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dc.contributor.author | Chiba R. | |
dc.contributor.author | Fomin S. | |
dc.contributor.author | Chugunov V. | |
dc.contributor.author | Niibori Y. | |
dc.contributor.author | Hashida T. | |
dc.date.accessioned | 2018-09-18T20:28:03Z | |
dc.date.available | 2018-09-18T20:28:03Z | |
dc.date.issued | 2007 | |
dc.identifier.issn | 0094-243X | |
dc.identifier.uri | https://dspace.kpfu.ru/xmlui/handle/net/140191 | |
dc.description.abstract | A computer program, which enables us the calculation of the non-Fickian diffusion in a fractured porous media, has been developed. The conventional mathematical model of solute transport in a rock is based on the Fick's law. In general, rock masses contain a number of preexisting fractures. In the fractured porous media, the conventional model tends to predict smaller solute travel distance than that in the actual transport process. In contrast, the non-Fickian diffusion model, which is described as a fractional advection-dispersion equation, can provide realistic representation of actual fluid flow in the heterogeneous media. We provide a numerical solution of the fractional advection-dispersion equation by using implicit-finite difference method. The numerical results obtained for one dimensional fractional advection-dispersion equation using the computer program was shown to be in a good agreement with the analytical solution. © 2007 American Institute of Physics. | |
dc.relation.ispartofseries | AIP Conference Proceedings | |
dc.subject | Fractinal derivative | |
dc.subject | Non-Fickian diffusion | |
dc.subject | Numerical simulation | |
dc.subject | Solute transport | |
dc.title | Numerical simulation of non-fickian diffusion and advection in a fractured porous aquifer | |
dc.type | Conference Paper | |
dc.relation.ispartofseries-volume | 898 | |
dc.collection | Публикации сотрудников КФУ | |
dc.relation.startpage | 75 | |
dc.source.id | SCOPUS0094243X-2007-898-SID34248210735 |