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地下水运动模拟
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  “地下水运动模拟”译为未确定词的双语例句
     In this paper, with the GIS as the main model piece, and with the Groundwater Modeling System(GMS) developed by the Ministry of Defence of the U S A and the surface subsidence modeling system (Compac) developed by D C Helm, S A Leak and others of the U S A being selected, the GIS and groundwater movement modeling and the surface subsidence modeling system integrated analysis and design were made.
     本文以GIS为主控模块,选择美国国防部开发的地下水运动模拟模型系统(GroundwaterModelingSys-tem简称GMS)和美国D.C.Helm、S.A.Leak等人开发的地面沉降模拟模型系统(Compac),进行苏锡常地区GIS与地下水运动模拟和地面沉降模拟模型系统集成分析和设计。
短句来源
     The author carries out the integrated analysis and design of GIS and groundwater movement modeling and ground subsidence modeling systems in the regions of Suzhou,Wuxi and Changzhou with GIS as the master control module and selects the Groundwater Modeling System(GMS)developed by U.S.Department of Defence and ground subsidence modeling system(Compac) developed by D. C. Helm and S.A.
     以GIS为主控模块,选择美国国防部开发的地下水运动模拟模型系统(GroundwaterModelingSystem简称GMS)和美国D.C.Helm等人开发的地面沉降模拟模型系统(Compac),进行苏锡常地区GIS与地下水运动模拟和地面沉降模拟模型系统集成分析和设计。
短句来源
     The GIS is applied to combine with FEFLOW,the special software modeling groundwater flow with finite element method,to model groundwater flow affected by vegetation in Sangong River basin,Xinjiang Autonomous Region,China.
     以流域水量均衡为基础,以植被变化对地下水的影响作为源汇项,建立了内陆河流域二维地下水运动模拟模型。 根据荒漠植被区的气候条件,依地下水埋深划分并合并植被变化方式为几种类型,以面状因子处理源汇项。
短句来源
  相似匹配句对
     Simulation of Moving Targets
     运动目标的模拟
短句来源
     GEOCHEMICAL MODELING OF GROUND WATER
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短句来源
     Groundwater Numerical Simulation Model for Shuishiying Area, Dalian
     大连水师营地区地下水运动的数值模拟
短句来源
     Numerical Simulation of Groundwater Around a Uranium Milling Dam
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     Numerical Simulation of Ship's Maneuvering Motion
     船舶操纵运动数值模拟
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The author carries out the integrated analysis and design of GIS and groundwater movement modeling and ground subsidence modeling systems in the regions of Suzhou,Wuxi and Changzhou with GIS as the master control module and selects the Groundwater Modeling System(GMS)developed by U.S.Department of Defence and ground subsidence modeling system(Compac) developed by D.C.Helm and S.A.Leak(Am).Based on the supply and need requirements of GIS,GMS and Compac...

The author carries out the integrated analysis and design of GIS and groundwater movement modeling and ground subsidence modeling systems in the regions of Suzhou,Wuxi and Changzhou with GIS as the master control module and selects the Groundwater Modeling System(GMS)developed by U.S.Department of Defence and ground subsidence modeling system(Compac) developed by D.C.Helm and S.A.Leak(Am).Based on the supply and need requirements of GIS,GMS and Compac concept models,the author analyses and explains the characteristics and design thinkings to the integrated system,and states the multi data compatibility,data analysis and treatment,integrated calculation and functions of visual and structured results of the integrated systme.

以GIS为主控模块,选择美国国防部开发的地下水运动模拟模型系统(GroundwaterModelingSystem简称GMS)和美国D.C.Helm等人开发的地面沉降模拟模型系统(Compac),进行苏锡常地区GIS与地下水运动模拟和地面沉降模拟模型系统集成分析和设计。从GIS、GMS和Compac概念模型供需要求,分析说明集成系统的特点和设计思路,且对集成系统的多种数据兼容性、数据分析处理及集成计算、结果可视化和构件化修改功能进行阐述。

In this paper, with the GIS as the main model piece, and with the Groundwater Modeling System(GMS) developed by the Ministry of Defence of the U S A and the surface subsidence modeling system (Compac) developed by D C Helm, S A Leak and others of the U S A being selected, the GIS and groundwater movement modeling and the surface subsidence modeling system integrated analysis and design were made. In accordance with the demand supply requirements of the GIS, GMS and Compac conceptual models, the characteristics...

In this paper, with the GIS as the main model piece, and with the Groundwater Modeling System(GMS) developed by the Ministry of Defence of the U S A and the surface subsidence modeling system (Compac) developed by D C Helm, S A Leak and others of the U S A being selected, the GIS and groundwater movement modeling and the surface subsidence modeling system integrated analysis and design were made. In accordance with the demand supply requirements of the GIS, GMS and Compac conceptual models, the characteristics and train of thoughts of design of the integrated system are analyzed and explained, the compatibility of various data of the integrated system, the analysis, processing of data and integrated calculation, the visibility of results and the revisin function are elucidated.

本文以GIS为主控模块,选择美国国防部开发的地下水运动模拟模型系统(GroundwaterModelingSys-tem简称GMS)和美国D.C.Helm、S.A.Leak等人开发的地面沉降模拟模型系统(Compac),进行苏锡常地区GIS与地下水运动模拟和地面沉降模拟模型系统集成分析和设计。从GIS、GMS和Compac概念模型供需要求,分析说明集成系统的特点和设计思路,且对集成系统的多种数据兼容性、数据分析处理及集成计算、结果可视化和构件化修改功能进行阐述。

The GIS is applied to combine with FEFLOW,the special software modeling groundwater flow with finite element method,to model groundwater flow affected by vegetation in Sangong River basin,Xinjiang Autonomous Region,China.The spatial variation of vegetation change is regarded as source/sink factors of groundwater.The result shows that the model successfully simulates the effect of vegetation with different types on groundwater table.It is indicated that the groundwater table of upper area of oasis will descend,but...

The GIS is applied to combine with FEFLOW,the special software modeling groundwater flow with finite element method,to model groundwater flow affected by vegetation in Sangong River basin,Xinjiang Autonomous Region,China.The spatial variation of vegetation change is regarded as source/sink factors of groundwater.The result shows that the model successfully simulates the effect of vegetation with different types on groundwater table.It is indicated that the groundwater table of upper area of oasis will descend,but in the lower area will rise continuously.This situation will result in the regression of vegetation in the upper area and salinization becomes more serious in lower area.

以流域水量均衡为基础,以植被变化对地下水的影响作为源汇项,建立了内陆河流域二维地下水运动模拟模型。根据荒漠植被区的气候条件,依地下水埋深划分并合并植被变化方式为几种类型,以面状因子处理源汇项。绿洲区的灌水、抽水等源汇因子对地下水影响最大,根据不同作物的灌溉制度详细计算随时间变化的源汇量。其他植被变化类型上的源汇因子相对次要,主要是有限的降水和凝结水入渗及蒸散,具体数量分配在某一时段。用GIS处理区域植被变化的空间数据,与专业计算地下水流的FEFLOW软件结合,模拟了植被变化对地下水位的影响。结果表明:扇缘带上部地下水位仍然保持下降,冲洪积平原地下水位继续上升的趋势;其结果将是扇缘带上部植被有趋于退化,冲洪积平原土壤盐化进一步发展的趋势。

 
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