FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1567244836> ?p ?o ?g. }

• W1567244836 abstract "The Niobrara River of Nebraska is a geologically, ecologically, and economically significant resource. The State of Nebraska has recognized the need to better manage the surface- and ground-water resources of the Niobrara River so they are sustainable in the long term. In cooperation with the Nebraska Game and Parks Commission, the U.S. Geological Survey is investigating the hydrogeomorphic settings and hydraulic geometry of the Niobrara River to assist in characterizing the types of broad-scale physical habitat attributes that may be of importance to the ecological resources of the river system. This report includes an inventory of surface-water and ground-water hydrology data, surface water-quality data, a longitudinal geomorphic segmentation and characterization of the main channel and its valley, and hydraulic geometry relations for the 330-mile section of the Niobrara River from Dunlap Diversion Dam in western Nebraska to the Missouri River confluence. Hydraulic microhabitats also were analyzed using available data from discharge measurements to demonstrate the potential application of these data and analysis methods. The main channel of the Niobrara was partitioned into three distinct fluvial geomorphic provinces: an upper province characterized by open valleys and a sinuous, equiwidth channel; a central province characterized by mixed valley and channel settings, including several entrenched canyon reaches; and a lower province where the valley is wide, yet restricted, but the river also is wide and persistently braided. Within the three fluvial geomorphic provinces, 36 geomorphic segments were identified using a customized, process-orientated classification scheme, which described the basic physical characteristics of the Niobrara River and its valley. Analysis of the longitudinal slope characteristics indicated that the Niobrara River longitudinal profile may be largely bedrock-controlled, with slope inflections co-located at changes in bedrock type at river level. Hydraulic geometry relations indicated that local (at-a-station) channel adjustments of the Niobrara River to changing discharge are accommodated mainly by changes in velocity, and streamwise adjustments are accommodated through changes in channel width. Downstream hydraulic geometry relations are in general agreement with values previously published for rivers of the Great Plains, but coefficients are likely skewed low because the locations of the streamflow-gaging stations used in this analysis are located at natural or engineered constrictions and may not be accurately representing downstream adjustment processes of the Niobrara River. A demonstration analysis of hydraulic microhabitat attributes at a single station indicated that changes in velocity-related habitat types is the primary microhabitat adjustment over a range of discharges, but the magnitude of that adjustment for any particular discharge is temporally variable." @default.
• W1567244836 created "2016-06-24" @default.
• W1567244836 creator A5009217876 @default.
• W1567244836 creator A5089440952 @default.
• W1567244836 creator A5090114283 @default.
• W1567244836 date "2009-01-01" @default.
• W1567244836 modified "2023-09-27" @default.
• W1567244836 title "Geomorphic segmentation, hydraulic geometry, and hydraulic microhabitats of the Niobrara River, Nebraska — Methods and initial results" @default.
• W1567244836 cites W143066625 @default.
• W1567244836 cites W1486243219 @default.
• W1567244836 cites W1522357428 @default.
• W1567244836 cites W1536513441 @default.
• W1567244836 cites W1557871810 @default.
• W1567244836 cites W1569116404 @default.
• W1567244836 cites W1587869157 @default.
• W1567244836 cites W1595783456 @default.
• W1567244836 cites W1598320745 @default.
• W1567244836 cites W1600888215 @default.
• W1567244836 cites W1604487127 @default.
• W1567244836 cites W1968076659 @default.
• W1567244836 cites W1970878662 @default.
• W1567244836 cites W2002349416 @default.
• W1567244836 cites W2008881367 @default.
• W1567244836 cites W2009055995 @default.
• W1567244836 cites W2011370232 @default.
• W1567244836 cites W2017136510 @default.
• W1567244836 cites W2025017677 @default.
• W1567244836 cites W2028325448 @default.
• W1567244836 cites W2047566650 @default.
• W1567244836 cites W2049873036 @default.
• W1567244836 cites W2055634287 @default.
