Philip Gardner
Philip Gardner is a Hydrologist and the Groundwater Specialist for the Nevada Water Science Center.
Phil has worked as a hydrologist with the US Geological Survey since 2001 and is currently the Groundwater Specialist at the Nevada Water Science Center in Carson City, NV. Much of his work has focused on the development of conceptual and numerical models of hydrologic systems and groundwater-surface water interaction throughout the eastern Great Basin and Colorado Plateau.
Science and Products
Aquifer Tests in Nevada
Many aquifer tests have been conducted by the U.S. Geological Survey to estimate hydraulic properties of aquifers in Nevada and adjacent states. Transmissivity is the principal hydraulic property that has been estimated from the aquifer tests in Nevada because these values directly affect estimates of ground-water flow.
Evaluation of Streamflow Depletion Related to Groundwater Withdrawal, Humboldt River Basin
The Humboldt River Basin (HRB) is the only major river basin that is entirely within the State of Nevada. Precipitation supplies all the water that enters the basin; consequently, the variability in climate has significant impacts on the hydrology of the area.
Evapotranspiration Studies in Nevada
Evapotranspiration (ET) is the process that transfers water from land surface to the atmosphere as evaporation (or sublimation when below freezing) from open water, soil, and plant canopies and as transpiration by plants. ET is measured by scientists for many different reasons. Hydrologists from the Nevada Water Scientist Center (NVWSC) typically measure ET to help quantify water budgets...
Science in the Humboldt River Basin
The Humboldt River is in north-central Nevada. The river is about 330 miles long and provides water for mostly agricultural purposes. One of the largest industries in Nevada is gold mining and the majority of those mines are in the Humboldt River Basin on the Carlin Trend. Gold mines in Nevada produce close to 80 percent of all the gold in the U.S. and are the 4th largest in the world. In 2010...
Spring Valley-Snake Valley Aquifers
Supplementary water supplies are needed for a rapidly growing population in southern Nevada. Ground-water resources from basin-fill and consolidated rock aquifers in southern Spring and Snake valleys in eastern Nevada have been identified as a potential water-supply source. These aquifers provide water to springs, streams, wetlands, limestone caves, and other biologically sensitive areas on...
Science and Products
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Aquifer Tests in Nevada
Many aquifer tests have been conducted by the U.S. Geological Survey to estimate hydraulic properties of aquifers in Nevada and adjacent states. Transmissivity is the principal hydraulic property that has been estimated from the aquifer tests in Nevada because these values directly affect estimates of ground-water flow.Evaluation of Streamflow Depletion Related to Groundwater Withdrawal, Humboldt River Basin
The Humboldt River Basin (HRB) is the only major river basin that is entirely within the State of Nevada. Precipitation supplies all the water that enters the basin; consequently, the variability in climate has significant impacts on the hydrology of the area.Evapotranspiration Studies in Nevada
Evapotranspiration (ET) is the process that transfers water from land surface to the atmosphere as evaporation (or sublimation when below freezing) from open water, soil, and plant canopies and as transpiration by plants. ET is measured by scientists for many different reasons. Hydrologists from the Nevada Water Scientist Center (NVWSC) typically measure ET to help quantify water budgets...Science in the Humboldt River Basin
The Humboldt River is in north-central Nevada. The river is about 330 miles long and provides water for mostly agricultural purposes. One of the largest industries in Nevada is gold mining and the majority of those mines are in the Humboldt River Basin on the Carlin Trend. Gold mines in Nevada produce close to 80 percent of all the gold in the U.S. and are the 4th largest in the world. In 2010...Spring Valley-Snake Valley Aquifers
Supplementary water supplies are needed for a rapidly growing population in southern Nevada. Ground-water resources from basin-fill and consolidated rock aquifers in southern Spring and Snake valleys in eastern Nevada have been identified as a potential water-supply source. These aquifers provide water to springs, streams, wetlands, limestone caves, and other biologically sensitive areas on... - Data
- Maps