The Louisville Water Company is using riverbank filtration wells to draw water from the Ohio River through the aquifer at their B.E. Payne Water Treatment Plant near Prospect, Kentucky. The northeast portion of the alluvium— a 6.4-mi reach running from Beargrass Creek upriver to Harrods Creek is an especially prolific water-bearing formation with the total groundwater storage in the area estimated at 7 billion gallons (Rorabaugh, 1956).
Water-level data for the alluvial aquifer at Louisville, Kentucky, have been collected by the USGS in cooperation with various local and State agencies since September 1943. Data are presently being collected in cooperation with the Louisville Water Company. Special attention is given to the northeast portion of the alluvial aquifer where the Louisville Water Company is beginning to use riverbank filtration wells to draw water from the Ohio River through the aquifer at their B.E. Payne Water Treatment Plant near Prospect, Kentucky.
Regional Network Sampling Schedule
- 26 wells are measured quarterly (January, April, July, October)
- 7 wells are equipped with continuously recording pressure transducers
- measure water levels and water temperature, 30-minute intervals
Riverbank Filtration Sampling Schedule
- 2 collector wells and their respective observation well
- total of 8 wells
- all equipped with recording transducers
- measured in 30-minute intervals
- serviced on same quarterly schedule as regional wells
Data were collected in July 2011 and July 2013 to assess the conditions of the riverbed adjacent to the riverbank filtration system and to measure changes in the potentiometric surface beneath the river resulting from the groundwater withdrawals. Data collection activities included a check for clogging and/or compaction of the riverbed sediments, the installation of temporary piezometers for measuring groundwater levels, and the measuring of infiltration rates with a seepage meter. The riverbank filtration system began operations approximately 5 months prior to the July 2011 data collection exercise. By July 2013, the system had been in near constant operation for over 30 months, though the flow rate varied throughout the time period due to system demands.
In September 2014, the LWC was awarded a grant from the Kentucky Division of Water’s Source Water Protection Assistance Program to complete a well inventory throughout the LWC’s wellhead protection areas (WHPA) and take steps to secure or close any wells that pose a danger to the groundwater resources of the area. As part of the cooperative program, the USGS is working with the Louisville Water Company to provide assistance with assessing the current condition of existing wells within the LWC’s wellhead protection areas as shown in figure 4. The USGS completed the inventory of wells in the WHPA 1 in 2014. Work continued during 2015 to inventory wells in the WHPA 2 and 3 delineations. The inventory has been completed for wells in WHPA 2A and 2B.
Water samples will be collected from the 4 collector wells and 4 additional wells and piezometers (Henry Wallace Farm, Holland Farm, Juniper Beach domestic well, and Hays Kennedy piezometer) located throughout the riverbank filtration tunnel and collector well system’s wellhead protection areas (fig. 5). The wells will be sampled twice during the year – first in May (typically when groundwater levels are at their highest) and second in November (lower groundwater levels). Standard USGS field techniques and protocols for the collection of groundwater samples from wells will be followed.
Due in part to a lack of accessible existing wells in up-gradient positions, additional sampling sites were installed for the wellhead protection water-quality monitoring program. Three 2-in PVC monitoring wells were installed on LWC property up-gradient from the riverbank filtration collector well and tunnel system (fig. 6). Each borehole was advanced to the bedrock surface. Each well was constructed with two 10-ft screened intervals; one screen installed above the bedrock surface and a second screen positioned across the water table. The double screen well installation allows for monitoring contaminants that may travel on top of the water table and others that are denser than water.
Below are multimedia items associated with this project.
Below are publications associated with this project.
Hydrogeology and simulation of ground-water flow in the alluvial aquifer at Louisville, Kentucky
Ground-water levels in and pumpage from the alluvial aquifer at Louisville, Kentucky, May 1989-May 1991
Ground-water levels in the alluvial aquifer at Louisville, Kentucky, 1987-88
Ground-water levels in the alluvial aquifer at Louisville, Kentucky, 1982-87
Chloroform contamination in part of the alluvial aquifer, southwest Louisville, Kentucky
Problems of rising ground-water levels in urban areas with special reference to the Louisville, Kentucky area
Rising ground-water level in downtown Louisville, Kentucky, 1972-1977
Summary of hydrologic conditions of the Louisville area, Kentucky
Progress report on the ground-water resources of the Louisville area, Kentucky, 1949-55
Ground water in northeastern Louisville, Kentucky with reference to induced filtration
Water resources of the Louisville area, Kentucky and Indiana
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- Overview
The Louisville Water Company is using riverbank filtration wells to draw water from the Ohio River through the aquifer at their B.E. Payne Water Treatment Plant near Prospect, Kentucky. The northeast portion of the alluvium— a 6.4-mi reach running from Beargrass Creek upriver to Harrods Creek is an especially prolific water-bearing formation with the total groundwater storage in the area estimated at 7 billion gallons (Rorabaugh, 1956).
