Distributions and sea-to-air fluxes of volatile halocarbons in the East China Sea in early winter

The concentrations of six volatile halogenated organic compounds (VHOC)-chloroform (CHCl(3)), trichloroethylene (C(2)HCl(3)), tetrachloroethylene (C(2)Cl(4)), carbon tetrachloride (CCl(4)), methylchloroform (CH(3)CCl(3)), and bromoform (CHBr(3)) in the East China Sea (ECS) in November and December 2010 were measured by a purge and trap system coupled to a gas chromatograph with an electron capture detection (ECD). Mean (range) concentrations of CHCl(3), C(2)HCl(3), C(2)Cl(4), CH(3)CCl(3), CCl(4) and CHBr(3) in the surface water were 16.90 (0.40-62.92), 16.27 (2.78-83.33), 2.40 (0.39-9.33), 32.29 (19.72-57.68), 1.70 (0.39-8.73) and 17.11 (4.33-34.46) pM, respectively. With the exception of C(2)HCl(3), the concentrations of other five kinds of VHOC generally exhibited a decreasing trend with distance from the coast, with the low values found in the open sea. The anthropogenic sources contributed to the elevated levels of CCl(4) and CH(3)CCl(3), whereas a combination of the anthropogenic and biogenic sources might be responsible for the elevated levels of CHCl(3), C(2)HCl(3), C(2)Cl(4) and CHBr(3). In the depth profiles, vertical distributions of the six VHOC in the water column were complicated, with the maxima occurring at 0-100 m depths. The mean sea-to-air fluxes of CHCl(3), C(2)HCl(3), C(2)Cl(4) and CHBr(3) were estimated to be 21.08, 29.94, 2.05 and 35.50 nmol m(-2) d(-1), respectively, indicating that the ECS was a source for the four VHOC in the atmosphere.

Assessing California groundwater susceptibility using trace concentrations of halogenated volatile organic compounds

Twenty-four halogenated volatile organic compounds (hVOCs) and SF₆ were measured in groundwater samples collected from 312 wells across California at concentrations as low as 10⁻¹² grams per kilogram groundwater. The hVOCs detected are predominately anthropogenic (i.e., "ahVOCs") and as such their distribution delineates where groundwaters are impacted and susceptible to human activity. ahVOC detections were broadly consistent with air-saturated water concentrations in equilibrium with a combination of industrial-era global and regional hVOC atmospheric abundances. However, detection of ahVOCs in nearly all of the samples collected, including ancient groundwaters, suggests the presence of a sampling or analytical artifact that confounds interpretation of the very-low concentration ahVOC data. To increase our confidence in ahVOC detections we establish screening levels based on ahVOC concentrations in deep wells drawing ancient groundwater in Owens Valley. Concentrations of ahVOCs below the Owens Valley screening levels account for a large number of the detections in prenuclear groundwater across California without significant loss of ahVOC detections in shallow, recently recharged groundwaters. Over 80% of the groundwaters in this study contain at least one ahVOC after screening, indicating that the footprint of human industry is nearly ubiquitous and that most California groundwaters are vulnerable to contamination from land-surface activities.