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• W2134723171 abstract "Vertical diffusion rates (K(Kz) were determined by measuring for several weeks the vertical spread of an injection of tritiated water into the thermoclines and hypolimnia of Lake 227 and Lake 224 in the Experimental Lakes Area (ELA) of northwestern Ontario. Kz values of 5×10−5 and 8×10−4 cm2· s−1 were determined from the tracer experiments in the thermoclines of L227 and L224; in the hypolimnia, similar Kz determinations of 1.7×10−3 and 1.8×10−2cm2·s−1 are 20−30 times greater than the thermocline rates. Vertical diffusion rates of heat were determined over the same time and depth intervals as the tracer experiments. In each lake, heat is diffusing vertically faster than mass in the thermocline and at more equal rates in the hypolimnion. The low Kz values and the greater diffusion rate of heat than mass (tritium) indicate that molecular diffusion is important in determining the rate of vertical transport in the thermoclines of these highly stratified lakes. Vertical eddy diffusion rates (Kz') determined by the tracer experiments show an inverse proportionality to the static stability of the water column (N2), such that Kz′ ∝ (N2)−0·8. However, Kz′ values determined by measuring the hypolimnetic heating rates of eight ELA lakes (including L227 and L224) and three lakes outside ELA indicate that Kz′ ∝ (N2)−0.44. These observations suggest that in the absence of large shear where Kz′ < 10−2cm2 · s−1 the vertical diffusion rates of mass and heat show different inverse correlations to the static stability of the water column." @default.
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• W2134723171 date "1980-03-01" @default.
• W2134723171 modified "2023-10-06" @default.
• W2134723171 title "Vertical diffusion rates determined by tritium tracer experiments in the thermocline and hypolimnion of two lakes1,2" @default.
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• W2134723171 doi "https://doi.org/10.4319/lo.1980.25.2.0201" @default.
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