Formation of iodinated products in Fe (II)/peroxydisulfate (PDS) system

The transformation of iodide (I−) and hypoiodous acid (IO−) by Fe (II)-activated peroxydisulfate (PDS) in the presence of natural organic matter (NOM) was investigated. In the water of a reservoir in Shenzhen, four kinds of organic matter were detected: iodoform > diiodo-bromomethane > dibromo...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Zijun Dong, Mu Li, Meifen Chen, Yurong Gu, Chengchun Jiang, Feiyun Sun
Formato: article
Lenguaje:EN
Publicado: IWA Publishing 2021
Materias:
Acceso en línea:https://doaj.org/article/58c4ed89b4f142379c639373d40e8549
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:doaj.org-article:58c4ed89b4f142379c639373d40e8549
record_format dspace
spelling oai:doaj.org-article:58c4ed89b4f142379c639373d40e85492021-11-06T07:12:08ZFormation of iodinated products in Fe (II)/peroxydisulfate (PDS) system1606-97491607-079810.2166/ws.2020.254https://doaj.org/article/58c4ed89b4f142379c639373d40e85492021-05-01T00:00:00Zhttp://ws.iwaponline.com/content/21/3/1016https://doaj.org/toc/1606-9749https://doaj.org/toc/1607-0798The transformation of iodide (I−) and hypoiodous acid (IO−) by Fe (II)-activated peroxydisulfate (PDS) in the presence of natural organic matter (NOM) was investigated. In the water of a reservoir in Shenzhen, four kinds of organic matter were detected: iodoform > diiodo-bromomethane > dibromo-iodomethane > dichloromethane. As pH increased from 3 to 10, I− conversion rate decreased from 31.0% to 11.0%. There is basically no iodic acid () generated under alkaline conditions, probably due to these organic matters. When PDS concentration is low, PDS can oxidize part of I− to IO−, and the oxidation of I− into reaction and continued oxidation reaction exist at the same time, so some is generated in the system. As the proportion of Fe (II) increases, the generation rate of gradually increases. When Fe2+/PDS is 1:5, 2:5, and 3:5, the conversion rates of are 4.7%, 6.5%, and 8.4%, respectively. There are two main reasons for this: (i) the reaction of IO− produced in the system with humic acid (HA) inhibits the further conversion of IO− to ; (ii) both HA and I- in the system can react with PDS, resulting in a reduction in the oxidation rate of I−. HIGHLIGHTS Formation of I-DBPs by Fe (II)/PDS process in real water was evaluated.; I-DBPs generation in various reaction conditions was examined.; Existence of HA showed apparent inhibition on IO3− generation.;Zijun DongMu LiMeifen ChenYurong GuChengchun JiangFeiyun SunIWA Publishingarticlefe (ii)iodidenatural organic matter (nom)peroxydisulfate (pds)Water supply for domestic and industrial purposesTD201-500River, lake, and water-supply engineering (General)TC401-506ENWater Supply, Vol 21, Iss 3, Pp 1016-1024 (2021)
institution DOAJ
collection DOAJ
language EN
topic fe (ii)
iodide
natural organic matter (nom)
peroxydisulfate (pds)
Water supply for domestic and industrial purposes
TD201-500
River, lake, and water-supply engineering (General)
TC401-506
spellingShingle fe (ii)
iodide
natural organic matter (nom)
peroxydisulfate (pds)
Water supply for domestic and industrial purposes
TD201-500
River, lake, and water-supply engineering (General)
TC401-506
Zijun Dong
Mu Li
Meifen Chen
Yurong Gu
Chengchun Jiang
Feiyun Sun
Formation of iodinated products in Fe (II)/peroxydisulfate (PDS) system
description The transformation of iodide (I−) and hypoiodous acid (IO−) by Fe (II)-activated peroxydisulfate (PDS) in the presence of natural organic matter (NOM) was investigated. In the water of a reservoir in Shenzhen, four kinds of organic matter were detected: iodoform > diiodo-bromomethane > dibromo-iodomethane > dichloromethane. As pH increased from 3 to 10, I− conversion rate decreased from 31.0% to 11.0%. There is basically no iodic acid () generated under alkaline conditions, probably due to these organic matters. When PDS concentration is low, PDS can oxidize part of I− to IO−, and the oxidation of I− into reaction and continued oxidation reaction exist at the same time, so some is generated in the system. As the proportion of Fe (II) increases, the generation rate of gradually increases. When Fe2+/PDS is 1:5, 2:5, and 3:5, the conversion rates of are 4.7%, 6.5%, and 8.4%, respectively. There are two main reasons for this: (i) the reaction of IO− produced in the system with humic acid (HA) inhibits the further conversion of IO− to ; (ii) both HA and I- in the system can react with PDS, resulting in a reduction in the oxidation rate of I−. HIGHLIGHTS Formation of I-DBPs by Fe (II)/PDS process in real water was evaluated.; I-DBPs generation in various reaction conditions was examined.; Existence of HA showed apparent inhibition on IO3− generation.;
format article
author Zijun Dong
Mu Li
Meifen Chen
Yurong Gu
Chengchun Jiang
Feiyun Sun
author_facet Zijun Dong
Mu Li
Meifen Chen
Yurong Gu
Chengchun Jiang
Feiyun Sun
author_sort Zijun Dong
title Formation of iodinated products in Fe (II)/peroxydisulfate (PDS) system
title_short Formation of iodinated products in Fe (II)/peroxydisulfate (PDS) system
title_full Formation of iodinated products in Fe (II)/peroxydisulfate (PDS) system
title_fullStr Formation of iodinated products in Fe (II)/peroxydisulfate (PDS) system
title_full_unstemmed Formation of iodinated products in Fe (II)/peroxydisulfate (PDS) system
title_sort formation of iodinated products in fe (ii)/peroxydisulfate (pds) system
publisher IWA Publishing
publishDate 2021
url https://doaj.org/article/58c4ed89b4f142379c639373d40e8549
work_keys_str_mv AT zijundong formationofiodinatedproductsinfeiiperoxydisulfatepdssystem
AT muli formationofiodinatedproductsinfeiiperoxydisulfatepdssystem
AT meifenchen formationofiodinatedproductsinfeiiperoxydisulfatepdssystem
AT yuronggu formationofiodinatedproductsinfeiiperoxydisulfatepdssystem
AT chengchunjiang formationofiodinatedproductsinfeiiperoxydisulfatepdssystem
AT feiyunsun formationofiodinatedproductsinfeiiperoxydisulfatepdssystem
_version_ 1718443795744292864