Groundwater Contaminant Transport: Prediction Under Uncertainty, With Application to the MADE Transport Experiment
Transport of solutes in porous media at the laboratory scale is governed by an Advection Dispersion Equation (ADE). The advection is by the fluid velocity U and dispersion by DdL = UαdL, where the longitudinal dispersivity αdL is of the order of the pore size. Numerous data revealed that the longitu...
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Frontiers Media S.A.
2019-06-01
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| Series: | Frontiers in Environmental Science |
| Subjects: | |
| Online Access: | https://www.frontiersin.org/article/10.3389/fenvs.2019.00079/full |