Impact of microbial iron oxide reduction on the transport of diffusible tracers and non-diffusible nanoparticles in soils

In subsurface bioremediation, electron donor addition promotes microbial Fe(III)-oxide mineral reduction that could change soil pore structure, release colloids, and alter soil surface properties. These processes in turn may impact bioremediation rates and the ultimate fate of contaminants. Columns...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Chemosphere (Oxford) 2019-04, Vol.220, p.391-402
Hauptverfasser: Liang, Xiaolong, Radosevich, Mark, Löffler, Frank, Schaeffer, Sean M., Zhuang, Jie
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 402
container_issue
container_start_page 391
container_title Chemosphere (Oxford)
container_volume 220
creator Liang, Xiaolong
Radosevich, Mark
Löffler, Frank
Schaeffer, Sean M.
Zhuang, Jie
description In subsurface bioremediation, electron donor addition promotes microbial Fe(III)-oxide mineral reduction that could change soil pore structure, release colloids, and alter soil surface properties. These processes in turn may impact bioremediation rates and the ultimate fate of contaminants. Columns packed with water-stable, Fe-oxide-rich soil aggregates were infused with acetate-containing artificial groundwater and operated for 20 d or 60 d inside an anoxic chamber. Soluble Fe(II) and soil colloids were detected in the effluent within one week after initiation of the acetate addition, demonstrating Fe(III)-bioreduction and colloid formation. Diffusible Br−, less diffusible 2,6-difluorobenzoate (DFBA), and non-diffusible silica-shelled silver nanoparticles (SSSNP) were used as tracers in transport experiments before and after the bioreduction. The transport of Br− was not influenced by the bioreduction. DFBA showed earlier breakthrough and less tailing after the bioreduction, suggesting alterations in flow paths and soil surface chemistry during the 20-d bioreduction treatment. Similarly, the bioreduction increased the transport of SSSNP very significantly, with mass recovery increasing from 1.7% to 25.1%. Unexpectedly, the SSSNP was completely retained in the columns when the acetate injection was extended from 20 to 60 d, while the mass recovery of DFBA decreased from 89.1% to 84.1% and Br− showed no change. The large change in the transport of SSSNP was attributed to soil aggregate breakdown and colloid release (causing mechanical straining of SSSNP) and the exposure of iron oxide surfaces previously unavailable within aggregate interiors (facilitating attachment of SSSNP). These results suggest a time-dependent fashion of microbial effect on the transport of diffusivity-varying tracers. [Display omitted] •Fe(III)-bioreduction causes time-dependent aggregate breakdown and colloid release.•Short-term bioreduction alters soil surface chemistry and solute/nanoparticle transport.•Electron donor amendment enhances transport of nanoparticles.
doi_str_mv 10.1016/j.chemosphere.2018.12.165
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_2162495020</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S0045653518325062</els_id><sourcerecordid>2162495020</sourcerecordid><originalsourceid>FETCH-LOGICAL-c428t-723820a49d6b3b8c81e9e96ff62699ddbfccbcd68a0c71742b0a294f12f38ed33</originalsourceid><addsrcrecordid>eNqNkE-P2yAQxVHVqsmm_QoVvfViF7CN4VhF-0-K1MvuGWEYFCIbXLCr5tuvk2xXOe5pNDPvzdP8EPpOSUkJ5T8PpdnDEPO4hwQlI1SUlJWUNx_QmopWFpRJ8RGtCambgjdVs0I3OR8IWcyN_IxWFWlkWzVyjY6Pw6jNhKPDgzcpdl732KcYcPznLeAEdjaTP_UBT3vAU9IhjzGdLdY7N2ff9ee5gZSxDhaHGIqrVdAhjjpN3vSQsQ84R9_nL-iT032Gr691g57vbp-2D8Xu9_3j9teuMDUTU9GySjCia2l5V3XCCAoSJHeOMy6ltZ0zpjOWC01MS9uadUQzWTvKXCXAVtUG_bjcHVP8M0Oe1OCzgb7XAeKcFaOc1bIhjCxSeZEuIHJO4NSY_KDTUVGiTuTVQV2RVyfyijK1UF28315j5m4A--b8j3oRbC8CWJ796yGpbDwEA9YnMJOy0b8j5gV4eJ3x</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2162495020</pqid></control><display><type>article</type><title>Impact of microbial iron oxide reduction on the transport of diffusible tracers and non-diffusible nanoparticles in soils</title><source>Elsevier