SwePub
Sök i LIBRIS databas

  Extended search

L773:1435 0157 OR L773:1431 2174
 

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
  • Journal article (peer-reviewed)
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

Search outside SwePub

Kungliga biblioteket hanterar dina personuppgifter i enlighet med EU:s dataskyddsförordning (2018), GDPR. Läs mer om hur det funkar här.
Så här hanterar KB dina uppgifter vid användning av denna tjänst.

 
pil uppåt Close

Copy and save the link in order to return to this view