Robert Holmes, Jr., Ph.D., P.E., F.ASCE, F.EWRI, D.WRE (Former Employee)
Science and Products
Filter Total Items: 101
Ground-water age and atmospheric tracers: Simulation studies and analysis of field data from the Mirror Lake site, New Hampshire
The use of environmental tracers in characterization of ground-water systems is investigated through mathematical modeling of ground-water age and atmospheric tracer transport, and by a field study at the Mirror Lake site, New Hampshire. Theory is presented for modeling ground-water age using the advective-dispersive transport equation. The transport equation includes a zero-order source of unit s
Authors
Daniel J. Goode
Review of Aquifer Test Results for the Lansdale Area, Montgomery County, Pennsylvania, 1980–95
Aquifer and aquifer-isolation test results in and around North Penn Area 6 Superfund site, Lansdale, Montgomery County, Pennsylvania are reviewed to provide estimated aquifer properties for use in a numerical model of ground-water flow. This review was made to support of remedial action investigations by U.S. Environmental Protection Agency (USEPA), Region III, Philadelphia. The data reviewed are
Authors
Daniel J. Goode, Lisa A. Senior
Upper Illinois River basin
During the past 25 years, industry and government made large financial investments that resulted in better water quality across the Nation; however, many water-quality concerns remain. Following a 1986 pilot project, the U.S. Geological Survey began implementation of the National Water-Quality Assessment (NAWQA) Program in 1991. This program differs from other national water-quality assessment stu
Authors
Michael J. Friedel
Characterizing a ground water basin in a New England mountain and valley terrain
A ground water basin is defined as the volume of subsurface through which ground water flows from the water table to a specified discharge location. Delineating the topographically defined surface water basin and extending it vertically downward does not always define the ground water basin. Instead, a ground water basin is more appropriately delineated by tracking ground water flowpaths with a ca
Authors
Claire R. Tiedeman, Daniel J. Goode, Paul A. Hsieh
Flood tracking chart for the Illinois River basin
This Flood Tracking Chart for the Illinois River Basin in Illinois can be used to record and compare the predicted or current flood-crest stage to past flood-crest information. This information can then be used by residents and emergency-response personnel to make informed decisions concerning the threat of flooding to life and property. The chart shows a map of the Illinois River Basin (see below
Authors
Charles F. Avery, Robert R. Holmes, Jennifer B. Sharpe
Physical and chemical data on sediments deposited in the Missouri and the Mississippi River flood plains during the July through August 1993 flood
Because sediments deposited by the 1993 floods on the Missouri and Mississippi rivers were thought to contain elevated concentrations of nutrients and trace elements, sediment deposits were sampled at 25 floodplain locations. The samples were analyzed for particle size, water content, volatile solids, nutrients, carbon, selected trace elements, pesticides, and semivolatile organic compounds. Prefl
Authors
Gregg K. Schalk, Robert R. Holmes, Gary P. Johnson
Floods in northern Illinois, July 1996
No abstract available.
Authors
Robert R. Holmes, Amit Kapadia
Numerical simulation of ground-water flow through glacial deposits and crystalline bedrock in the Mirror Lake area, Grafton County, New Hampshire
This report documents the development of a computer model to simulate steady-state (long-term average) flow of ground water in the vicinity of Mirror Lake, which lies at the eastern end of the Hubbard Brook valley in central New Hampshire. The 10-km2 study area includes Mirror Lake, the three streams that flow into Mirror Lake, Leeman's Brook, Paradise Brook, and parts of Hubbard Brook and the Pem
Authors
Claire R. Tiedeman, Daniel J. Goode, Paul A. Hsieh
Composite recovery type curves in normalized time from Theis' exact solution
Type curves derived from Theis’ exact nonequilibrium well function solution are proposed for graphical estimation of aquifer hydraulic properties, transmissivity (T), and storage coefficient (S), from water‐level recovery data after cessation of a constant‐rate discharge test. Drawdown (on log scale) is plotted versus the ratio of time since pumping stopped to duration of pumping, a normalized tim
Authors
Daniel J. Goode
Floods of July 18-20, 1996, in northern Illinois
Record flooding occurred on many streams in northern Ilinois during July 18-20, 1996. Over 16 inches of rain fell at some locations during and just prior to this period. Peak of record discharges were recorded at 19 U.S. Geological Survey (USGS) streamflow-gaging stations. The USGS, in cooperation with the Illinois Department of Natural Resources, Office of Water Resources (IDNROWR), has compiled
Authors
Robert R. Holmes, Amanda Kupka
Suspended-sediment budget for the Kankakee River Basin, 1993-95
A suspended-sediment budget was constructed for the Kankakee River Basin using suspended-sediment data collected from January 1993 through December 1995 at six existing U.S. Geological Survey streamflow-gaging stations. The Iroquois River delivered almost twice as much suspended-sediment load to the Kankakee River main stem as did the Kankakee River above its junction with the Iroquois River. For
Authors
Robert R. Holmes
Sediment transport in the lower Missouri and the central Mississippi rivers, June 26 through September 14, 1993
Sediment data were collected for five sediment stations on the lower Missouri and the central Mississippi rivers during the 1993 flood. During the period of June 26 to September 14, 1993, 55 million metric tons was transported past St. Louis, Missouri by the Mississippi River. Sediment was stored in the Missouri River floodplain above the Mississippi River as more than 22,000 hectares of floodplai
Authors
Robert R. Holmes
Non-USGS Publications**
Watson, Chester C., Holmes, Jr., R.R., and Biedenharn, D.S..,2013, Mississippi River Streamflow Measurement Techniques at St. Louis, Missouri, Journal of Hydraulic Engineering, 139 (10), pp 1062-1070
