The objective of this study is to develop a county-wide assessment of groundwater availability within the fractured-rock aquifer system in Wake County that will prepare the County for planning into the future. The goal is to develop a comprehensive groundwater budget for the county, including sources and distribution of water into the system and out of the system. Since fractured rock aquifers dominate the landscape, key tasks include characterization of the fractured rock aquifers. The study will assist Wake County in the management of their groundwater resources by providing information on sustainable quantity of groundwater, which will be based on water-budget components including potential recharge, distribution of well yields, and locating possible instances of well interference and competing uses.
Water-level data and results for slug tests performed in 17 wells in Wake County, North Carolina, 2020 and 2021
A water-supply plan is being developed for Wake County, North Carolina, in accordance with the 50-year planning window used by the North Carolina Division of Water Resources for residents in unincorporated areas of the county. To develop this supply plan, Wake County seeks to better understand the sustainability of groundwater resources of the regolith/fractured-rock aquifer system. Slug tests wer
Soil-Water-Balance (SWB) model datasets for the Greater Wake County area, North Carolina, 1981-2019
A Soil-Water-Balance (SWB) model was developed to estimate annual net infiltration below the root-zone for the Greater Wake County area, North Carolina for the period 1981 through 2019. The model was developed as part of a study to assess groundwater availability in the fractured-rock aquifers underlying Wake County. Curve number, maximum net infiltration rate, and root-zone depth parameters for a
Groundwater Well Yield in Wake County, North Carolina
The U.S. Geological Survey, in cooperation with Wake County Environmental Services, initiated a comprehensive groundwater resource investigation to better understand the quantity and quality of groundwater in Wake County, North Carolina. In 2020, as part of the investigation, groundwater records were compiled electronically from 7,689 wells in and within five miles of Wake County and groundwater y
Assessment of well yield, dominant fractures, and groundwater recharge in Wake County, North Carolina
A cooperative study led by the U.S. Geological Survey and Wake County Environmental Services was initiated to characterize the fractured-rock aquifer system and assess the sustainability of groundwater resources in and around Wake County. This report contributes to the development of a comprehensive groundwater budget for the study area, thereby helping to enable resource managers to make sound an
Authors
Dominick J. Antolino, Laura N. Gurley
Hydrogeology, groundwater seepage, nitrate distribution, and flux at the Raleigh hydrologic research station, Wake County, North Carolina, 2005-2007
rom 2005 to 2007, the U.S. Geological Survey and the North Carolina Department of Environment and Natural Resources, Division of Water Quality, conducted a study to describe the geologic framework, measure groundwater quality, characterize the groundwater-flow system, and describe the groundwater/surface-water interaction at the 60-acre Raleigh hydrogeologic research station (RHRS) located at the
Authors
Kristen Bukowski McSwain, Richard E. Bolich, Melinda J. Chapman
Fluctuations in groundwater levels related to regional and local withdrawals in the fractured-bedrock groundwater system in northern Wake County, North Carolina, March 2008-February 2009
A study of dewatering of the fractured-bedrock aquifer in a localized area of east-central North Carolina was conducted from March 2008 through February 2009 to gain an understanding of why some privately owned wells and monitoring wells were intermittently dry. Although the study itself was localized in nature, the resulting water-resources data and information produced from the study will help e
Authors
Melinda J. Chapman, Naser Almanaseer, Bryce McClenney, Natalie Hinton
Hydrogeologic setting, ground-water flow, and ground-water quality at the Lake Wheeler Road research station, 2001-03 : North Carolina Piedmont and Mountains Resource Evaluation Program
Results of a 2-year field study of the regolith-fractured bedrock ground-water system at the Lake Wheeler Road research station in Wake County, North Carolina, indicate both disconnection and interaction among components of the ground-water system. The three components of the ground-water system include (1) shallow, porous regolith; (2) a transition zone, including partially weathered rock, having
Authors
Melinda J. Chapman, Richard E. Bolich, Brad A. Huffman
- Overview
The objective of this study is to develop a county-wide assessment of groundwater availability within the fractured-rock aquifer system in Wake County that will prepare the County for planning into the future. The goal is to develop a comprehensive groundwater budget for the county, including sources and distribution of water into the system and out of the system. Since fractured rock aquifers dominate the landscape, key tasks include characterization of the fractured rock aquifers. The study will assist Wake County in the management of their groundwater resources by providing information on sustainable quantity of groundwater, which will be based on water-budget components including potential recharge, distribution of well yields, and locating possible instances of well interference and competing uses.
