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Reshanau Lake Management Plan <br />• IV. History /Summary of Existing Data <br />Reshanau Lake was formed by dredging the swampy area, roughly where the <br />lake now exist, in the late 1960's and early 1970's. The material removed <br />from the lake was used to make what is now Chomonix Golf course and to <br />make build able lots on the lake's perimeter. For a number of years, the lake <br />was treated annually by a commercial applier but was discontinued for some <br />reason before 1995. <br />Over the years individual property owners have applied some chemical <br />treatments with marginal or no apparent success. <br />Attempts have been made over the years to form an Association of property <br />owners but have been unsuccessful. <br />In 1995 a study of Reshanau Lake was conducted by Montgomery Watson <br />(Attachment A), which provides some historical and benchmark data. This <br />report shows that Reshanau Lake is Eutrophic (high in nutrients) and does not <br />support swimming or other contact water activity according to Minnesota <br />Pollution Control Agency (MPCA) standards. The report also suggests that <br />the growth of the exotic curly -leaf pondweed contributes significant <br />phosphorus to the lake. <br />A summary of the 1995 lake monitoring report shows that the in -lake total <br />phosphorus (TP) levels averaged 110 ug /L during the growing season. TP is <br />the nutrient that drives algal productivity in most northern latitude states. This <br />nutrient is generally the limiting factor for plant growth. Since this nutrient is <br />often associated with man induced activities, it is almost always the nutrient <br />that lake managers target to reduce the frequency and duration of algae <br />blooms and to help control SAV growth. TP entering the lake is coming from <br />four primary sources. Theses sources are County Ditch 25 (CD25) which <br />enters on the east side of the lake, a small tributary creek which enters the lake <br />on the south side, internal cycling of TP from the die off and decomposition of <br />curlyleaf pondweed, and direct drainage from manicured lawn runoff and <br />possible failing septic tanks. The early summer TP levels are 70 pg /L and <br />peak at 140 µg /L in late July. This peak TP concentration coincides with the <br />die -off and decomposition of curlyleaf pondweed in the lake. Looking back at <br />the 1995 stream monitoring data also suggests that during the flashier stream <br />flow period of July and August TP export from CD 25 is higher. The <br />Chlorophyll -a (CHLA) concentration averaged 3911g /L during the growing <br />season and was at a low of 11 p.g /L in early June and peaked at 121 µg /L in <br />early August. CHLA measurement is a measurement of plant productivity in a <br />lake. All vascular plants produce CHLA and this measurement is related to the <br />amount of algae when a surface water sample is collected and analyzed. <br />CHLA concentrations generally increase with an increase in TP <br />concentrations. The CHLA cycle is also attributable to the die -off and <br />G: \Admin \Board \Agenda Paks \2005 Agenda Paks \2005 -04 -13 \Reshanau mgmt plan.doc4 <br />