AIR WATER EXCHANGE DYNAMICS OF 13 VOLATILE CHLORINATED C1-HYDROCARBONS AND C2-HYDROCARBONS AND MONOCYCLIC AROMATIC-HYDROCARBONS IN THE SOUTHERN NORTH-SEA AND THE SCHELDT ESTUARY/
Jp. Dewulf et al., AIR WATER EXCHANGE DYNAMICS OF 13 VOLATILE CHLORINATED C1-HYDROCARBONS AND C2-HYDROCARBONS AND MONOCYCLIC AROMATIC-HYDROCARBONS IN THE SOUTHERN NORTH-SEA AND THE SCHELDT ESTUARY/, Environmental science & technology, 32(7), 1998, pp. 903-911
Whereas a lot of marine research work has been done on heavy metals an
d semivolatile organic compounds, far less attention has been paid to
the fate of volatile organic compounds in this area. This work focuses
on 13 volatile organic compounds in marine waters and the marine atmo
sphere. During six campaigns in September 1994-December 1995, simultan
eous air and water sampling was carried out in both the southern North
Sea area and the Scheldt Estuary. Mean water concentrations for indiv
idual compounds were in the 2.2-72.9 ppt range (n = 38), whereas atmos
pheric concentrations varied between 2.3 and 854 pptv. Samples from th
e Scheldt Estuary proved to have elevated concentrations of chlorinate
d compounds. A number of water and air samples showed enhanced concent
rations of C-2-substituted monocyclic aromatic hydrocarbons, which cou
ld not clearly be linked to anthropogenic activities. Back-trajectory
calculations showed that a number of over sea atmospheric samples were
affected by atmospheric transport from industrial sites, 250-300 km u
p wind. Fugacity modeling showed that the North Sea acts as a source t
o the atmosphere, not as a sink. Mean water to air mass transfer rates
varied between 0.6-52.7 mu g m(-2) day(-1) for all VOCs. it was stati
stically shown that water to air exchange rates of tetrachloroethylene
, benzene, and toluene were slowed when air masses from continental or
igin were at the marine sampling sites instead of air masses from remo
te non-continental origin.