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Scale dependency of fractional flow dimension in a fractured formation

dc.citation.epage2178en_US
dc.citation.issue7en_US
dc.citation.spage2165en_US
dc.citation.volume15en_US
dc.citation.woscount3
dc.contributor.authorChang, Y. -C.en_US
dc.contributor.authorYeh, H. -D.en_US
dc.contributor.authorLiang, K. -F.en_US
dc.contributor.authorKuo, M. -C. T.en_US
dc.contributor.department環境工程研究所zh_TW
dc.contributor.departmentInstitute of Environmental Engineeringen_US
dc.date.accessioned2014-12-08T15:37:44Z
dc.date.available2014-12-08T15:37:44Z
dc.date.issued2011en_US
dc.description.abstractThe flow dimensions of fractured media were usually predefined before the determination of the hydraulic parameters from the analysis of field data in the past. However, it would be improper to make assumption about the flow geometry of fractured media before site characterization because the hydraulic structures and flow paths are complex in the fractured media. An appropriate way to investigate the hydrodynamic behavior of a fracture system is to determine the flow dimension and aquifer parameters simultaneously. The objective of this study is to analyze a set of field data obtained from four observation wells during an 11-day hydraulic test at Chingshui geothermal field (CGF) in Taiwan in determining the hydrogeologic properties of the fractured formation. Based on the generalized radial flow (GRF) model and the optimization scheme, simulated annealing, an approach is therefore developed for the data analyses. The GRF model allows the flow dimension to be integer or fractional. We found that the fractional flow dimension of CGF increases near linearly with the distance between the pumping well and observation well, i.e. the flow dimension of CGF exhibits scale-dependent phenomenon. This study provides insights into interpretation of fracture flow at CGF and gives a reference for characterizing the hydrogeologic properties of fractured media.en_US
dc.identifier.doi10.5194/hess-15-2165-2011en_US
dc.identifier.issn1027-5606en_US
dc.identifier.journalHYDROLOGY AND EARTH SYSTEM SCIENCESen_US
dc.identifier.urihttp://dx.doi.org/10.5194/hess-15-2165-2011en_US
dc.identifier.urihttps://ir.lib.nycu.edu.tw/handle/11536/25938
dc.identifier.wosnumberWOS:000293268200008
dc.language.isoen_USen_US
dc.titleScale dependency of fractional flow dimension in a fractured formationen_US
dc.typeArticleen_US

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