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書(shū)目名稱Groundwater Flow and Quality Modelling影響因子(影響力)




書(shū)目名稱Groundwater Flow and Quality Modelling影響因子(影響力)學(xué)科排名




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書(shū)目名稱Groundwater Flow and Quality Modelling讀者反饋




書(shū)目名稱Groundwater Flow and Quality Modelling讀者反饋學(xué)科排名

goodwill

細(xì)頸瓶

dermatomyositis

Basin-Scale Transport of Dissolved Species in Groundwateraquifer-scale analysis through probabilistic arguments developed for basin contaminant responses to rainfall pulses (Rinaldo and Marani, 1987). The class of models investigated is related to the law of mass conservation interpreted in the context of the probability theory. Under fairly general condi

壟斷

Variable Density Fluid Flow in the Brackish Transition Zone between Fresh and Saline Groundwaterands. Artificial recharge with infiltration ponds is applied since 1955 to increase the fresh water reservoir. At this moment experiments are carried out with infiltration wells for artificial recharge in the deep aquifers, where both fresh and saline water occurs. Most techniques available for mode

先鋒派

先鋒派

An Overview of Groundwater Modellingf saturated media. Soil scientists introduced unsaturated flow concepts to modelling. Concern about groundwater quality led to the simulation of contaminant transport, beginning with problems of salt-water intrusion. Modelling multiphase flow, particularly the flow of hydrocarbons, water and air is

陶器

Incorporating Assurance into Groundwater Quality Management Modelsough there are many origins of model prediction uncertainty, model misspecification represents a significant one. Two types of model misspecification have been addressed. First is inadequate description of spatial variability of hydraulic conductivities. The latest approach has been to develop robus

Scintigraphy

Lumbar-Spine

New Method for Diffusive Transportion of Herrera’s algebraic theory of numerical methods [2–7]. This approach has been developed for general linear operators. Within the algebraic theory, careful choice of the weighting functions in a weak form statement of the problem leads to a numerical approximation that inherently accommodates