1. Dichloromethane in the Indian Ocean: Evidence for in-situ production in seawater
- Author
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Ooki, Atsushi and Yokouchi, Yoko
- Subjects
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DICHLOROMETHANE , *HALOCARBONS , *MARINE phytoplankton , *TEMPERATURE , *SEAWATER , *SUMMER , *CARBENES - Abstract
Abstract: We measured partial pressures of CH2Cl2 (dichloromethane) and CCl3F (CFC-11) in air and surface seawater of the Indian and Southern Oceans from November 2009 to January 2010. The excess CH2Cl2 saturation anomaly (ΔSACH2Cl2 >0) in surface seawater between 10°S and 40°S, which is the corrected value of saturation anomaly after subtracting the effects of summertime sea-surface temperature increase and of summertime decrease of atmospheric CH2Cl2 level, provides evidence for in-situ production of CH2Cl2. Depth profiles from the South Indian Ocean at 5°S, 20°S and 30°S showed concentration maxima of dihalomethanes (CH2I2, CH2ClI and CH2Cl2) and chlorophyll-a in the subsurface layer (20–150m). Our data suggest that phytoplankton production of dihalomethanes leads to concentration maxima in the subsurface layer and ΔSACH2Cl2 >0 in surface seawater between 10°S and 40°S. The average oceanic emission of CH2Cl2 derived from the region between 10°S and 40°S in the South Indian Ocean was calculated to be 0.29–0.43μg m−2 d−1. [Copyright &y& Elsevier]
- Published
- 2011
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