FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1996853006> ?p ?o ?g. }

• W1996853006 endingPage "269" @default.
• W1996853006 startingPage "254" @default.
• W1996853006 abstract "Over the past two decades there has been a growing interest in the geomorphological mosaic along large floodplain rivers where channel dynamics are seen to drive habitat-patch creation and turnover and to contribute to high biological diversity. This has required a new perspective on fluvial geomorphology that focuses on biological scales of space and time. This study examines the spatial pattern of surface fine sediment accumulations along a reach of a large gravel-bed river, the Tagliamento River in NE Italy; an area with a moist Mediterranean climate and seasonal flow regime. The study investigates changes in sediment characteristics during the summer low-flow period between April and September. Focussing on five areas representing a gradient from open, bar-braided to wooded island-braided morphologies, the paper demonstrates the importance of riparian vegetation and aeolian–fluvial interactions. Significant contrasts in particle size distributions and organic content of freshly deposited sand and finer sediments were found between sampling areas, geomorphological settings, and sampling dates. In particular, wooded floodplain and established islands supported consistently finer sediment deposits than both open bar surfaces and the lee of pioneer islands, and in September significantly finer sediments were also found in deposits located in the lee of pioneer islands than on open bar surfaces. Overall, the September samples had a greater variability in particle size characteristics than those obtained from the same sites in April, with a general coarsening of the D5 (φ) (i.e., the coarse tail of the particle size distribution). Also in September, crusts of fine sediment (30 μm < D50 < 64 μm) had formed on the surface of some of the open bar and pioneer island deposits within the more open sampling areas along the study reach. These crusts possessed similar particle size characteristics to aeolian crusts found in more arid environments. They were significantly finer than April samples and September subcrust samples obtained from the same sites and had similar particle size characteristics to some samples taken from wooded floodplain, established island surfaces and the lee of pioneer islands that were not crusted. Local climatological and river level data confirm significant wind and rainfall events during a period of consistently low river levels between the April and September sampling periods. These support deflation, deposition and rain wash of finer sediment during the summer, with windblown sediments being deposited on bar surfaces and in the lee of pioneer islands where wood and young trees provide foci for accelerated sedimentation and island growth as well as on marginal floodplains and established islands. We conclude that along braided rivers in moist settings but with a distinct dry season, aeolian reworking of sediment deposits may have a more important role in driving habitat dynamics than previously considered." @default.
• W1996853006 created "2016-06-24" @default.
• W1996853006 creator A5051315067 @default.
• W1996853006 creator A5083948425 @default.
• W1996853006 creator A5088420023 @default.
• W1996853006 date "2008-07-01" @default.
• W1996853006 modified "2023-09-26" @default.
• W1996853006 title "Characteristics of freshly deposited sand and finer sediments along an island-braided, gravel-bed river: The roles of water, wind and trees" @default.
• W1996853006 cites W106221628 @default.
• W1996853006 cites W125677457 @default.
• W1996853006 cites W1966746778 @default.
• W1996853006 cites W1974489992 @default.
• W1996853006 cites W2002349416 @default.
• W1996853006 cites W2005299269 @default.
• W1996853006 cites W2006274358 @default.
• W1996853006 cites W2007082722 @default.
• W1996853006 cites W2025873959 @default.
• W1996853006 cites W2028051313 @default.
• W1996853006 cites W2033056548 @default.
• W1996853006 cites W2040802187 @default.
• W1996853006 cites W2044946456 @default.
• W1996853006 cites W2046368430 @default.
• W1996853006 cites W2049630649 @default.
• W1996853006 cites W2051202629 @default.
• W1996853006 cites W2056578221 @default.
• W1996853006 cites W2059748385 @default.
• W1996853006 cites W2066769242 @default.
• W1996853006 cites W2067432181 @default.
• W1996853006 cites W2077267127 @default.
• W1996853006 cites W2080101287 @default.
• W1996853006 cites W2092040144 @default.
