Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

The use of Pb-210 to normalize fluxes and burdens of atmospheric contaminants in lake sediment cores

Conference · · EOS, Transactions, American Geophysical Union; (United States)
OSTI ID:6620539
It is possible to estimate the local annual atmospheric flux (Bq/m[sup 2] [sm bullet] yr) of Pb-210 to land and lake surfaces from measurements of the integral of excess Pb-210 in soil and peat profiles. If you compare this average Pb-210 flux to the soil surface, to the Pb-210 flux to deep lake sediments, you will usually find that the lake sediment flux is a factor of 2 to 6 greater. This is because most of the clay-sized and organic material added to the lake (and resuspended in the lake) each year is funneled into the deeper parts of the lake basin. The ratio of the deep lake Pb-210 sediment flux to the average terrestrial soil Pb-210 flux will be called the focusing factor, which can be used to crudely estimate whole lake sedimentation rates (g/m[sup 2] lake surface area [sm bullet] yr). Many industrial and agricultural contaminants are delivered to remote lakes by atmospheric deposition, and those contaminants that are strongly particle reactive will usually be resuspended and funneled into the deeper parts of the lake basin similar to Pb-210. Often a single sediment core history of deposition is used to estimate contaminant burdens and fluxes at the coring site in a lake basin. These deep basin contaminant burdens and fluxes can be divided by the focusing factor to estimate the burden per unit lake surface area and the atmospheric deposition rate to the lake surface area.
OSTI ID:
6620539
Report Number(s):
CONF-9002174--
Conference Information:
Journal Name: EOS, Transactions, American Geophysical Union; (United States) Journal Volume: 71:2
Country of Publication:
United States
Language:
English