Lake restoration by dilution: Moses lake, Washington

Dilution water, low in macronutrients, was added to Moses Lake on three occasions in 1977 and once in 1978 during the spring-summer period. The addition resulted in reducing the annual average inflow concentration of phosphorus from about 130–140 μg l⁻¹ to 100 μg l⁻¹. The water exchange rate in Parker Horn, which is 8% of the lake volume, increased from about 1% day⁻¹ normally to 7 and 11% day⁻¹ for the May–September period in 1977 and 1978, respectively. Lake water was displaced at a predictable rate in the whole lake as well as the areas proximal to the input, as verified by specific conductance.Improvements in lake quality, compared to values from 1969–70, were rather good with greater reductions in algal biomass occurring than might have been expected to result from the less impressive reductions in total P content. Chlorophyll a decreased by about 60–80% and total P decreased by about 50–60%, depending on the area of the lake. However, Chl a averaged only 15 μg l⁻¹ during May–September 1978, while total P was rather high at 70–80 μg l⁻¹. The fraction of the phytoplankton composed by blue-green algae decreased from 96% in 1970 to 68% in 1977–78. The cause for the effect on biomass and species composition is unknown, but may be related to dilution of blue-green excretory products.A dilution water input of about 6 m³ s⁻¹ continuously during April–September would require 20% less total water and should provide adequate control of eutrophication in at least 30% of the lake volume proximal to the input and Parker Horn. That would provide an exchange rate of 5% day⁻¹ for Parker Horn and should achieve lake water residuals by midsummer of 50%. Two additional inputs to the lake are also proposed as two more phases in the restoration project.