Bruce G Campbell
Bruce Campbell is a Physical Scientist at the South Atlantic Water Science Center.
Currently serves as a Hydrologist for the USGS South Atlantic Water Science Center in Columbia, SC. Have 35+ years experience in geology and groundwater hydrology and have specialized in numerical simulation of groundwater flow and solute transport. Much of this work has focused on the groundwater resources of the Atlantic Coastal Plain. Have had several overseas assignments including a 2 year project in Cyprus and a project in Saudia Arabia.
Science and Products
Filter Total Items: 28
Development of a conceptual model of groundwater flow, Chesterfield County, South Carolina
Chesterfield County is located in the north central part of South Carolina (SC) and is adjacent to the North Carolina border. The County lies along the Fall Line, the geologic boundary between the Atlantic Coastal Plain (ACP) and Piedmont physiographic provinces. Between 2000 and 2007, the population increased from 42,768 to 43,191 people (U.S. Census Bureau, 2007). Associated with this...
Authors
Bruce G. Campbell, James Landmeyer
Contamination of groundwater by the fumigants ethylene dibromide (EDB) and dibromochloropropane (DBCP) near McBee, South Carolina
McBee is a small town of about 700 people located in Chesterfield County, South Carolina, in the Sandhills region of the upper Coastal Plain. The halogenated organic compounds ethylene dibromide (EDB) and dibromochloropropane (DBCP) have been detected in several public and domestic supply and irrigation wells since 2002 at concentrations above their U.S. Environmental Protection Agency...
Authors
James Landmeyer, Bruce G. Campbell
Simulation of Reclaimed-Water Injection and Pumping Scenarios and Particle-Tracking Analysis near Mount Pleasant, South Carolina
The effect of injecting reclaimed water into the Middendorf aquifer beneath Mount Pleasant, South Carolina, was simulated using a groundwater-flow model of the Coastal Plain Physiographic Province of South Carolina and parts of Georgia and North Carolina. Reclaimed water, also known as recycled water, is wastewater or stormwater that has been treated to an appropriate level so that the...
Authors
Matthew D. Petkewich, Bruce G. Campbell
Dielectric properties of lava flows west of Ascraeus Mons, Mars
The SHARAD instrument on the Mars Reconnaissance Orbiter detects subsurface interfaces beneath lava flow fields northwest of Ascraeus Mons. The interfaces occur in two locations; a northern flow that originates south of Alba Patera, and a southern flow that originates at the rift zone between Ascraeus and Pavonis Montes. The northern flow has permittivity values, estimated from the time...
Authors
Lynn M. Carter, Bruce G. Campbell, John W Holt, Roger J. Phillips, Nathaniel E. Putzig, Stefania Mattei, Roberto Seu, Chris Okubo, Anthony F. Egan
Shallow radar (SHARAD) sounding observations of the Medusae Fossae Formation, Mars
The SHARAD (shallow radar) sounding radar on the Mars Reconnaissance Orbiter detects subsurface reflections in the eastern and western parts of the Medusae Fossae Formation (MFF). The radar waves penetrate up to 580 m of the MFF and detect clear subsurface interfaces in two locations: west MFF between 150 and 155° E and east MFF between 209 and 213° E. Analysis of SHARAD radargrams...
Authors
Lynn M. Carter, Bruce G. Campbell, Thomas R. Watters, Roger J. Phillips, Nathaniel E. Putzig, Ali Safaeinili, Jeffrey J. Plaut, Chris Okubo, Anthony F. Egan, Roberto Seu, Daniela Biccari, Roberto Orosei
Hydrogeology and simulation of ground-water flow near Mount Pleasant, South Carolina: Predevelopment, 2004, and predicted scenarios for 2030
Heavy water use from the Cretaceous Middendorf aquifer in South Carolina has created a large, regional cone of depression in the potentiometric surface of the Middendorf aquifer in Charleston and Berkeley Counties, South Carolina. Water-level declines of up to 249 feet have been observed in wells over the past 125 years and are a result of ground-water use for public-water supply...
Authors
Matthew D. Petkewich, Bruce G. Campbell
A framework for assessing the sustainability of monitored natural attenuation
The sustainability of monitored natural attenuation (MNA) over time depends upon (1) the presence of chemical/biochemical processes that transform wastes to innocuous byproducts, and (2) the availability of energy to drive these processes to completion. The presence or absence of contaminant-transforming chemical/biochemical processes can be determined by observing contaminant mass loss...