Water-level data for the alluvial aquifer at Louisville, Kentucky, have been collected by the USGS in cooperation with various local and State agencies since September 1943. Data are presently being collected in cooperation with the Louisville Water Company. Special attention is given to the northeast portion of the alluvial aquifer where the Louisville Water Company is beginning to use riverbank filtration wells to draw water from the Ohio River through the aquifer at their B.E. Payne Water Treatment Plant near Prospect, Kentucky.
Regional Network Sampling Schedule
- 26 wells are measured quarterly (January, April, July, October)
- 7 wells are equipped with continuously recording pressure transducers
- measure water levels and water temperature, 30-minute intervals
Riverbank Filtration Sampling Schedule
- 2 collector wells and their respective observation well
- total of 8 wells
- all equipped with recording transducers
- measured in 30-minute intervals
- serviced on same quarterly schedule as regional wells
Map of the well sampling locations (Click to open interactive map for access to the associated data) Data were collected in July 2011 and July 2013 to assess the conditions of the riverbed adjacent to the riverbank filtration system and to measure changes in the potentiometric surface beneath the river resulting from the groundwater withdrawals. Data collection activities included a check for clogging and/or compaction of the riverbed sediments, the installation of temporary piezometers for measuring groundwater levels, and the measuring of infiltration rates with a seepage meter. The riverbank filtration system began operations approximately 5 months prior to the July 2011 data collection exercise. By July 2013, the system had been in near constant operation for over 30 months, though the flow rate varied throughout the time period due to system demands.
Figure 4. Wellhead protection area In September 2014, the LWC was awarded a grant from the Kentucky Division of Water’s Source Water Protection Assistance Program to complete a well inventory throughout the LWC’s wellhead protection areas (WHPA) and take steps to secure or close any wells that pose a danger to the groundwater resources of the area. As part of the cooperative program, the USGS is working with the Louisville Water Company to provide assistance with assessing the current condition of existing wells within the LWC’s wellhead protection areas as shown in figure 4. The USGS completed the inventory of wells in the WHPA 1 in 2014. Work continued during 2015 to inventory wells in the WHPA 2 and 3 delineations. The inventory has been completed for wells in WHPA 2A and 2B.
Figure 5. Wellhead protection sampling sites Water samples will be collected from the 4 collector wells and 4 additional wells and piezometers (Henry Wallace Farm, Holland Farm, Juniper Beach domestic well, and Hays Kennedy piezometer) located throughout the riverbank filtration tunnel and collector well system’s wellhead protection areas (fig. 5). The wells will be sampled twice during the year – first in May (typically when groundwater levels are at their highest) and second in November (lower groundwater levels). Standard USGS field techniques and protocols for the collection of groundwater samples from wells will be followed.
Figure 6. Locations of additional wellhead protection wells Due in part to a lack of accessible existing wells in up-gradient positions, additional sampling sites were installed for the wellhead protection water-quality monitoring program. Three 2-in PVC monitoring wells were installed on LWC property up-gradient from the riverbank filtration collector well and tunnel system (fig. 6). Each borehole was advanced to the bedrock surface. Each well was constructed with two 10-ft screened intervals; one screen installed above the bedrock surface and a second screen positioned across the water table. The double screen well installation allows for monitoring contaminants that may travel on top of the water table and others that are denser than water.
Table of well sites. (Click the image title above to view interactive table of data and photos.) - Multimedia
Below are multimedia items associated with this project.
- Publications
Below are publications associated with this project.
