The in-lake remediation process is guided by expert consultants and an intergovernmental working group. On September 11, 2019 a staff report and business case was brought to the CRD Board outlining the environmental, recreational, community and economic values of the lake (over $10 million annually) and a recommendation to remediate the lake. The CRD Board approved the recommendation to move ahead with the in-lake remediation of Elk/Beaver Lake, subject to receiving at least 50% capital grant funds for the project.
The construction of an oxygenation system and related components for Elk Lake was completed in late 2023. This system is anticipated to help address internal nutrient loading in Elk Lake. These nutrients have accumulated over decades in the lake and bottom sediments and are continually recycled back into the water column under low-oxygen conditions.
The total capital cost of this project was $1.6 million with additional annual operational costs related to water quality monitoring and system maintenance. The CRD is grateful for the Government of British Columbia's $750,000 contribution to help purchase the oxygenation system equipment.
The oxygenation system in Elk Lake directly pumps highly oxygenated air into the deepest part of the lake along a perforated pipe with small bubbles to improve deep water oxygen levels. Since the operationalization of the system in late 2023, initial water quality results show that oxygen levels in the hypolimnion (deepest part of the lake) are generally greater than in previous years. The system was turned on in November 2023 when deep lake waters are cold and readily mixed with surface waters. During this time, deeper water oxygen levels are naturally elevated, because colder water holds more oxygen.
As water temperatures warm in early spring, the lake generally becomes stratified with warmer, oxygenated waters at the surface and colder, less oxygenated waters in the deeper part of the lake.
Prior to installing the oxygenation system, we would expect oxygen levels to decrease significantly in the deeper water during spring/summer resulting in anoxic conditions, causing the release of sediment-bound phosphorus into the water column. Elevated deep water phosphorus levels would then be available at the lake surface in the fall when temperatures drop and the lake mixes, providing optimal conditions for blue-green algae growth.
It is anticipated that the oxygenation system will maintain elevated oxygenated levels during the spring/summer in the deepest lake waters to ensure phosphorus remains bound to the sediment and following lake mixing in the fall, does not become readily available for blue-green algae growth.
Ongoing monitoring of the lake through in situ water quality data collection and analysis, as well as remote dissolved oxygen sensors at discrete depths provide real-time information on water quality metrics and inform the ongoing operation of the system to meet the oxygen demand of the lake.