Cheney Reservoir and Water Quality Studies
Science Center Objects
Cheney Reservoir is located on the North Fork Ninnescah River in south-central Kansas, 20 miles west of Wichita. Cheney Reservoir is the primary drinking water supply for the city and a popular recreational resource for the region. After cyanobacterial blooms in 1990 and 1991, which caused servere taste-and-odor events, the USGS Kansas Water Science Center partnered with the City of Wichita and began studies to better understand and improve the water-quality of Cheney Reservoir because of the potential economic and public health concerns for drinking water and recreational activities. “Knowledge gained from USGS studies in the Cheney Reservoir Watershed has assisted in the development, implementation, maintenance, and assessment of watershed-management goals and plans. This data has allowed us to ensure a safe and reliable water supply and put us ahead of the curve in terms of sediment management.” – Don Henry, Assistant Director of the City of Wichita’s Public Works and Utilities, 2017.
During 1996 to 2001 efforts were made to study the loading of contaminants, nutrients, and sediment to Cheney Reservoir from the watershed. A network of study sites, along with two continuous water-quality monitoring sites and collection of sediment cores, were used to analyze subwatershed sources of nutrient and sediment loading from the watershed into Cheney Reservoir.
Continuing Reservoir Studies
Starting in 2001, the focus of the studies shifted focus to analyzing suspended sediment and nutrient concentrations; presence of cyanobacteria, cyanotoxins and taste-and-odor compounds; and enviromental variables (specific condunctance, pH, temperature, turbidity, dissolved oxygen, and chlorophyll). The data is collected through the use of continuous water-quality monitoring and discrete sampling.
As part of the efforts to assess water quality in Cheney Reservoir, a Cheney Reservoir Task Force was formed in 1994 to establish water quality standards to quantify primary pollutants (nutrients and sediment) and understand their relation to cyanobacterial blooms. The studies showed that total phosphorus concentrations in the watershed were about three times the natural conditions, an estimated 65 percent of that originating from agricultural sources. Based on the findings of the Task Force, the long term goals of phosphorus concentrations may not be realistic without changes to watershed management. As of 2001, sediment accumulation in the reservoir was less than expected. A substantial portion of the accumulation was delivered to Cheney Reservoir during very short time periods with extreme hydrological conditions. Overall, studies showed no discernible patterns in nutrient and suspended-sediment concentrations or loads during 1996 through 2013 because of hydrologic variability.
Continuing Reservoir Studies
During 2001 through 2016, the U.S. Geological Survey, in cooperation with the city of Wichita, conducted a study to develop reliable tools to estimate the onset of cyanobacterial-related taste-and-odor occurrences in Cheney Reservoir. cyanobacteria and microcystin concentrations in Cheney Reservoir showed seasonal patterns, however the abundance and concentration varied by orders of magnitude across years. Peaks were seen in late summer or early fall with smaller peaks seen in December. Seasonal patterns were less consistent but present for the taste-and-odor compound geosmin. Water quality models were developed based on hourly measurements since 2001; the models are available at the USGS National Real-Time Water Quality website at https://nrtwq.usgs.gov. These models demonstrate the need for continuous reevaluation of toxin and taste-and-odor models due to changing environmental conditions.