Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/50007
DC FieldValueLanguage
dc.contributor.authorMenéndez, I.en_US
dc.contributor.authorMoreno, G.en_US
dc.contributor.authorGallardo, J. F.en_US
dc.contributor.authorSaavedra, J.en_US
dc.date.accessioned2018-11-24T12:30:44Z-
dc.date.available2018-11-24T12:30:44Z-
dc.date.issued2007en_US
dc.identifier.issn0885-6087en_US
dc.identifier.urihttp://hdl.handle.net/10553/50007-
dc.description.abstractThree techniques for obtaining soil water solutions (gravitational and matrical waters extracted using both in situ tension lysimeters and in vitro pressure chambers) and their later chemical analysis were performed in order to know the evolution of the soil‐solution composition when water moves down through the soil, from the Ah soil horizon to the BwC‐ or C‐horizons of forest soils located in western Spain. Additionally, ion concentrations and water volumes of input waters to soil (canopy washout) and exported waters (drainage solutions from C‐horizons) were determined to establish the net balance of solutes in order to determine the rates of leaching or retention of ions. A generalized process of sorption or retention of most components (even Cl−) was observed, from the soil surface to the C‐horizon, in both gravitational and matrical waters, with H4SiO4, Mn2+, Na+, and SO42− being the net exported components from the soil through the groundwater. These results enhance the role of the recycling effect in these forest soils. The net percentages of elements retained in these forest soils, considering the inputs and the outputs balance, were 68% K+, 85% Ca2+, 58% Mg2+, 7% Al3+, 5% Fe3+, 34% Zn2+, 57% Cl−, and 20% NO3−, and about 75% of dissolved organic carbon was mineralized.en_US
dc.languageengen_US
dc.publisher0885-6087-
dc.relation.ispartofHydrological Processesen_US
dc.sourceHydrological Processes [ISSN 0885-6087], v. 21, p. 1949-1956en_US
dc.subject2511 Ciencias del suelo (Edafología)en_US
dc.subject251104 Química de suelosen_US
dc.subject250605 Hidrogeologíaen_US
dc.subject.otherSoil hydrologyen_US
dc.subject.otherSoil chemistryen_US
dc.subject.otherSoil water balanceen_US
dc.subject.otherSoil foresten_US
dc.titleHydrogeochemical balance of forest umbrisol profiles ('Sierra de Gata', central western Spain)en_US
dc.typeinfo:eu-repo/semantics/Articleen_US
dc.typeArticleen_US
dc.identifier.doi10.1002/hyp.6406
dc.identifier.scopus34447306858-
dc.identifier.isi000248234100015
dc.contributor.authorscopusid6701688947-
dc.contributor.authorscopusid20734998800-
dc.contributor.authorscopusid7101888500-
dc.contributor.authorscopusid7202229189-
dc.description.lastpage1956-
dc.description.firstpage1949-
dc.relation.volume21-
dc.investigacionCienciasen_US
dc.type2Artículoen_US
dc.contributor.daisngid30771427
dc.contributor.daisngid181295
dc.contributor.daisngid3189036
dc.contributor.daisngid29546741
dc.utils.revisionen_US
dc.contributor.wosstandardWOS:Menendez, J
dc.contributor.wosstandardWOS:Moreno, G
dc.contributor.wosstandardWOS:Gallardo, JF
dc.contributor.wosstandardWOS:Saavedra, J
dc.date.coverdateJulio 2007
dc.identifier.ulpgces
dc.description.jcr1,798
dc.description.jcrqQ1
dc.description.scieSCIE
item.fulltextSin texto completo-
item.grantfulltextnone-
crisitem.author.deptGIR IOCAG:Geología Aplicada y Regional-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.deptDepartamento de Física-
crisitem.author.orcid0000-0002-1801-5177-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.fullNameMenéndez González, Inmaculada-
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