Organophilization of a Brazilian Mg-montmorillonite without prior sodium activation
The use of Mg-montmorillonite in the production of organoclay without sodium activation was investigated. For this purpose, organophilization experiments were carried out by varying the concentration of two surfactants: hexadecyltrimethylammonium (HDTMA+) and dodecyltrimethylammonium (DTMA+) ions. T...
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description | The use of Mg-montmorillonite in the production of organoclay without sodium activation was investigated. For this purpose, organophilization experiments were carried out by varying the concentration of two surfactants: hexadecyltrimethylammonium (HDTMA+) and dodecyltrimethylammonium (DTMA+) ions. These surfactants were used at concentrations 0.7, 1.0 and 1.5 times that of the cation exchange capacity (62.6 meq/100 g) of the clay, with a reaction time of 8 h at temperatures of 25 and 80°C. X-ray diffraction (XRD) results confirmed the intercalation for both in natura and activated samples. The Fourier-transform infrared (FTIR) spectroscopy and XRD results showed that the ratio of gauche/trans conformers decreased with increased basal spacing. The results of thermodifferential and thermogravimetric analysis (DTA/DTG) confirmed the thermal stability of the organoclay up to 200°C, permitting the use of such material in the synthesis of polymer/clay nanocomposites obtained by the melt blending. Thus, Mg-montmorillonite can be intercalated with alkylammonium ions without prior Na-activation to form organoclays. The possibility of using natural (non-activated) Mg-montmorillonite represents a significant difference in terms of processing cost in comparison with existing Ca-montmorillonite in Brazil or even with imported bentonites that require Na-activation during beneficiation. |
doi_str_mv | 10.1180/claymin.2016.051.1.04 |
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For this purpose, organophilization experiments were carried out by varying the concentration of two surfactants: hexadecyltrimethylammonium (HDTMA+) and dodecyltrimethylammonium (DTMA+) ions. These surfactants were used at concentrations 0.7, 1.0 and 1.5 times that of the cation exchange capacity (62.6 meq/100 g) of the clay, with a reaction time of 8 h at temperatures of 25 and 80°C. X-ray diffraction (XRD) results confirmed the intercalation for both in natura and activated samples. The Fourier-transform infrared (FTIR) spectroscopy and XRD results showed that the ratio of gauche/trans conformers decreased with increased basal spacing. The results of thermodifferential and thermogravimetric analysis (DTA/DTG) confirmed the thermal stability of the organoclay up to 200°C, permitting the use of such material in the synthesis of polymer/clay nanocomposites obtained by the melt blending. Thus, Mg-montmorillonite can be intercalated with alkylammonium ions without prior Na-activation to form organoclays. The possibility of using natural (non-activated) Mg-montmorillonite represents a significant difference in terms of processing cost in comparison with existing Ca-montmorillonite in Brazil or even with imported bentonites that require Na-activation during beneficiation.</description><identifier>ISSN: 0009-8558</identifier><identifier>EISSN: 1471-8030</identifier><identifier>DOI: 10.1180/claymin.2016.051.1.04</identifier><language>eng</language><publisher>Mineralogical Society</publisher><subject>Activation ; alkali metals ; alkaline earth metals ; bentonite ; cation exchange capacity ; chemical properties ; clastic rocks ; Clay (material) ; clay mineralogy ; clay minerals ; experimental studies ; FTIR spectra ; geochemistry ; infrared spectra ; Infrared spectroscopy ; Ion exchange ; magnesium ; metals ; Mg-montmorillonite ; montmorillonite ; organoclay ; organophilization ; rock, sediment, soil ; sed rocks, sediments ; Sedimentary petrology ; sedimentary rocks ; sheet silicates ; silicates ; smectite ; Sodium ; sodium activation ; spectra ; Surfactants ; Synthesis (chemistry) ; X-ray diffraction ; X-ray diffraction data</subject><ispartof>Clay minerals, 2016-03, Vol.51 (1), p.39-54</ispartof><rights>GeoRef, Copyright 2020, American Geosciences Institute. Reference includes data from GeoScienceWorld @Alexandria, VA @USA @United States. Abstract, Copyright, Mineralogical Society of Great Britain and Ireland</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a484t-5968c29fec5aa391f19242d58f6a21c0c362973a71baa3f37537aa5d243d08943</citedby><cites>FETCH-LOGICAL-a484t-5968c29fec5aa391f19242d58f6a21c0c362973a71baa3f37537aa5d243d08943</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27923,27924</link.rule.ids></links><search><creatorcontrib>Cavalcante, Manoella