Analysis of extinction in ultraviolet and visible spectra of water bodies of the Paraguay and Brazil wetlands
The extinction spectra in ultraviolet and visible radiation were analyzed using filtered and unfiltered water samples obtained in 11 open water bodies in the Ñeembucù (Paraguay) and Pantanal (Brazil) wetlands. The role of dissolved and suspended matter in the total extinction was analyzed between 26...
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Published in | Chemosphere (Oxford) Vol. 57; no. 10; pp. 1245 - 1255 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
Oxford
Elsevier Ltd
01.12.2004
Elsevier |
Subjects | |
Online Access | Get full text |
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Summary: | The extinction spectra in ultraviolet and visible radiation were analyzed using filtered and unfiltered water samples obtained in 11 open water bodies in the Ñeembucù (Paraguay) and Pantanal (Brazil) wetlands. The role of dissolved and suspended matter in the total extinction was analyzed between 260
nm and 700
nm. The chromophoric dissolved organic matter (CDOM) was the major component in extinction of considered ultraviolet radiation (260–400
nm). The differences in CDOM concentrations explained the main pattern of extinction of the ultraviolet radiation in the samples. Nevertheless, differences between the studied water bodies were found also to depend on the rate of photodegradation and photobleaching. The methodology developed in the present study was to distinguish “humic optic waters” according to quantity and quality of dissolved and suspended matter present. In the “humic optic water”, the penetration of 10% of incident UV radiation and the photoactive layer are estimated. The influence of particulate matter increases in the total extinction of the wavelengths higher than 400
nm. The integral of the extinction curve of suspended matter in the visible wavelengths (400–700
nm) was found to relate with the total suspended solids and chlorophyll concentrations. |
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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0045-6535 1879-1298 |
DOI: | 10.1016/j.chemosphere.2004.08.050 |