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-152- ,<br />

(figure 4-3). Propyl benzene showed a strong negative deviation (-80%)<br />

from its mean ratio to o-xylene in August. Ethyl benzene also showed this<br />

effect, although less pronounced (-50%). Grob and Grob (1974) also saw<br />

strong relative removal of these compounds in Lake Zurich when water temper-<br />

o<br />

atures were above 20 C. They suggested that biological degradation was<br />

occurring by a microorganism suited to these warm temperatures and capable<br />

of metabolizing the elongated sidechains. A warm-weather metabolic degrada-<br />

tion of these compounds may also occur in the coastal zone near CD.<br />

Mesitylene (1,3, 5-trimethyl benzene) showed a 3-fold relative maximum<br />

in September at CD. This compound was also found in relative abundance in<br />

marsh samples (Schwarzenbach et al., 1978). Possibly an unknbwn biological<br />

source of this compound exists.<br />

O-xylene in Seawater from Other Vineyarò Sound Stations.<br />

Four investigations of the concentrations of the C2- and C3-alkylated<br />

benzenes in surface water from Vineyard - Nantucket Sound were conducted.<br />

Samples were obtained within 3 km of CD. Salinity data are available from<br />

3 of these studies (figure 4-4) and, along with knowledge of the tide at<br />

the time of sampling, have been used to draw the lines of flow shown.<br />

Salinity always increased offshore from CD. It appears that the shoals,<br />

about 2 km off CD, do not provide a major barrier to mixing of surface<br />

waters.<br />

The concentrations of o-xylene in seawater from these stations are<br />

shown in figure 4-5. No trends were consistently observed. Al though there<br />

were always significant concentration differences, e.g. between samples from<br />

stations at CD and 0.8 km. offshore, sometimes offshore levels were lower

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