4.8 Article

Chlorate Formation Mechanism in the Presence of Sulfate Radical, Chloride, Bromide and Natural Organic Matter

期刊

ENVIRONMENTAL SCIENCE & TECHNOLOGY
卷 52, 期 11, 页码 6317-6325

出版社

AMER CHEMICAL SOC
DOI: 10.1021/acs.est.8b00576

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资金

  1. Natural Science Foundation of China [21677181, 51378515]
  2. National Key Research Development Program of China [2016YFC0502803]
  3. Tip-top Scientific and Technical Innovative Youth Talents of Guangdong Special Support Program [2015TQ01Z552]
  4. Guangzhou Science Technology and Innovation Commission [201707010249]
  5. Science and Technology Project of Zhejiang Province [2017G33036]
  6. Fundamental Research Funds for the Central Universities [17lgzd21]
  7. University of Cincinnati
  8. Herman Schneider Professorship in the College of Engineering and Applied Sciences

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Halides and natural organic matter (NOM) are inevitable in aquatic environment and influence the degradation of contaminants in sulfate radical (SO4 center dot-)-based advanced oxidation processes. This study investigated the formation of chlorate in the coexposure of SO4 center dot-, chloride (Cl-), bromide (Br-) and/or NOM in UV/persulfate (UV/PDS) and cobalt(II)/ peroxymonosulfate (Co/PMS) systems. The formation of chlorate increased with increasing Cl- concentration in the UV/PDS system, however, in the Co/PMS system, it initially increased and then decreased. The chlorate formation involved the formation of hypochlorous acid/hypochlorite (HOCl/OCl-) as an intermediate in both systems. The formation was primarily attributable to SO4 center dot- in the UV/PDS system, whereas Co(III) played a significant role in the oxidation of Cl- to HOCl/OCl- and SO4 center dot- was important for the oxidation of HOCl/OCl- to chlorate in the Co/PMS system. The pseudo-first-order rate constants (k') of the transformation from Cl- to HOCl/OCl- were 3.32 x 10(-6) s(-1) and 9.23 X 10(-3) s(-1) in UV/PDS and Co/PMS, respectively. Meanwhile, k' of HOCl/OCl- to chlorate in UV/PDS and Co/PMS were 2.43 x 10(-3) s(-1) and 2.70 X 10(-4) s(-1), respectively. Br- completely inhibited the chlorate formation in UV/PDS, but inhibited it by 45.2% in Co/PMS. The k' of SO(4)(center dot-)reacting with Br- to form hypobromous acid/hypobromite (HOBr/OBr-) was calculated to be 378 times higher than that of Cl- to HOCl/OCl-, but the k' of Co(III) reacting with Br- to form HOBr/OBr- was comparable to that of Cl- to HOClOCl-. NOM also significantly inhibited the chlorate formation, due to the consumption of SO4 center dot- - and reactive chlorine species (RCS, such as Cl center dot, ClO center dot and HOCl/OCl-). This study demonstrated the formation of chlorate in SO4 center dot- -based AOPs, which should to be considered in their application in water treatment.

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