ScienceDirect Journals Complete</source><creator>Liang, Xiaolong ; Radosevich, Mark ; Löffler, Frank ; Schaeffer, Sean M. ; Zhuang, Jie</creator><creatorcontrib>Liang, Xiaolong ; Radosevich, Mark ; Löffler, Frank ; Schaeffer, Sean M. ; Zhuang, Jie</creatorcontrib><description>In subsurface bioremediation, electron donor addition promotes microbial Fe(III)-oxide mineral reduction that could change soil pore structure, release colloids, and alter soil surface properties. These processes in turn may impact bioremediation rates and the ultimate fate of contaminants. Columns packed with water-stable, Fe-oxide-rich soil aggregates were infused with acetate-containing artificial groundwater and operated for 20 d or 60 d inside an anoxic chamber. Soluble Fe(II) and soil colloids were detected in the effluent within one week after initiation of the acetate addition, demonstrating Fe(III)-bioreduction and colloid formation. Diffusible Br−, less diffusible 2,6-difluorobenzoate (DFBA), and non-diffusible silica-shelled silver nanoparticles (SSSNP) were used as tracers in transport experiments before and after the bioreduction. The transport of Br− was not influenced by the bioreduction. DFBA showed earlier breakthrough and less tailing after the bioreduction, suggesting alterations in flow paths and soil surface chemistry during the 20-d bioreduction treatment. Similarly, the bioreduction increased the transport of SSSNP very significantly, with mass recovery increasing from 1.7% to 25.1%. Unexpectedly, the SSSNP was completely retained in the columns when the acetate injection was extended from 20 to 60 d, while the mass recovery of DFBA decreased from 89.1% to 84.1% and Br− showed no change. The large change in the transport of SSSNP was attributed to soil aggregate breakdown and colloid release (causing mechanical straining of SSSNP) and the exposure of iron oxide surfaces previously unavailable within aggregate interiors (facilitating attachment of SSSNP). These results suggest a time-dependent fashion of microbial effect on the transport of diffusivity-varying tracers. [Display omitted] •Fe(III)-bioreduction causes time-dependent aggregate breakdown and colloid release.•Short-term bioreduction alters soil surface chemistry and solute/nanoparticle transport.•Electron donor amendment enhances transport of nanoparticles.</description><identifier>ISSN: 0045-6535</identifier><identifier>EISSN: 1879-1298</identifier><identifier>DOI: 10.1016/j.chemosphere.2018.12.165</identifier><identifier>PMID: 30597359</identifier><language>eng</language><publisher>England: Elsevier Ltd</publisher><subject>Biostimulation ; Iron reduction ; Nanoparticles ; Soil aggregates ; Transport</subject><ispartof>Chemosphere (Oxford), 2019-04, Vol.220, p.391-402</ispartof><rights>2018 Elsevier Ltd</rights><rights>Copyright © 2018 Elsevier Ltd. All rights reserved.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c428t-723820a49d6b3b8c81e9e96ff62699ddbfccbcd68a0c71742b0a294f12f38ed33</citedby><cites>FETCH-LOGICAL-c428t-723820a49d6b3b8c81e9e96ff62699ddbfccbcd68a0c71742b0a294f12f38ed33</cites><orcidid>0000-0002-5472-9118 ; 0000-0002-3759-3976</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.chemosphere.2018.12.165$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,780,784,3550,27924,27925,45995</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/30597359$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Liang, Xiaolong</creatorcontrib><creatorcontrib>Radosevich, Mark</creatorcontrib><creatorcontrib>Löffler, Frank</creatorcontrib><creatorcontrib>Schaeffer, Sean M.