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dc.contributor.authorBentabol-Manzanares, Maria Jose 
dc.date.accessioned2017-07-25T08:51:41Z
dc.date.available2017-07-25T08:51:41Z
dc.date.created2017
dc.date.issued2017
dc.identifier.citationScientific Research Abstracts XVI-International Clay Conference Vol. 7, p. 79, 2017es_ES
dc.identifier.urihttp://hdl.handle.net/10630/14341
dc.description.abstractDuring diagenesis, several reactions induce changes both in phyllosilicates and organic matter, which in basins associated to the production of hydrocarbons leads to ammonium fixation in illite and micas [1] and to dissolution induced by organic acids [2] [3]. Dissolution processes may contribute to the smectite-to-illite transformation, stabilized by fixation of K (and NH4 +). Ammonium is a weak acid in solution. Under neutral conditions where the concentration of hydronium is very low (<10-7 M), ammonium contributes to smectite dissolution. The effect of organic acid on silicates dissolution is partially known, but the potential role of ammonium is completely novel.es_ES
dc.description.sponsorshipUniversidad de Málaga. Campus de Excelencia Internacional Andalucía Tech.es_ES
dc.language.isoenges_ES
dc.publisherAlberto López Galindoes_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.subjectFilosilicatoses_ES
dc.subjectAmonioes_ES
dc.subject.otherAmmoniumes_ES
dc.subject.otherillitees_ES
dc.subject.othersmectitees_ES
dc.subject.otherhydrothermal synthesises_ES
dc.titleInfluence of presence of ammonium in the hydrothermal illitization of smectitees_ES
dc.typeinfo:eu-repo/semantics/conferenceObjectes_ES
dc.centroFacultad de Cienciases_ES
dc.relation.eventtitleXVI International Clay Conferencees_ES
dc.relation.eventplaceGranadaes_ES
dc.relation.eventdate17-07-2017es_ES
dc.cclicenseby-nc-ndes_ES


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