Isotope signatures and hydrochemistry as tools in assessing groundwater occurrence and dynamics in a coastal arid aquifer

dc.creatorNancy Edith Ornelas Soto
dc.creatorArturo Hernández Antonio
dc.creatorJurgen Mahlknecht
dc.date2016
dc.date.accessioned2018-10-19T14:22:09Z
dc.date.available2018-10-19T14:22:09Z
dc.descriptionGroundwater from the La Paz arid coastal aquifer in Baja California, Mexico, is essentially the only source of drinking water for the local population and tourists, as well as irrigation water for agricultural needs. The intensive exploitation of the aquifer and water cycling has resulted in groundwater abatement (up to 10 m) and high salinity (up to ~5800 mg l−1). A study using hydrochemistry, isotopic (deuterium, oxygen-18 and carbon-14) and gaseous tracers (chlorofluorocarbons CFC-11, CFC-12, CFC-113), as well as multivariate statistics, was developed to elucidate groundwater composition, flow and occurrence. Groundwater is of meteoric origin, and a large proportion is subject to evaporation. The primary natural recharge is generated in the El Novillo and Las Cruces ranges, and groundwater subsequently flows in a SE–NW direction toward the coast. The initial water type is the result of discordant dissolution of silicate minerals and ion exchange on soils. In the lower plain portion, the aquifer system is recharged from irrigation return flow and seawater intrusion, which significantly affects groundwater chemistry. Nitrate and chloride concentrations indicate that groundwater is highly affected by an overuse of fertilizers in agricultural activities, but there is little effect from urban activities. Seawater intrusion has progressed rapidly during the past decade, and the impact currently extends 13 km inland. Radiocarbon residence time calculations suggest that groundwater is modern, with the exception of Chametla and El Centerario sites in the central and western lowlands with ages of up to ~5000 years. These waters indicate an additional recharge source for the upconing of fossil groundwater or regional flow. © 2016, The Author(s).
dc.identifier.doi10.1007/s12665-016-5617-2
dc.identifier.issn18666280
dc.identifier.issue9
dc.identifier.urihttp://hdl.handle.net/11285/630647
dc.identifier.volume75
dc.languageeng
dc.publisherSpringer Verlag
dc.relationhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-84966332550&doi=10.1007%2fs12665-016-5617-2&partnerID=40&md5=f687661236dbef2eb9c3c6e85f43d924
dc.relationInvestigadores
dc.relationEstudiantes
dc.rightsinfo:eu-repo/semantics/openAccess
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0
dc.sourceEnvironmental Earth Sciences
dc.subjectAgriculture
dc.subjectAquifers
dc.subjectArid regions
dc.subjectCarbon
dc.subjectContamination
dc.subjectGroundwater
dc.subjectGroundwater geochemistry
dc.subjectGroundwater pollution
dc.subjectGroundwater resources
dc.subjectHydrochemistry
dc.subjectHydrogeology
dc.subjectIon exchange
dc.subjectIrrigation
dc.subjectIsotopes
dc.subjectMercury (metal)
dc.subjectMultivariant analysis
dc.subjectPotable water
dc.subjectSalt water intrusion
dc.subjectSeawater
dc.subjectSilicate minerals
dc.subjectSilicates
dc.subjectWater
dc.subjectAgricultural activities
dc.subjectChloride concentrations
dc.subjectCoastal aquifers
dc.subjectGroundwater composition
dc.subjectHydro geochemistries
dc.subjectIntensive exploitations
dc.subjectIrrigation return flows
dc.subjectMultivariate statistics
dc.subjectRecharging (underground waters)
dc.subjectaquifer pollution
dc.subjectarid region
dc.subjectcoastal aquifer
dc.subjectconcentration (composition)
dc.subjectdrinking water
dc.subjectexploitation
dc.subjecthydrogeochemistry
dc.subjecthydrology
dc.subjection exchange
dc.subjectisotopic composition
dc.subjectmultivariate analysis
dc.subjectrecharge
dc.subjectresidence time
dc.subjectsaline intrusion
dc.subjectsalinity
dc.subjectsilicate mineral
dc.subjecttracer
dc.subjectBaja California Sur
dc.subjectLa Paz [Baja California Sur]
dc.subjectLas Cruces
dc.subjectMexico [North America]
dc.subjectNew Mexico
dc.subjectUnited States
dc.subject.classification7 INGENIERÍA Y TECNOLOGÍA
dc.titleIsotope signatures and hydrochemistry as tools in assessing groundwater occurrence and dynamics in a coastal arid aquifer
dc.typeArtículo
refterms.dateFOA2018-10-19T14:22:09Z

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