Identificador persistente para citar o vincular este elemento: http://hdl.handle.net/10553/53985
Campo DC Valoridioma
dc.contributor.authorEstevez, E.en_US
dc.contributor.authorCabrera, M. C.en_US
dc.contributor.authorFernandez-Vera, J. R.en_US
dc.contributor.authorMolina-Diaz, A.en_US
dc.contributor.authorRobles-Molina, J. R.en_US
dc.contributor.authorPalacios-Diaz, M. P.en_US
dc.contributor.otherCabrera, Maria del Carmen-
dc.date.accessioned2019-02-04T19:08:11Z-
dc.date.available2019-02-04T19:08:11Z-
dc.date.issued2013en_US
dc.identifier.issn1106-5516en_US
dc.identifier.urihttp://hdl.handle.net/10553/53985-
dc.description.abstractThe presence of emerging contaminants has been previously described in reclaimed water and groundwater of Gran Canaria (Spain). Despite of the environmental risk associated to irrigation with reclaimed water (R), this practice is necessary considering sustainability of the hydrological cycle in semiarid zones, especially regarding agricultural activity. The aim of this study was: i) to analyse the evolution during two years of contaminants of emerging concern, priority substances (2008/105/EC) and heavy metals in reclaimed water (R) and in a volcanic aquifer in the NE of Gran Canaria where a golf course has been irrigated with R since 1976 and ii) to relate this presence with physicochemical water properties and hydrogeological media. Reclaimed water and groundwater (GW) were monitoring quarterly from July 2009 to September 2011. Sorption and degradation processes in soil account for more compounds being detected in R. Diazinon and chlorfenvinphos were detected always in R and terbuthylazine, terbutryn and diuron at 90% of frequency. Considering all the samples, the most frequent compounds were chlorpyrifos ethyl, fluorene, phenanthrene and pyrene. Although their concentrations were frequently below 50 ngL-1, some contaminants, were occasionally detected at higher concentrations. Chlorpyrifos ethyl and diuron are priority substances detected frequently and at high concentrations so they must be included in monitoring studies. Geology and location seem to be related to the emerging compounds presence due to occasional contamination events (not related to R irrigation) and therefore not to an existence of a dangerous diffuse contamination level. Thus, it is preferable to select wells with less stable chemical water quality, in order to monitor the risk of emerging compounds presence. Considering the relationship between contaminant presence, chemical water quality, seasonal variation, hydrogeological characteristics and wells location we can conclude that chlorpyrifos ethyl and diuron were the most dangerous priority substances in terms of GW quality so they must be included in all of the monitoring studies, at least in Canary Islands.en_US
dc.languageengen_US
dc.publisher1106-5516
dc.relation.ispartofProceedings of the Conference on Environmental Science and Technologyen_US
dc.sourceProceedings Of The 13Th International Conference On Environmental Science And Technology [ISSN 1106-5516]en_US
dc.subject.otherEmerging contaminantsen_US
dc.subject.otherPriority substancesen_US
dc.subject.otherHeavy metalsen_US
dc.subject.otherReclaimed wateren_US
dc.subject.otherGroundwateren_US
dc.subject.otherIrrigationen_US
dc.subject.otherVolcanic zoneen_US
dc.titleTemporal Evolution Of Emerging Contaminants, Priority Substances And Heavy Metals Most Frequently Detected In Reclaimed Water And Groundwater In A Volcanic Aquiferen_US
dc.typeinfo:eu-repo/semantics/conferenceObjecten_US
dc.typeConferenceObjecten_US
dc.relation.conference13th International Conference on Environmental Science and Technology (CEST)
dc.identifier.isi000346067900357-
dcterms.isPartOfProceedings Of The 13Th International Conference On Environmental Science And Technology
dcterms.sourceProceedings Of The 13Th International Conference On Environmental Science And Technology[ISSN 1106-5516]
dc.investigacionCienciasen_US
dc.type2Actas de congresosen_US
dc.identifier.wosWOS:000346067900357-
dc.contributor.daisngid7230964-
dc.contributor.daisngid2942267-
dc.contributor.daisngid3913703-
dc.contributor.daisngid150287
dc.contributor.daisngid2012676-
dc.contributor.daisngid26509784-
dc.contributor.daisngid2739199-
dc.identifier.investigatorRIDR-9825-2018-
dc.utils.revisionen_US
dc.contributor.wosstandardWOS:Estevez, E
dc.contributor.wosstandardWOS:Cabrera, MC
dc.contributor.wosstandardWOS:Fernandez-Vera, JR
dc.contributor.wosstandardWOS:Molina-Diaz, A
dc.contributor.wosstandardWOS:Robles-Molina, JR
dc.contributor.wosstandardWOS:Palacios-Diaz, MP
dc.date.coverdate2013
dc.identifier.conferenceidevents120885
dc.identifier.ulpgces
item.grantfulltextnone-
item.fulltextSin texto completo-
crisitem.author.deptGIR IUNAT: Geología de Terrenos Volcánicos-
crisitem.author.deptIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.deptDepartamento de Física-
crisitem.author.deptGIR IUNAT: Geología de Terrenos Volcánicos-
crisitem.author.deptIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.deptDepartamento de Patología Animal, Producción Animal, Bromatología y Tecnología de Los Alimentos-
crisitem.author.orcid0000-0002-4556-4665-
crisitem.author.orcid0000-0003-4075-2592-
crisitem.author.parentorgIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.parentorgIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.fullNameCabrera Santana, María Del Carmen-
crisitem.author.fullNamePalacios Díaz, María Del Pino-
crisitem.event.eventsstartdate05-09-2013-
crisitem.event.eventsenddate07-09-2013-
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