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Turbulent mixing in the hypolimnion of Baldeggersee (Switzerland) traced by natural radon-222

Journal Article · · Limnol. Oceanogr.; (United States)
Three analytical diffusion models are used to describe the distribution of a nonconservative tracer in the hypolimnion of a lake: the one-dimensional vertical (1-DV) model, developed for tracers in the deep sea, leads to a significant overestimation of vertical diffusivity K/sub z/ in lakes; the one-dimensional topographic vertical (1-DTV) model, applicable if horizontal mixing is fast compared to in situ decay, demonstrates that, except for the deepest layers, vertical tracer distributions are insensitive to K/sub z/; the one-dimensional topographic horizontal (1-DTH) model, in which horizontal mixing is incomplete and vertical diffusion is disregarded, is the appropriate model for the interpretation of vertical excess /sup 222/Rn profiles a few meters above the lake bottom. The radon flux F from the bottom is calculated from /sup 226/Ra in the sediments and corrected for depth variation of porosity and radium activity. Horizontal diffusivity in the hypolimnion decreases from June to October; vertical diffusivity is roughly 10 times larger than values calculated from temperature in the upper hypolimnion. The large K/sub z/ and the transient, often irregular shape of the radon profiles are the result of horizontal bottom currents previously measured by other methods.
Research Organization:
Swiss Federal Inst. of Tech., Duebendorf
OSTI ID:
6138322
Journal Information:
Limnol. Oceanogr.; (United States), Journal Name: Limnol. Oceanogr.; (United States) Vol. 29:4; ISSN LIOCA
Country of Publication:
United States
Language:
English