dc.contributor.author |
Suzuki A. |
|
dc.contributor.author |
Niibori Y. |
|
dc.contributor.author |
Fomin S. |
|
dc.contributor.author |
Chugunov V. |
|
dc.contributor.author |
Hashida T. |
|
dc.date.accessioned |
2018-09-18T20:09:08Z |
|
dc.date.available |
2018-09-18T20:09:08Z |
|
dc.date.issued |
2015 |
|
dc.identifier.issn |
0375-6505 |
|
dc.identifier.uri |
https://dspace.kpfu.ru/xmlui/handle/net/137024 |
|
dc.description.abstract |
The fractional advection-dispersion equation (fADE) has been proposed to describe mass transport in a fractured reservoir. This study develops a finite discrete method to solve the fADE and tests its accuracy against analytical solutions. Tracer simulation uses a three-dimensional simulation of flow analysis (FRACSIM-3D). The solution to the fADE incorporating a spatial fractional derivative shows reasonable agreement with the tracer response from FRACSIM-3D, which shows highly anomalous behaviors such as a long tail. The prediction by the fADE model is reasonably similar to those of FRACSIM-3D irrespective of differing well intervals. © 2014 Elsevier Ltd. |
|
dc.relation.ispartofseries |
Geothermics |
|
dc.subject |
Fractal geometry |
|
dc.subject |
Fractional advection-dispersion |
|
dc.subject |
Fractured reservoir |
|
dc.subject |
Geothermal resources |
|
dc.subject |
Mass transport |
|
dc.subject |
Reinjection |
|
dc.title |
Fractional derivative-based tracer analysis method for the characterization of mass transport in fractured geothermal reservoirs |
|
dc.type |
Article |
|
dc.relation.ispartofseries-volume |
53 |
|
dc.collection |
Публикации сотрудников КФУ |
|
dc.relation.startpage |
125 |
|
dc.source.id |
SCOPUS03756505-2015-53-SID84902436913 |
|