By Thomas D. Brock
Lake Mendota has usually been known as "the so much studied lake on the planet. " starting within the "classic" interval of limnology within the past due nineteenth century and carrying on with in the course of the current time, this lake has been the topic of a wide selection of experiences. even supposing lots of those reports were released in obtainable journals, an important quantity have seemed in neighborhood monographs and reviews, ephemeral records, or poorly disbursed journals. thus far, there was no try at a man-made remedy ofthe huge volume of labor that has been released. One motive of the current publication is to give a com prehensive compilation of the main early reports on Lake Mendota and to ascertain how they impinge on very important present-day organic questions. additionally, this publication provides a precis of box and laboratory paintings conducted in my very own laboratory over a interval of approximately 6 years and indicates the place correlations with past paintings exist. The publication might be ofinterest to limnologists needing a prepared connection with information and released papers in this vital lake, to biogeochemists, ocean ographers, and low-temperature geochemists attracted to lakes as version sys tems for international tactics, and to lake managers attracted to figuring out momentary and long term alterations in lake platforms. even though the key thrust ofthe current ebook is ecologicaland environmental, enough history has been offered on different points ofLake Mendota's limnology in order that the publication also needs to be beneficial to nonbiologists.
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Extra resources for A Eutrophic Lake: Lake Mendota, Wisconsin
Groundwater seepage should also be affected by pumping from water supply wells (Cline, 1965; Lathrop, 1979). Although the mean annual precipitation in the Madison, Wisconsin area is 77 em (31 inches), there has been wide variation over the past 100 years, from a low of 35 em (14 inches) to a high of 132 ern (53 inches) (McCaskey, 1955). Stewart (1965) used a sensitive water-level recorder to measure the response of Lake Mendota to rain fall events, as well as occurrences of surface seiche. 3, an event on 12 May 1964 caused the lake to rise 8-9 em in less than 3 hours.
A. Birge, A Memoir, by G. C. Sellery. University of Wisconsin Press, Madison. e. 1956. Recent sediments of three Wisconsin lakes. Bulletin of Geological Society ofAmerica, 67: 883-910. W. Bunge. 1956. A. Birge on the temperature of Lake Mendota; Part 1. Transactions of the Wisconsin Academy of Sciences, Arts and Letters, 45: 193-208. W. Bunge. 1957. A. Birge on the temperature of Lake Mendota; Part 2. Transact ions of the Wisconsin Academy of Sciences, Arts and Letters, 46: 31-89. A. 1978. Heat budgets of lakes.
10 ' 94 0 I 1950 1960 1910 1980 II LAKE KEGONSA ':1 lNOAGA PHOSPHORUS 1"'9" 1 80 60 60 l 40 40 .. 80 @ 1940 1950 1960 TROGEN 1ln9111 60 t I (j)(i) 80 . 4 0 80 1920 LAKE MONONA . 1920 19 30 1980 I @ @ . '94 0 1950 1960 1970 1980 The circled numbers on the graphs refer to the following historic events : 1) 1922, DeForest discharge begins, discharged to Upper Yahara; 2) 1926,First unit operational, Nine Springs Treatment Plant , most sewagestill treated at Burke Plant, discharged to Monona; 3) 1928, Waunakee discharge begins, discharged to Six Mile Creek; 4) 1936, Burke Plant closed, all sewage to Nine Springs, discharged to Waubesa; 5) 1942, Burke Plant reopened for Army, discharged to Monona; 6) 1950, Burke Plant closed, all sewage to Nine Springs, discharged to Waubesa; 7) 1952, Brewery discharge to Monona ends ; 8) 1958, Nine Springs discharge diverted to Badfish Creek; 9) 1962, Windsor discharge begins, discharged to Upper Yahara ; 10) 1971 , DeForest, Waunakee, Windsor discharges in Mendota Watershed end.