FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1986218183> ?p ?o ?g. }

• W1986218183 endingPage "639" @default.
• W1986218183 startingPage "618" @default.
• W1986218183 abstract "Abstract: Over the past 35 years, a trend of decreasing water clarity has been documented in Lake Tahoe, attributable in part to the delivery of fine‐grained sediments emanating from upland and channel sources. The overall objective of the research reported here was to determine the amount of fine sediment delivered to Lake Tahoe from each of the 63 contributing watersheds. The research described in this report used combinations of field‐based observations of channel and bank stability with measured and simulated data on fine‐sediment loadings to estimate fine‐sediment loadings from unmonitored basins throughout the Lake Tahoe Basin. Loadings were expressed in the conventional format of mass per unit time but also in the number of particles finer than 20 μm, the latter for future use in a lake‐clarity model. The greatest contributors of fine sediment happened to be those with measured data, not requiring extrapolation. In descending order, they are as follows: Upper Truckee River [1,010 tonnes per year (T/year)], Blackwood Creek (846 T/year), Trout Creek (462 T/year), and Ward Creek (412 T/year). Summing estimated values from the contributing watersheds provided an average, annual estimate of fine‐sediment (<0.063 mm) loadings to the lake of 5,206 T/year. A total of 7.79E + 19 particles in the 5‐20 μm fraction were calculated to enter Lake Tahoe in an average year with the Upper Truckee River accounting for almost 25% of the total. Contributions from Blackwood, Ward, Trout, and Third creeks account for another 23% of these very fine particles. Thus, these five streams making up about 40% of the basin area, account for almost 50% of all fine‐sediment loadings to the lake. Contribution of fine sediment from streambank erosion were estimated by developing empirical relations between measured or simulated bank‐erosion rates with a field‐based measure of the extent of bank instability along given streams. An average, annual fine‐sediment loading from streambank erosion of 1,305 T/year was calculated. This represents about 25% of the average, annual fine‐sediment load delivered to the lake from all sources. The two largest contributors, the Upper Truckee River (639 T/year) and Blackwood Creek (431 T/year), account for slightly more than 80% of all fines emanating from streambanks, representing about 20% of the fine sediment delivered to Lake Tahoe from all sources. Extrapolations of fine‐sediment loadings to the unmonitored watersheds are based on documented empirical relations, yet contain a significant amount of uncertainty. Except for those values derived directly from measured data, reported results should be considered as estimates." @default.
• W1986218183 created "2016-06-24" @default.
• W1986218183 creator A5030842644 @default.
• W1986218183 date "2008-04-04" @default.
• W1986218183 modified "2023-10-16" @default.
• W1986218183 title "Fine-Sediment Loadings to Lake Tahoe" @default.
• W1986218183 cites W1997463466 @default.
• W1986218183 cites W2069687604 @default.
• W1986218183 cites W2159068937 @default.
• W1986218183 doi "https://doi.org/10.1111/j.1752-1688.2008.00188.x" @default.
• W1986218183 hasPublicationYear "2008" @default.
• W1986218183 type Work @default.
• W1986218183 sameAs 1986218183 @default.
• W1986218183 citedByCount "11" @default.
• W1986218183 countsByYear W19862181832012 @default.
• W1986218183 countsByYear W19862181832013 @default.
• W1986218183 countsByYear W19862181832014 @default.
• W1986218183 countsByYear W19862181832018 @default.
• W1986218183 crossrefType "journal-article" @default.
• W1986218183 hasAuthorship W1986218183A5030842644 @default.
• W1986218183 hasConcept C109007969 @default.
• W1986218183 hasConcept C114793014 @default.
• W1986218183 hasConcept C119599485 @default.
• W1986218183 hasConcept C126645576 @default.
• W1986218183 hasConcept C127162648 @default.
• W1986218183 hasConcept C127313418 @default.
• W1986218183 hasConcept C127413603 @default.
• W1986218183 hasConcept C166390339 @default.
• W1986218183 hasConcept C168329928 @default.
• W1986218183 hasConcept C187320778 @default.
• W1986218183 hasConcept C205649164 @default.
• W1986218183 hasConcept C2816523 @default.
• W1986218183 hasConcept C39432304 @default.
• W1986218183 hasConcept C58640448 @default.
• W1986218183 hasConcept C65589250 @default.
• W1986218183 hasConcept C76886044 @default.
• W1986218183 hasConceptScore W1986218183C109007969 @default.
• W1986218183 hasConceptScore W1986218183C114793014 @default.
• W1986218183 hasConceptScore W1986218183C119599485 @default.
• W1986218183 hasConceptScore W1986218183C126645576 @default.
• W1986218183 hasConceptScore W1986218183C127162648 @default.
• W1986218183 hasConceptScore W1986218183C127313418 @default.
• W1986218183 hasConceptScore W1986218183C127413603 @default.
• W1986218183 hasConceptScore W1986218183C166390339 @default.
• W1986218183 hasConceptScore W1986218183C168329928 @default.
• W1986218183 hasConceptScore W1986218183C187320778 @default.
• W1986218183 hasConceptScore W1986218183C205649164 @default.
• W1986218183 hasConceptScore W1986218183C2816523 @default.
• W1986218183 hasConceptScore W1986218183C39432304 @default.
• W1986218183 hasConceptScore W1986218183C58640448 @default.
• W1986218183 hasConceptScore W1986218183C65589250 @default.
• W1986218183 hasConceptScore W1986218183C76886044 @default.
• W1986218183 hasIssue "3" @default.
• W1986218183 hasLocation W19862181831 @default.
• W1986218183 hasOpenAccess W1986218183 @default.
• W1986218183 hasPrimaryLocation W19862181831 @default.
• W1986218183 hasRelatedWork W1574262502 @default.
• W1986218183 hasRelatedWork W1672492540 @default.
• W1986218183 hasRelatedWork W1999622724 @default.
• W1986218183 hasRelatedWork W2048159113 @default.
• W1986218183 hasRelatedWork W2097324746 @default.
• W1986218183 hasRelatedWork W2351827777 @default.
• W1986218183 hasRelatedWork W2354678068 @default.
• W1986218183 hasRelatedWork W2357299096 @default.
• W1986218183 hasRelatedWork W2389863717 @default.
• W1986218183 hasRelatedWork W2789353201 @default.
• W1986218183 hasVolume "44" @default.
• W1986218183 isParatext "false" @default.
• W1986218183 isRetracted "false" @default.
• W1986218183 magId "1986218183" @default.
• W1986218183 workType "article" @default.