Formation of schwertmannite and its transformation to jarosite in the presence of acidophilic iron-oxidizing microorganisms
Schwertmannite [Fe 8O 8(OH) 6SO 4] and jarosite [XFe 3(SO 4) 2(OH) 6] were synthesized from FeSO 4-mineral salts solutions that were inoculated with acidophilic iron-oxidizing bacteria ( Acidithiobacillus ferrooxidans). Schwertmannite was transformed to NH 4 +/H 3O + jarosite upon increasing the agi...
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Veröffentlicht in: | Materials Science & Engineering C 2006-05, Vol.26 (4), p.588-592 |
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creator | Wang, Hongmei Bigham, Jerry M. Tuovinen, Olli H. |
description | Schwertmannite [Fe
8O
8(OH)
6SO
4] and jarosite [XFe
3(SO
4)
2(OH)
6] were synthesized from FeSO
4-mineral salts solutions that were inoculated with acidophilic iron-oxidizing bacteria (
Acidithiobacillus ferrooxidans). Schwertmannite was transformed to NH
4
+/H
3O
+ jarosite upon increasing the aging time (19 to 40 days), temperature (36 to 45 °C), or the ammonium concentration (11.4 to 111.4 mM) in acid (about pH 2.0) media. Thus, in this phase transformation, metastable schwertmannite served as a solid phase precursor for jarosite formation. Scanning electron microscope and chemical analyses showed that the morphology, specific surface area and chemical composition of the jarosites thus produced varied depending on the experimental conditions. Because the surface areas and the molar ratios of Fe:S in the two Fe(III) hydroxysulfates are different, the transformation of schwertmannite to jarosite impacts the biogeochemistry of Fe and S as well as minor and trace metals in acid mine drainage. |
doi_str_mv | 10.1016/j.msec.2005.04.009 |
format | Article |
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8O
8(OH)
6SO
4] and jarosite [XFe
3(SO
4)
2(OH)
6] were synthesized from FeSO
4-mineral salts solutions that were inoculated with acidophilic iron-oxidizing bacteria (
Acidithiobacillus ferrooxidans). Schwertmannite was transformed to NH
4
+/H
3O
+ jarosite upon increasing the aging time (19 to 40 days), temperature (36 to 45 °C), or the ammonium concentration (11.4 to 111.4 mM) in acid (about pH 2.0) media. Thus, in this phase transformation, metastable schwertmannite served as a solid phase precursor for jarosite formation. Scanning electron microscope and chemical analyses showed that the morphology, specific surface area and chemical composition of the jarosites thus produced varied depending on the experimental conditions. Because the surface areas and the molar ratios of Fe:S in the two Fe(III) hydroxysulfates are different, the transformation of schwertmannite to jarosite impacts the biogeochemistry of Fe and S as well as minor and trace metals in acid mine drainage.</description><identifier>ISSN: 0928-4931</identifier><identifier>EISSN: 1873-0191</identifier><identifier>DOI: 10.1016/j.msec.2005.04.009</identifier><language>eng</language><publisher>Elsevier B.V</publisher><subject>Acidithiobacillus ferrooxidans ; Iron-oxidizing bacteria ; Jarosite ; Schwertmannite ; Transformation</subject><ispartof>Materials Science & Engineering C, 2006-05, Vol.26 (4), p.588-592</ispartof><rights>2005 Elsevier B.V.</rights><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c472t-95c7c9d3eb42e42217fe43fe4d187683bb144d797809d1deb885128ae1fb18cd3</citedby><cites>FETCH-LOGICAL-c472t-95c7c9d3eb42e42217fe43fe4d187683bb144d797809d1deb885128ae1fb18cd3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.msec.2005.04.009$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,780,784,3548,27922,27923,45993</link.rule.ids></links><search><creatorcontrib>Wang, Hongmei</creatorcontrib><creatorcontrib>Bigham, Jerry M.</creatorcontrib><creatorcontrib>Tuovinen, Olli H.</creatorcontrib><title>Formation of schwertmannite and its transformation to jarosite in the presence of acidophilic iron-oxidizing microorganisms</title><title>Materials Science & Engineering C</title><description>Schwertmannite [Fe
8O
8(OH)
6SO
4] and jarosite [XFe
3(SO
4)
2(OH)
6] were synthesized from FeSO
4-mineral salts solutions that were inoculated with acidophilic iron-oxidizing bacteria (
Acidithiobacillus ferrooxidans). Schwertmannite was transformed to NH
4
+/H
3O