Authors
Francis H. Chapelle, John T. Novak, John T.C. Parker, Bruce G. Campbell, Mark A. Widdowson
Hydrologic and geochemical evaluation of aquifer storage recovery in the Santee Limestone/Black Mingo Aquifer, Charleston, South Carolina, 1998-2002
The hydrologic and geochemical effects of aquifer storage recovery were evaluated to determine the potential for supplying the city of Charleston, South Carolina, with large quantities of potable water during emergencies, such as earthquakes, hurricanes, or hard freezes. An aquifer storage recovery system, including a production well and three observation wells, was installed at a site...
Authors
Matthew D. Petkewich, David L. Parkhurst, Kevin J. Conlon, Bruce G. Campbell, June Elizabeth Mirecki
The roughness of natural terrain: A planetary and remote sensing perspective
We examine the various methods and parameters in common use for quantifying and reporting surface topographic "roughness." It is shown that scale-dependent roughness parameters are almost always required, though not widely used. We suggest a method of standardizing the parameters that are computed and reported so that topographic data gathered by different workers using different field...
Authors
Michael K. Shepard, Bruce G. Campbell, Mark H. Bulmer, Lisa Gaddis, Tom G. Farr, Jeffrey J. Plaut
Evaluation of aquifer storage recovery in the Santee Limestone/Black Mingo Aquifer near Charleston, South Carolina, 1993-95
No abstract available.
Authors
B. G. Campbell, K.J. Conlon, June Elizabeth Mirecki
Documentation of model input and output values for the simulation of the ground-water flow system in the Cretaceous-age Coastal Plain aquifers of South Carolina
This report and the attached 3 1/2-inch diskette contain, in compressed format, the data sets for the model of ground-water flow in the Cretaceous-age Coastal Plain aquifers of South Carolina. The data sets can be uncompressed using a program provided with this report. The uncompressed files require approximately 3.7 megabytes of disk space on an IBM-compatible microcomputer1 using the...
Authors
B. G. Campbell, Marijke van Heeswijk
Ground-water hydrology, historical water use, and simulated ground-water flow in Cretaceous-age Coastal Plain aquifers near Charleston and Florence, South Carolina
A quasi-three-dimensional, transient, digital, ground-water flow model representing the Coastal Plain aquifers of South Carolina, has been constructed to assist in defining the ground- water-flow system of Cretaceous aquifers near Charleston and Florence, S.C. Both cities are near the centers of large (greater than 150 feet) potentiometric declines in the Middendorf aquifer. In 1989, the...
Authors
B. G. Campbell, Marijke van Heeswijk
Non-USGS Publications**
Campbell, B.G., and A.L. Coes, 2007, Numerical Simulation of Ground-Water Flow within the Atlantic Coastal Plain Aquifers of North and South Carolina (abstract): Clemson University Hydrogeological Symposium
Halford. K.J., and B.G. Campbell, 2004, A unique approach to estimating lateral anisotropy in complex geohydrologic environments: Journal of Hydraulic Research, vol. 42, p. 70-79.
Campbell, B.G., and T.R. Campbell, 2000, Hydrogeology and numerical simulation of ground-water flow in the surficial aquifer at the former Naval Station Charleston, SC: Pacific Environmental Restoration Conference, Honolulu, Hawaii, 10pp.http://www.perc2000.org/private/proceedings/GWCostEst.htm
Mirecki, J.E., B.G. Campbell, K.J. Conlon and, M.D. Petkewich 1998, Solute changes during aquifer storage recovery testing in a limestone/clastic aquifer: Ground Water, vol. 36, no. 3, pp. 394-403.
Campbell, B.G., J.E. Mirecki, K.J. Conlon, and M.D. Petkewich, 1997, Evaluation of aquifer storage recovery within the Santee Limestone / Black Mingo aquifer near Charleston, South Carolina 1993-95: American Water Resources Association Proceedings, Conjunctive Use of Water Resources: Aquifer Storage Recovery, Long Beach, California, pp.231-240.
Campbell, B.G., M.D. Petkewich, J.E. Landmeyer and F.H. Chapelle, 1995, Hydrogeology and intrinsic bioremediation potential of a manufactured gas plant site, Charleston, South Carolina: U.S. Geological Survey Circular 1108.
Mirecki, J.E., K.J. Conlon and B.G. Campbell, 1995, Geochemical evolution of injected municipal water during an aquifer storage and recovery project, Charleston, South Carolina: American Geophysical Union, Baltimore, Maryland.
Campbell, B.G., 1992, Water-level declines in the Middendorf aquifer, Charleston, Berkeley and Dorchester counties, South Carolina: American Water Resources Association National Symposium on the Future Availability of Ground Water Resources, Raleigh, North Carolina.
Gohn, G.S. and B.G. Campbell, 1991, Stratigraphic analysis of Cretaceous aquifers in the greater Charleston, South Carolina area: Geological Society of America Abstracts with Programs vol. 23.
