Water Quality of Arkansas' Significant Publicly-Owned Lakes

Water Division

Technical Assistance Manager - (501) 682-0660


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Background

The Water Quality Act of 1987, in Section (314), the Clean Lakes Section and Section 305(b) mandates the development of a public lakes assessment program. The primary objectives of the Lakes assessments were to:

  1. Identify lakes which were not currently meeting water quality standards;
  2. Identify degraded, impaired, or threatened lakes; and
  3. Identify the trophic status of each of these lakes.

Sampling Methodology

All sampling was conducted in mid to late summer after significant run-off had ceased and summer stratification had occurred on most lakes. Each sampling trip was restricted to no more than two days so the samples could be analyzed within the 48-hour maximum holding time. The Environmental Preservation and Technical Services Division of the Department of Environmental Quality analyzed water quality parameters. The Water Quality Planning Branch of ADEQ collected samples, measured dissolved oxygen profiles, pH and secchi transparency (visibility into water) in the field.

A shore to shore transect in the lower portion near the dam of each man-made lake was established; depths along transects were determined; and a sample station was established at the deepest point. Lakes of approximately 2000 surface acres or larger had more than one sample transect. These included one near the dam and one in the upper one-third of the lake. Naturally occurring lakes were sampled at their deepest point, which was normally near the middle of the lake.

Water temperature and dissolved oxygen concentrations were measured at 1 to 5 feet intervals within the epilimnion (upper strata); at 1 to 2 feet intervals in the thermocline (transition zone); and 1 to 5 feet intervals in the hypolimnion (lower strata).

Water quality grab samples were collected at one meter (epilimnion) and at 0.8 (80%) maximum depth (hypolimnion) over the main channel. Bacteria samples were collected one-half meter below the surface at five locations along the transect. One sample was collected approximately 50 feet from each shore, at each quarter point and at the mid-point of the transect. Chlorophyll a samples were collected from the five bacteria sample sites along the transect and composited.

Lakes Classification

Using size, average depth and ecoregion all lakes were placed into one of five different lake types.

Type A Lakes

These are the larger lakes, usually of several thousand acres in size. They have average depths normally 30 to 60 feet. They are located in the montane areas of the state in the Ozark Highlands, Ouachita Mountains and Boston Mountains. The primary purposes for construction of these lakes was hydropower and/or flood control. The watershed to lake area ratios (W/A) are normally large, but most of these lakes have large storage volumes and a relatively long hydraulic residence time.

Type B Lakes

These include the smaller lakes of the uplands or steeper terrain. Most are around 500 acres or less in size, but probably are the most heterogenous group of lakes. Most are located in the Ozark Highlands, Ouachita Mountains and Boston Mountains; however, several are located in the more mountainous areas of the Arkansas River Valley. Average depths are relatively deep and range generally from 10 to 25 feet. Watersheds are normally dominated by forest lands. Most lakes of this type were constructed for the primary purpose of multi-purpose recreation or specifically for public fishing. The watershed to lake area ratios are generally very large. This results in a rather high flushing rate and low water retention time.

Type C Lakes

This group is composed of the smaller lakes of the lowland or flat terrain areas. Sizes generally range from 300 to 1,000 acres with average depth of normally less than 10 feet. These lakes are located in the flatter terrain of the Arkansas River Valley, Gulf Coastal and Delta Ecoregions. The Delta lakes of this group are generally associated with the Crowley's Ridge region. Watersheds of these lakes include timberlands of both lowland hardwoods and pines, but some are broken by pasture land and small farms. Almost all lakes of this group were constructed specifically for public fishing with other types of recreation as secondary uses. The watershed to lake area ratios vary significantly. As a result of the shallow average depth and relatively small storage volume, high flushing takes place on the lakes that have high W/A ratios.

Type D Lakes

These are small impoundments of the Delta area of the state, but include two similar type lakes from the large river alluvium of the Gulf Coastal Ecoregion. These type lakes are generally 200 to 500 acres in size with average depths of five feet. This group includes several natural, oxbow-cutoff lakes which have been modified by a water control structure to increase their isolation form the parent stream and maintain higher dry-season water levels. These lakes are only occasionally flooded by the parent stream and generally have very small direct runoff watersheds. Other lakes of this type are man-made, but they are almost totally isolated from their watershed by levees. Water levels are maintained through occasional pumping from adjacent waterways. Where watersheds exist that discharge directly to the oxbow lakes in this group, the runoff is primarily from row crop agriculture.

Type E Lakes

These are the large lowland lakes of the Delta, Gulf Coastal and the large alluvial areas of the Arkansas River Valley Ecoregion. They range from several thousand to over 30,000 acres in size, but average depth is usually less than 10 feet. This group also includes four large, oxbow-cutoff lakes which have been substantially modified by construction of drainage ditches, levees and other water control structures. Watershed types include mixtures of intensive row crop agriculture, small farms and pastures. The range of watershed to lake area ratios within this type of lake is extremely large. The largest is on navigation impoundments on the main stream of the large rivers. The flood control reservoirs, as might be expected, also have relatively large W/A ratios. In contrast the large oxbow lakes have W/A ratios of usually less than 10.

Water Quality Data

Summary information and a location map can be found in the document Arkansas' Significant Publicly-owned Lakes.

The following table has links to detailed information for each of the significant publicly-owned lakes.

Arkansas' Significant Publicly-owned Lakes
Lake Name
Lake Name
Lake Name
1st Old River
DeQueen - Lower
Maumelle - Lower
Ashbaugh
DeQueen - Upper
Maumelle - Upper
Atkins
DesArc
Millwood - Lower
Bailey
Dierks - Lower
Millwood - Upper
Barnett
Dierks - Upper
Nimrod
Bear Creek
Elmdale
Norfork - Lower
Beaver - Lower
Enterprise
Norfork - Middle
Beaver - Middle
Erling - Lower
Norfork - Upper
Beaver - Upper
Erling - Upper
Old Town
Beaverfork
Fayetteville
Ouachita - Lower
Blue Mountain - Lower
Felsenthal - Lower
Ouachita - Middle
Blue Mountain - Upper
Felsenthal - Upper
Ouachita - Upper
Bobb Kidd
Frierson
Overcup
Bois D’ Arc
Ft. Smith
Pickthorne
Brewer - Lower
Georgia Pacific
Pine Bluff
Brewer - Upper
Gillham - Lower
Poinsett
Bull Shoals - Lower
Gillham - Upper
Sequoyah
Bull Shoals - Middle
Grampus
Shepherd Springs
Bull Shoals - Upper
Grand
Shores
Calion
Greenlee
Spring
Cane Creek
Greers Ferry - Lower
Storm Creek
Catherine - Lower
Greers Ferry - Middle
Sugarloaf
Catherine - Upper
Greers Ferry - Upper
SWEPCO
Charles
Greeson - Lower
Tricounty
Chicot - Lower
Greeson - Upper
Wallace
Chicot - Upper
Hamilton - Lower
Weddington
Columbia - Lower
Hamilton - Upper
White Oak - Lower
Columbia - Upper
Harris Brake
White Oak - Upper
Conway - Lower
Hinkle
Wilhelmena
Conway - Upper
Hogue
Wilson
Cove
Horsehead
Winona - Lower
Cox Creek
Horseshoe
Winona - Upper
Crystal
Hurricane
Wright (Nolan)
Dardanelle
June
 
DeGray - Lower
Lee Creek
 
DeGray - Upper
Mallard