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Uptake and migration of tracers in lake sediments

Journal Article · · Limnol. Oceanogr., v. 20, no. 4, pp. 497-510
Mathematical solutions are given for an equation describing transient and steady state concentrations in lake water and sediments, in the presence of adsorption, decay, sedimentation, and diffusion. The results of the model are compared with the distributions of two tracers, $sup 90$Sr and $sup 137$Cs, in the sediments of Lakes Erie and Ontario. Adsorption of the two tracers by sediment particles, supported by experimental data, can be treated as a linear exchange reaction. $sup 90$Sr is adsorbed less strongly than $sup 137$Cs by sediments, and this feature accounts for the greater depths of $sup 90$Sr occurrence in lake sediments. Distribution of the radionuclide activities in sediments is compatible with a model based on mean steady input to the lakes for 16 years (1953-1969), and the following values of diffusion coefficients in pore waters: for $sup 90$Sr, 2 x 10$sup -6$ to to 4 x 10$sup -6$ cm$sup 2$$s$$sup -1$, and for $sup 137$Cs, 2 x 10$sup -5$ cm$sup 2$ s$sup -1$. An additional transport mechanism in sediments, sedimentation, is more significant in Lake Erie (0.3-0.6 cm yr$sup -1$, according to the model) than in Lake Ontario (0.05 cm yr$sup -1$). Conditions are outlined under which the fluxes from lake water to sediments are important in the chemical balance of medium and large lakes. (auth)
Research Organization:
Northwestern Univ., Evanston, IL
Sponsoring Organization:
USDOE
NSA Number:
NSA-33-002988
OSTI ID:
4183059
Journal Information:
Limnol. Oceanogr., v. 20, no. 4, pp. 497-510, Journal Name: Limnol. Oceanogr., v. 20, no. 4, pp. 497-510; ISSN LIOCA
Country of Publication:
United States
Language:
English