FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1516586638> ?p ?o ?g. }

• W1516586638 endingPage "1211" @default.
• W1516586638 startingPage "1195" @default.
• W1516586638 abstract "Sediment dynamics were investigated in Lake Maggiore, Italy, with field observations from October to mid-December 2012. Three moorings were deployed in Pallanza Bay, a small embayment on the western side of the lake near the Toce River inflow, to measure temperature and currents throughout the water column and suspended sediment concentration (SSC) was estimated with acoustic instrumentation. River intrusions are shown to dominate observed SSC, although a small amount of sediment resuspension was observed at the site of the shallowest mooring during a large wind event that produced strong upwelling of the thermocline followed by downwelling. Although vertical turbulent sediment flux is typically assumed to indicate resuspension and the upward transport of sediment ( ), downward turbulent sediment flux was observed ( ) near the bed during the largest observed intrusion event. The downward turbulent sediment flux significantly contributes to net deposition rates, which are one order of magnitude larger than rates of erosion measured during the two major events observed. Horizontal transport of sediment occurs in vertically confined layers due to buoyancy-driven intrusions. Beneath the intrusions, sediment settles out of the water column at settling rates that appear to be constant with depth based on acoustic Doppler current profiler backscatter measurements. The effective settling velocities needed to produce the observed vertical transport of SSC during an inflow intrusion are one order of magnitude larger than those due to the Stokes settling velocity ( ) alone. Particle flocculation and possible convective instabilities may play a role in generating the large observed effective settling rates." @default.
• W1516586638 created "2016-06-24" @default.
• W1516586638 creator A5033279409 @default.
• W1516586638 creator A5044457198 @default.
• W1516586638 creator A5059398561 @default.
• W1516586638 creator A5062742041 @default.
• W1516586638 date "2015-04-22" @default.
• W1516586638 modified "2023-10-10" @default.
• W1516586638 title "Sediment transport dynamics near a river inflow in a large alpine lake" @default.
• W1516586638 cites W1751567077 @default.
• W1516586638 cites W1966153369 @default.
• W1516586638 cites W1966577111 @default.
• W1516586638 cites W1970059382 @default.
• W1516586638 cites W1970759232 @default.
• W1516586638 cites W1971051192 @default.
• W1516586638 cites W1973402500 @default.
• W1516586638 cites W1983201256 @default.
• W1516586638 cites W1984826748 @default.
• W1516586638 cites W1989198781 @default.
• W1516586638 cites W1990439949 @default.
• W1516586638 cites W1992396834 @default.
• W1516586638 cites W1994465004 @default.
• W1516586638 cites W1995052551 @default.
• W1516586638 cites W1998096948 @default.
• W1516586638 cites W1999257004 @default.
• W1516586638 cites W2001080679 @default.
• W1516586638 cites W2006694335 @default.
• W1516586638 cites W2008107143 @default.
• W1516586638 cites W2029048677 @default.
• W1516586638 cites W2038742869 @default.
• W1516586638 cites W2041624527 @default.
• W1516586638 cites W2044953841 @default.
• W1516586638 cites W2061655171 @default.
• W1516586638 cites W2067346708 @default.
• W1516586638 cites W2068695328 @default.
• W1516586638 cites W2070056258 @default.
• W1516586638 cites W2078985635 @default.
• W1516586638 cites W2082701078 @default.
• W1516586638 cites W2083367737 @default.
• W1516586638 cites W2093002477 @default.
• W1516586638 cites W2093169773 @default.
• W1516586638 cites W2104700021 @default.
• W1516586638 cites W2125334604 @default.
• W1516586638 cites W2136867178 @default.
• W1516586638 cites W2137631780 @default.
• W1516586638 cites W2145757414 @default.
• W1516586638 cites W2147243747 @default.
• W1516586638 cites W2150556265 @default.
• W1516586638 cites W2166431417 @default.
• W1516586638 cites W2318079549 @default.
• W1516586638 cites W4211053668 @default.
• W1516586638 cites W4234865475 @default.
• W1516586638 doi "https://doi.org/10.1002/lno.10089" @default.
• W1516586638 hasPublicationYear "2015" @default.
• W1516586638 type Work @default.
• W1516586638 sameAs 1516586638 @default.
• W1516586638 citedByCount "20" @default.
• W1516586638 countsByYear W15165866382016 @default.
• W1516586638 countsByYear W15165866382017 @default.
• W1516586638 countsByYear W15165866382018 @default.
• W1516586638 countsByYear W15165866382019 @default.
• W1516586638 countsByYear W15165866382020 @default.
• W1516586638 countsByYear W15165866382021 @default.
• W1516586638 countsByYear W15165866382022 @default.
• W1516586638 countsByYear W15165866382023 @default.
• W1516586638 crossrefType "journal-article" @default.
• W1516586638 hasAuthorship W1516586638A5033279409 @default.
• W1516586638 hasAuthorship W1516586638A5044457198 @default.
• W1516586638 hasAuthorship W1516586638A5059398561 @default.
• W1516586638 hasAuthorship W1516586638A5062742041 @default.
• W1516586638 hasBestOaLocation W15165866381 @default.
• W1516586638 hasConcept C111368507 @default.
• W1516586638 hasConcept C114793014 @default.
• W1516586638 hasConcept C119601563 @default.
• W1516586638 hasConcept C122846477 @default.
• W1516586638 hasConcept C127313418 @default.
• W1516586638 hasConcept C148043351 @default.
• W1516586638 hasConcept C149348798 @default.
• W1516586638 hasConcept C173209714 @default.
• W1516586638 hasConcept C187320778 @default.
• W1516586638 hasConcept C191897082 @default.
• W1516586638 hasConcept C192562407 @default.
• W1516586638 hasConcept C2776132308 @default.
• W1516586638 hasConcept C2779365185 @default.
• W1516586638 hasConcept C2816523 @default.
• W1516586638 hasConcept C39432304 @default.
• W1516586638 hasConcept C65589250 @default.
• W1516586638 hasConcept C68709404 @default.
• W1516586638 hasConcept C76886044 @default.
• W1516586638 hasConcept C87717796 @default.
• W1516586638 hasConceptScore W1516586638C111368507 @default.
• W1516586638 hasConceptScore W1516586638C114793014 @default.
• W1516586638 hasConceptScore W1516586638C119601563 @default.
• W1516586638 hasConceptScore W1516586638C122846477 @default.
• W1516586638 hasConceptScore W1516586638C127313418 @default.
• W1516586638 hasConceptScore W1516586638C148043351 @default.
• W1516586638 hasConceptScore W1516586638C149348798 @default.
• W1516586638 hasConceptScore W1516586638C173209714 @default.

• next