John Izbicki
John Izbicki - California Water Science Center
Science and Products
Filter Total Items: 103
Hydrogeology and geochemistry of aquifers underlying the San Lorenzo and San Leandro areas of the East Bay Plain, Alameda County, California Hydrogeology and geochemistry of aquifers underlying the San Lorenzo and San Leandro areas of the East Bay Plain, Alameda County, California
The East Bay Plain, on the densely populated eastern shore of San Francisco Bay, contains an upper aquifer system to depths of 250 feet below land surface and an underlying lower aquifer system to depths of more than 650 feet. Injection and recovery of imported water has been proposed for deep aquifers at two sites within the lower aquifer system. Successful operation requires that the...
Authors
John A. Izbicki, James W. Borchers, David A. Leighton, Justin T. Kulongoski, Latoya Fields, Devin L. Galloway, Robert L. Michel
Helium isotope studies in the Mojave Desert, California: Implications for groundwater chronology and regional seismicity Helium isotope studies in the Mojave Desert, California: Implications for groundwater chronology and regional seismicity
We report helium isotope and concentration results for groundwaters from the western Mojave River Basin (MRB), 130 km east of Los Angeles, CA. The basin lies adjacent to the NW-SE trending San Andreas Fault (SAF) system. Samples were collected along two groundwater flowpaths that originate in the San Gabriel Mountains and discharge to the Mojave River located ???32 km to the northeast...
Authors
J.T. Kulongoski, David R. Hilton, J. A. Izbicki
Evaluation of unsaturated zone water fluxes in heterogeneous alluvium at a Mojave Basin Site Evaluation of unsaturated zone water fluxes in heterogeneous alluvium at a Mojave Basin Site
Vertical and horizontal water fluxes in the unsaturated zone near intermittent streams critically affect ecosystems, water supply, and contaminant transport in arid and semiarid regions. The subsurface near the Oro Grande Wash is typical in having great textural diversity, pronounced layer contrasts, and extremely low hydraulic conductivities associated with nearly dry media. These...
Authors
John R. Nimmo, Jeffrey A. Deason, John A. Izbicki, Peter Martin
Movement of water through the thick unsaturated zone underlying Oro Grande and Sheep Creek Washes in the western Mojave Desert, USA Movement of water through the thick unsaturated zone underlying Oro Grande and Sheep Creek Washes in the western Mojave Desert, USA
Previous studies indicate that a small quantity of recharge occurs from infiltration of streamflow in intermittent streams in the upper Mojave River basin, in the western Mojave Desert, near Victorville, California. Chloride, tritium, and stable isotope data collected in the unsaturated zone between 1994 and 1998 from boreholes drilled in Oro Grande and Sheep Creek Washes indicate that
Authors
J. A. Izbicki, J. Radyk, R. L. Michel
Water movement through a thick unsaturated zone underlying an intermittent stream in the western Mojave Desert, southern California, USA Water movement through a thick unsaturated zone underlying an intermittent stream in the western Mojave Desert, southern California, USA
Previous studies indicated that small amounts of recharge occur as infiltration of intermittent streamflow in washes in the upper Mojave River basin, in the western Mojave Desert, near Victorville, California. These washes flow only a few days each year after large storms. To reach the water table, water must pass through an unsaturated zone that is more than 130 m thick. Results of this...
Authors
J. A. Izbicki, J. Radyk, R. L. Michel
Water resources of the Blackstone River basin, Massachusetts Water resources of the Blackstone River basin, Massachusetts
By 2020, demand for water in the Blackstone River Basin is expected to be 52 million gallons per day, one-third greater than the demand of 39 million gallons per day in 1980. Most of this increase is expected to be supplied by increased withdrawals of ground water from stratified-drift aquifers in the eastern and northern parts of the basin. Increased withdrawals from stratified-drift...
Authors
John A. Izbicki
Data from a thick unsaturated zone underlying Oro Grande and Sheep Creek washes in the western part of the Mojave Desert, near Victorville, San Bernardino County, California Data from a thick unsaturated zone underlying Oro Grande and Sheep Creek washes in the western part of the Mojave Desert, near Victorville, San Bernardino County, California
This report presents data on the physical properties of unsaturated alluvial deposits and on the chemical and isotopic composition of soil water and soil gas collected at 12 monitoring sites in the western part of the Mojave Desert, near Victorville, California. Sites were installed using the ODEX air-hammer method. Seven sites were located in the active channels of Oro Grande and Sheep...
Authors
John A. Izbicki, Dennis A. Clark, Maria I. Pimental, Michael Land, John C. Radyk, Robert L. Michel
Stormflow chemistry in the Santa Ana River below Prado Dam and at the diversion downstream from Imperial Highway, southern California, 1995-98 Stormflow chemistry in the Santa Ana River below Prado Dam and at the diversion downstream from Imperial Highway, southern California, 1995-98
The Santa Ana River drains about 2,670 square miles of the densely populated coastal area of southern California, near Los Angeles. Almost all the flow in the river, more than 200,000 acre-feet annually, is diverted into ponds where it infiltrates and recharges underlying aquifers. About 2 million people are dependent on these aquifers for water supply. Stormflow in the Santa Ana River...
