Enhancement of wadi recharge using dams coupled with aquifer storage and recovery wells

dc.contributor.authorMissimer, Thomas M. M.
dc.contributor.authorMissimer, Thomas M. M.
dc.contributor.authorGuo, Weixing
dc.contributor.authorMaliva, Robert G.
dc.contributor.authorRosas, Jorge
dc.contributor.authorJadoon, Khan
dc.contributor.departmentBiological and Environmental Sciences and Engineering (BESE) Division
dc.contributor.departmentEnvironmental Science and Engineering Program
dc.contributor.departmentWater Desalination and Reuse Research Center (WDRC)
dc.contributor.institutionSchlumberger Water Services, 1567 Hayley Lane, Suite 202, Fort Myers, FL, United States
dc.contributor.institutionFlorida Gulf Coast University, U. A. Whitaker College of Engineering, 10501 FGCU Boulevard South, Fort Myers, FL, United States
dc.date.accessioned2015-08-03T11:55:36Z
dc.date.available2015-08-03T11:55:36Z
dc.date.issued2014-06-25
dc.date.published-online2014-06-25
dc.date.published-print2015-06
dc.description.abstractWadi channel recharge to the underlying alluvial aquifer is naturally limited by the flashy nature of flood events, evapotranspiration losses of water from the vadose zone, and aquifer heterogeneity, particularly low vertical hydraulic conductivity. Anthropogenic lowering of the water table in many wadi aquifers has also reduced the potential recharge by increasing the thickness of the vadose zone, causing interflow water loss from surface emergence and evaporation. A method to enhance recharge is to slow the flow within wadi channels by placement of dam structures, thereby ponding water and increasing the vertical head gradient to create a more rapid rate of infiltration and percolation. Effectiveness of wadi dams to enhance aquifer recharge reduces over time due to mud deposition within the reservoir caused by storm events. Up to 80 % of the water in old wadi reservoirs is lost to free-surface evaporation before infiltration and recharge can occur. One method to maintain or increase the rate of recharge is to convey clean water by gravity flow from the reservoir down-gradient to artificially recharge the aquifer using existing wells. This type of system is a low-cost and low-energy recharge method which could greatly enhance groundwater storage in wadi aquifers. Modeling results show that existing wells could store up to 1,000 m3/day under gravity-feed conditions and up to 3,900 m3/day with the shut-in of the well to produce a pressurized system. © 2014 Springer-Verlag Berlin Heidelberg.
dc.identifier.citationMissimer, T. M., Guo, W., Maliva, R. G., Rosas, J., & Jadoon, K. Z. (2014). Enhancement of wadi recharge using dams coupled with aquifer storage and recovery wells. Environmental Earth Sciences, 73(12), 7723–7731. doi:10.1007/s12665-014-3410-7
dc.identifier.doi10.1007/s12665-014-3410-7
dc.identifier.issn18666280
dc.identifier.journalEnvironmental Earth Sciences
dc.identifier.urihttp://hdl.handle.net/10754/563609
dc.publisherSpringer Nature
dc.subjectAquifer storage and recovery
dc.subjectDams
dc.subjectGroundwater modeling
dc.subjectRecharge
dc.subjectWadi aquifers
dc.titleEnhancement of wadi recharge using dams coupled with aquifer storage and recovery wells
dc.typeArticle
