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Gschwend%20thesis.pdf

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-28-<br />

Recently, methods have been developed for the semiquantitative<br />

analysis of volatile organic compounds in aqueous samples (Zlatkis<br />

et aL., 1973; Grob, 1973; Bellar and Lichtenberg, 1974; May et aLi,<br />

1975; Grob and ZUrcher, 1976). Study of this fraction of the<br />

organic matter in seawater has been neglected in the past due to a<br />

lack of suitable methods.<br />

It was the intention of this work to apply gas-phase stripping<br />

and solid-adsorbent trapping methods to the analysis of open-ocean<br />

seawater samples in order to assess the importance of this volatile<br />

organic fraction. Moreover, because the method is based only on<br />

the criterion of "stripability" (see Methods), many diverse organic<br />

compounds containing alkyl -, alkenyl -, aryl -, carbonyl -, alkoxy-,<br />

acyl-, and/or halo-functional groups could be represented and be<br />

used to study the chemistry of compounds containing these moieties<br />

in the environment.<br />

Three markedly different open-ocean regions were investigated:<br />

the Sargasso Sea near Bermuda, the western Equatorial Atlantic, and<br />

the Peru upwelling region. The first two have low primary produc-<br />

tivity while the third is known for its extremely high production.<br />

The western Equatorial Atlantic is influenced by a riverine input<br />

(Amzon) (Ryther et al., 1967). Different atmospheric transport<br />

patterns would be expected for these regions as the Sargasso Sea<br />

receives volatile inputs, including industrial materials, from the<br />

North American continent (Harvey and Steinhauer, 197 6), but the<br />

western Equatorial Atlantic and the region off Peru should show the<br />

effect of dust and organic vapor transport from arid land.s (Zuta et<br />

aL., 1975; Simoneit et al.,. 1977). The Peru upwelling region is<br />

oxygen deficient in midwater and is underlain by anoxic sediments.

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