Please use this identifier to cite or link to this item: http://hdl.handle.net/11455/68791
標題: Chromate removal as influenced by the structural changes of soil components upon carbonization at different temperatures
作者: Chen, K.Y.
Liu, J.C.
Chiang, P.N.
Wang, S.L.
Kuan, W.H.
Tzou, Y.M.
Deng, Y.
Tseng, K.J.
Chen, C.C.
Wang, M.K.
關鍵字: Chromate
Carbonization
Reduction
Soil organic matter
organic-matter
fulvic-acid
cr(vi)
reduction
fire
mechanisms
adsorption
chromium
forest
carbon
期刊/報告no:: Environmental Pollution, Volume 162, Page(s) 151-158.
摘要: Surface fire could induce heat transferring into the soil, creating a carbonized environment, which may alter the chemical compositions of soil organic matters (SOM). In the study, a surface soil was carbonized at up to 600 degrees C with limited air to simulate soils experiencing a surface fire, and Cr(VI) removal on the carbonized soils was investigated. NMR and FTIR analyses demonstrated a remarkable change of SOM structures at 300-400 degrees C. TGA-MS spectra indicated that (e.g. C2H4, CH3OH and C3H8) were the major components in the evolved gases from the pyrolyzed soil. A maximum amount of Cr(VI) removal (ca. 4 mg g(-1) soil) occurred for the 200 degrees C-carbonized soils, attributed mainly to a significant increase of Cr(VI) reduction by 0.1 M KCl extractable organic carbon (EOC) with abundant carboxylic groups. Nonetheless, the formation of aromatic C upon carbonization of the soil at >400 degrees C may be responsible for Cr(VI) reduction. (C) 2011 Elsevier Ltd. All rights reserved.
URI: http://hdl.handle.net/11455/68791
ISSN: 0269-7491
文章連結: http://dx.doi.org/10.1016/j.envpol.2011.10.036
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