</creatorcontrib><creatorcontrib>Zhuang, Jie</creatorcontrib><title>Impact of microbial iron oxide reduction on the transport of diffusible tracers and non-diffusible nanoparticles in soils</title><title>Chemosphere (Oxford)</title><addtitle>Chemosphere</addtitle><description>In subsurface bioremediation, electron donor addition promotes microbial Fe(III)-oxide mineral reduction that could change soil pore structure, release colloids, and alter soil surface properties. These processes in turn may impact bioremediation rates and the ultimate fate of contaminants. Columns packed with water-stable, Fe-oxide-rich soil aggregates were infused with acetate-containing artificial groundwater and operated for 20 d or 60 d inside an anoxic chamber. Soluble Fe(II) and soil colloids were detected in the effluent within one week after initiation of the acetate addition, demonstrating Fe(III)-bioreduction and colloid formation. Diffusible Br−, less diffusible 2,6-difluorobenzoate (DFBA), and non-diffusible silica-shelled silver nanoparticles (SSSNP) were used as tracers in transport experiments before and after the bioreduction. The transport of Br− was not influenced by the bioreduction. DFBA showed earlier breakthrough and less tailing after the bioreduction, suggesting alterations in flow paths and soil surface chemistry during the 20-d bioreduction treatment. Similarly, the bioreduction increased the transport of SSSNP very significantly, with mass recovery increasing from 1.7% to 25.1%. Unexpectedly, the SSSNP was completely retained in the columns when the acetate injection was extended from 20 to 60 d, while the mass recovery of DFBA decreased from 89.1% to 84.1% and Br− showed no change. The large change in the transport of SSSNP was attributed to soil aggregate breakdown and colloid release (causing mechanical straining of SSSNP) and the exposure of iron oxide surfaces previously unavailable within aggregate interiors (facilitating attachment of SSSNP). These results suggest a time-dependent fashion of microbial effect on the transport of diffusivity-varying tracers. [Display omitted] •Fe(III)-bioreduction causes time-dependent aggregate breakdown and colloid release.•Short-term bioreduction alters soil surface chemistry and solute/nanoparticle transport.•Electron donor amendment enhances transport of nanoparticles.</description><subject>Biostimulation</subject><subject>Iron reduction</subject><subject>Nanoparticles</subject><subject>Soil aggregates</subject><subject>Transport</subject><issn>0045-6535</issn><issn>1879-1298</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><recordid>eNqNkE-P2yAQxVHVqsmm_QoVvfViF7CN4VhF-0-K1MvuGWEYFCIbXLCr5tuvk2xXOe5pNDPvzdP8EPpOSUkJ5T8PpdnDEPO4hwQlI1SUlJWUNx_QmopWFpRJ8RGtCambgjdVs0I3OR8IWcyN_IxWFWlkWzVyjY6Pw6jNhKPDgzcpdl732KcYcPznLeAEdjaTP_UBT3vAU9IhjzGdLdY7N2ff9ee5gZSxDhaHGIqrVdAhjjpN3vSQsQ84R9_nL-iT032Gr691g57vbp-2D8Xu9_3j9teuMDUTU9GySjCia2l5V3XCCAoSJHeOMy6ltZ0zpjOWC01MS9uadUQzWTvKXCXAVtUG_bjcHVP8M0Oe1OCzgb7XAeKcFaOc1bIhjCxSeZEuIHJO4NSY_KDTUVGiTuTVQV2RVyfyijK1UF28315j5m4A--b8j3oRbC8CWJ796yGpbDwEA9YnMJOy0b8j5gV4eJ3x</recordid><startdate>201904</startdate><enddate>201904</enddate><creator>Liang, Xiaolong</creator><creator>Radosevich, Mark</creator><creator>Löffler, Frank</creator><creator>Schaeffer, Sean M.</creator><creator>Zhuang, Jie</creator><general>Elsevier Ltd</general><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7X8</scope><orcidid>https://orcid.org/0000-0002-5472-9118</orcidid><orcidid>https://orcid.org/0000-0002-3759-3976</orcidid></search><sort><creationdate>201904</creationdate><title>Impact of microbial iron oxide reduction on the transport of diffusible tracers and non-diffusible nanoparticles in soils</title><author>Liang, Xiaolong ; Radosevich, Mark ; Löffler, Frank ; Schaeffer, Sean M. ; Zhuang, Jie</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c428t-723820a49d6b3b8c81e9e96ff62699ddbfccbcd68a0c71742b0a294f12f38ed33</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><topic>Biostimulation</topic><topic>Iron reduction</topic><topic>Nanoparticles</topic><topic>Soil aggregates</topic><topic>Transport</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Liang, Xiaolong</creatorcontrib><creatorcontrib>Radosevich, Mark</creatorcontrib><creatorcontrib>Löffler, Frank</creatorcontrib><creatorcontrib>Schaeffer, Sean M.</creatorcontrib><creatorcontrib>Zhuang, Jie</creatorcontrib><collection>PubMed</collection><collection>CrossRef</collection><collection>MEDLINE - Academic</collection><jtitle>Chemosphere (Oxford)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Liang, Xiaolong</au><au>Radosevich, Mark</au><au>Löffler, Frank</au><au>Schaeffer, Sean M.