**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: 101
Ground-water age and atmospheric tracers: Simulation studies and analysis of field data from the Mirror Lake site, New Hampshire
The use of environmental tracers in characterization of ground-water systems is investigated through mathematical modeling of ground-water age and atmospheric tracer transport, and by a field study at the Mirror Lake site, New Hampshire. Theory is presented for modeling ground-water age using the advective-dispersive transport equation. The transport equation includes a zero-order source of unit s
Authors
Daniel J. Goode
Review of Aquifer Test Results for the Lansdale Area, Montgomery County, Pennsylvania, 1980–95
Aquifer and aquifer-isolation test results in and around North Penn Area 6 Superfund site, Lansdale, Montgomery County, Pennsylvania are reviewed to provide estimated aquifer properties for use in a numerical model of ground-water flow. This review was made to support of remedial action investigations by U.S. Environmental Protection Agency (USEPA), Region III, Philadelphia. The data reviewed are
Authors
Daniel J. Goode, Lisa A. Senior
Upper Illinois River basin
During the past 25 years, industry and government made large financial investments that resulted in better water quality across the Nation; however, many water-quality concerns remain. Following a 1986 pilot project, the U.S. Geological Survey began implementation of the National Water-Quality Assessment (NAWQA) Program in 1991. This program differs from other national water-quality assessment stu
Authors
Michael J. Friedel
Characterizing a ground water basin in a New England mountain and valley terrain
A ground water basin is defined as the volume of subsurface through which ground water flows from the water table to a specified discharge location. Delineating the topographically defined surface water basin and extending it vertically downward does not always define the ground water basin. Instead, a ground water basin is more appropriately delineated by tracking ground water flowpaths with a ca
Authors
Claire R. Tiedeman, Daniel J. Goode, Paul A. Hsieh
Flood tracking chart for the Illinois River basin
This Flood Tracking Chart for the Illinois River Basin in Illinois can be used to record and compare the predicted or current flood-crest stage to past flood-crest information. This information can then be used by residents and emergency-response personnel to make informed decisions concerning the threat of flooding to life and property. The chart shows a map of the Illinois River Basin (see below
Authors
Charles F. Avery, Robert R. Holmes, Jennifer B. Sharpe
Physical and chemical data on sediments deposited in the Missouri and the Mississippi River flood plains during the July through August 1993 flood
Because sediments deposited by the 1993 floods on the Missouri and Mississippi rivers were thought to contain elevated concentrations of nutrients and trace elements, sediment deposits were sampled at 25 floodplain locations. The samples were analyzed for particle size, water content, volatile solids, nutrients, carbon, selected trace elements, pesticides, and semivolatile organic compounds. Prefl
Authors
Gregg K. Schalk, Robert R. Holmes, Gary P. Johnson
Floods in northern Illinois, July 1996
No abstract available.
Authors
Robert R. Holmes, Amit Kapadia
Numerical simulation of ground-water flow through glacial deposits and crystalline bedrock in the Mirror Lake area, Grafton County, New Hampshire
This report documents the development of a computer model to simulate steady-state (long-term average) flow of ground water in the vicinity of Mirror Lake, which lies at the eastern end of the Hubbard Brook valley in central New Hampshire. The 10-km2 study area includes Mirror Lake, the three streams that flow into Mirror Lake, Leeman's Brook, Paradise Brook, and parts of Hubbard Brook and the Pem
Authors
Claire R. Tiedeman, Daniel J. Goode, Paul A. Hsieh
Composite recovery type curves in normalized time from Theis' exact solution
Type curves derived from Theis’ exact nonequilibrium well function solution are proposed for graphical estimation of aquifer hydraulic properties, transmissivity (T), and storage coefficient (S), from water‐level recovery data after cessation of a constant‐rate discharge test. Drawdown (on log scale) is plotted versus the ratio of time since pumping stopped to duration of pumping, a normalized tim
Authors
Daniel J. Goode
Floods of July 18-20, 1996, in northern Illinois
Record flooding occurred on many streams in northern Ilinois during July 18-20, 1996. Over 16 inches of rain fell at some locations during and just prior to this period. Peak of record discharges were recorded at 19 U.S. Geological Survey (USGS) streamflow-gaging stations. The USGS, in cooperation with the Illinois Department of Natural Resources, Office of Water Resources (IDNROWR), has compiled
Authors
Robert R. Holmes, Amanda Kupka
Suspended-sediment budget for the Kankakee River Basin, 1993-95
A suspended-sediment budget was constructed for the Kankakee River Basin using suspended-sediment data collected from January 1993 through December 1995 at six existing U.S. Geological Survey streamflow-gaging stations. The Iroquois River delivered almost twice as much suspended-sediment load to the Kankakee River main stem as did the Kankakee River above its junction with the Iroquois River. For
Authors
Robert R. Holmes
Sediment transport in the lower Missouri and the central Mississippi rivers, June 26 through September 14, 1993
Sediment data were collected for five sediment stations on the lower Missouri and the central Mississippi rivers during the 1993 flood. During the period of June 26 to September 14, 1993, 55 million metric tons was transported past St. Louis, Missouri by the Mississippi River. Sediment was stored in the Missouri River floodplain above the Mississippi River as more than 22,000 hectares of floodplai
Authors
Robert R. Holmes
Non-USGS Publications**
Watson, Chester C., Holmes, Jr., R.R., and Biedenharn, D.S..,2013, Mississippi River Streamflow Measurement Techniques at St. Louis, Missouri, Journal of Hydraulic Engineering, 139 (10), pp 1062-1070
**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.