- Data
Water-level data and results for slug tests performed in 17 wells in Wake County, North Carolina, 2020 and 2021
A water-supply plan is being developed for Wake County, North Carolina, in accordance with the 50-year planning window used by the North Carolina Division of Water Resources for residents in unincorporated areas of the county. To develop this supply plan, Wake County seeks to better understand the sustainability of groundwater resources of the regolith/fractured-rock aquifer system. Slug tests werSoil-Water-Balance (SWB) model datasets for the Greater Wake County area, North Carolina, 1981-2019
A Soil-Water-Balance (SWB) model was developed to estimate annual net infiltration below the root-zone for the Greater Wake County area, North Carolina for the period 1981 through 2019. The model was developed as part of a study to assess groundwater availability in the fractured-rock aquifers underlying Wake County. Curve number, maximum net infiltration rate, and root-zone depth parameters for aGroundwater Well Yield in Wake County, North Carolina
The U.S. Geological Survey, in cooperation with Wake County Environmental Services, initiated a comprehensive groundwater resource investigation to better understand the quantity and quality of groundwater in Wake County, North Carolina. In 2020, as part of the investigation, groundwater records were compiled electronically from 7,689 wells in and within five miles of Wake County and groundwater y - Publications
Assessment of well yield, dominant fractures, and groundwater recharge in Wake County, North Carolina
A cooperative study led by the U.S. Geological Survey and Wake County Environmental Services was initiated to characterize the fractured-rock aquifer system and assess the sustainability of groundwater resources in and around Wake County. This report contributes to the development of a comprehensive groundwater budget for the study area, thereby helping to enable resource managers to make sound anAuthorsDominick J. Antolino, Laura N. GurleyHydrogeology, groundwater seepage, nitrate distribution, and flux at the Raleigh hydrologic research station, Wake County, North Carolina, 2005-2007
rom 2005 to 2007, the U.S. Geological Survey and the North Carolina Department of Environment and Natural Resources, Division of Water Quality, conducted a study to describe the geologic framework, measure groundwater quality, characterize the groundwater-flow system, and describe the groundwater/surface-water interaction at the 60-acre Raleigh hydrogeologic research station (RHRS) located at theAuthorsKristen Bukowski McSwain, Richard E. Bolich, Melinda J. ChapmanFluctuations in groundwater levels related to regional and local withdrawals in the fractured-bedrock groundwater system in northern Wake County, North Carolina, March 2008-February 2009
A study of dewatering of the fractured-bedrock aquifer in a localized area of east-central North Carolina was conducted from March 2008 through February 2009 to gain an understanding of why some privately owned wells and monitoring wells were intermittently dry. Although the study itself was localized in nature, the resulting water-resources data and information produced from the study will help eAuthorsMelinda J. Chapman, Naser Almanaseer, Bryce McClenney, Natalie HintonHydrogeologic setting, ground-water flow, and ground-water quality at the Lake Wheeler Road research station, 2001-03 : North Carolina Piedmont and Mountains Resource Evaluation Program
Results of a 2-year field study of the regolith-fractured bedrock ground-water system at the Lake Wheeler Road research station in Wake County, North Carolina, indicate both disconnection and interaction among components of the ground-water system. The three components of the ground-water system include (1) shallow, porous regolith; (2) a transition zone, including partially weathered rock, havingAuthorsMelinda J. Chapman, Richard E. Bolich, Brad A. Huffman