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Environmental chemistry of rivers and lakes, part v: a comparative study of the chemical and physicochemical characteristics of organic carbon dissolved in river and lake waters
To determine the chemical and physicochemical characteristics of dissolved organic carbon in the Ado River and the Yasu River, the main rivers flowing into Lake Biwa, the adsorption behavior onto hydrous iron oxide (HIO) and the reactivity to KMnO sub(4) oxidant were investigated in parallel with me...
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Published in: | Limnology 2000-12, Vol.1 (3), p.171-176 |
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Main Authors: | , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that cite this one |
Online Access: | Get full text |
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Summary: | To determine the chemical and physicochemical characteristics of dissolved organic carbon in the Ado River and the Yasu River, the main rivers flowing into Lake Biwa, the adsorption behavior onto hydrous iron oxide (HIO) and the reactivity to KMnO sub(4) oxidant were investigated in parallel with measurement of the distribution profiles of dissolved organic carbon (DOC) along the rivers. In one year of observation at the mouths of the two rivers, DOC concentrations were found to vary in the Ado over the range 0.28-1.21 mg C l super(-1) and in the Yasu over the range 1.01-2.68 mg C l super(-1). Act-DOC, one of the fractions separated from the total DOC by its adsorption-active character onto HIO at pH 4, was thought primarily to control the variation of total DOC, as in Lake Biwa. The int-DOC, another fraction separated by its adsorption-inert or -inactive character onto HIO, remained at almost a steady value around 0.18 plus or minus 0.07 mg C l super(-1) in the Ado, which was lower than that (0.35 plus or minus 0.05 mg C l super(-1)) in Lake Biwa. The act-DOC in river waters was reactive to KMnO sub(4) oxidant, showing a linear relation with the amount of permanganate consumed for the reaction (chemical oxygen demand: COD). In river waters, the relation can be approximated by a straight line expressed as COD (mg O sub(2) l super(-1)) = 0.64 act-DOC (mg C l super(-1)) - 0.02. In contrast, in the lake water the relation was COD (mg O sub(2) l super(-1)) = 0.97 act-DOC (mg C l super(-1)) - 0.50. |
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ISSN: | 1439-8621 1439-863X |
DOI: | 10.1007/s102010070003 |