Characteristics of settling matter and its role in nutrient cycles in a deep oligotrophic lake
Sediment/water interactions. Proc. 4th symposium, Melbourne, 1987, Page: 279-295
1989
- 4Citations
- 2Captures
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Book Chapter Description
The settling flux of seston (dry weight, DW), chlorophyll a (Chl a), particulate organic carbon (POC), particulate organic nitrogen (PON), and particulate phosphorus (PP) was measured monthly in 1981-1983 at 10 different depths in Lake Chuzenji, Japan; an oligotrophic lake with a maximum depth of 163 m. Decomposition rates and those near the sediment interface were used to explain dissolved oxygen depletion and nitrate increase in the hypolimnion during stratification. The average sinking velocities were 1.82 m d for seston and 1.16 m d for Chl a at 30 m, they were influenced by Chl a content of seston. -from Authors
Bibliographic Details
http://www.scopus.com/inward/record.url?partnerID=HzOxMe3b&scp=0024923885&origin=inward; http://dx.doi.org/10.1007/978-94-009-2376-8_25; http://link.springer.com/10.1007/978-94-009-2376-8_25; http://link.springer.com/content/pdf/10.1007/978-94-009-2376-8_25.pdf; http://www.springerlink.com/index/10.1007/978-94-009-2376-8_25; http://www.springerlink.com/index/pdf/10.1007/978-94-009-2376-8_25; https://dx.doi.org/10.1007/978-94-009-2376-8_25; https://link.springer.com/chapter/10.1007/978-94-009-2376-8_25
Springer Science and Business Media LLC
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