<?xml version="1.0" encoding="UTF-8"?><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>2026-10-19T00:39:25Z</responseDate><request verb="GetRecord" identifier="oai:ebyu-rdlopen.rawdatalibrary.net:ebyu/15754" metadataPrefix="oai_dc">https://ebyu-rdlopen.rawdatalibrary.net/oai/request</request><GetRecord><record><header><identifier>oai:ebyu-rdlopen.rawdatalibrary.net:ebyu/15754</identifier><datestamp>2026-10-18T20:43:04Z</datestamp><setSpec>openaire</setSpec><setSpec>driver</setSpec><setSpec>com_ebyu_10000</setSpec><setSpec>col_ebyu_10001</setSpec></header><metadata><oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" 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>Structural characterization of aniline-bentonite composite by FTIR, DTA/TG, and PXRD analyses and BET measurement</dc:title><dc:creator>Koksal, E.</dc:creator><dc:creator>Afsin, B.</dc:creator><dc:creator>Tabak, A.</dc:creator><dc:creator>Caglar, B.</dc:creator><dc:subject>anline species</dc:subject><dc:subject>bentonite</dc:subject><dc:subject>intercalation</dc:subject><dc:subject>surface properties</dc:subject><dc:subject>thermal analysis</dc:subject><dc:description>The aniline species incorporated into the acid-activated bentonite matrices leads to the decay of the skeletal stretches centered at 1041 cm-1 and the rise of new features in the phenyl ring frequency region, 1700-1400 cm-1, demonstrates clearly the influence of the acid activation on the Lewis sites necessary for coordination of aniline to bentonite. The exothermic DTA features at 507, 684, and 725°C indicate the release of both the clusters and the decomposed fragments of the aniline-clay composite, and the highly stable carbonaceous residue, respectively. The basal difference by ∼1.0 nm and the much smaller surface area (33.8 m2/g) than that of the nonintercalated bentonite (129.2 m2/g) prove the presence of the tilted aniline species between the interlamellar grooves of the bentonite framework. Copyright © Taylor &amp; Francis Group, LLC.</dc:description><dc:publisher>TAYLOR &amp; FRANCIS INC</dc:publisher><dc:date>2011</dc:date><dc:type>Article</dc:type><dc:identifier>https://rdlopen.rawdatalibrary.net/r/ebyu/15754</dc:identifier><dc:identifier>https://doi.org/10.1080/00387010903555953</dc:identifier><dc:identifier>1532-2289</dc:identifier><dc:language>en</dc:language><dc:relation>Spectroscopy Letters</dc:relation><dc:rights>info:eu-repo/semantics/openAccess</dc:rights><dc:type>info:eu-repo/semantics/article</dc:type><dc:identifier>https://ebyu-rdlopen.rawdatalibrary.net/tr/items/ebyu/15754</dc:identifier></oai_dc:dc></metadata></record></GetRecord></OAI-PMH>