Significance of dissolved organic carbon in the prediction of thermocline depth in small Canadian shield lakes

被引:79
作者
Pérez-Fuentetaja A. [1 ,3 ]
Dillon P.J. [2 ]
Yan N.D. [2 ]
McQueen D.J. [1 ]
机构
[1] Department of Biology, York University, 4700 Keele Street, Toronto
[2] Ontario Ministry of the Environment, Dorset Research Centre, Bellwood Acres Road, Dorset
[3] Alaska Department of Fish and Game, 211 Mission Rd., Kodiak
关键词
DOC; Dystrophic; Fetch; Humic; Light; Oligotrophic; Thermocline;
D O I
10.1023/A:1009998118504
中图分类号
学科分类号
摘要
Empirical models used to predict thermocline depths of lakes have typically been based on physical and morphometric variables. However, lakes with appreciable levels of dissolved organic material, including those found on the Canadian Precambrian Shield (DOC levels 1.4-12.41 mg l-1), have seldom been included in these models. Our analysis suggests that for such lakes, thermocline depth is linked strongly to light penetration (Secchi depth r = 0.83, light extinction r = -0.85) which is strongly related to DOC concentration (Secchi depth r = -0.91, light extinction r = 0.97). A multivariate regression based on small Canadian Shield lakes suggests that DOC is the most important predictor of thermocline depth. Maximum effective length, maximum depth, and chlorophyll a contribute significantly to the prediction power of the regression model, but are of secondary importance in the presence of DOC.
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页码:127 / 133
页数:6
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