1996
DOI: 10.1007/bf00877112
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Dissolved organic carbon in a eutrophic lake; dynamics, biodegradability and origin

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Cited by 72 publications
(38 citation statements)
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“…It is Japan's second largest lake, with a surface area of 171 km 2 , an average depth of 4 m, and a maximum depth of 7.3 m (only for Nishiura). This lake is considered hypertrophic because of its high loads of nutrients and shallow depth [13]. Although average Chl-a has decreased from 87 to 61 mg•m −3 during the past three decades, the mean total phosphorus concentration increased from 116 to 138 mg•m −3 .…”
Section: Study Areasmentioning
confidence: 99%
“…It is Japan's second largest lake, with a surface area of 171 km 2 , an average depth of 4 m, and a maximum depth of 7.3 m (only for Nishiura). This lake is considered hypertrophic because of its high loads of nutrients and shallow depth [13]. Although average Chl-a has decreased from 87 to 61 mg•m −3 during the past three decades, the mean total phosphorus concentration increased from 116 to 138 mg•m −3 .…”
Section: Study Areasmentioning
confidence: 99%
“…The quality of the dissolved organic matter was measured using specific ultraviolet absorbance (SUV A), defined as the UV absorbance of a water sample at a given wavelength normalized against DOC concentration. A spectrophotometer (Shimadzu UV-1601PC, Japan) was used to measure the UV absorbance (at 260 nm) in the water samples (Fukushima et al, 1996;Zieliński and Górniak, 1999;Weishar et al, 2003;Aoki et al, 2004).…”
Section: > Physical and Chemical Analysesmentioning
confidence: 99%
“…The dissolved organic carbon (DOC) content in water increases because of the microbiological degradation of organic matter produced in the lake, but mainly because of its release by aquatic organisms, i.e., algal exudation, the lysis of phytoplankton cells, and direct and indirect release by zooplankton and other aquatic animals (Wetzel, 1983;Hoppe, 1984). Apart from autochthonous sources, both forms of organic matter also originate from watersheds as labile and refractory compounds (Fukushima et al, 1996). Allochthonous sources of organic matter may significantly fuel the pelagic food web, but seasonal variability exists in terrestrial carbon subsidies (Tranvik, 1992;Grey et al, 2001).…”
Section: Introductionmentioning
confidence: 99%
“…The ratios of E260/DOC for pedogenic DOC and autochthonous DOC were reported to be 23 -58 and 8 -16 cm -1 (g C) -1 l, respectively. 11,12 Seasonal changes in the ratios of E260/DOC in Lake Biwa are shown in Fig. 8.…”
Section: Characteristics Of Humic Substances and Doc In Lake Biwa Andmentioning
confidence: 99%