| Literature DB >> 33255777 |
Carol J Miller1,2, Melissa Runge-Morris1,3, Andrea E Cassidy-Bushrow1,4, Jennifer K Straughen1,4, Timothy M Dittrich1,2, Tracie R Baker1,3,5, Michael C Petriello1,3,5, Gil Mor1,6, Douglas M Ruden1,3,5,7, Brendan F O'Leary1,2, Sadaf Teimoori2, Chandra M Tummala2, Samantha Heldman5, Manisha Agarwal3, Katherine Roth3, Zhao Yang3, Bridget B Baker1,3.
Abstract
Volatile organic compounds (VOCs) are a group of aromatic or chlorinated organic chemicals commonly found in manufactured products that have high vapor pressure, and thus vaporize readily at room temperature. While airshed VOCs are well studied and have provided insights into public health issues, we suggest that belowground VOCs and the related vapor intrusion process could be equally or even more relevant to public health. The persistence, movement, remediation, and human health implications of subsurface VOCs in urban landscapes remain relatively understudied despite evidence of widespread contamination. This review explores the state of the science of subsurface movement and remediation of VOCs through groundwater and soils, the linkages between these poorly understood contaminant exposure pathways and health outcomes based on research in various animal models, and describes the role of these contaminants in human health, focusing on birth outcomes, notably low birth weight and preterm birth. Finally, this review provides recommendations for future research to address knowledge gaps that are essential for not only tackling health disparities and environmental injustice in post-industrial cities, but also protecting and preserving critical freshwater resources.Entities:
Keywords: adverse birth outcomes; health disparities; remediation; urban; vapor intrusion; volatile organic compounds
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Substances:
Year: 2020 PMID: 33255777 PMCID: PMC7728359 DOI: 10.3390/ijerph17238755
Source DB: PubMed Journal: Int J Environ Res Public Health ISSN: 1660-4601 Impact factor: 4.614
Figure 1Vapor intrusion pathways [62].
Figure 2Detroit brownfield locations that can serve as sources of VOCs [68]. Note that Highland Park and Hamtramck are not part of the city of Detroit.
Figure 3Regional flow features of shallow groundwater in Detroit. Flow rate is primarily towards the southeast.
Figure 4Local flow features of shallow groundwater in Recovery Park, Detroit. Flow rate is directed towards the north/northeast.