</au><au>Zhuang, Jie</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Impact of microbial iron oxide reduction on the transport of diffusible tracers and non-diffusible nanoparticles in soils</atitle><jtitle>Chemosphere (Oxford)</jtitle><addtitle>Chemosphere</addtitle><date>2019-04</date><risdate>2019</risdate><volume>220</volume><spage>391</spage><epage>402</epage><pages>391-402</pages><issn>0045-6535</issn><eissn>1879-1298</eissn><abstract>In subsurface bioremediation, electron donor addition promotes microbial Fe(III)-oxide mineral reduction that could change soil pore structure, release colloids, and alter soil surface properties. These processes in turn may impact bioremediation rates and the ultimate fate of contaminants. Columns packed with water-stable, Fe-oxide-rich soil aggregates were infused with acetate-containing artificial groundwater and operated for 20 d or 60 d inside an anoxic chamber. Soluble Fe(II) and soil colloids were detected in the effluent within one week after initiation of the acetate addition, demonstrating Fe(III)-bioreduction and colloid formation. Diffusible Br−, less diffusible 2,6-difluorobenzoate (DFBA), and non-diffusible silica-shelled silver nanoparticles (SSSNP) were used as tracers in transport experiments before and after the bioreduction. The transport of Br− was not influenced by the bioreduction. DFBA showed earlier breakthrough and less tailing after the bioreduction, suggesting alterations in flow paths and soil surface chemistry during the 20-d bioreduction treatment. Similarly, the bioreduction increased the transport of SSSNP very significantly, with mass recovery increasing from 1.7% to 25.1%. Unexpectedly, the SSSNP was completely retained in the columns when the acetate injection was extended from 20 to 60 d, while the mass recovery of DFBA decreased from 89.1% to 84.1% and Br− showed no change. The large change in the transport of SSSNP was attributed to soil aggregate breakdown and colloid release (causing mechanical straining of SSSNP) and the exposure of iron oxide surfaces previously unavailable within aggregate interiors (facilitating attachment of SSSNP). These results suggest a time-dependent fashion of microbial effect on the transport of diffusivity-varying tracers. [Display omitted] •Fe(III)-bioreduction causes time-dependent aggregate breakdown and colloid release.•Short-term bioreduction alters soil surface chemistry and solute/nanoparticle transport.•Electron donor amendment enhances transport of nanoparticles.</abstract><cop>England</cop><pub>Elsevier Ltd</pub><pmid>30597359</pmid><doi>10.1016/j.chemosphere.2018.12.165</doi><tpages>12</tpages><orcidid>https://orcid.org/0000-0002-5472-9118</orcidid><orcidid>https://orcid.org/0000-0002-3759-3976</orcidid><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 0045-6535
ispartof Chemosphere (Oxford), 2019-04, Vol.220, p.391-402
issn 0045-6535
1879-1298
language eng
recordid cdi_proquest_miscellaneous_2162495020
source Elsevier ScienceDirect Journals Complete
subjects Biostimulation
Iron reduction
Nanoparticles
Soil aggregates
Transport
title Impact of microbial iron oxide reduction on the transport of diffusible tracers and non-diffusible nanoparticles in soils
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-04T03%3A40%3A11IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Impact%20of%20microbial%20iron%20oxide%20reduction%20on%20the%20transport%20of%20diffusible%20tracers%20and%20non-diffusible%20nanoparticles%20in%20soils&rft.jtitle=Chemosphere%20(Oxford)&rft.au=Liang,%20Xiaolong&rft.date=2019-04&rft.volume=220&rft.spage=391&rft.epage=402&rft.pages=391-402&rft.issn=0045-6535&rft.eissn=1879-1298&rft_id=info:doi/10.1016/j.chemosphere.2018.12.165&rft_dat=%3Cproquest_cross%3E2162495020%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2162495020&rft_id=info:pmid/30597359&rft_els_id=S0045653518325062&rfr_iscdi=true