FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W69550608> ?p ?o ?g. }

• W69550608 abstract "A three-dimensional, transient numerical model of groundwater and surface-water flow was constructed for Chamokane Creek basin to better understand the groundwater-flow system and its relation to surface-water resources. The model described in this report can be used as a tool by water-management agencies and other stakeholders to quantitatively evaluate the effects of potential increases in groundwater pumping on groundwater and surface-water resources in the basin. The Chamokane Creek model was constructed using the U.S. Geological Survey (USGS) integrated model, GSFLOW. GSFLOW was developed to simulate coupled groundwater and surface-water resources. The model uses 1,000-foot grid cells that subdivide the model domain by 102 rows and 106 columns. Six hydrogeologic units in the model are represented using eight model layers. Daily precipitation and temperature were spatially distributed and subsequent groundwater recharge was computed within GSFLOW. Streamflows in Chamokane Creek and its major tributaries are simulated in the model by routing streamflow within a stream network that is coupled to the groundwater-flow system. Groundwater pumpage and surface-water diversions and returns specified in the model were derived from monthly and annual pumpage values previously estimated from another component of this study and new data reported by study partners. The model simulation period is water years 1980-2010 (October 1, 1979, to September 30, 2010), but the model was calibrated to the transient conditions for water years 1999-2010 (October 1, 1998, to September 30, 2010). Calibration was completed by using traditional trial-and-error methods and automated parameter-estimation techniques. The model adequately reproduces the measured time-series groundwater levels and daily streamflows. At well observation points, the mean difference between simulated and measured hydraulic heads is 7 feet with a root-mean-square error divided by the total difference in water levels of 4.7 percent. Simulated streamflow was compared to measured streamflow at the USGS streamflow-gaging station-Chamokane Creek below Falls, near Long Lake (12433200). Annual differences between measured and simulated streamflow for the site ranged from -63 to 22 percent. Calibrated model output includes a 31-year estimate of monthly water budget components for the hydrologic system. Five model applications (scenarios) were completed to obtain a better understanding of the relation between groundwater pumping and surface-water resources. The calibrated transient model was used to evaluate: (1) the connection between the upper- and middle-basin groundwater systems, (2) the effect of surface-water and groundwater uses in the middle basin, (3) the cumulative impacts of claims registry use and permit-exempt wells on Chamokane Creek streamflow, (4) the frequency of regulation due to impacted streamflow, and (5) the levels of domestic and stockwater use that can be regulated. The simulation results indicated that streamflow is affected by existing groundwater pumping in the upper and middle basins. Simulated water-management scenarios show streamflow increased relative to historical conditions as groundwater and surface-water withdrawals decreased." @default.
• W69550608 created "2016-06-24" @default.
• W69550608 creator A5063516008 @default.
• W69550608 creator A5073751283 @default.
• W69550608 date "2012-01-01" @default.
• W69550608 modified "2023-10-02" @default.
• W69550608 title "Simulation of groundwater and surface-water resources and evaluation of water-management alternatives for the Chamokane Creek basin, Stevens County, Washington" @default.
• W69550608 cites W148303171 @default.
• W69550608 cites W1494559594 @default.
• W69550608 cites W1511269951 @default.
• W69550608 cites W1512740276 @default.
• W69550608 cites W1513810172 @default.
• W69550608 cites W151593474 @default.
• W69550608 cites W1525370878 @default.
• W69550608 cites W1547904935 @default.
• W69550608 cites W1557171307 @default.
• W69550608 cites W1567127719 @default.
• W69550608 cites W158322383 @default.
• W69550608 cites W1795911209 @default.
• W69550608 cites W1984129257 @default.
• W69550608 cites W1989172564 @default.
• W69550608 cites W2038795280 @default.
• W69550608 cites W2123506914 @default.
• W69550608 cites W2124307977 @default.
• W69550608 cites W2163850148 @default.
• W69550608 cites W2176478590 @default.
• W69550608 cites W2736867504 @default.
• W69550608 cites W3192977800 @default.
• W69550608 cites W41139122 @default.
