A Reconnaissance Of Hydrogeology And Ground Water Quality In Three Hillside Basins At The Perimeter Of The Rathdrum Prairie Aquifer Kootenai County Idaho PDF Download

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A Reconnaissance of Hydrogeology and Ground Water Quality in Three Hillside Basins at the Perimeter of the Rathdrum Prairie Aquifer, Kootenai County, Idaho

A Reconnaissance of Hydrogeology and Ground Water Quality in Three Hillside Basins at the Perimeter of the Rathdrum Prairie Aquifer, Kootenai County, Idaho
Author: Deanna L. Clarkson
Publisher:
Total Pages: 216
Release: 1998
Genre: Groundwater
ISBN:

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"From July to September, 1997, a reconnaissance investigation was completed of the hydrogeology and ground water quality in three hillside basins adjoining the Rathdrum Prairie aquifer in Kootenai County, Idaho. These basins contribute recharge to the Rathdrum Prairie-Spokane Valley aquifer system, a drinking water source protected by both state and federal designations requiring maintenance of the high quality of its water. The investigation of hillside basins was implemented in response to the 1996 discovery of nitrate contamination in public drinking water supplies at the southern margin of the Rathdrum Prairie in South Post Falls, Idaho. Nitrate contamination is linked to septic discharge and fertilizers, and causes a potentially fatal illness in infants. To assess the quality of ground water in the hillside regions, three study areas were chosen to represent basins of relatively high, intermediate, and low residential development density as measured by the number of onsite septic systems they contained. These basins were: high density, Nettleton Gulch, east of Coeur d'Alene; intermediate density, the South Greenferry Road basin south of the Spokane River; and low density, Hidden Valley, southwest of Rathdrum. Ground water samples were collected from ten existing wells in each basin. To establish the quality of the ground water, the samples were analyzed for conductivity, temperature, pH, alkalinity, total major ions (calcium, magnesium, sodium, sulfate, chloride), total iron, and nitrite plus nitrate as nitrogen. Analysis of the ground water samples was accomplished in the field and by the Coeur d'Alene branch of the Idaho State Laboratory. Two sampling rounds were completed: in July, when the water table was high, and in September, when the water table was falling. No statistically significant differences were found between the July and September water samples. The measurements of the depth to the water table in each basin established that ground water flow in the basins was toward the Rathdrum Prairie aquifer. The ground water in the study basins was compared with the Rathdrum Prairie aquifer water, as represented by the results of the July 1997 Panhandle Health District monitoring of 29 public drinking water wells on the Rathdrum Prairie. The ground water in the study basins and Rathdrum Prairie aquifer presented similar calcium bicarbonate major ion profiles, although in Hidden Valley and Nettleton Gulch, the ground water, as evidenced by its higher conductivity, was more mineralized than the water of the main aquifer. In the Rathdrum Prairie aquifer, the median nitrate concentration was 0.971 milligrams per liter (mg/L), while the median chloride concentration was 2.0 mg/L. In the low density development, Hidden Valley, the median nitrate concentration was the lowest of the study basins at 0.241 milligrams per liter (mg/L). The median chloride concentration in samples of Hidden Valley was 1.3 mg/L, also the lowest among the study basins. In Nettleton Gulch, where development density was high, the median nitrate was 1.09 mg/L, intermediate among the study basins, while the median chloride concentration was the highest at 4.0 mg/L. The highest nitrate concentrations were detected in the basin of intermediate development, the South Greenferry Road study basin, where the median nitrate concentration was 2.61 mg/L, and the median chloride concentration was 3.0 mg/L. The highest nitrate concentration of the study was 10.5 mg/L found in a well at the site of a small farm and commercial greenhouse in the South Greenferry Road basin. The highest nitrate concentration in Nettleton Gulch was 3.90 mg/L. The elevated chloride and nitrate concentrations in the South Greenferry Road basin and Nettleton Gulch suggest the influence of septic discharge on the ground water. In addition, fertilizer was a probable source of the unexpectedly high nitrate concentrations in the South Greenferry Road basin. The areas of the basins most vulnerable to ground water contamination are those with highly permeable, low water capacity soils. An estimate of total nitrogen loading in the study basins suggests that the use of fertilizers may introduce a load at least equivalent to septic discharge. One small farm in the South Greenferry Road basin alone produces an annual nitrogen load equivalent to the estimated nitrogen load from the basin's total septic discharge. The results of the current study imply that limiting the use of onsite septic systems and constructing sewers is an essential part of protecting the ground water of Kootenai County, because septic discharge is the critical component of the nitrate load that can be addressed through land use planning and regulation. Control of the additional source of nitrate contamination, fertilizer use, is dependent on the voluntary compliance of residents educated in best management practices"--Document.


