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-197-<br />

markedly during the late-winter phytoplankton blooms of 1977 and 1978.<br />

.-.<br />

Oxidation of algal unsaturated fatty ac!d~ may also produce these alde-<br />

hydes in coastal seawater as suggested for open-ocean seawater.<br />

In addition, C12-C15 aldehydes occurred at very high concentrations<br />

in February, 1978. Tridecanal was recovered at more than 100 ng/kg.<br />

Cultures in log and stationary growth phase of Thalassiosira nordenskioeldii,<br />

the predominant diatom found in the late-winter bloom, did not produce<br />

these aldehydes. Oxidation by zooplankton or photochemically-produced free<br />

radicals may be necessary to produce these aldehydes from algal metabolites.<br />

Dimethyl di-, tri-, and tetrasulfides were found at up to 20 ng/kg<br />

in coastal seawater. The observation that the first 2 hours of stripping<br />

frequently recovered less of these polysulfides than Æn additional 2 hours<br />

of stripping led to the conclusion that formation of these volatile sulfur<br />

compounds must occur within the sample. Marine microorganisms are known<br />

to produce methyl mercaptan, which may be oxidized to dimethyldisulfide.<br />

Reaction 0~methyl mercaptan or dimethyldisulfide with elemental sulfur<br />

will yield other polysulfides. These polysulfides may also be derived<br />

from degradation of other polysulfide metabolites.<br />

Ci- and C1-benzenes in Coastal Seawater<br />

Additional work was performed to describe the sources of the C2- and<br />

C3-benzenes to coastal seawater. Short-term studies carried out over<br />

sumer weekends showed that large inputs of these pollutants occurred at<br />

these times (2-10 fold concentration. increases). The highest concentrations<br />

ever found coincided with ski boat activity in the immediate vicinity of<br />

the sampling site. The C2- and C3-benzene isomer distribution of the

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