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  4. Spatial distribution of acid-volatile sulfur in the sediments of Canadohta Lake, PA
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Spatial distribution of acid-volatile sulfur in the sediments of Canadohta Lake, PA

Persistent URL
http://hdl.handle.net/10456/45404
Author(s)
Oehm, N.J.
Luben, T.J.
Ostrofsky, Milton L.
Date Issued
February 1997
Abstract
Lake sediments are an important source of dissolvedsubstances and can be the site of processes importantto the biogeochemical cycling of nutrients and metals. Most studies which examine these processes, however,are based on the analysis of a single or a very fewsediment cores taken at or near the deepest area ofthe lake. The implicit assumption is that lakesediments are spatially homogeneous and thatextrapolations from such limited samples arerepresentative of the lake sediments throughout thelake basin. We examined this assumption with respectto concentrations of acid volatile sulfides (S2-vol) – sulfur species which have beenimplicated in eutrophication, acid-neutralization, andheavy-metal toxicity. S2-volconcentrations measured in the surficial sediments ofCanadohta Lake, PA, a lake of very simple morphometry,ranged from 0.07 to 30.32 μg g-1 sediment dryweight. Concentrations were directly correlated withdepth and inversely correlated with organic matter. These results suggest that results extrapolated froma few deep-water cores can lead to a seriousoverestimation of S2-vol in the lakesediments.
Journal
Hydrobiologia
Department
Biology
Citation
Oehm, N.J., Luben, T.J., and Ostrofsky, M.L. (1997). Spatial distribution of acid-volatile sulfur in the sediments of Canadohta Lake, PA. Hydrobiologia 345(1): 79-85. doi: 10.1023/A:1002971130433
Publisher
Kluwer Academic Publishers
Version of Article
Published article
DOI
10.1023/A:1002971130433
ISSN
0018-8158
e1573-5117
Rights
This article is published. Copyright is retained by reprint author and publisher. Please contact the publisher for further use of this material.
Subjects

acid volatile sulfide...

lake sediments

spatial heterogeneity...

Pennsylvania lakes

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