Semi-analytical solutions for solute transport in fractured porous media using a strip source of finite width |
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| Institution: | 1. Computational Earth Science (EES-16), Earth and Environmental Sciences Division, Los Alamos National Laboratory, Los Alamos New Mexico, USA;2. Spanish National Research Council (IDAEA-CSIC), Barcelona, Spain;1. BRGM, D3E, NRE, Indo-French Center for Groundwater Research, Uppal Road, 500007 Hyderabad, India;2. OSUR, Géosciences Rennes, UMR6118 CNRS – Université de Rennes 1, Campus de Beaulieu, 35042 Rennes Cedex, France;3. Department of Geological Sciences, California State University Long Beach, Long Beach, California, 90840, United States;4. Indo-French Center for Groundwater Research, Uppal Road, 500007 Hyderabad, India;5. National Geophysical Research Institute, Indo-French Center for Groundwater Research, Uppal Road, 500007 Hyderabad, India;6. BRGM, D3E, NRE, 1039 rue de Pinville, 34000 Montpellier, France |
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| Abstract: | Transient and steady-state analytical solutions are derived to investigate solute transport in a fractured porous medium consisting of evenly spaced, parallel discrete fractures. The solutions incorporate a finite width strip source, longitudinal and transverse dispersion in the fractures, source decay, aqueous phase decay, one-dimensional diffusion into the matrix, sorption to fracture walls, and sorption within the matrix. The solutions are derived using Laplace and Fourier transforms, and inverted by interchanging the order of integration and utilizing a numerical Laplace inversion algorithm. The solutions are verified for simplified cases by comparison to solutions derived by Batu Batu V. A generalized two-dimensional analytical solution for hydrodynamic dispersion in bounded media with the first-type condition at the source. Wat Resour Res 1989;25(6):1125] and Sudicky and Frind Sudicky EA, Frind EO. Contaminant transport in fractured porous media: analytical solutions for a system of parallel fractures. Wat Resour Res 1982;18(6):1634]. The application of the solutions to a fractured sandstone demonstrates that narrower source widths and larger values of transverse dispersivity both lead to lower downstream concentrations in the fractures and shorter steady-state plumes. The incorporation of aqueous phase decay and source concentration decay both lead to lower concentrations and shorter plumes, with even moderate amounts of decay significantly shortening the persistence of contamination. |
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