FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W94401125> ?p ?o ?g. }

• W94401125 endingPage "102" @default.
• W94401125 startingPage "87" @default.
• W94401125 abstract "The threshold of bedload motion is important for predictions of sediment transport rates, channel migration and stability, and for river restoration and structure design. For a given grain size, the dimensionless critical shear stress can vary significantly between rivers. Estimates of the reach-averaged critical shear stress are typically from competence, reference transport rate, or visual measurements. Each of these three methods includes inherent bias, which complicate comparisons between methods and the use of one reference critical Shields stress. Furthermore, the grain-size distribution influences the relative mobility of a given particle through hiding effects, which enhance the exposure and relative motion of coarse grains and reduce the mobility of finer sediment. Sediment motion is fundamentally controlled by the balance of forces acting on a grain and is partially influenced by the local particle arrangement (e.g., particle protrusion and friction angle). Turbulence fluctuations drive sediment motion and are generally approximated using distribution functions in stochastic predictions of particle motion. However, the exact turbulence parameters responsible for motion are still relatively uncertain. Despite the variability in sediment motion between streams, finer sediment is generally easier to move than coarser particles because of the effects of grain weight. Such selective transport of fine sediment is partially responsible for the formation of armor layers in many streams. Armor layers also largely result from a low upstream sediment supply relative to the transport capacity of the flow." @default.
• W94401125 created "2016-06-24" @default.
• W94401125 creator A5005755370 @default.
• W94401125 creator A5040995233 @default.
• W94401125 date "2013-01-01" @default.
• W94401125 modified "2023-09-26" @default.
• W94401125 title "9.7 The Initiation of Sediment Motion and Formation of Armor Layers" @default.
• W94401125 cites W1493840608 @default.
• W94401125 cites W1499996122 @default.
• W94401125 cites W1501149413 @default.
• W94401125 cites W1512388559 @default.
• W94401125 cites W1513807038 @default.
• W94401125 cites W1540308477 @default.
• W94401125 cites W1545435111 @default.
• W94401125 cites W1574283409 @default.
• W94401125 cites W1575923677 @default.
• W94401125 cites W1577858001 @default.
• W94401125 cites W1582110812 @default.
• W94401125 cites W1587551732 @default.
• W94401125 cites W1631784209 @default.
• W94401125 cites W1654418050 @default.
• W94401125 cites W1668837699 @default.
• W94401125 cites W1725729894 @default.
• W94401125 cites W1748317622 @default.
• W94401125 cites W1846289495 @default.
• W94401125 cites W1924166902 @default.
• W94401125 cites W1969076473 @default.
• W94401125 cites W1969154956 @default.
• W94401125 cites W1971362045 @default.
• W94401125 cites W1971959116 @default.
• W94401125 cites W1975527068 @default.
• W94401125 cites W1979756022 @default.
• W94401125 cites W1981553165 @default.
• W94401125 cites W1981769764 @default.
• W94401125 cites W1981841918 @default.
• W94401125 cites W1983792850 @default.
• W94401125 cites W1985121885 @default.
• W94401125 cites W1985333565 @default.
• W94401125 cites W1985552270 @default.
• W94401125 cites W1986615142 @default.
• W94401125 cites W1987221452 @default.
• W94401125 cites W1988519738 @default.
• W94401125 cites W1990628338 @default.
• W94401125 cites W1991105812 @default.
• W94401125 cites W1991466525 @default.
• W94401125 cites W1991802427 @default.
• W94401125 cites W1993795808 @default.
• W94401125 cites W1995151669 @default.
• W94401125 cites W1996533558 @default.
• W94401125 cites W2000052304 @default.
• W94401125 cites W2001080835 @default.
• W94401125 cites W2001648515 @default.
• W94401125 cites W2003859782 @default.
• W94401125 cites W2004122326 @default.
• W94401125 cites W2004588747 @default.
• W94401125 cites W2006249852 @default.
• W94401125 cites W2006376525 @default.
• W94401125 cites W2007823307 @default.
• W94401125 cites W2011416258 @default.
• W94401125 cites W2011954022 @default.
• W94401125 cites W2014025394 @default.
• W94401125 cites W2014798051 @default.
• W94401125 cites W2017749765 @default.
• W94401125 cites W2021299669 @default.
• W94401125 cites W2021775598 @default.
• W94401125 cites W2026134530 @default.
• W94401125 cites W2027555715 @default.
• W94401125 cites W2030978440 @default.
• W94401125 cites W2034634640 @default.
• W94401125 cites W2035241555 @default.
• W94401125 cites W2035268147 @default.
• W94401125 cites W2038241945 @default.
• W94401125 cites W2038663547 @default.
• W94401125 cites W2038767604 @default.
• W94401125 cites W2039557087 @default.
• W94401125 cites W2041549905 @default.
• W94401125 cites W2042055062 @default.
• W94401125 cites W2043528418 @default.
• W94401125 cites W2044273623 @default.
• W94401125 cites W2046365734 @default.
• W94401125 cites W2049635304 @default.
• W94401125 cites W2053099875 @default.
• W94401125 cites W2053782510 @default.
• W94401125 cites W2054142290 @default.
• W94401125 cites W2056840918 @default.
• W94401125 cites W2057911414 @default.
• W94401125 cites W2060019039 @default.
• W94401125 cites W2060973136 @default.
• W94401125 cites W2061491824 @default.
• W94401125 cites W2063690733 @default.
• W94401125 cites W2065171814 @default.
• W94401125 cites W2065720540 @default.
• W94401125 cites W2066645607 @default.
• W94401125 cites W2067318158 @default.
• W94401125 cites W2067721410 @default.
• W94401125 cites W2068216535 @default.
• W94401125 cites W2070359372 @default.
• W94401125 cites W2071673407 @default.

• next