@article{
 title = {Depth profiles of volatile halogenated hydrocarbons in seawater in the Bay of Bengal.},
 type = {article},
 year = {2001},
 identifiers = {[object Object]},
 keywords = {Environmental Monitoring,Hydrocarbons, Halogenated,Hydrocarbons, Halogenated: analysis,Phytoplankton,Tropical Climate,Volatilization,Water Movements,Water Pollutants, Chemical,Water Pollutants, Chemical: analysis},
 pages = {371-7},
 volume = {45},
 websites = {http://www.ncbi.nlm.nih.gov/pubmed/11592427},
 month = {10},
 id = {93b83a46-3509-3d15-a1b8-4ec75ff6c3a6},
 created = {2014-05-31T04:15:19.000Z},
 file_attached = {true},
 profile_id = {9edae5ec-3a23-3830-8934-2c27bef6ccbe},
 group_id = {63e349d6-2c70-3938-9e67-2f6483f6cbab},
 last_modified = {2014-11-19T06:03:13.000Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 abstract = {Measurements were made of bromocarbons (CHBr3 and CH2Br2), iodocarbons (CH2I2 and CH2ClI), and dimethylsulfide (DMS, CH3SCH3) in seawater collected from the Bay of Bengal under tropical stratified conditions. These compounds showed different depth profiles, characteristic of each group. CH2I2 and CH2ClI showed very similar depth profiles to chlorophyll-a, suggesting their production by phytoplankton followed by rapid decay in seawater. The CH2I2 maximum at a depth a little below the CH2ClI maximum was consistent with its more significant photolytic decay. The bromocarbons were less localized in their distributions than were the iodocarbons, suggesting their longer residence time in seawater after their release from phytoplankton. Both of these profiles were different from the pattern of DMS, which had its maxima above the chlorophyll-a maximum layer near the surface.},
 bibtype = {article},
 author = {Yamamoto, H and Yokouchi, Y and Otsuki, a and Itoh, H},
 journal = {Chemosphere},
 number = {3}
}

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