Publications—Scientific Investigation Report
By Joel M. Galloway and W. Reed Green
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Beaver Lake is a large, deep-storage reservoir located in the upper White River Basin in northwestern Arkansas. The purpose of this report is to describe the ambient hydrologic and water-quality conditions in Beaver Lake and its inflows and describe a two-dimensional model developed to simulate the hydrodynamics and water quality of Beaver Lake from 2001 through 2003.
Water-quality samples were collected at the three main inflows to Beaver Lake; the White River near Fayetteville, Richland Creek at Goshen, and War Eagle Creek near Hindsville.
Nutrient concentrations varied among the tributaries because of land use and contributions of nutrients from point sources. The median concentrations of total ammonia plus organic nitrogen were greater for the White River than Richland and War Eagle Creeks. The greatest concentrations of nitrite plus nitrate and total nitrogen, however, were observed at War Eagle Creek. Phosphorus concentrations were relatively low, with orthophosphorus and dissolved phosphorus concentrations mostly below the laboratory reporting limit at the three sites. War Eagle Creek had significantly greater median orthophosphorus
and total phosphorus concentrations than the White River and Richland Creek. Dissolved organic-carbon concentrations
were significantly greater at the White River than at War Eagle and Richland Creeks. The White River also had significantly
greater turbidity than War Eagle Creek and Richland Creek.
The temperature distribution in Beaver Lake exhibits the typical seasonal cycle of lakes and reservoirs located within similar latitudes. Beaver Lake is a monomictic system, in which thermal stratification occurs annually during the summer and fall and complete mixing occurs in the winter. Isothermal conditions
exist throughout the winter and early spring.
Nitrogen concentrations varied temporally, longitudinally, and vertically in Beaver Lake for 2001 through 2003. Nitrite plus nitrate concentrations generally decreased from the upstream portion of Beaver Lake to the downstream portion and generally were greater in the hypolimnion. Total ammonia plus organic nitrogen concentrations also decreased from the upstream end of Beaver Lake to the downstream end and were substantially greater in the hypolimnion of Beaver Lake. Phosphorus
concentrations mostly were near or below laboratory detection limits in the epilimnion and metalimnion in Beaver Lake and were substantially greater in the hypolimnion in the upstream and middle parts of the reservoir. Measured total and dissolved organic carbon in Beaver Lake was relatively uniform spatially, longitudinally, and vertically in the reservoir from January 2001 through December 2003. Chlorophyll a concentrations
measured at sites in the upstream portion of the lake were significantly greater than at the other sites in the downstream
portion of Beaver Lake.
During the study period, water clarity in Beaver Lake was significantly greater at the downstream end of the reservoir than at the upstream end. The greatest Secchi depths at the downstream
end of the reservoir generally were observed in 2001 compared to 2002 and 2003, but did not have a seasonal pattern as observed at sites in the middle and upstream portion of the reservoir. Similar to Secchi depth results, turbidity results indicated
greater water clarity in the downstream portion of Beaver Lake compared to the upstream portion. Turbidity also was greater in the hypolimnion than in the epilimnion in the reservoir
during the stratification season.
A two-dimensional, laterally averaged, hydrodynamic, and water-quality model using CE-QUAL-W2 Version 3.1 was developed for Beaver Lake and calibrated based on vertical profiles
of temperature and dissolved oxygen, and water-quality constituent concentrations collected at various depths at four sites in the reservoir from April 2001 to April 2003. Simulated temperatures and dissolved-oxygen concentrations compared reasonably well with measured temperatures and dissolved-oxygen concentrations and differences varied spatially in Beaver
Lake for April 2001 to April 2003. The greatest differences between measured and simulated temperature data occurred in the upstream portion of the reservoir, which is the most dynamic part of the reservoir. In general, the differences between measured and simulated temperature were the least in 2001 at the two upstream sites and in 2002 at the two downstream
sites, and greatest in 2003 for all four sites. Similar to temperature, differences between simulated and measured values
of dissolved-oxygen concentrations were greater in the upstream portion of the reservoir compared to differences in the downstream portion. At the upstream portion of the reservoir, the greatest differences between simulated and measured dissolved
oxygen generally occurred in 2002 and the least differences
occurred in 2003. Simulated ammonia and total nitrogen
concentrations in Beaver Lake compared relatively well with the measured concentrations and simulated nitrite plus nitrate concentrations generally were less then the measured concentrations.
Simulated values for orthophosphorus were comparable
to measured concentrations and simulated total phosphorus concentrations generally were greater than the measured concentrations
in Beaver Lake. Simulated chlorophyll a values were comparable to measured chlorophyll a values both spatially and temporally in Beaver Lake.
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