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M.R. Have

Publications and source records attributed to M.R. Have.

7 recordsLinked to original sources

Streamflow entering and leaving Lake Bemidji, Beltrami County, Minnesota, July 1987 through September 1989

The U.S. Geological Survey, in cooperation with the Minnesota Department of Natural Resources, operated three streamflow-gaging stations from July 1987 through September 1989 to determine the volume of streamflow entering and leaving Lake Bemidji. Suspended- and bottom-sediment data were also collected at the gaging stations. Two gaging stations were located upstream and one was located downstream from the lake. Daily mean discharges were determined except for the November 1987 to March 1988 winter period. During the 1989 water year, the only complete year of data, the mean annual discharge for the two upstream stations was 111 ft /s (cubic feet per second) for Mississippi River at Bemidji and 71 ft /s for Schoolcraft River near Bemidji. The station downstream from Lake Bemidji, Mississippi River near Bemidji, had a mean annual discharge of 228 ft /s during water year 1989.

Minnesota

Selected water-quality characteristics in the upper Mississippi River basin, Royalton to Hastings, Minnesota

The upper Mississippi River basin from Royalton to Hastings, Minnesota, includes seven subbasins in east-central Minnesota that cover an area of 8,500 square miles. Results of a study, using data from the Minnesota Pollution Control Agency, Metropolitan Waste Control Commission, and the U.S. Geological Survey, indicate that selected water-quality characteristics differ significantly among subbasins. Results of the study also indicate that the quality of water leaving the basin at Hastings is affected primarily by inflow from the Minnesota River and by effluent from the Metropolitan sewage-treatment plant. Subbasins in the western part of the study area are underlain by prairie soils and cultivation of row crops is a common land use. Streams draining these subbasins have a median dissolved-solids concentration of 389 mg/L (milligrams per Liter) and a median concentration of nitrite plus nitrate nitrogen of 0.59 mg/L. Subbasins in the northern and eastern parts of the study area are underlain by more acidic podzol soils. Land use in these subbasins is less devoted to cultivated crops; forested areas, pastures, and wetlands are common. Streams draining these subbasins have a median dissolved- solids concentration of 184 mg/L and a median concentration of nitrite plus nitrate nitrogen of 0.17 mg/L. The quality of water changes dramatically in the most downstream subbasin, which includes the Twin Cities Metropolitan Area. On the basis of hourly data from automatic monitors, specific conductance increases from 345 / μ S/cm (microsiemens per centimeter) at 25° Celsius above the confluence with the Minnesota River to 467 / μ S/cm below it. Specific conductance increases to a median of 513 / μ S/cm where effluent from the Metropolitan sewage-treatment plant enters the Mississippi River. Dissolved-oxygen concentrations in the Mississippi River begin to decline below the confluence with the Minnesota River. Concentrations of dissolved oxygen reach a minimum median value in summer of 6.3 mg/L at a point about 9 miles downstream from the Metropolitan sewage-treatment plant. In winter, minimum median concentration is downstream at Lock and Dam 2, which is approximately 20 miles below the plant. Results of this study show that the quality of water in the Mississippi River as it leaves the accounting unit at Hastings is not representative of water quality in most of the accounting unit. Three water-quality regions have been identified, and sampling sites are needed in each region to assess the quality of streams throughout the study area adequately.

Minnesota

Water-quality data for Orwell reservoir and the Otter Tail River near Fergus Falls, Minnesota

Water-quality data were collected at five sites on Orwell Reservoir and two sites on the Otter Tail River, at the inflow and outflow points of the reservoir. The data, collected from April 1983 to July 1966, consist mainly of streamflow and nutrient concentrations at the river sites and nutrient concentrations, alkalinity, Secchi-disk transparency, phytoplankton counts, chlorophyll concentrations, and profiles of specific conductance, temperature, pU, and dissolved oxygen at the reservoir sites. Additional data collected at the outflow site include alkalinity and concentrations of major ions and organic carbon.

Minnesota

Water quality of Alimagnet, Farquar, and Long Lakes in Apple Valley, Minnesota

Alimagnet, Farquar, and Long Lakes, in Apple Valley, Minnesota, were sampled from 1973-79 to determine their physical and chemical characteristics. A storm-sewer inlet to Alimagnet Lake was also sampled during two storms in 1978. The 1976-77 drought caused a more noticeable effect on the quality of the lakes than any other factor. Chloride concentrations were 10 to 15 milligrams per liter before the drought, but increased 2 to 4 times during the drought. Dissolved solids reacted similarly. Dissolved oxygen and pH were governed mainly by biological activity. In February 1977, dissolved-oxygen concentration was less than 0.5 milligrams per liter in the three lakes. Ratios between mean total nitrogen and mean total phosphorus ranged from 22:1 to 26:1. Trophic-state indices indicate that the lakes are eutrophic. Blue-green algae dominated the phytoplankton populations. Storms sampled at a storm-sewer inlet to Alimagnet Lake showed higher concentrations of chromium, copper, nickel, and zinc than of lead, arsenic, cadmium, and mercury. Total phosphorus for the September 1978 storm had a concentration of 1.7 milligrams per liter, which means that approximately 29 pounds entered the lake during the 5.5-hour sampling period.

Minnesota

Water quality of Rogers Lake, Dakota County, Minnesota

Construction of an interstate highway is planned near Rogers Lake in Dakota County, Minn. Samples of water and bed material were collected at six sites during March 1976 to April 1978 to determine selected physical, chemical, and biological characteristics before construction. Samples were collected at least twice during each season of the year. Data derived from these samples will provide baseline information to aid in assessing the impact of highway construction on the water quality of the lake. Rogers Lake is separated into an upper and lower lake by a culvert; both were eutrophic and dominated by blue-green algae year around. Analyses of water from Rogers Lake suggest that sodium and chloride concentrations were higher than in ground water or in water in some surrounding lakes . Sodium ranged from 7.2 to 55 milligrams per liter, and chloride ranged from 15 to 30 milligrams per liter. Concentrations were highest in March 1978, when most of the lake water was frozen. Much of the sodium and chloride may have been derived from road salts used for deicing.

Minnesota

Water quality of four lakes in Lakeville, Minnesota

Water-quality characteristics were determined for four selected lakes to provide background data for evaluating changes that may occur in the lakes because of urbanization. Precipitation of calcium carbonate is suggested by high pH values and a decrease in the calcium concentration when magnesium, sodium, and chloride concentrations increase. Pollution is indicated by chloride concentrations that increased from 18 to 57 milligrams per liter in 1978. The eutrophic state of the lakes is suggested by dissolved oxygen supersaturated near the surface and less than 0.1 milligram per liter near the deepest parts of the lakes. Determination of the trophic state of the lakes provided trophic state indices as high as 69-2. Phosphorus concentrations were significantly higher in two of the lakes sampled. Anacystic and Oscillatoria were the dominant phytoplankton genera. Phytoplankton blooms occurred throughout the year with the highest sampled concentration yielding 890,000 cells per milliliter.

Minnesota

Some limnological aspects of 20 selected lakes in Eagan and Apple Valley, Minnesota

Selected physical, chemical, and biological parameters were determined to assess the quality of 20 lakes in the cities of Eagan and Apple Valley, Minn. All the lakes are eutrophic except Holland and Fish Lakes, which are mesotrophic. Some lakes (including Fish Lake) have storm sewer inlets but are not discernibly different in quality than lakes with no such inlets.

Minnesota