• W1567244836 cites W2065448132 @default.
• W1567244836 cites W2067659920 @default.
• W1567244836 cites W2071258520 @default.
• W1567244836 cites W2078402640 @default.
• W1567244836 cites W2085663892 @default.
• W1567244836 cites W2086939578 @default.
• W1567244836 cites W2108828594 @default.
• W1567244836 cites W2113284578 @default.
• W1567244836 cites W2116935344 @default.
• W1567244836 cites W2120544827 @default.
• W1567244836 cites W2124951184 @default.
• W1567244836 cites W2132695741 @default.
• W1567244836 cites W2146119311 @default.
• W1567244836 cites W2169835201 @default.
• W1567244836 cites W2169938632 @default.
• W1567244836 cites W2273370527 @default.
• W1567244836 cites W2739392624 @default.
• W1567244836 cites W2773118521 @default.
• W1567244836 cites W2912954225 @default.
• W1567244836 cites W2971770296 @default.
• W1567244836 cites W3086845757 @default.
• W1567244836 cites W597626533 @default.
• W1567244836 doi "https://doi.org/10.3133/sir20095008" @default.
• W1567244836 hasPublicationYear "2009" @default.
• W1567244836 type Work @default.
• W1567244836 sameAs 1567244836 @default.
• W1567244836 citedByCount "10" @default.
• W1567244836 countsByYear W15672448362014 @default.
• W1567244836 countsByYear W15672448362018 @default.
• W1567244836 countsByYear W15672448362020 @default.
• W1567244836 countsByYear W15672448362021 @default.
• W1567244836 crossrefType "journal-article" @default.
• W1567244836 hasAuthorship W1567244836A5009217876 @default.
• W1567244836 hasAuthorship W1567244836A5089440952 @default.
• W1567244836 hasAuthorship W1567244836A5090114283 @default.
• W1567244836 hasBestOaLocation W15672448361 @default.
• W1567244836 hasConcept C109007969 @default.
• W1567244836 hasConcept C112959462 @default.
• W1567244836 hasConcept C114793014 @default.
• W1567244836 hasConcept C119599485 @default.
• W1567244836 hasConcept C126645576 @default.
• W1567244836 hasConcept C127162648 @default.
• W1567244836 hasConcept C127313418 @default.
• W1567244836 hasConcept C127413603 @default.
• W1567244836 hasConcept C151730666 @default.
• W1567244836 hasConcept C16828302 @default.
• W1567244836 hasConcept C187320778 @default.
• W1567244836 hasConcept C205649164 @default.
• W1567244836 hasConcept C2781113848 @default.
• W1567244836 hasConcept C58640448 @default.
• W1567244836 hasConcept C76886044 @default.
• W1567244836 hasConcept C84859931 @default.
• W1567244836 hasConceptScore W1567244836C109007969 @default.
• W1567244836 hasConceptScore W1567244836C112959462 @default.
• W1567244836 hasConceptScore W1567244836C114793014 @default.
• W1567244836 hasConceptScore W1567244836C119599485 @default.
• W1567244836 hasConceptScore W1567244836C126645576 @default.
• W1567244836 hasConceptScore W1567244836C127162648 @default.
• W1567244836 hasConceptScore W1567244836C127313418 @default.
• W1567244836 hasConceptScore W1567244836C127413603 @default.
• W1567244836 hasConceptScore W1567244836C151730666 @default.
• W1567244836 hasConceptScore W1567244836C16828302 @default.
• W1567244836 hasConceptScore W1567244836C187320778 @default.
• W1567244836 hasConceptScore W1567244836C205649164 @default.
• W1567244836 hasConceptScore W1567244836C2781113848 @default.
• W1567244836 hasConceptScore W1567244836C58640448 @default.
• W1567244836 hasConceptScore W1567244836C76886044 @default.
• W1567244836 hasConceptScore W1567244836C84859931 @default.
• W1567244836 hasLocation W15672448361 @default.

• next