scholarly journals Bladder Cancer and Exposure to Water Disinfection By-Products through Ingestion, Bathing, Showering, and Swimming in Pools

2006 ◽  
Vol 165 (2) ◽  
pp. 148-156 ◽  
Author(s):  
C. M. Villanueva ◽  
K. P. Cantor ◽  
J. O. Grimalt ◽  
N. Malats ◽  
D. Silverman ◽  
...  
2011 ◽  
Vol 68 (5) ◽  
pp. 379-385 ◽  
Author(s):  
N. Costet ◽  
C. M. Villanueva ◽  
J. J. K. Jaakkola ◽  
M. Kogevinas ◽  
K. P. Cantor ◽  
...  

2015 ◽  
Vol 15 (4) ◽  
pp. 667-674 ◽  
Author(s):  
Steve E. Hrudey ◽  
John Fawell

2014 marks the 40th anniversary of the seminal discovery by Johannes Rook, in 1974, that trihalomethanes (THMs) were formed by the chlorination of natural organic matter (NOM) in drinking water. Since this discovery, which revolutionized how we viewed drinking water safety and quality, hundreds of other classes of disinfection by-products (DBPs) have been discovered. The finding in 1976 by the US National Cancer Institute that chloroform, the dominant THM, was a rodent carcinogen spurred a large number of epidemiology and toxicology studies into chlorinated drinking water. In 1985, this cancer finding was shown to be wrong. We should now be asking: What do we know about the human health impacts of DBPs in drinking water? Bladder cancer has been the most consistent finding from epidemiologic studies in North America and Europe and the possibility that chlorinated drinking water contributes an increased risk of bladder cancer remains a viable hypothesis. Despite some recent improvements in exposure assessments to focus on inhalation and dermal exposures rather than ingestion, no causal agent with sufficient carcinogenic potency has been identified, nor has a mechanistic model been validated. Consequently, a sensible precautionary approach to managing DBPs remains the only viable option based on four decades of evidence.


2021 ◽  
Vol 204 ◽  
pp. 117648
Author(s):  
Fatima El-Athman ◽  
Lisa Zehlike ◽  
Alexander Kämpfe ◽  
Ralf Junek ◽  
Hans-Christoph Selinka ◽  
...  

2002 ◽  
Vol 40 (2) ◽  
pp. 134-142 ◽  
Author(s):  
Michael J. Plewa ◽  
Yahya Kargalioglu ◽  
Danielle Vankerk ◽  
Roger A. Minear ◽  
Elizabeth D. Wagner

2016 ◽  
Vol 24 (2) ◽  
pp. 1509-1517 ◽  
Author(s):  
Yu Hu ◽  
Li Tan ◽  
Shao-Hui Zhang ◽  
Yu-Ting Zuo ◽  
Xue Han ◽  
...  

2007 ◽  
Vol 115 (11) ◽  
pp. 1569-1572 ◽  
Author(s):  
Dominique S. Michaud ◽  
Manolis Kogevinas ◽  
Kenneth P. Cantor ◽  
Cristina M. Villanueva ◽  
Monteserrat Garcia-Closas ◽  
...  

2008 ◽  
Vol 43 (1) ◽  
pp. 11-22 ◽  
Author(s):  
Rocio Aranda Rodriguez ◽  
Boniface Koudjonou ◽  
Brian Jay ◽  
Guy L. LeBel ◽  
Frank M. Benoit

Abstract A study was initiated to determine the presence of organic disinfection by-products (DBPs) in drinking water treated with chlorine dioxide (ClO2). One potential advantage for the use of ClO2 as a disinfectant is the reduced formation of organic DBPs. Generally, water treated with ClO2 produces chlorite and chlorate ions, but there is limited information regarding the presence of halogenated organic DBPs. Eight systems that use chlorine dioxide as part of the water disinfection process were investigated. All systems in this study applied chlorine as a primary or secondary disinfectant in addition to ClO2. To evaluate seasonal and spatial variations, water samples were collected during cold water (February to March 2003) and warm water (July to August 2003) months at five sites for each system: raw water (R, before treatment), treated water (T, after treatment but before distribution), and three points along the same distribution line (D1, D2, D3). Sampling and analysis were conducted according to established protocols. A suite of 27 organic DBPs including haloacetic acids (HAA), trihalomethanes (THM), haloacetonitriles (HAN), haloketones, haloacetaldehydes (HA), chloropicrin, and cyanogen chloride were examined. In addition, the concentration of oxyhalides (chlorite and chlorate ions) and auxiliary parameters were also determined. Chlorite was found in treated (T) and distributed (Dx) waters. The chlorite ion levels decreased along the distribution system (T > D1 > D2 > D3). At T sites, the levels ranged from 10 to 870 µg/L (winter), and from 300 to 1,600 µg/L (summer). Chlorite was not found in treated or distributed water in the one system that used ozone. Chlorate ion levels ranged from 20 to 310 µg/L (winter), and 80 to 318 µg/L (summer). Chlorate levels remained relatively constant throughout the distribution system. THM and eight HAA (HAA8) accounted for approximately 85% of the total DBPs (wt/wt) analyzed, followed by total HA (up to 7%) and HAN (3%). THM in distributed water were found at concentrations between 1.8 and 30.6 µg/L (winter), and 3.3 and 93.6 µg/L (summer). For HAA8, the levels ranged from 13 to 52 µg/L (winter), and 16 to 111 µg/L (summer). Chloral hydrate ranged from 0.2 to 5.2 µg/L (winter), and 0.4 to 12.2 µg/L (summer). The temporal and spatial variations observed in previous studies were confirmed in the current study as well.


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