Silva</creatorcontrib><creatorcontrib>Paz, Simone Patricia Aranha</creatorcontrib><creatorcontrib>Angelica, Romulo Simoes</creatorcontrib><creatorcontrib>Ito, Edson Noryuki</creatorcontrib><creatorcontrib>Neves, Roberto Freitas</creatorcontrib><title>Organophilization of a Brazilian Mg-montmorillonite without prior sodium activation</title><title>Clay minerals</title><description>The use of Mg-montmorillonite in the production of organoclay without sodium activation was investigated. For this purpose, organophilization experiments were carried out by varying the concentration of two surfactants: hexadecyltrimethylammonium (HDTMA+) and dodecyltrimethylammonium (DTMA+) ions. These surfactants were used at concentrations 0.7, 1.0 and 1.5 times that of the cation exchange capacity (62.6 meq/100 g) of the clay, with a reaction time of 8 h at temperatures of 25 and 80°C. X-ray diffraction (XRD) results confirmed the intercalation for both in natura and activated samples. The Fourier-transform infrared (FTIR) spectroscopy and XRD results showed that the ratio of gauche/trans conformers decreased with increased basal spacing. The results of thermodifferential and thermogravimetric analysis (DTA/DTG) confirmed the thermal stability of the organoclay up to 200°C, permitting the use of such material in the synthesis of polymer/clay nanocomposites obtained by the melt blending. Thus, Mg-montmorillonite can be intercalated with alkylammonium ions without prior Na-activation to form organoclays. The possibility of using natural (non-activated) Mg-montmorillonite represents a significant difference in terms of processing cost in comparison with existing Ca-montmorillonite in Brazil or even with imported bentonites that require Na-activation during beneficiation.</description><subject>Activation</subject><subject>alkali metals</subject><subject>alkaline earth metals</subject><subject>bentonite</subject><subject>cation exchange capacity</subject><subject>chemical properties</subject><subject>clastic rocks</subject><subject>Clay (material)</subject><subject>clay mineralogy</subject><subject>clay minerals</subject><subject>experimental studies</subject><subject>FTIR spectra</subject><subject>geochemistry</subject><subject>infrared spectra</subject><subject>Infrared spectroscopy</subject><subject>Ion exchange</subject><subject>magnesium</subject><subject>metals</subject><subject>Mg-montmorillonite</subject><subject>montmorillonite</subject><subject>organoclay</subject><subject>organophilization</subject><subject>rock, sediment, soil</subject><subject>sed rocks, sediments</subject><subject>Sedimentary petrology</subject><subject>sedimentary rocks</subject><subject>sheet silicates</subject><subject>silicates</subject><subject>smectite</subject><subject>Sodium</subject><subject>sodium activation</subject><subject>spectra</subject><subject>Surfactants</subject><subject>Synthesis (chemistry)</subject><subject>X-ray diffraction</subject><subject>X-ray diffraction data</subject><issn>0009-8558</issn><issn>1471-8030</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><recordid>eNqNkM1u1DAURi0EEkPhEZCyREIJvnac2EtaUUAq6gJYWxfHmbpy7MF2GE2fHg-pxA6x8t_3HfkeQl4D7QAkfWc8nhYXOkZh6KiADjraPyE76EdoJeX0KdlRSlUrhZDPyYuc7-uR95LvyNfbtMcQD3fOuwcsLoYmzg02lwkf6hWG5su-XWIoS0zO-xhcsc3Rlbu4luaQXExNjpNblwZNcb_-EF6SZzP6bF89rhfk-_WHb1ef2pvbj5-v3t-02Mu-tEIN0jA1WyMQuYIZFOvZJOQ8IANDDR-YGjmO8KO-z3wUfEQUE-v5RKXq-QV5s3EPKf5cbS56cdlY7zHYuGYNdV4ugQH9jygfOYNxgBoVW9SkmHOys65jLphOGqg--9aPvvXZt66-NWh6_s3l1juiLzZNdp_WU93o-7imUD38uy8AuKqQtxtkb2M2zgZjjzH56S9kKw2KD5z_BjZ3mwk</recordid><startdate>201603</startdate><enddate>201603</enddate><creator>Cavalcante, Manoella Silva</creator><creator>Paz, Simone Patricia Aranha</creator><creator>Angelica, Romulo Simoes</creator><creator>Ito, Edson Noryuki</creator><creator>Neves, Roberto Freitas</creator><general>Mineralogical Society</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TV</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><scope>7QQ</scope><scope>7SR</scope><scope>8FD</scope><scope>JG9</scope></search><sort><creationdate>201603</creationdate><title>Organophilization of a Brazilian Mg-montmorillonite without prior sodium activation</title><author>Cavalcante, Manoella Silva ; Paz, Simone Patricia Aranha ; Angelica, Romulo Simoes ; Ito, Edson Noryuki ; Neves, Roberto