• W1996853006 cites W2095274233 @default.
• W1996853006 cites W2112841957 @default.
• W1996853006 cites W2134598475 @default.
• W1996853006 cites W2137024708 @default.
• W1996853006 cites W2142600201 @default.
• W1996853006 cites W2149647935 @default.
• W1996853006 cites W2159675182 @default.
• W1996853006 cites W2160732210 @default.
• W1996853006 cites W2161964273 @default.
• W1996853006 cites W2162121861 @default.
• W1996853006 cites W2168584170 @default.
• W1996853006 cites W2245700388 @default.
• W1996853006 cites W4206132802 @default.
• W1996853006 doi "https://doi.org/10.1016/j.geomorph.2007.11.009" @default.
• W1996853006 hasPublicationYear "2008" @default.
• W1996853006 type Work @default.
• W1996853006 sameAs 1996853006 @default.
• W1996853006 citedByCount "34" @default.
• W1996853006 countsByYear W19968530062012 @default.
• W1996853006 countsByYear W19968530062013 @default.
• W1996853006 countsByYear W19968530062014 @default.
• W1996853006 countsByYear W19968530062015 @default.
• W1996853006 countsByYear W19968530062016 @default.
• W1996853006 countsByYear W19968530062017 @default.
• W1996853006 countsByYear W19968530062018 @default.
• W1996853006 countsByYear W19968530062019 @default.
• W1996853006 countsByYear W19968530062020 @default.
• W1996853006 countsByYear W19968530062021 @default.
• W1996853006 countsByYear W19968530062022 @default.
• W1996853006 countsByYear W19968530062023 @default.
• W1996853006 crossrefType "journal-article" @default.
• W1996853006 hasAuthorship W1996853006A5051315067 @default.
• W1996853006 hasAuthorship W1996853006A5083948425 @default.
• W1996853006 hasAuthorship W1996853006A5088420023 @default.
• W1996853006 hasConcept C100970517 @default.
• W1996853006 hasConcept C109007969 @default.
• W1996853006 hasConcept C112959462 @default.
• W1996853006 hasConcept C114793014 @default.
• W1996853006 hasConcept C11731853 @default.
• W1996853006 hasConcept C127313418 @default.
• W1996853006 hasConcept C155681218 @default.
• W1996853006 hasConcept C180093795 @default.
• W1996853006 hasConcept C185933670 @default.
• W1996853006 hasConcept C187320778 @default.
• W1996853006 hasConcept C18903297 @default.
• W1996853006 hasConcept C205649164 @default.
• W1996853006 hasConcept C2816523 @default.
• W1996853006 hasConcept C4646841 @default.
• W1996853006 hasConcept C76886044 @default.
• W1996853006 hasConcept C86803240 @default.
• W1996853006 hasConceptScore W1996853006C100970517 @default.
• W1996853006 hasConceptScore W1996853006C109007969 @default.
• W1996853006 hasConceptScore W1996853006C112959462 @default.
• W1996853006 hasConceptScore W1996853006C114793014 @default.
• W1996853006 hasConceptScore W1996853006C11731853 @default.
• W1996853006 hasConceptScore W1996853006C127313418 @default.
• W1996853006 hasConceptScore W1996853006C155681218 @default.
• W1996853006 hasConceptScore W1996853006C180093795 @default.
• W1996853006 hasConceptScore W1996853006C185933670 @default.
• W1996853006 hasConceptScore W1996853006C187320778 @default.
• W1996853006 hasConceptScore W1996853006C18903297 @default.
• W1996853006 hasConceptScore W1996853006C205649164 @default.
• W1996853006 hasConceptScore W1996853006C2816523 @default.
• W1996853006 hasConceptScore W1996853006C4646841 @default.
• W1996853006 hasConceptScore W1996853006C76886044 @default.
• W1996853006 hasConceptScore W1996853006C86803240 @default.
• W1996853006 hasIssue "1-4" @default.

• next