• W69550608 doi "https://doi.org/10.3133/sir20125224" @default.
• W69550608 hasPublicationYear "2012" @default.
• W69550608 type Work @default.
• W69550608 sameAs 69550608 @default.
• W69550608 citedByCount "7" @default.
• W69550608 countsByYear W695506082014 @default.
• W69550608 countsByYear W695506082015 @default.
• W69550608 countsByYear W695506082016 @default.
• W69550608 countsByYear W695506082017 @default.
• W69550608 countsByYear W695506082022 @default.
• W69550608 countsByYear W695506082023 @default.
• W69550608 crossrefType "journal-article" @default.
• W69550608 hasAuthorship W69550608A5063516008 @default.
• W69550608 hasAuthorship W69550608A5073751283 @default.
• W69550608 hasBestOaLocation W695506081 @default.
• W69550608 hasConcept C109007969 @default.
• W69550608 hasConcept C114793014 @default.
• W69550608 hasConcept C12129029 @default.
• W69550608 hasConcept C126197015 @default.
• W69550608 hasConcept C126645576 @default.
• W69550608 hasConcept C127313418 @default.
• W69550608 hasConcept C131227075 @default.
• W69550608 hasConcept C153823671 @default.
• W69550608 hasConcept C16828302 @default.
• W69550608 hasConcept C174091901 @default.
• W69550608 hasConcept C176650113 @default.
• W69550608 hasConcept C187320778 @default.
• W69550608 hasConcept C18903297 @default.
• W69550608 hasConcept C205649164 @default.
• W69550608 hasConcept C2779313249 @default.
• W69550608 hasConcept C33556824 @default.
• W69550608 hasConcept C39432304 @default.
• W69550608 hasConcept C39769621 @default.
• W69550608 hasConcept C49204034 @default.
• W69550608 hasConcept C53739315 @default.
• W69550608 hasConcept C58640448 @default.
• W69550608 hasConcept C75622301 @default.
• W69550608 hasConcept C76177295 @default.
• W69550608 hasConcept C76886044 @default.
• W69550608 hasConcept C8625798 @default.
• W69550608 hasConcept C86803240 @default.
• W69550608 hasConcept C87717796 @default.
• W69550608 hasConceptScore W69550608C109007969 @default.
• W69550608 hasConceptScore W69550608C114793014 @default.
• W69550608 hasConceptScore W69550608C12129029 @default.
• W69550608 hasConceptScore W69550608C126197015 @default.
• W69550608 hasConceptScore W69550608C126645576 @default.
• W69550608 hasConceptScore W69550608C127313418 @default.
• W69550608 hasConceptScore W69550608C131227075 @default.
• W69550608 hasConceptScore W69550608C153823671 @default.
• W69550608 hasConceptScore W69550608C16828302 @default.
• W69550608 hasConceptScore W69550608C174091901 @default.
• W69550608 hasConceptScore W69550608C176650113 @default.
• W69550608 hasConceptScore W69550608C187320778 @default.
• W69550608 hasConceptScore W69550608C18903297 @default.
• W69550608 hasConceptScore W69550608C205649164 @default.
• W69550608 hasConceptScore W69550608C2779313249 @default.
• W69550608 hasConceptScore W69550608C33556824 @default.
• W69550608 hasConceptScore W69550608C39432304 @default.
• W69550608 hasConceptScore W69550608C39769621 @default.
• W69550608 hasConceptScore W69550608C49204034 @default.
• W69550608 hasConceptScore W69550608C53739315 @default.
• W69550608 hasConceptScore W69550608C58640448 @default.
• W69550608 hasConceptScore W69550608C75622301 @default.
• W69550608 hasConceptScore W69550608C76177295 @default.
• W69550608 hasConceptScore W69550608C76886044 @default.
• W69550608 hasConceptScore W69550608C8625798 @default.
• W69550608 hasConceptScore W69550608C86803240 @default.
• W69550608 hasConceptScore W69550608C87717796 @default.
• W69550608 hasLocation W695506081 @default.
• W69550608 hasOpenAccess W69550608 @default.

• next