Hydrogeology and simulation of ground-water flow in the alluvial aquifer at Louisville, Kentucky
The alluvial aquifer at Louisville, Ky., lies in a valley eroded by glacial meltwater that was later partly filled with outwash sand and gravel deposits. The aquifer is primarily unconfined, and the direction of flow is from the adjacent limestone and shale valley wall toward the Ohio River and major pumping centers. Pumpage and water-level data indicate that the alluvial aquifer was in a steady-sAuthorsM. A. Lyverse, J.J. Starn, M.D. UnthankGround-water levels in and pumpage from the alluvial aquifer at Louisville, Kentucky, May 1989-May 1991
Water-level data have been collected in the alluvial aquifer at Louisville, Ky., by the U.S. Geological Survey since 1943. Interpretations of these data are published periodically to update the record and help local officials manage this ground-water supply. Maps and hydrographs are presented on two sheets to aid in the interpretation of water-level changes for the period May 1989-May 1991. The alAuthorsMichael D. UnthankGround-water levels in the alluvial aquifer at Louisville, Kentucky, 1987-88
Water-level data have been collected in the alluvial aquifer at Louisville, Kentucky by the U.S. Geological Survey since 1943. Summaries and analysis of these data are published periodically to update the record and to help public officials who must manage this groundwater supply. Maps and hydrographs are presented in this report to update the record for 1987-88 and to interpret recent trends in wAuthorsR.J. Faust, B.E. LyonsGround-water levels in the alluvial aquifer at Louisville, Kentucky, 1982-87
Water level data have been collected in the alluvial aquifer at Louisville, Kentucky by the U.S. Geological Survey since 1943. Interpretations of these data have been published in several reports by the Survey, but none have been published since 1983. Contour maps and hydrographs are presented in this report to document and to help interpret water level changes for the period 1982-87. Maps and hydAuthorsR.J. Faust, M. A. LyverseChloroform contamination in part of the alluvial aquifer, southwest Louisville, Kentucky
No abstract available.AuthorsR. W. Davis, Edward W. MatthewsProblems of rising ground-water levels in urban areas with special reference to the Louisville, Kentucky area
Rising ground-water levels are a problem for cities such as San Bernadino, California; Greely and Fort Collins, Colorado; New York City boroughs of Brooklyn and Queens; and Louisville, Kentucky. Ground-water levels showed a steeply rising trend in the alluvial aquifer underlying Louisville during the early and middle 1970 's in response to above average precipitation and a decrease in ground-waterAuthorsD. V. Whitesides, R.J. Faust, D.D. ZettwochRising ground-water level in downtown Louisville, Kentucky, 1972-1977
Ground-water levels in the alluvial aquifer in Louisville, Jefferson County, Kentucky, are rising at a rate which could cause wet basements and possible structural damage tc buildings in the downtown area by 1982. The predicted water level for 1982 is based on the nearly linear increase which has been observed from 1972 to 1977, during which period a rise of as much as 32 feet was recorded in wateAuthorsJ. M. Kernodle, D. V. WhitesidesSummary of hydrologic conditions of the Louisville area, Kentucky
Water problems and their solutions have been associated with the growth and development of the Louisville area for more than a century. Many hydrologic data that aided water users in the past can be applied to present water problems and will be helpful for solving many similar problems in the future. Most of the water problems of Louisville, a water-rich area, concern management and are associatedAuthorsEdwin Allen BellProgress report on the ground-water resources of the Louisville area, Kentucky, 1949-55
In the Louisville area, the principal water-bearing formations are the glacial-outwash sand and gravel and, in places, the underlying limestone. During the period 1949 through 1955 pumpage from the two aquifers averaged about 30 mgd (million gallons per day). The pumpage was approximately in balance with the normal net recharge to the area but was only about 8 percent of the estimated potential suAuthorsEdwin A. Bell, Robert W. Kellogg, Willis K. KulpGround water in northeastern Louisville, Kentucky with reference to induced filtration
In cooperation with the city of Louisville, Ky., the U. S. Geological Survey made a detailed investigation during the period February 1945 to March 1947 of the ground-water resources of a 3-square-mile area along the Ohio River north-east of Louisville. Test drilling shows that the principal aquifer consists of about 80 feet of glacial-outwash sands and gravels lying in an old river channel whichAuthorsM. I. RorabaughWater resources of the Louisville area, Kentucky and Indiana
[No abstract available]AuthorsM. I. Rorabaugh, F. F. Schrader, L.B. Laird - Partners
Below are partners associated with this project.