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Barbeau, C., Bougie, R., Côté, J.-E. (1981) Variations spatiales et temporelles du césium-137 et du carbone dans des sédiments du fjord du Saguenay. Canadian Journal of Earth Sciences, 18 (6) 1004-1011 doi:10.1139/e81-096

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Reference TypeJournal (article/letter/editorial)
TitleVariations spatiales et temporelles du césium-137 et du carbone dans des sédiments du fjord du Saguenay
JournalCanadian Journal of Earth Sciences
AuthorsBarbeau, C.Author
Bougie, R.Author
Côté, J.-E.Author
Year1981 (June 1)Volume18
Issue6
PublisherCanadian Science Publishing
DOIdoi:10.1139/e81-096Search in ResearchGate
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Mindat Ref. ID477127Long-form Identifiermindat:1:5:477127:6
GUID0
Full ReferenceBarbeau, C., Bougie, R., Côté, J.-E. (1981) Variations spatiales et temporelles du césium-137 et du carbone dans des sédiments du fjord du Saguenay. Canadian Journal of Earth Sciences, 18 (6) 1004-1011 doi:10.1139/e81-096
Plain TextBarbeau, C., Bougie, R., Côté, J.-E. (1981) Variations spatiales et temporelles du césium-137 et du carbone dans des sédiments du fjord du Saguenay. Canadian Journal of Earth Sciences, 18 (6) 1004-1011 doi:10.1139/e81-096
In(1981, June) Canadian Journal of Earth Sciences Vol. 18 (6) Canadian Science Publishing
Abstract/Notes The accumulation rate of sediments in the Saguenay Fjord, Quebec, Canada, established from 137Cs activity measured in 19 cores, varies between > 1.0 cm/year upstream and 0.2 cm/year downstream. Cesium-137 profiles in cores from the northern basin follow that of fallouts on the ground and reflect the impact of a sudden inflow of clay from a major mudslide. However, 137Cs accumulation in the larger basin seems less sensitive to external influences.Carbon content and the C/N ratio are higher upstream than downstream. Based on 137Cs dating, core sections show carbon contents that reflect changes caused by the forest industry over the years. [Journal Translation]


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