Authors
John A. Izbicki, Gregory O. Mendez, Carmen A. Burton
Application of flowmeter and depth-dependent water quality data for improved production well construction Application of flowmeter and depth-dependent water quality data for improved production well construction
Ground water production wells commonly are designed to maximize well yield and, therefore, may be screened over several water-bearing zones. These water-bearing zones usually are identified, and their hydrogeologic characteristics and water quality are inferred, on the basis of indirect data such as geologic and geophysical logs. Production well designs based on these data may result in...
Authors
M.A. Gossell, Tracy Nishikawa, Randall T. Hanson, John A. Izbicki, M.A. Tabidian, K. Bertine
Numerical model of a tracer test on the Santa Clara River, Ventura County, California Numerical model of a tracer test on the Santa Clara River, Ventura County, California
To better understand the flow processes, solute-transport processes, and ground-water/surface-water interactions on the Santa Clara River in Ventura County, California, a 24-hour fluorescent-dye tracer study was performed under steady-state flow conditions on a 45-km reach of the river. The study reach includes perennial (uppermost and lowermost) subreaches and ephemeral subreaches of...
Authors
Tracy Nishikawa, Katherine S. Paybins, John A. Izbicki, Eric G. Reichard
U.S. Geological Survey combined well-bore flow and depth-dependent water sampler U.S. Geological Survey combined well-bore flow and depth-dependent water sampler
The U.S. Geological Survey has developed a combined well-bore flow and depth-dependent sample collection tool. It is suitable for use in existing production wells having limited access and clearances as small as 1 inch. The combination of well-bore flow and depth-dependent water-quality data is especially effective in assessing changes in aquifer properties and water quality with depth...
Authors
John A. Izbicki, Allen H. Christensen, Randall T. Hanson, Peter Martin, Steven M. Crawford, Gregory A. Smith
Statistical analysis and mathematical modeling of a tracer test on the Santa Clara River, Ventura County, California Statistical analysis and mathematical modeling of a tracer test on the Santa Clara River, Ventura County, California
To better understand flow processes, solute-transport processes, and ground-water/surface-water interactions on the Santa Clara River in Ventura County, California, a 24-hour fluorescent-dye tracer study was performed under steady-state flow conditions on a 28-mile reach of the river. The study reach includes perennial (uppermost and lowermost) subreaches and ephemeral subreaches of the...
Authors
Katherine S. Paybins, Tracy Nishikawa, John A. Izbicki, Eric G. Reichard
Science and Products
Filter Total Items: 103
Hydrogeology and geochemistry of aquifers underlying the San Lorenzo and San Leandro areas of the East Bay Plain, Alameda County, California Hydrogeology and geochemistry of aquifers underlying the San Lorenzo and San Leandro areas of the East Bay Plain, Alameda County, California
The East Bay Plain, on the densely populated eastern shore of San Francisco Bay, contains an upper aquifer system to depths of 250 feet below land surface and an underlying lower aquifer system to depths of more than 650 feet. Injection and recovery of imported water has been proposed for deep aquifers at two sites within the lower aquifer system. Successful operation requires that the...
Authors
John A. Izbicki, James W. Borchers, David A. Leighton, Justin T. Kulongoski, Latoya Fields, Devin L. Galloway, Robert L. Michel
Helium isotope studies in the Mojave Desert, California: Implications for groundwater chronology and regional seismicity Helium isotope studies in the Mojave Desert, California: Implications for groundwater chronology and regional seismicity
We report helium isotope and concentration results for groundwaters from the western Mojave River Basin (MRB), 130 km east of Los Angeles, CA. The basin lies adjacent to the NW-SE trending San Andreas Fault (SAF) system. Samples were collected along two groundwater flowpaths that originate in the San Gabriel Mountains and discharge to the Mojave River located ???32 km to the northeast...
Authors
J.T. Kulongoski, David R. Hilton, J. A. Izbicki
Evaluation of unsaturated zone water fluxes in heterogeneous alluvium at a Mojave Basin Site Evaluation of unsaturated zone water fluxes in heterogeneous alluvium at a Mojave Basin Site
Vertical and horizontal water fluxes in the unsaturated zone near intermittent streams critically affect ecosystems, water supply, and contaminant transport in arid and semiarid regions. The subsurface near the Oro Grande Wash is typical in having great textural diversity, pronounced layer contrasts, and extremely low hydraulic conductivities associated with nearly dry media. These...
