<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-05-30T11:42:22Z</responseDate><request verb="GetRecord" identifier="oai:riuma.uma.es:10630/14341" metadataPrefix="oai_dc">https://riuma.uma.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:riuma.uma.es:10630/14341</identifier><datestamp>2026-02-03T12:03:58Z</datestamp><setSpec>com_10630_2254</setSpec><setSpec>col_10630_37959</setSpec></header><metadata><oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:doc="http://www.lyncode.com/xoai" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
   <dc:title>Influence of presence of ammonium in the hydrothermal illitization of smectite</dc:title>
   <dc:creator>Bentabol-Manzanares, María José</dc:creator>
   <dc:subject>Filosilicatos</dc:subject>
   <dc:subject>Amonio</dc:subject>
   <dc:subject>Ammonium</dc:subject>
   <dc:subject>illite</dc:subject>
   <dc:subject>smectite</dc:subject>
   <dc:subject>hydrothermal synthesis</dc:subject>
   <dc:description>During diagenesis, several reactions induce changes both in phyllosilicates and organic matter, which in basins&#xd;
associated to the production of hydrocarbons leads to ammonium fixation in illite and micas [1] and to dissolution&#xd;
induced by organic acids [2] [3]. Dissolution processes may contribute to the smectite-to-illite transformation,&#xd;
stabilized by fixation of K (and NH4&#xd;
+). Ammonium is a weak acid in solution. Under neutral conditions where the&#xd;
concentration of hydronium is very low (&lt;10-7 M), ammonium contributes to smectite dissolution. The effect of&#xd;
organic acid on silicates dissolution is partially known, but the potential role of ammonium is completely novel.</dc:description>
   <dc:description>Universidad de Málaga. Campus de Excelencia Internacional Andalucía Tech.</dc:description>
   <dc:date>2017-07-25T08:51:41Z</dc:date>
   <dc:date>2017-07-25T08:51:41Z</dc:date>
   <dc:date>2017</dc:date>
   <dc:date>2017</dc:date>
   <dc:type>conference output</dc:type>
   <dc:identifier>Scientific Research Abstracts XVI-International Clay Conference Vol. 7, p. 79, 2017</dc:identifier>
   <dc:identifier>http://hdl.handle.net/10630/14341</dc:identifier>
   <dc:language>eng</dc:language>
   <dc:relation>XVI International Clay Conference</dc:relation>
   <dc:relation>Granada</dc:relation>
   <dc:relation>17-07-2017</dc:relation>
   <dc:rights>by-nc-nd</dc:rights>
   <dc:rights>open access</dc:rights>
   <dc:format>application/pdf</dc:format>
   <dc:publisher>Alberto López Galindo</dc:publisher>
</oai_dc:dc>
</metadata></record></GetRecord></OAI-PMH>