Full metadata record
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Changyu Moon | - |
| dc.contributor.author | Sang Hyun Kim | - |
| dc.contributor.author | Jaeshik Chung | - |
| dc.contributor.author | Kyoungphile Nam | - |
| dc.date.accessioned | 2026-02-06T07:30:07Z | - |
| dc.date.available | 2026-02-06T07:30:07Z | - |
| dc.date.created | 2026-02-04 | - |
| dc.date.issued | 2025-12 | - |
| dc.identifier.issn | 1598-6438 | - |
| dc.identifier.uri | https://pubs.kist.re.kr/handle/201004/154235 | - |
| dc.description.abstract | This study evaluated the potential of montmorillonite as a reactive medium for Cr(VI) remediation through dithionitemediatedreduction of structural Fe(III) to Fe(II). Batch experiments revealed that dithionite treatment generated up to 19.1 mg/gFe(II), representing 83% of total structural iron (23 mg/g). The reduction behavior was governed by redox potentialequilibrium rather than reductant concentration. The generated Fe(II) effectively reduced Cr(VI) following a 3:1 stoichiometry,with all Fe(II) quantitatively consumed for Cr(VI) removal. Solid-phase analysis using SEM-EDS and XPS confirmed thatreduced Cr(III) was immobilized as Cr(OH)3 on clay surfaces, with no aqueous total chromium detected. In the columnexperiments, a 2 PV pulse injection of 50 mM dithionite lowered the ORP to -200 mV and generated structural Fe(II)within the medium. Following dithionite flushing, continuous injection of Cr(VI) solution exhibited delayed breakthroughup to 10 PV, indicating that the structural Fe(II) within the solid matrix served as an electron donor for Cr(VI) reduction. Sectional analysis and EPMA mapping confirmed immobilized Cr associated with montmorillonite particles. Dithionitereinjection successfully regenerated the reductive zone and restored the Cr(VI) removal capacity, thereby extending theoperational lifetime of the reactive medium. | - |
| dc.language | Korean | - |
| dc.publisher | 한국지하수토양환경학회 | - |
| dc.title | 철 함유 점토광물의 전자 매개를 이용한 환원구역 생성과이를 통한 6가 크롬의 고정화 | - |
| dc.title.alternative | Immobilization of Hexavalent Chromium Through Reductive Zones Generated by Fe-bearing Clay Mineral Acting as an Electron Mediator | - |
| dc.type | Article | - |
| dc.identifier.doi | 10.7857/JSGE.2025.30.6.063 | - |
| dc.description.journalClass | 2 | - |
| dc.identifier.bibliographicCitation | 지하수토양환경, v.30, no.6, pp.63 - 72 | - |
| dc.citation.title | 지하수토양환경 | - |
| dc.citation.volume | 30 | - |
| dc.citation.number | 6 | - |
| dc.citation.startPage | 63 | - |
| dc.citation.endPage | 72 | - |
| dc.description.isOpenAccess | N | - |
| dc.description.journalRegisteredClass | kci | - |
| dc.identifier.kciid | ART003291717 | - |
| dc.type.docType | Y | - |
| dc.subject.keywordAuthor | Hexavalent chromium | - |
| dc.subject.keywordAuthor | Fe-bearing montmorillonite | - |
| dc.subject.keywordAuthor | Structural Fe(II) | - |
| dc.subject.keywordAuthor | In situ reductive zone | - |
Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.