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- Autorius: U S Department of the Interior
- Leidėjas: CreateSpace Independent Publishing Platform
- Metai: 2014
- Puslapiai: 50
- ISBN-10: 149618372X
- ISBN-13: 9781496183729
- Formatas: 15.2 x 22.9 x 0.3 cm, minkšti viršeliai
- Kalba: Anglų
Transient Calibration of a Groundwater-Flow Model of Chimacum Creek Basin and Vicinity, Jefferson County, Washington?A Supplement to Scientific Investigations Report 2013-5160 (el. knyga) (skaityta knyga) | knygos.lt
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Aprašymas
A steady-state groundwater-flow model described in Scientific Investigations Report 2013-5160, "Numerical Simulation of the Groundwater-Flow System in Chimacum Creek Basin and Vicinity, Jefferson County, Washington" was developed to evaluate potential future impacts of growth and of water-management strategies on water resources in the Chimacum Creek Basin. This supplement to that report describes the unsuccessful attempt to perform a calibration to transient conditions on the model. The modeled area is about 64 square miles on the Olympic Peninsula in northeastern Jefferson County, Washington. The geologic setting for the model area is that of unconsolidated deposits of glacial and interglacial origin typical of the Puget Sound Lowlands.
- Autorius: U S Department of the Interior
- Leidėjas: CreateSpace Independent Publishing Platform
- Metai: 2014
- Puslapiai: 50
- ISBN-10: 149618372X
- ISBN-13: 9781496183729
- Formatas: 15.2 x 22.9 x 0.3 cm, minkšti viršeliai
- Kalba: Anglų
A steady-state groundwater-flow model described in Scientific Investigations Report 2013-5160, "Numerical Simulation of the Groundwater-Flow System in Chimacum Creek Basin and Vicinity, Jefferson County, Washington" was developed to evaluate potential future impacts of growth and of water-management strategies on water resources in the Chimacum Creek Basin. This supplement to that report describes the unsuccessful attempt to perform a calibration to transient conditions on the model. The modeled area is about 64 square miles on the Olympic Peninsula in northeastern Jefferson County, Washington. The geologic setting for the model area is that of unconsolidated deposits of glacial and interglacial origin typical of the Puget Sound Lowlands.
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