoff parameterization which dynamically represents both the horton and dunne runoff generation mechanisms within within a model grid cell together with a consideration of the subgrid - scale het - erogeneity , which can be applied to not only humid regions but also droughty regions as well 3 , 4 . regard - ing the soil water movement , xie et al . 5 developed an unsaturated flow numerical model based on the finite element method , and xie et al . 6 presented another numerical model to compute soil moisture and water flow flux together by means of a mixed finite element method
  在地表径流方面,文献1 3发展了一种同时考虑蓄满超渗产流机制及次网格非均匀性的新的径流机制模型,并用其改进了陆面模式vic variable infiltration capacity中的径流计算,该模型既适用于湿润地区也适用于干旱地区4 .在土壤水模型方面,文献5采用有限元质量集中法发展了非饱和土壤水流的数值模型,文献6则采用混合有限元法建立了非饱和土壤水分含量和通量计算的数值模型