Authors
John R. Nimmo, Jeffrey A. Deason, John A. Izbicki, Peter Martin
Movement of water through the thick unsaturated zone underlying Oro Grande and Sheep Creek Washes in the western Mojave Desert, USA Movement of water through the thick unsaturated zone underlying Oro Grande and Sheep Creek Washes in the western Mojave Desert, USA
Previous studies indicate that a small quantity of recharge occurs from infiltration of streamflow in intermittent streams in the upper Mojave River basin, in the western Mojave Desert, near Victorville, California. Chloride, tritium, and stable isotope data collected in the unsaturated zone between 1994 and 1998 from boreholes drilled in Oro Grande and Sheep Creek Washes indicate that
Authors
J. A. Izbicki, J. Radyk, R. L. Michel
Water movement through a thick unsaturated zone underlying an intermittent stream in the western Mojave Desert, southern California, USA Water movement through a thick unsaturated zone underlying an intermittent stream in the western Mojave Desert, southern California, USA
Previous studies indicated that small amounts of recharge occur as infiltration of intermittent streamflow in washes in the upper Mojave River basin, in the western Mojave Desert, near Victorville, California. These washes flow only a few days each year after large storms. To reach the water table, water must pass through an unsaturated zone that is more than 130 m thick. Results of this...
Authors
J. A. Izbicki, J. Radyk, R. L. Michel
Water resources of the Blackstone River basin, Massachusetts Water resources of the Blackstone River basin, Massachusetts
By 2020, demand for water in the Blackstone River Basin is expected to be 52 million gallons per day, one-third greater than the demand of 39 million gallons per day in 1980. Most of this increase is expected to be supplied by increased withdrawals of ground water from stratified-drift aquifers in the eastern and northern parts of the basin. Increased withdrawals from stratified-drift...
Authors
John A. Izbicki
Data from a thick unsaturated zone underlying Oro Grande and Sheep Creek washes in the western part of the Mojave Desert, near Victorville, San Bernardino County, California Data from a thick unsaturated zone underlying Oro Grande and Sheep Creek washes in the western part of the Mojave Desert, near Victorville, San Bernardino County, California
This report presents data on the physical properties of unsaturated alluvial deposits and on the chemical and isotopic composition of soil water and soil gas collected at 12 monitoring sites in the western part of the Mojave Desert, near Victorville, California. Sites were installed using the ODEX air-hammer method. Seven sites were located in the active channels of Oro Grande and Sheep...
Authors
John A. Izbicki, Dennis A. Clark, Maria I. Pimental, Michael Land, John C. Radyk, Robert L. Michel
Stormflow chemistry in the Santa Ana River below Prado Dam and at the diversion downstream from Imperial Highway, southern California, 1995-98 Stormflow chemistry in the Santa Ana River below Prado Dam and at the diversion downstream from Imperial Highway, southern California, 1995-98
The Santa Ana River drains about 2,670 square miles of the densely populated coastal area of southern California, near Los Angeles. Almost all the flow in the river, more than 200,000 acre-feet annually, is diverted into ponds where it infiltrates and recharges underlying aquifers. About 2 million people are dependent on these aquifers for water supply. Stormflow in the Santa Ana River...
Authors
John A. Izbicki, Gregory O. Mendez, Carmen A. Burton
Application of flowmeter and depth-dependent water quality data for improved production well construction Application of flowmeter and depth-dependent water quality data for improved production well construction
Ground water production wells commonly are designed to maximize well yield and, therefore, may be screened over several water-bearing zones. These water-bearing zones usually are identified, and their hydrogeologic characteristics and water quality are inferred, on the basis of indirect data such as geologic and geophysical logs. Production well designs based on these data may result in...
Authors
M.A. Gossell, Tracy Nishikawa, Randall T. Hanson, John A. Izbicki, M.A. Tabidian, K. Bertine
Numerical model of a tracer test on the Santa Clara River, Ventura County, California Numerical model of a tracer test on the Santa Clara River, Ventura County, California
To better understand the flow processes, solute-transport processes, and ground-water/surface-water interactions on the Santa Clara River in Ventura County, California, a 24-hour fluorescent-dye tracer study was performed under steady-state flow conditions on a 45-km reach of the river. The study reach includes perennial (uppermost and lowermost) subreaches and ephemeral subreaches of...
Authors
Tracy Nishikawa, Katherine S. Paybins, John A. Izbicki, Eric G. Reichard
U.S. Geological Survey combined well-bore flow and depth-dependent water sampler U.S. Geological Survey combined well-bore flow and depth-dependent water sampler
The U.S. Geological Survey has developed a combined well-bore flow and depth-dependent sample collection tool. It is suitable for use in existing production wells having limited access and clearances as small as 1 inch. The combination of well-bore flow and depth-dependent water-quality data is especially effective in assessing changes in aquifer properties and water quality with depth...
Authors
John A. Izbicki, Allen H. Christensen, Randall T. Hanson, Peter Martin, Steven M. Crawford, Gregory A. Smith
Statistical analysis and mathematical modeling of a tracer test on the Santa Clara River, Ventura County, California Statistical analysis and mathematical modeling of a tracer test on the Santa Clara River, Ventura County, California
To better understand flow processes, solute-transport processes, and ground-water/surface-water interactions on the Santa Clara River in Ventura County, California, a 24-hour fluorescent-dye tracer study was performed under steady-state flow conditions on a 28-mile reach of the river. The study reach includes perennial (uppermost and lowermost) subreaches and ephemeral subreaches of the...
Authors
Katherine S. Paybins, Tracy Nishikawa, John A. Izbicki, Eric G. Reichard