Gohn ,G.S. and B.G. Campbell, 1991, Recent revisions to the stratigraphy of subsurface Cretaceous sediments in the Charleston, South Carolina area: South Carolina Geology vol. 34, nos. 1 and 2.
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
Science and Products
Filter Total Items: 28
Development of a conceptual model of groundwater flow, Chesterfield County, South Carolina
Chesterfield County is located in the north central part of South Carolina (SC) and is adjacent to the North Carolina border. The County lies along the Fall Line, the geologic boundary between the Atlantic Coastal Plain (ACP) and Piedmont physiographic provinces. Between 2000 and 2007, the population increased from 42,768 to 43,191 people (U.S. Census Bureau, 2007). Associated with this...
Authors
Bruce G. Campbell, James Landmeyer
Contamination of groundwater by the fumigants ethylene dibromide (EDB) and dibromochloropropane (DBCP) near McBee, South Carolina
McBee is a small town of about 700 people located in Chesterfield County, South Carolina, in the Sandhills region of the upper Coastal Plain. The halogenated organic compounds ethylene dibromide (EDB) and dibromochloropropane (DBCP) have been detected in several public and domestic supply and irrigation wells since 2002 at concentrations above their U.S. Environmental Protection Agency...
Authors
James Landmeyer, Bruce G. Campbell
Simulation of Reclaimed-Water Injection and Pumping Scenarios and Particle-Tracking Analysis near Mount Pleasant, South Carolina
The effect of injecting reclaimed water into the Middendorf aquifer beneath Mount Pleasant, South Carolina, was simulated using a groundwater-flow model of the Coastal Plain Physiographic Province of South Carolina and parts of Georgia and North Carolina. Reclaimed water, also known as recycled water, is wastewater or stormwater that has been treated to an appropriate level so that the...
Authors
Matthew D. Petkewich, Bruce G. Campbell
Dielectric properties of lava flows west of Ascraeus Mons, Mars
The SHARAD instrument on the Mars Reconnaissance Orbiter detects subsurface interfaces beneath lava flow fields northwest of Ascraeus Mons. The interfaces occur in two locations; a northern flow that originates south of Alba Patera, and a southern flow that originates at the rift zone between Ascraeus and Pavonis Montes. The northern flow has permittivity values, estimated from the time...
Authors
Lynn M. Carter, Bruce G. Campbell, John W Holt, Roger J. Phillips, Nathaniel E. Putzig, Stefania Mattei, Roberto Seu, Chris Okubo, Anthony F. Egan
Shallow radar (SHARAD) sounding observations of the Medusae Fossae Formation, Mars
The SHARAD (shallow radar) sounding radar on the Mars Reconnaissance Orbiter detects subsurface reflections in the eastern and western parts of the Medusae Fossae Formation (MFF). The radar waves penetrate up to 580 m of the MFF and detect clear subsurface interfaces in two locations: west MFF between 150 and 155° E and east MFF between 209 and 213° E. Analysis of SHARAD radargrams...
Authors
Lynn M. Carter, Bruce G. Campbell, Thomas R. Watters, Roger J. Phillips, Nathaniel E. Putzig, Ali Safaeinili, Jeffrey J. Plaut, Chris Okubo, Anthony F. Egan, Roberto Seu, Daniela Biccari, Roberto Orosei
Hydrogeology and simulation of ground-water flow near Mount Pleasant, South Carolina: Predevelopment, 2004, and predicted scenarios for 2030
Heavy water use from the Cretaceous Middendorf aquifer in South Carolina has created a large, regional cone of depression in the potentiometric surface of the Middendorf aquifer in Charleston and Berkeley Counties, South Carolina. Water-level declines of up to 249 feet have been observed in wells over the past 125 years and are a result of ground-water use for public-water supply...
Authors
Matthew D. Petkewich, Bruce G. Campbell
A framework for assessing the sustainability of monitored natural attenuation
The sustainability of monitored natural attenuation (MNA) over time depends upon (1) the presence of chemical/biochemical processes that transform wastes to innocuous byproducts, and (2) the availability of energy to drive these processes to completion. The presence or absence of contaminant-transforming chemical/biochemical processes can be determined by observing contaminant mass loss...
Authors
Francis H. Chapelle, John T. Novak, John T.C. Parker, Bruce G. Campbell, Mark A. Widdowson
Hydrologic and geochemical evaluation of aquifer storage recovery in the Santee Limestone/Black Mingo Aquifer, Charleston, South Carolina, 1998-2002
The hydrologic and geochemical effects of aquifer storage recovery were evaluated to determine the potential for supplying the city of Charleston, South Carolina, with large quantities of potable water during emergencies, such as earthquakes, hurricanes, or hard freezes. An aquifer storage recovery system, including a production well and three observation wells, was installed at a site...
