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"Also, short range transport and deposition should be measured in<br />

field studies performed in coastal regions relatively close to<br />

maj or urban sources. A prime site for such a study is the area<br />

off the northeast coast of the United States. "<br />

NAS, 1978<br />

Chapter 4. SOURCE OF Ci- and C~-ALKYLATED BENZENES TO COASTAL SEAWATER<br />

INTRODUCTION<br />

Recently there has been a great deal of discussion concerning the<br />

tropospheric transport of petroleum-derived hydrocarbons to the oceans<br />

(Duce et al., 1974; NAS, 1975b; Garrett and Smagin, 1976; NAS, 1978).<br />

5<br />

Approximately 6 x lO metric tons of petroleum hydrocarbons per year are<br />

estimated to be delivered to the sea by the atmosphere (NAS, 1975b). This<br />

amounts to 10% of the estimated total petroleum hydrocarbon input to the<br />

marine environment.<br />

The gaseous hydrocarbons in urban air are chiefly benzene homologues<br />

(NAS, 1978). Several investigators have reported between i and 40 ng<br />

individuaIC2- and C3-benzenes/l-urban-air (Grob and Grob, 1971; Altshuller<br />

et al." 1971; Bertsch et al., 1974; Ciccioli et al., 1976). Lonneman et<br />

al. (1978) have found 0.2-4 ng/l-air in regions of Florida, including the<br />

Everglades. If air parcels with these concentrations were equilibrated<br />

wi th coas tal seawater, water levels of 0.3- 120 ng/kg-seawa ter would result.<br />

This includes the range of values found for the C2- and C3-benzenes in a<br />

year-round study of coastal seawater (Chapter 3; Schwarzenbach et al. ,1978).<br />

-141-

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