+ jarosite upon increasing the aging time (19 to 40 days), temperature (36 to 45 °C), or the ammonium concentration (11.4 to 111.4 mM) in acid (about pH 2.0) media. Thus, in this phase transformation, metastable schwertmannite served as a solid phase precursor for jarosite formation. Scanning electron microscope and chemical analyses showed that the morphology, specific surface area and chemical composition of the jarosites thus produced varied depending on the experimental conditions. Because the surface areas and the molar ratios of Fe:S in the two Fe(III) hydroxysulfates are different, the transformation of schwertmannite to jarosite impacts the biogeochemistry of Fe and S as well as minor and trace metals in acid mine drainage.</description><subject>Acidithiobacillus ferrooxidans</subject><subject>Iron-oxidizing bacteria</subject><subject>Jarosite</subject><subject>Schwertmannite</subject><subject>Transformation</subject><issn>0928-4931</issn><issn>1873-0191</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><recordid>eNqFkUtrHDEQhEVwIGvHf8AnnXybiV7rkcCXYGInYPAlOQuN1OPtZUfaSHLix5-Phg0-2oemafiqoLoIOeOs54xffNn2cwHfC8bWPVM9Y-YDWXE9yI5xw4_IihmhO2Uk_0SOS9kydqHlIFbk5Trl2VVMkaaJFr_5C7nOLkasQF0MFGuhNbtYplewJrp1OZUFwXZugO4zFIgeFhPnMaT9BnfoKeYUu_SIAZ8x3tMZfU4p37uIZS6fycfJ7Qqc_t8n5Nf1t59X37vbu5sfV19vO68GUTuz9oM3QcKoBCgh-DCBkm1CC9hijCNXKgxm0MwEHmDUes2FdsCnkWsf5Ak5P_juc_r9AKXaGYuH3c5FSA_FCiM1k4a_DzK9ZlqKBooD2OKUkmGy-4yzy0-WM7sUYrd2KcQuhVimbCukiS4PImhZ_yBkWzwuTwuYwVcbEr4l_wfKpZep</recordid><startdate>20060501</startdate><enddate>20060501</enddate><creator>Wang, Hongmei</creator><creator>Bigham, Jerry M.</creator><creator>Tuovinen, Olli H.</creator><general>Elsevier B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7QL</scope><scope>7ST</scope><scope>7T7</scope><scope>7U6</scope><scope>8FD</scope><scope>C1K</scope><scope>FR3</scope><scope>P64</scope><scope>7SR</scope><scope>7TB</scope><scope>7U5</scope><scope>8BQ</scope><scope>JG9</scope><scope>L7M</scope></search><sort><creationdate>20060501</creationdate><title>Formation of schwertmannite and its transformation to jarosite in the presence of acidophilic iron-oxidizing microorganisms</title><author>Wang, Hongmei ; Bigham, Jerry M. ; Tuovinen, Olli H.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c472t-95c7c9d3eb42e42217fe43fe4d187683bb144d797809d1deb885128ae1fb18cd3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2006</creationdate><topic>Acidithiobacillus ferrooxidans</topic><topic>Iron-oxidizing bacteria</topic><topic>Jarosite</topic><topic>Schwertmannite</topic><topic>Transformation</topic><toplevel>online_resources</toplevel><creatorcontrib>Wang, Hongmei</creatorcontrib><creatorcontrib>Bigham, Jerry M.</creatorcontrib><creatorcontrib>Tuovinen, Olli H.</creatorcontrib><collection>CrossRef</collection><collection>Bacteriology Abstracts (Microbiology B)</collection><collection>Environment Abstracts</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Sustainability Science Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Engineering Research Database</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>Engineered Materials Abstracts</collection><collection>Mechanical & Transportation Engineering Abstracts</collection><collection>Solid State and Superconductivity Abstracts</collection><collection>METADEX</collection><collection>Materials Research Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Materials Science & Engineering C</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Wang, Hongmei</au><au>Bigham, Jerry M.</au><au>Tuovinen, Olli H.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Formation of schwertmannite and its transformation to jarosite in the presence of acidophilic iron-oxidizing microorganisms</atitle><jtitle>Materials Science & Engineering C</jtitle><date>2006-05-01</date><risdate>2006</risdate><volume>26</volume><issue>4</issue><spage>588</spage><epage>592</epage><pages>588-592</pages><issn>0928-4931</issn><eissn>1873-0191</eissn><abstract>Schwertmannite [Fe
8O
8(OH)
6SO
4] and jarosite [XFe
3(SO
4)
2(OH)
6] were synthesized from FeSO
4-mineral salts solutions that were inoculated with acidophilic iron-oxidizing bacteria (
Acidithiobacillus ferrooxidans). Schwertmannite was transformed to NH
4
+/H
3O
+ jarosite upon increasing the aging time (19 to 40 days), temperature (36 to 45 °C), or the ammonium concentration (11.4 to 111.4 mM) in acid (about pH 2.0) media. Thus, in this phase transformation, metastable schwertmannite served as a solid phase precursor for jarosite formation. Scanning electron microscope and chemical analyses showed that the morphology, specific surface area and chemical composition of the jarosites thus produced varied depending on the experimental conditions. Because the surface areas and the molar ratios of Fe:S in the two Fe(III) hydroxysulfates are different, the transformation of schwertmannite to jarosite impacts the biogeochemistry of Fe and S as well as minor and trace metals in acid mine drainage.</abstract><pub>Elsevier B.V</pub><doi>10.1016/j.msec.2005.04.009</doi><tpages>5</tpages><oa>free_for_read</oa></addata></record> |
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issn | 0928-4931 1873-0191 |
language | eng |
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source | Elsevier ScienceDirect Journals Complete - AutoHoldings |
subjects | Acidithiobacillus ferrooxidans Iron-oxidizing bacteria Jarosite Schwertmannite Transformation |
title | Formation of schwertmannite and its transformation to jarosite in the presence of acidophilic iron-oxidizing microorganisms |
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