Abstract
AbstractVinyl chloride (VC) is a common risk driver in vapor intrusion (VI) studies. At many sites, initial screening shows potential indoor air impacts for VC at unacceptable levels. During follow‐up site characterization, however, the VI pathway for VC is rarely if ever found to be complete. This paper sets forth a conceptual model for understanding these results and summarizes data from several field sites to illustrate the concepts. VC can be formed under anaerobic conditions via reductive dechlorination of tetrachloroethylene or trichloroethylene. The ultimate fate of any VC that is produced depends on the amount of available oxygen. If sufficient oxygen is available, VC will readily undergo aerobic biodegradation. Data are presented for multiple field sites to illustrate the fate and transport of VC. The sites are drawn from various regions of the United States and cover a range of conditions. At these sites, VC was detected at relatively high concentrations in groundwater. It may also have been detected in deeper soil gas, but generally was fully attenuated before reaching shallow soil depths. Indoor air results were consistently non‐detect. The behavior is also discussed for sites with very shallow groundwater, where VC was found in some subslab soil gas samples but not in the overlying indoor air.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
