作者: Mohammad Hossein Mohammadi , Mohammad Reza Neishabouri , Hosseingholi Rafahi
DOI: 10.1097/SS.0B013E3181998FA7
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摘要: AbstractSoil hydrodynamic dispersivity and therefore inert solute transport are largely determined by soil hydraulic properties. In short travel times or long distances, diffusion is not a significant process. Thus, in these cases, only the convection of fluid different pores determines break