Search: L773:1435 0157 OR L773:1431 2174
> (2010-2014) >
Understanding the e...
Understanding the effect of single fracture heterogeneity from single well injection withdrawal (SWIW) tests
-
- Larsson, Martin, 1980- (author)
- Swedish University of Agricultural Sciences,Sveriges lantbruksuniversitet,Uppsala universitet,Luft-, vatten- och landskapslära,Institutionen för vatten och miljö,Department of Aquatic Sciences and Assessment,Uppsala University
-
- Doughty, Christine (author)
- Lawrence Berkeley National Laboratory, CA, USA
-
- Tsang, Chin-Fu (author)
- Uppsala universitet,Luft-, vatten- och landskapslära
-
show more...
-
- Niemi, Auli (author)
- Uppsala universitet,Institutionen för geovetenskaper
-
show less...
-
(creator_code:org_t)
-
- 2013-05-07
- 2013
- English.
-
In: Hydrogeology Journal. - New York : Springer-Verlag New York. - 1431-2174 .- 1435-0157. ; 21:8, s. 1691-1700
- Related links:
-
https://urn.kb.se/re...
-
show more...
-
https://doi.org/10.1...
-
https://res.slu.se/i...
-
show less...
Abstract
Subject headings
Close
- The single well injection withdrawal (SWIW) tracer test on a fracture or fracture zone is a method used to estimate its tracer retardation properties. In this study, the effects of single fracture aperture heterogeneity on SWIW test tracer breakthrough curves are examined by numerical modelling. The effects of the matrix diffusion and sorption is accounted for by using a particle tracking method through the addition of a time delay added to the advective transport time. For a given diffusion and sorption property value (Pm) and for a heterogeneous fracture, the peak concentration is larger compared to a homogeneous fracture. The cumulative breakthrough curve for a heterogeneous fracture is similar to that for a homogeneous fracture and a less sorptive/diffusive tracer. It is demonstrated that the fracture area that meets the flowing water, the so-called specific flow-wetted surface (sFWS) of the fracture, can be determined by comparing the observed breakthrough curve for a heterogeneous fracture with that for a homogeneous fracture. SWIW tests are also simulated with a regional pressure gradient present. The results point to the possibility of distinguishing the effect of the regional pressure gradient from that of diffusion through the use of multiple tracers with different Pm-values.
Subject headings
- NATURVETENSKAP -- Geovetenskap och miljövetenskap -- Oceanografi, hydrologi och vattenresurser (hsv//swe)
- NATURAL SCIENCES -- Earth and Related Environmental Sciences -- Oceanography, Hydrology and Water Resources (hsv//eng)
- NATURVETENSKAP -- Geovetenskap och miljövetenskap -- Geologi (hsv//swe)
- NATURAL SCIENCES -- Earth and Related Environmental Sciences -- Geology (hsv//eng)
Keyword
- tracer test
- SWIW test
- flow channelling
- flow-wetted surface
- fractured rock
- aperture heterogeneity
- Hydrology
- Hydrologi
Publication and Content Type
- ref (subject category)
- art (subject category)
Find in a library
To the university's database