水均衡 meaning in Chinese
hydrologic budget
hydrologicbudget
water balance
waterbalance
Examples
- Then , the results of bp are compared with that of rbf model and regional water equilibrium method . this tests the reliability of forecast results
并进行了rbf模型与区域水均衡法的检验与对比，进一步验证了预测结果的可靠性。 - The most important criteria that used to check the calibrated model are root mean square error ( rms ) , the mean absolute error normalized rms error , and mass balance
模型参数使用试错法识别，识别过程中最重要的指标是均方差、平均绝对误差、标准均方差和水均衡。 - Mining exploitation activities have imposed increasingly grave harm on social and ecological environment , including occupation of plowland , initiating geologic hazards , destroying water equilibrium , physiognomy and sights
摘要矿业开发活动对社会生态环境的危害越来越严重：占用耕地，诱发地质灾害，破坏水均衡，破坏地貌景观等。 - Take middle - east district of taipusi banner as study area in the paper , combining field observation test ( pumping test and field survey ) with indoor experiment ( granule analysis and organic matter analysis etc ) , based on the relationship between hydrological parameters and physical - chemistry characteristic parameters of formation , the variability of aquifer parameters and physical - chemistry parameters of unsaturated zone have been also analyzed . the aquifer system of the taipusi banner is identified and analyzed by using the internal and outside information . on the basis of real pumping of ground water , the water resources evaluated by the water balance method
本文以太仆寺旗中东部地区为研究区域，采用野外试验（抽水试验、实地调查）和室内实验（颗分、有机质等实验）相结合的方法，推求了研究区含水层系统的水文水利参数，在系统模拟含水层水理参数与岩性物理化学特征参数之间的关系基础上，进一步分析了含水层参数及其包气带的物理、化学特征参数的空间变化特征，并利用其内外部信息对太仆寺旗含水层系统进行了辩识与分析；以现状地下水开采量为依据，采用水均衡法评价了研究区水资源总量，并利用有限单元法来模拟分析验证。 - In analyzing the dynamic phenomenon in a groundwater for producing in type in different influence to take the foundation of the effect with characteristic and its environments , the influence mechanism for water matter activity to groundwater dynamic changes is studied , making use of theories the groundwater seepage flows and the water balance
在分析不同影响类型所产生的地下水动态的现象和特征及其环境负效应的基础上，利用地下水渗流和水均衡理论深入分析了水事活动对地下水动态的影响机理。