Freitas</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a484t-5968c29fec5aa391f19242d58f6a21c0c362973a71baa3f37537aa5d243d08943</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Activation</topic><topic>alkali metals</topic><topic>alkaline earth metals</topic><topic>bentonite</topic><topic>cation exchange capacity</topic><topic>chemical properties</topic><topic>clastic rocks</topic><topic>Clay (material)</topic><topic>clay mineralogy</topic><topic>clay minerals</topic><topic>experimental studies</topic><topic>FTIR spectra</topic><topic>geochemistry</topic><topic>infrared spectra</topic><topic>Infrared spectroscopy</topic><topic>Ion exchange</topic><topic>magnesium</topic><topic>metals</topic><topic>Mg-montmorillonite</topic><topic>montmorillonite</topic><topic>organoclay</topic><topic>organophilization</topic><topic>rock, sediment, soil</topic><topic>sed rocks, sediments</topic><topic>Sedimentary petrology</topic><topic>sedimentary rocks</topic><topic>sheet silicates</topic><topic>silicates</topic><topic>smectite</topic><topic>Sodium</topic><topic>sodium activation</topic><topic>spectra</topic><topic>Surfactants</topic><topic>Synthesis (chemistry)</topic><topic>X-ray diffraction</topic><topic>X-ray diffraction data</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Cavalcante, Manoella Silva</creatorcontrib><creatorcontrib>Paz, Simone Patricia Aranha</creatorcontrib><creatorcontrib>Angelica, Romulo Simoes</creatorcontrib><creatorcontrib>Ito, Edson Noryuki</creatorcontrib><creatorcontrib>Neves, Roberto Freitas</creatorcontrib><collection>CrossRef</collection><collection>Pollution Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Ceramic Abstracts</collection><collection>Engineered Materials Abstracts</collection><collection>Technology Research Database</collection><collection>Materials Research Database</collection><jtitle>Clay minerals</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Cavalcante, Manoella Silva</au><au>Paz, Simone Patricia Aranha</au><au>Angelica, Romulo Simoes</au><au>Ito, Edson Noryuki</au><au>Neves, Roberto Freitas</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Organophilization of a Brazilian Mg-montmorillonite without prior sodium activation</atitle><jtitle>Clay minerals</jtitle><date>2016-03</date><risdate>2016</risdate><volume>51</volume><issue>1</issue><spage>39</spage><epage>54</epage><pages>39-54</pages><issn>0009-8558</issn><eissn>1471-8030</eissn><abstract>The use of Mg-montmorillonite in the production of organoclay without sodium activation was investigated. For this purpose, organophilization experiments were carried out by varying the concentration of two surfactants: hexadecyltrimethylammonium (HDTMA+) and dodecyltrimethylammonium (DTMA+) ions. These surfactants were used at concentrations 0.7, 1.0 and 1.5 times that of the cation exchange capacity (62.6 meq/100 g) of the clay, with a reaction time of 8 h at temperatures of 25 and 80°C. X-ray diffraction (XRD) results confirmed the intercalation for both in natura and activated samples. The Fourier-transform infrared (FTIR) spectroscopy and XRD results showed that the ratio of gauche/trans conformers decreased with increased basal spacing. The results of thermodifferential and thermogravimetric analysis (DTA/DTG) confirmed the thermal stability of the organoclay up to 200°C, permitting the use of such material in the synthesis of polymer/clay nanocomposites obtained by the melt blending. Thus, Mg-montmorillonite can be intercalated with alkylammonium ions without prior Na-activation to form organoclays. The possibility of using natural (non-activated) Mg-montmorillonite represents a significant difference in terms of processing cost in comparison with existing Ca-montmorillonite in Brazil or even with imported bentonites that require Na-activation during beneficiation.</abstract><pub>Mineralogical Society</pub><doi>10.1180/claymin.2016.051.1.04</doi><tpages>16</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Activation alkali metals alkaline earth metals bentonite cation exchange capacity chemical properties clastic rocks Clay (material) clay mineralogy clay minerals experimental studies FTIR spectra geochemistry infrared spectra Infrared spectroscopy Ion exchange magnesium metals Mg-montmorillonite montmorillonite organoclay organophilization rock, sediment, soil sed rocks, sediments Sedimentary petrology sedimentary rocks sheet silicates silicates smectite Sodium sodium activation spectra Surfactants Synthesis (chemistry) X-ray diffraction X-ray diffraction data |
title | Organophilization of a Brazilian Mg-montmorillonite without prior sodium activation |
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