High-resolution {sup 210}Pb dating of Lake Constance sediments: Stable lead in Lake Constance
Journal Article
·
· Environmental Geology and Water Sciences
OSTI ID:86432
- Heidelberger Akademie der Wissenschaften (Germany); and others
Two sediment cores (BO90/13b and BO90/17b) from Lake Constance were investigated by {gamma}-spectrometry for {sup 210}Pb, {sup 134}Cs, {sup 137}Cs, {sup 241}Am, {sup 234}Th, and other members of the {sup 238}U decay chain. The sediments were dated using the constant-flux model for {sup 210}Pb, and accumulation rates were determined. These range from 0.04 to 0.65 g/cm{sup 2}/yr (BO90/13b) and 0.04 to 0.8 g/cm{sup 2}/yr (BO90/17b), respectively. The mean accumulation rate amounts to 0.16 g/cm{sup 2}/yr for both cores. The cores had already been dated by lamination counting and reconstruction of high-water events at the Limnological Institute at Constance, so a very precise time scale was available. Both ages derived are in agreement within statistical error up to 1900, which means dating with the constant-flux model for {sup 210}Pb was confirmed up to that age. The position of the maxima of bomb cesium and americium confirm the stratigraphic and {sup 210}Pb datings. With {sup 241}Am a further radioactive isotope is available, which can be detected now by {gamma}-spectrometry and can serve as an additional time indicator, the maximum being dated at 1963. By applying the various time scales, the depth profiles of stable lead and zinc of core BO90/13b were dated. Both heavy metals show a very significant maximum located beneath the layer of the maxima of bomb cesium and americium, showing that these maxima are older than those of the bomb isotopes. It is remarkable in this context that the maximum of zinc concentration occurs a little later than that of stable lead. Similar concentration profiles are observable in core BO90/17b and other, older sediment cores (CS6-CS10) on a transect across the lake. The depth profile of stable lead in Lake Constance sediments does not reflect the anthropogenic gasoline lead emissions into the atmosphere for Germany, their maximum being dated at 1971. 19 refs., 13 figs., 2 tabs.
- OSTI ID:
- 86432
- Journal Information:
- Environmental Geology and Water Sciences, Journal Name: Environmental Geology and Water Sciences Journal Issue: 4 Vol. 24; ISSN EGWSEI; ISSN 0177-5146
- Country of Publication:
- United States
- Language:
- English
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Sun Feb 29 23:00:00 EST 1976
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·
OSTI ID:7286226
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Thu Oct 31 23:00:00 EST 1985
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OSTI ID:5418666
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Conference
·
Mon Jan 08 23:00:00 EST 1990
· EOS, Transactions, American Geophysical Union; (United States)
·
OSTI ID:6620539