display.details.left<span><h5>Type</h5>Article<br><br><h5>Authors</h5><a href="https://repository.kaust.edu.sa/search?spc.sf=dc.date.issued&spc.sd=DESC&f.author=Missimer, Thomas M. M.,equals">Missimer, Thomas M. M.</a><br><a href="https://repository.kaust.edu.sa/search?spc.sf=dc.date.issued&spc.sd=DESC&f.author=Missimer, Thomas M. M.,equals">Missimer, Thomas M. M.</a><br><a href="https://repository.kaust.edu.sa/search?spc.sf=dc.date.issued&spc.sd=DESC&f.author=Guo, Weixing,equals">Guo, Weixing</a><br><a href="https://repository.kaust.edu.sa/search?spc.sf=dc.date.issued&spc.sd=DESC&f.author=Maliva, Robert G.,equals">Maliva, Robert G.</a><br><a href="https://repository.kaust.edu.sa/search?spc.sf=dc.date.issued&spc.sd=DESC&f.author=Rosas, Jorge,equals">Rosas, Jorge</a><br><a href="https://repository.kaust.edu.sa/search?spc.sf=dc.date.issued&spc.sd=DESC&f.author=Jadoon, Khan,equals">Jadoon, Khan</a><br><br><h5>KAUST Department</h5><a href="https://repository.kaust.edu.sa/search?spc.sf=dc.date.issued&spc.sd=DESC&f.department=Biological and Environmental Sciences and Engineering (BESE) Division,equals">Biological and Environmental Sciences and Engineering (BESE) Division</a><br><a href="https://repository.kaust.edu.sa/search?spc.sf=dc.date.issued&spc.sd=DESC&f.department=Environmental Science and Engineering Program,equals">Environmental Science and Engineering Program</a><br><a href="https://repository.kaust.edu.sa/search?spc.sf=dc.date.issued&spc.sd=DESC&f.department=Water Desalination and Reuse Research Center (WDRC),equals">Water Desalination and Reuse Research Center (WDRC)</a><br><br><h5>Online Publication Date</h5>2014-06-25<br><br><h5>Print Publication Date</h5>2015-06<br><br><h5>Date</h5>2014-06-25</span>
display.details.right<span><h5>Abstract</h5>Wadi channel recharge to the underlying alluvial aquifer is naturally limited by the flashy nature of flood events, evapotranspiration losses of water from the vadose zone, and aquifer heterogeneity, particularly low vertical hydraulic conductivity. Anthropogenic lowering of the water table in many wadi aquifers has also reduced the potential recharge by increasing the thickness of the vadose zone, causing interflow water loss from surface emergence and evaporation. A method to enhance recharge is to slow the flow within wadi channels by placement of dam structures, thereby ponding water and increasing the vertical head gradient to create a more rapid rate of infiltration and percolation. Effectiveness of wadi dams to enhance aquifer recharge reduces over time due to mud deposition within the reservoir caused by storm events. Up to 80 % of the water in old wadi reservoirs is lost to free-surface evaporation before infiltration and recharge can occur. One method to maintain or increase the rate of recharge is to convey clean water by gravity flow from the reservoir down-gradient to artificially recharge the aquifer using existing wells. This type of system is a low-cost and low-energy recharge method which could greatly enhance groundwater storage in wadi aquifers. Modeling results show that existing wells could store up to 1,000 m3/day under gravity-feed conditions and up to 3,900 m3/day with the shut-in of the well to produce a pressurized system. © 2014 Springer-Verlag Berlin Heidelberg.<br><br><h5>Citation</h5>Missimer, T. M., Guo, W., Maliva, R. G., Rosas, J., & Jadoon, K. Z. (2014). Enhancement of wadi recharge using dams coupled with aquifer storage and recovery wells. Environmental Earth Sciences, 73(12), 7723–7731. doi:10.1007/s12665-014-3410-7<br><br><h5>Publisher</h5><a href="https://repository.kaust.edu.sa/search?spc.sf=dc.date.issued&spc.sd=DESC&f.publisher=Springer Nature,equals">Springer Nature</a><br><br><h5>Journal</h5><a href="https://repository.kaust.edu.sa/search?spc.sf=dc.date.issued&spc.sd=DESC&f.journal=Environmental Earth Sciences,equals">Environmental Earth Sciences</a><br><br><h5>DOI</h5><a href="https://doi.org/10.1007/s12665-014-3410-7">10.1007/s12665-014-3410-7</a></span>
kaust.personMissimer, Thomas M.
kaust.personRosas, Jorge
kaust.personJadoon, Khan
orcid.authorMissimer, Thomas M. M.
orcid.authorMissimer, Thomas M. M.
orcid.authorGuo, Weixing
orcid.authorMaliva, Robert G.
orcid.authorRosas, Jorge
orcid.authorJadoon, Khan
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