External sources of P are based on types of land use within the watershed and characterizations of septic systems based on distance from the lake combined with an estimate of seasonal homes. This information is then fed into a model that is adjusted for a best fit with actual P data obtained between 1990 and 2007.
Princeton Hydro Report Findley Lake – Lake Evaluation and Recommendations Town of Mina, Chautauqua County, NY, December 2021. Prepared for: Findley Lake Watershed Association. Prepared by: Princeton Hydro, LLC. The Princeton Hydro report addresses the internal loading of Phosphorus (P) for Findley Lake. Internal Loading is when nutrients are introduced into the water – primarily from the lake sediment and decaying aquatic plants (weeds) and algae. They designed a protocol to evaluate internal loading in the lake through sampling and modeling and to use this data to develop site specific recommendations for potential internal nutrient control. Such restoration techniques could therefore help reduce phosphorus loading and resulting harmful algal blooms. They conducted one water quality monitoring event on the lake at 3 locations in July 2021. RESULTS Results from one water quality monitoring event on the lake at 3 locations in July 2021 show the lake to be thermally stratified where the lake is separated into three distinct thermal layers. When this happens oxygen may become depleted in the deep/ cold waters and not able to be replenished from the atmosphere. And indeed, this is what was observed. Surface waters were supersaturated with dissolved oxygen (DO), indicative of high rates of photosynthetic activity, and the deep water (below 15 feet) was depleted of oxygen (see red line in Figure 2.2). The low dissolved oxygen levels have important implications not only as unhabitable area for fish and other aquatic organisms but can also trigger the release of P fueling algal growth.
Elevated phosphorus in the deep waters may be indicative of internal sediment release of this nutrient under anoxic conditions. Princeton Hydro estimated that approximately 25% of the lake area (74 acres) go anoxic for a period of ninety (90) days. This correlates with an anoxic depth of approximately 15’ and greater. INTERNAL LOADING ESTIMATE The internal loading estimate for Findley Lake is 498 lbs./yr which is 35% of the total annual load (939 lbs./yr from external sources plus 498 lbs./yr internal sources = 1,437 lbs./yr P). Management of this load would likely produce tangible water quality benefits in a cost-effective manner for Findley Lake. IN-LAKE MANAGEMENT OPTIONS While in-lake management focuses on mitigating internal phosphorus release under anoxic conditions in-lake controls donot replace the need for ongoing watershed management including streambank stabilization, stormwater management, waterfowl management, and septic/sewer management. Mitigating internal nutrient loading typically occurs in lake management via one of two means: (1) Nutrient Inactivation by applying an aluminum compound (such as alum) to create a stronger bond with Phosphorus than Iron, thereby keeping the Phosphorus in the sediments under anoxia and now allowing it to be released into the water. While alum has been used for over 40 years to control phosphorus, New York State is currently prohibiting the use of aluminum based nutrient inactivation projects. But they are evaluating this management technique and we’re hoping restrictions on the use of alum changes in the future. If Alum were a permittable option, one application could prevent internal release over a period of 5-10 years. Princeton Hydro’s estimates the cost of Alum treatment to be in the $120,000 to $170,000 range if permissible by NYSDEC in the future. (2) Destratification/ aeration the deep portions of the lake to maintain the iron-phosphorus bond during the summer months. A destratification/ aeration system typically creates air bubbles that vertically circulate the entire water column thereby preventing both thermal stratification and anoxic zones that generate the release of Phosphorus into the lake. The system consists of air compressors and lines running to diffusers strategically located throughout the lake, especially within the lake’s deeper reaches. Destratification systems are operated continuously; typically starting in early- to late-spring (before thermal stratification occurs), throughout the entire summer until early fall (when stratification normally breaks down and the lake would naturally turn over). Conclusion: Sewers are Crucial for Long-Term Water Quality of Findley Lake
We have significant and ongoing impairment of Findley Lake's water quality.
|
External sources of P are based on types of land use within the watershed and characterizations of septic systems based on distance from the lake combined with an estimate of seasonal homes. This information is then fed into a model that is adjusted for a best fit with actual P data obtained between 1990 and 2007.
