Asbestiform riebeckite (crocidolite) dissolution in the presence of Fe chelators; implications for mineral-induced disease
X-ray photoelectron spectroscopy (XPS) and solution chemistry were used to monitor the changes in surface composition of crocidolite fibres in a 50 mM NaCl solution at pH 7.5 and 22°C in the presence of several Fe chelators (citrate, EDTA, or desferrioxamine) for up to 30 days.
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Veröffentlicht in: | The American mineralogist 1995-12, Vol.80 (11-12), p.1093-1103 |
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container_issue | 11-12 |
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container_title | The American mineralogist |
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creator | Werner, Andrew J Hochella, Jr Guthrie, Jr Hardy, Jeanne A Aust, Ann E Rimstidt, J. Donald |
description | X-ray photoelectron spectroscopy (XPS) and solution chemistry were used to monitor the changes in surface composition of crocidolite fibres in a 50 mM NaCl solution at pH 7.5 and 22°C in the presence of several Fe chelators (citrate, EDTA, or desferrioxamine) for up to 30 days. |
doi_str_mv | 10.2138/am-1995-11-1201 |
format | Article |
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Donald</creatorcontrib><description>X-ray photoelectron spectroscopy (XPS) and solution chemistry were used to monitor the changes in surface composition of crocidolite fibres in a 50 mM NaCl solution at pH 7.5 and 22°C in the presence of several Fe chelators (citrate, EDTA, or desferrioxamine) for up to 30 days.</description><identifier>ISSN: 0003-004X</identifier><identifier>EISSN: 1945-3027</identifier><identifier>DOI: 10.2138/am-1995-11-1201</identifier><identifier>CODEN: AMMIAY</identifier><language>eng</language><publisher>Washington: Mineralogical Society of America</publisher><subject>amphibole group ; Asbestos ; chain silicates ; chelation ; chemical ratios ; Chemistry ; clinoamphibole ; crocidolite ; Disease ; Environmental geology ; experimental studies ; Fibers ; geochemistry ; geologic hazards ; medical geology ; Mineralogy ; Minerals ; oxidation ; reduction ; riebeckite ; SEM data ; silicates ; Sodium chloride ; solution ; spectra ; X-ray spectra</subject><ispartof>The American mineralogist, 1995-12, Vol.80 (11-12), p.1093-1103</ispartof><rights>GeoRef, Copyright 2020, American Geosciences Institute. 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Donald</creator><general>Mineralogical Society of America</general><general>Walter de Gruyter GmbH</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>199512</creationdate><title>Asbestiform riebeckite (crocidolite) dissolution in the presence of Fe chelators; implications for mineral-induced disease</title><author>Werner, Andrew J ; Hochella, Jr ; Guthrie, Jr ; Hardy, Jeanne A ; Aust, Ann E ; Rimstidt, J. 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Donald</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Asbestiform riebeckite (crocidolite) dissolution in the presence of Fe chelators; implications for mineral-induced disease</atitle><jtitle>The American mineralogist</jtitle><date>1995-12</date><risdate>1995</risdate><volume>80</volume><issue>11-12</issue><spage>1093</spage><epage>1103</epage><pages>1093-1103</pages><issn>0003-004X</issn><eissn>1945-3027</eissn><coden>AMMIAY</coden><abstract>X-ray photoelectron spectroscopy (XPS) and solution chemistry were used to monitor the changes in surface composition of crocidolite fibres in a 50 mM NaCl solution at pH 7.5 and 22°C in the presence of several Fe chelators (citrate, EDTA, or desferrioxamine) for up to 30 days.</abstract><cop>Washington</cop><pub>Mineralogical Society of America</pub><doi>10.2138/am-1995-11-1201</doi><tpages>11</tpages><oa>free_for_read</oa></addata></record> |
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source | EZB-FREE-00999 freely available EZB journals; Free Full-Text Journals in Chemistry |
subjects | amphibole group Asbestos chain silicates chelation chemical ratios Chemistry clinoamphibole crocidolite Disease Environmental geology experimental studies Fibers geochemistry geologic hazards medical geology Mineralogy Minerals oxidation reduction riebeckite SEM data silicates Sodium chloride solution spectra X-ray spectra |
title | Asbestiform riebeckite (crocidolite) dissolution in the presence of Fe chelators; implications for mineral-induced disease |
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