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Consecutive reduction of Cr(VI) by Fe(II) formed through photo-reaction of iron-dissolved organic matter originated from biochar

Authors
Kim, Hye-BinKim, Jong-GookKim, Seon-HeeKwon, Eilhann E.Baek, Kitae
Issue Date
Oct-2019
Publisher
ELSEVIER SCI LTD
Keywords
Biochar; Redox; Iron complex; Dissolved organic matter (DOM); Photo-induced Fe(III) reduction; Cr(VI)
Citation
ENVIRONMENTAL POLLUTION, v.253, pp.231 - 238
Indexed
SCIE
SCOPUS
Journal Title
ENVIRONMENTAL POLLUTION
Volume
253
Start Page
231
End Page
238
URI
https://scholarworks.bwise.kr/hanyang/handle/2021.sw.hanyang/189534
DOI
10.1016/j.envpol.2019.07.026
ISSN
0269-7491
Abstract
Employing biochar for environmental remediation has been widely practiced. Nonetheless, the reduction mechanisms of hexavalent chromium (Cr(VI)) in the presence of biochar have not been fully elucidated (i.e., direct or indirect reduction of Cr(VI) by biochar). In particular, the effect of light on Cr(VI) reduction by biochar was rarely reported. Thus, to clarify the reduction mechanisms of Cr(VI) by biochar at the fundamental level, this study laid great emphasis on the photo-induced reduction of Cr(VI) in the application of biochar. Biochar releases dissolved organic matter (DOM), the DOM can extract Fe(III) from soil by complexation, and the complexes can be photo-reacted under the light. In these respects, Fe(II) formed by the photo-induced reaction of DOM-Fe(III) was particularly evaluated in this study. To evaluate that, three biomass samples (rice straw, granular sludge from an up-flow anaerobic sludge blanket, and spent coffee ground) were torrefied to biochar. To circumvent the adsorption of Cr(VI) onto biochar, biochar extractives (served as a source for DOM) and Fe(III) solution were tested with/without UV light to prove Fe(II) formation. This study experimentally proved that the more Fe(II) under the UV radiation was formed in the co-existence with biochar extractives and Fe(III). All experimental data from three biochar samples were indeed very similar. Cr(VI) reduction by Fe(II) from GB, RB, and CB reached up to 96, 79, and 100%, respectively. The different reduction efficiency signified that the low molecular weight of organic acids, such as oxalate, were more sensitive to the UV light, thereby resulting in the enhanced Fe(II) formation. Such Fe(II) formation subsequently led to the high reduction efficiency of Cr(VI).
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Kwon, Eilhann E.
COLLEGE OF ENGINEERING (DEPARTMENT OF EARTH RESOURCES AND ENVIRONMENTAL ENGINEERING)
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