地下水水头的英文

• underground water head

• "地下水"英文翻译    groundwater; underground wat ...
• "水头"英文翻译    waterhead; head; flood peak
• "地下水水井" 英文翻译 :    groundwater well
• "地下水水库" 英文翻译 :    groundwater reservoir
• "地下水水面" 英文翻译 :    groundwater level; phreatic water level
• "地下水水位" 英文翻译 :    ground water level; groundwater level; groundwater table; phreatic water level; water level， phreatic
• "地下水水源" 英文翻译 :    groundwater source
• "地下水水质" 英文翻译 :    groundwater quality; quality of ground water; quality of groundwater; qualityofgroundwater
• "地下水水稻土" 英文翻译 :    ground water paddy soil
• "地下水水力学" 英文翻译 :    ground water hydraulics; groundwater hydraulics
• "地下水水文学" 英文翻译 :    geohydrology; ground water hydrology; groundwater hydrology; hydrology of groundwater
• "地下水水质图" 英文翻译 :    groundwater quality map
• "取地下水水样" 英文翻译 :    groundwater sampling
• "地下水头高程" 英文翻译 :    groundwater head level
• "地下水坡度（地下水水面坡度）" 英文翻译 :    hydraulic gradient of groundwater
• "地下水水化学图" 英文翻译 :    groundwater chemical map
• "地下水水位下降" 英文翻译 :    water table depression
• "地下水水位泄降" 英文翻译 :    groundwater drawdown
• "地下水水位增高" 英文翻译 :    increase in groundwater level
• "地下水水文工作者" 英文翻译 :    groundwater hydrologist
• "地下水水文因素" 英文翻译 :    groundwater hydrological factor
• "地下水水压测试" 英文翻译 :    groundwater pressure measurement
• "地下水水质监测" 英文翻译 :    ground water monitoring; groundwater quality monitoring
• "地下水水质模拟" 英文翻译 :    groundwater quality modeling
• "地下水水质模型" 英文翻译 :    groundwater quality model

• Impacts of storativity and porosity on the head potential fluctuation are investigated in this paper
  本文也同时检查饱和土壤储水系数及孔隙率对地下水水头扰动的影响。
• It is found , in one - dimensional subsurface flows , that porosity and storativity play an important role in the propagation of the head potential fluctuation
  由研究发现，一维地下水层中，受扰动地下水水头的传递快慢受饱和土壤储水系数及有效孔隙率的影响。
• ( 8 ) as for the runnel which is located at a karst zone with a high water level , external water load is the main one , and rock pressure is secondary
  门）在岩溶富水区隧道地下水水头较大时，外水荷载是衬砌结构的主要荷载，围岩压力相对来说是次要荷载。
• In addition , an asymptotic behavior of the head potential fluctuation is not reached until the head propagation travels more than three - fourths of the total length of the aquifer
  此外，由地下水水头扰动量传递特性发现，当传递距离超过0 . 75倍全长，此时传递之受扰动地下水水头愈趋近于渐近行为。
• Visual modflow computer code was selected to simulate heads distribution , calculate the zone budgets of the area , evaluate the effect of external stresses on the groundwater head , to determine how much water would be diverted from the river as the result of pumping and to demonstrate how the groundwater model can be used as a comparative technique to formulate a new approach for the quantitative groundwater vulnerability assessment in order to optimize utilization of the resource
  在分析河床沉积物渗透性对模型结果的影响时，采用了实际野外水文地质条件而不像前人所采用的假想模型。本论文用visualmodflow建立数值模型模拟预测了地下水水头分布，计算区域的水均衡，分析源汇项对地下水水位的影响。在此基础上进行了全区的地下水脆弱性评价，为地下水资源的合理开发利用提供依据。