Hydrogeology and Water Quality of Basin a Neck Area, Rocky Mountain Arsenal, Denver, Colorado

Hydrogeology and Water Quality of Basin a Neck Area, Rocky Mountain Arsenal, Denver, Colorado
Author: ARMY ENGINEER WATERWAYS EXPERIMENT STATION VICKSBURG MS GEOTECHNICAL LAB.
Publisher:
Total Pages: 60
Release: 1979
Genre:
ISBN:

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The purposes of this study were to accomplish the following tasks with the BANA(Basin a Neck Area): (1) Quantify the ground water flow regime at the neck of basin A for flow exiting Basin A to the northwest, (2) Quantify the distribution of various pollutants in the ground water flow system exiting basin A to the northwest, (3) Identify any other ground water flow paths (besides the exit flow to the northwest (in the alluvial aquifer)) leaving basin A, (4) To determine the areas of significant movement for pollutants in the ground water flow exiting Basin A. This report presents the findings of the above tasks performed by WES. The results of physical laboratory test on undisturbed samples are incomplete, and will be published as an addendum to this report.


Republican River Basin Study

Republican River Basin Study
Author: U. S. Department U.S. Department of the Interior
Publisher: Createspace Independent Publishing Platform
Total Pages: 90
Release: 2016-05-09
Genre:
ISBN: 9781533159373

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The Republican River Basin is an important region for the states of Nebraska, Colorado and Kansas (the States) that includes highly productive agricultural lands, large reservoirs with recreational and wildlife habitat features, and established communities that rely on the agriculturally-driven economy and the water supplies that sustain it. The water management issues in the Republican River Basin are extremely complex and involve a long history of stakeholder involvement and activities. Declines in groundwater levels and streamflows have and continue to be widespread throughout the Basin, creating competition for limited water supplies and litigation. This Basin Study provided an opportunity for the three States to work toward overcoming some of these challenges by coordinating with the Bureau of Reclamation (Reclamation) to identify and evaluate alternative management and infrastructure changes that might benefit water users within the Basin, while strengthening the local economy and protecting environmental resources. The inclusion of future climate change scenarios provided an indication of the robustness of the system under climate variability, such as how the reservoirs and canals might operate and adapt under severe drought conditions, and how physical and operational changes may impact local economic benefits relative to costs. Because of the legal, physical, and institutional complexity of water operations in the Basin, the models developed under this Basin Study may be especially important in helping the States investigate relationships between management decisions and physical responses to the Basin water supply. The achievements made through this Basin Study are owed to the high levels of professionalism and collaboration displayed among Basin Study partners. Coupled with recent and ongoing negotiations and agreements, sustainable, win-win solutions to solving the Basin's complex water supply issues appear promising.


Hydrogeology and ground-water quality in the sanders area, western puerco river basin, arizona a thesis submitted in partial fulfillment of the requirements fot the degree of master of science in geoscience

Hydrogeology and ground-water quality in the sanders area, western puerco river basin, arizona a thesis submitted in partial fulfillment of the requirements fot the degree of master of science in geoscience
Author: Earle Campbell Dixon
Publisher:
Total Pages:
Release: 1990
Genre:
ISBN:

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H-Area Seepage Basins

H-Area Seepage Basins
Author:
Publisher:
Total Pages: 441
Release: 1990
Genre:
ISBN:

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During the second quarter of 1990 the wells which make up the H-Area Seepage Basins (H-HWMF) monitoring network were sampled. Laboratory analyses were performed to measure levels of hazardous constituents, indicator parameters, tritium, nonvolatile beta, and gross alpha. A Gas Chromatograph Mass Spectrometer (GCMS) scan was performed on all wells sampled to determine any hazardous organic constituents present in the groundwater. The primary contaminants observed at wells monitoring the H-Area Seepage Basins are tritium, nitrate, mercury, gross alpha, nonvolatile beta, trichloroethylene (TCE), tetrachloroethylene, lead, cadmium, arsenic, and total radium. Concentrations of at least one of the following constituents: tritium, nitrate, total radium, gross alpha, nonvolatile beta, mercury, lead, cadmium, trichloroethylene chromium, and arsenic in excess of the primary drinking water standard (PDWS) were observed in at least one well monitoring the H-Area Seepage Basins. Elevated levels of tritium above the PDWS were exhibited in seventy-seven of the 105 (73%) groundwater monitoring wells. Elevated levels of nitrate in excess of the PDWS were exhibited in forty-four of the 105 (42%) monitoring wells.


National Water Summary

National Water Summary
Author:
Publisher:
Total Pages: 604
Release: 1993
Genre: Groundwater
ISBN:

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