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Gschwend%20thesis.pdf

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-190-<br />

study in some summer samples (Schwarzenbach et al., 1978; chapter 3)<br />

and in the August and October control seawater samples of this study.<br />

Two dihalomethanes were also found. These were produced at<br />

about 0.1 times the rate of the trihalomethanes. This may reflect<br />

the greater difficulty of cleavage of the dihalo-2-keto-compounds<br />

relative to that of the trihalo analogues. The presence of iodine<br />

in both of these dihalocompounds would serve to' enhance this cleavage.<br />

o "<br />

X3C--C--R<br />

o<br />

" k/10?<br />

HX C--C--R<br />

,.<br />

2<br />

k<br />

)i<br />

o<br />

"<br />

X3 CH + HOCR<br />

o "<br />

X2 CH2 + HOCR<br />

Release rates on the order of several nglgm dry weight/day sug-<br />

gest that standing stocks of less than 1 ng/liter seawater would re-<br />

suIt. Thus detection by the FID would not be expected and indeed<br />

the CD year-round samples did not reveal the presence of these com-<br />

pounds. However, future work utilizing an electron capture detec-<br />

tor may be fruitful, since thia detector is particularly sensitive<br />

to halogenated compounds.<br />

Undoubtedly, many other compounds substituting halogens for one<br />

another were present in the algae of this investigation, but were<br />

not seen due to limitations of the methodology (e.g., iodoform may be<br />

too soluble and have too high a boiling point to be stripped).<br />

One potential problem with this study is that algae may be<br />

artificially induced to release. the volatiles to seawater by<br />

the experimental conditions. However, since algae do not have root<br />

systems, they do not die upon disengagement from the seafloor.

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