Authors
Matthew D. Petkewich, David L. Parkhurst, Kevin J. Conlon, Bruce G. Campbell, June Elizabeth Mirecki
The roughness of natural terrain: A planetary and remote sensing perspective
We examine the various methods and parameters in common use for quantifying and reporting surface topographic "roughness." It is shown that scale-dependent roughness parameters are almost always required, though not widely used. We suggest a method of standardizing the parameters that are computed and reported so that topographic data gathered by different workers using different field...
Authors
Michael K. Shepard, Bruce G. Campbell, Mark H. Bulmer, Lisa Gaddis, Tom G. Farr, Jeffrey J. Plaut
Evaluation of aquifer storage recovery in the Santee Limestone/Black Mingo Aquifer near Charleston, South Carolina, 1993-95
No abstract available.
Authors
B. G. Campbell, K.J. Conlon, June Elizabeth Mirecki
Documentation of model input and output values for the simulation of the ground-water flow system in the Cretaceous-age Coastal Plain aquifers of South Carolina
This report and the attached 3 1/2-inch diskette contain, in compressed format, the data sets for the model of ground-water flow in the Cretaceous-age Coastal Plain aquifers of South Carolina. The data sets can be uncompressed using a program provided with this report. The uncompressed files require approximately 3.7 megabytes of disk space on an IBM-compatible microcomputer1 using the...
Authors
B. G. Campbell, Marijke van Heeswijk
Ground-water hydrology, historical water use, and simulated ground-water flow in Cretaceous-age Coastal Plain aquifers near Charleston and Florence, South Carolina
A quasi-three-dimensional, transient, digital, ground-water flow model representing the Coastal Plain aquifers of South Carolina, has been constructed to assist in defining the ground- water-flow system of Cretaceous aquifers near Charleston and Florence, S.C. Both cities are near the centers of large (greater than 150 feet) potentiometric declines in the Middendorf aquifer. In 1989, the...
Authors
B. G. Campbell, Marijke van Heeswijk
Non-USGS Publications**
Campbell, B.G., and A.L. Coes, 2007, Numerical Simulation of Ground-Water Flow within the Atlantic Coastal Plain Aquifers of North and South Carolina (abstract): Clemson University Hydrogeological Symposium
Halford. K.J., and B.G. Campbell, 2004, A unique approach to estimating lateral anisotropy in complex geohydrologic environments: Journal of Hydraulic Research, vol. 42, p. 70-79.
Campbell, B.G., and T.R. Campbell, 2000, Hydrogeology and numerical simulation of ground-water flow in the surficial aquifer at the former Naval Station Charleston, SC: Pacific Environmental Restoration Conference, Honolulu, Hawaii, 10pp.http://www.perc2000.org/private/proceedings/GWCostEst.htm
Mirecki, J.E., B.G. Campbell, K.J. Conlon and, M.D. Petkewich 1998, Solute changes during aquifer storage recovery testing in a limestone/clastic aquifer: Ground Water, vol. 36, no. 3, pp. 394-403.
Campbell, B.G., J.E. Mirecki, K.J. Conlon, and M.D. Petkewich, 1997, Evaluation of aquifer storage recovery within the Santee Limestone / Black Mingo aquifer near Charleston, South Carolina 1993-95: American Water Resources Association Proceedings, Conjunctive Use of Water Resources: Aquifer Storage Recovery, Long Beach, California, pp.231-240.
Campbell, B.G., M.D. Petkewich, J.E. Landmeyer and F.H. Chapelle, 1995, Hydrogeology and intrinsic bioremediation potential of a manufactured gas plant site, Charleston, South Carolina: U.S. Geological Survey Circular 1108.
Mirecki, J.E., K.J. Conlon and B.G. Campbell, 1995, Geochemical evolution of injected municipal water during an aquifer storage and recovery project, Charleston, South Carolina: American Geophysical Union, Baltimore, Maryland.
Campbell, B.G., 1992, Water-level declines in the Middendorf aquifer, Charleston, Berkeley and Dorchester counties, South Carolina: American Water Resources Association National Symposium on the Future Availability of Ground Water Resources, Raleigh, North Carolina.
Gohn, G.S. and B.G. Campbell, 1991, Stratigraphic analysis of Cretaceous aquifers in the greater Charleston, South Carolina area: Geological Society of America Abstracts with Programs vol. 23.
Gohn ,G.S. and B.G. Campbell, 1991, Recent revisions to the stratigraphy of subsurface Cretaceous sediments in the Charleston, South Carolina area: South Carolina Geology vol. 34, nos. 1 and 2.
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.