Princeton Hydro Report Findley Lake – Lake Evaluation and Recommendations Town of Mina, Chautauqua County, NY, December 2021. Prepared for: Findley Lake Watershed Association. Prepared by: Princeton Hydro, LLC. The Princeton Hydro report addresses the internal loading of Phosphorus (P) for Findley Lake. Internal Loading is when nutrients are introduced into the water – primarily from the lake sediment and decaying aquatic plants (weeds) and algae. They designed a protocol to evaluate internal loading in the lake through sampling and modeling and to use this data to develop site specific recommendations for potential internal nutrient control. Such restoration techniques could therefore help reduce phosphorus loading and resulting harmful algal blooms. They conducted one water quality monitoring event on the lake at 3 locations in July 2021. RESULTS Results from one water quality monitoring event on the lake at 3 locations in July 2021 show the lake to be thermally stratified where the lake is separated into three distinct thermal layers. When this happens oxygen may become depleted in the deep/ cold waters and not able to be replenished from the atmosphere. And indeed, this is what was observed. Surface waters were supersaturated with dissolved oxygen (DO), indicative of high rates of photosynthetic activity, and the deep water (below 15 feet) was depleted of oxygen (see red line in Figure 2.2). The low dissolved oxygen levels have important implications not only as unhabitable area for fish and other aquatic organisms but can also trigger the release of P fueling algal growth.
Elevated phosphorus in the deep waters may be indicative of internal sediment release of this nutrient under anoxic conditions. Princeton Hydro estimated that approximately 25% of the lake area (74 acres) go anoxic for a period of ninety (90) days. This correlates with an anoxic depth of approximately 15’ and greater. INTERNAL LOADING ESTIMATE The internal loading estimate for Findley Lake is 498 lbs./yr which is 35% of the total annual load (939 lbs./yr from external sources plus 498 lbs./yr internal sources = 1,437 lbs./yr P). Management of this load would likely produce tangible water quality benefits in a cost-effective manner for Findley Lake. IN-LAKE MANAGEMENT OPTIONS While in-lake management focuses on mitigating internal phosphorus release under anoxic conditions in-lake controls donot replace the need for ongoing watershed management including streambank stabilization, stormwater management, waterfowl management, and septic/sewer management. Mitigating internal nutrient loading typically occurs in lake management via one of two means: (1) Nutrient Inactivation by applying an aluminum compound (such as alum) to create a stronger bond with Phosphorus than Iron, thereby keeping the Phosphorus in the sediments under anoxia and now allowing it to be released into the water. While alum has been used for over 40 years to control phosphorus, New York State is currently prohibiting the use of aluminum based nutrient inactivation projects. But they are evaluating this management technique and we’re hoping restrictions on the use of alum changes in the future. If Alum were a permittable option, one application could prevent internal release over a period of 5-10 years. Princeton Hydro’s estimates the cost of Alum treatment to be in the $120,000 to $170,000 range if permissible by NYSDEC in the future. (2) Destratification/ aeration the deep portions of the lake to maintain the iron-phosphorus bond during the summer months. A destratification/ aeration system typically creates air bubbles that vertically circulate the entire water column thereby preventing both thermal stratification and anoxic zones that generate the release of Phosphorus into the lake. The system consists of air compressors and lines running to diffusers strategically located throughout the lake, especially within the lake’s deeper reaches. Destratification systems are operated continuously; typically starting in early- to late-spring (before thermal stratification occurs), throughout the entire summer until early fall (when stratification normally breaks down and the lake would naturally turn over). Conclusion: Sewers are Crucial for Long-Term Water Quality of Findley Lake
We have significant and ongoing impairment of Findley Lake's water quality.
|