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Article: Use of boron as a tracer for recycled water in brackish aquifers

TitleUse of boron as a tracer for recycled water in brackish aquifers
Authors
KeywordsGround-Water Recharge
Hawaii
Isotopes
Tracers
Wastewater Management
Issue Date2006
PublisherAmerican Society of Civil Engineers. The Journal's web site is located at http://www.pubs.asce.org/journals/ee.html
Citation
Journal of Environmental Engineering, 2006, v. 132 n. 8, p. 862-871 How to Cite?
AbstractAn investigation was conducted to develop a simple method for tracking the fate and transport of recycled water following recharge into a shallow brackish aquifer (caprock aquifer) in a coastal area on the Island of Oahu, Hawaii. Several naturally present chemical constituents including the boron isotopic signature (δ 11B) were used to characterize each of the caprock aquifer source waters and the recycled water. Because of the influence of seawater, only δ 11B could be used to clearly distinguish the recycled water from the source waters and the caprock aquifer water. Estimates of the mixing ratios of source waters in the aquifer were made and a method was developed to determine the fraction of wastewater present in a brackish water sample recovered from a monitoring well during recharge operations without addition of a tracer. This method can be adapted to monitor any other brackish aquifer subjected to wastewater recharge. © 2006 ASCE.
Persistent Identifierhttp://hdl.handle.net/10722/91095
ISSN
2023 Impact Factor: 1.6
2023 SCImago Journal Rankings: 0.475
ISI Accession Number ID
References

 

DC FieldValueLanguage
dc.contributor.authorBabcock Jr, Ren_HK
dc.contributor.authorLin, Ben_HK
dc.contributor.authorSpengler, Sen_HK
dc.date.accessioned2010-09-17T10:12:57Z-
dc.date.available2010-09-17T10:12:57Z-
dc.date.issued2006en_HK
dc.identifier.citationJournal of Environmental Engineering, 2006, v. 132 n. 8, p. 862-871en_HK
dc.identifier.issn0733-9372en_HK
dc.identifier.urihttp://hdl.handle.net/10722/91095-
dc.description.abstractAn investigation was conducted to develop a simple method for tracking the fate and transport of recycled water following recharge into a shallow brackish aquifer (caprock aquifer) in a coastal area on the Island of Oahu, Hawaii. Several naturally present chemical constituents including the boron isotopic signature (δ 11B) were used to characterize each of the caprock aquifer source waters and the recycled water. Because of the influence of seawater, only δ 11B could be used to clearly distinguish the recycled water from the source waters and the caprock aquifer water. Estimates of the mixing ratios of source waters in the aquifer were made and a method was developed to determine the fraction of wastewater present in a brackish water sample recovered from a monitoring well during recharge operations without addition of a tracer. This method can be adapted to monitor any other brackish aquifer subjected to wastewater recharge. © 2006 ASCE.en_HK
dc.languageengen_HK
dc.publisherAmerican Society of Civil Engineers. The Journal's web site is located at http://www.pubs.asce.org/journals/ee.htmlen_HK
dc.relation.ispartofJournal of Environmental Engineeringen_HK
dc.subjectGround-Water Rechargeen_HK
dc.subjectHawaiien_HK
dc.subjectIsotopesen_HK
dc.subjectTracersen_HK
dc.subjectWastewater Managementen_HK
dc.titleUse of boron as a tracer for recycled water in brackish aquifersen_HK
dc.typeArticleen_HK
dc.identifier.emailLin, B:blin@hku.hken_HK
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.doi10.1061/(ASCE)0733-9372(2006)132:8(862)en_HK
dc.identifier.scopuseid_2-s2.0-33746135147en_HK
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-33746135147&selection=ref&src=s&origin=recordpageen_HK
dc.identifier.volume132en_HK
dc.identifier.issue8en_HK
dc.identifier.spage862en_HK
dc.identifier.epage871en_HK
dc.identifier.isiWOS:000239076000005-
dc.identifier.issnl0733-9372-

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