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Abstrakty
Sediment supply governs the bedload transport and bed morphology in rivers. Up to the present, the impacts of magnitude and texture of variable sediment supply (e.g., induced by flash flood from tributaries) on bedload transport are unknown, limiting the capacity of flood control and river management significantly. The present study conducted flume experiments to investigate the responses of bedload transport to variable sediment supply regimes with different peak supply rates and grain size distributions. The experimental results indicate that: the bedload rate and mass increase with increasing the peak rate of the variable sediment supply, and decrease with an increase in the proportion of coarse particles; the particles coarser than the median grain size of the supplied sediment D50 are primarily stored in the bed, while those finer than D50 are mainly transported downstream; during the variable sediment supply process, the critical Shields stress of sediment has a similar development trend to that of the bedload rate but with a slight ahead of time.
Wydawca
Czasopismo
Rocznik
Tom
Strony
593--602
Opis fizyczny
Bibliogr. 37 poz.
Twórcy
autor
- State Key Laboratory of Hydraulics and Mountain River Engineering, College of Water Resource and Hydropower, Sichuan University, Chengdu 610065, China
autor
- State Key Laboratory of Hydraulics and Mountain River Engineering, College of Water Resource and Hydropower, Sichuan University, Chengdu 610065, China
autor
- State Key Laboratory of Hydraulics and Mountain River Engineering, College of Water Resource and Hydropower, Sichuan University, Chengdu 610065, China
autor
- State Key Laboratory of Hydraulics and Mountain River Engineering, College of Water Resource and Hydropower, Sichuan University, Chengdu 610065, China
autor
- State Key Laboratory of Hydraulics and Mountain River Engineering, College of Water Resource and Hydropower, Sichuan University, Chengdu 610065, China
Bibliografia
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- 4. Curran JC, Tan L (2014) Effect of bed sand content on the turbulent flows associated with clusters on an armored gravel bed surface. J Hydraul Eng 140(2):137-148. https://doi.org/10.1061/(ASCE) HY.1943-7900.0000810
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- 6. Elgueta-Astaburuaga MA, Hassan MA (2017) Experiment on temporal variation of bed load transport in response to changes in sediment supply in streams. Water Resour Res 53(1):763-778. https://doi.org/10.1002/2016WR019460
- 7. Elgueta-Astaburuaga MA, Hassan MA (2019) Sediment storage, partial transport, and the evolution of an experimental gravel bed under changing sediment supply regimes. Geomorphology 330:1-12. https://doi.org/10.1016/j.geomorph.2018.12.018
- 8. Elgueta-Astaburuaga MA, Hassan MA, Saletti M, Clarke GKC (2018) The effect of episodic sediment supply on bedload variability and sediment mobility. Water Resour Res 54(9):6319-6335. https://doi.org/10.1029/2017WR022280
- 9. Ferrer-Boix C, Hassan MA (2014) Influence of the sediment supply texture on morphological adjustments in gravel-bed rivers. Water Resour Res 50(11):8868-8890. https://doi.org/10.1002/2013WR015117
- 10. Hassan MA, Saletti M, Johnson JPL, Ferrer-Boix C, Venditti JG, Church M (2020) Experimental insights into the threshold of motion in alluvial channels: Sediment supply and streambed state. J Geophys Res Earth Surf 125(12):e2020JF005736. https://doi.org/10.1029/2020JF005736
- 11. Hauer FR, Locke H, Dreitz VJ, Hebblewhite M, Lowe WH, Muhlfeld CC, Nelson CR, Proctor MF, Rood SB (2016) Gravel-bed river floodplains are the ecological nexus of glaciated mountain landscapes. Sci Adv 2(6):e1600026. https://doi.org/10.1126/sciadv. 1600026
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- 14. Johnson JPL (2016) Gravel threshold of motion: a state function of sediment transport disequilibrium? Earth Surf Dyn 4(3):685-703. https://doi.org/10.5194/esurf-4-685-2016
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- 18. Luzi D, Hassan MA, Papangelakis E, Eaton B (2021) Cycles of aggradation and degradation in gravel-bed rivers mediated by sediment storage and morphologic evolution. Geomorphology 395:108001. https://doi.org/10.1016/j.geomorph.2021.108001
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- 21. Muller T, Hassan MA (2018) Fluvial response to changes in the magnitude and frequency of sediment supply in a 1-D model. Earth Surf Dyn 6(4):1041-1057. https://doi.org/10.5194/esurf-6-1041-2018
- 22. Pasternack GB, Wang CL, Merz JE (2004) Application of a 2D hydrodynamic model to design of reach-scale spawning gravel replenishment on the Mokelumne River. Calif River Res Appl 20(2):205-225. https://doi.org/10.1002/rra.748
- 23. Podolak CJP, Wilcock PR (2013) Experimental study of the response of a gravel streambed to increased sediment supply. Earth Surf Proc Land 38(14):1748-1764. https://doi.org/10.1002/esp.3468
- 24. Rickenmann D (2018) Variability of bed load transport during six summers of continuous measurements in two Austrian mountain streams (Fischbach and Ruetz). Water Resour Res 54(1):107-131. https://doi.org/10.1002/2017WR021376
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- 28. Venditti JG, Dietrich WE, Nelson PA, Wydzga MA, Fadde J, Sklar L (2010a) Effect of sediment pulse grain size on sediment transport rates and bed mobility in gravel bed rivers. J Geophys Res Earth Surf 115:F03039. https://doi.org/10.1029/2009JF001418
- 29. Venditti JG, Dietrich WE, Nelson PA, Wydzga MA, Fadde J, Sklar L (2010b) Mobilization of coarse surface layers in gravel-bedded rivers by finer gravel bed load. Water Resour Res 46:W07506. https://doi.org/10.1029/2009WR008329
- 30. Wang J, Hassan MA, Saletti M, Chen X, Fu X, Zhou H, Yang X (2021) On how episodic sediment supply influences the evolution of channel morphology, bedload transport and channel stability in an experimental step-pool channel. Water Resour Res 57(7):e2020WR029133. https://doi.org/10.1029/2020WR029133
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- 33. Wilcock PR, Kenworthy ST, Crowe JC (2001) Experimental study of the transport of mixed sand and gravel. Water Resour Res 37(12):3349-3358. https://doi.org/10.1029/2001WR000683
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- 35. Wong M, Parker G (2006) Reanalysis and correction of bed-load relation of Meyer-Peter and Muller using their own database. J Hydraul Eng 132(11):1159-1168. https://doi.org/10.1061/(ASCE) 0733-9429(2006)132:11(1159)
- 36. Xiong J, Tang C, Chen M, Gong L, Li N, Zhang X, Shi Q (2021) Longterm changes in the landslide sediment supply capacity for debris flow occurrence in Wenchuan County. China Catena 203:105340. https://doi.org/10.1016/j.catena.2021.105340
- 37. Zheng X, Chen R, Luo M, Kazemi E, Liu X (2019) Dynamic hydraulic jump and retrograde sedimentation in an open channel induced by sediment supply: experimental study and SPH simulation. J Mt Sci 16(8):1913-1927. https://doi.org/10.1007/s11629-019-5397-8
Uwagi
Opracowanie rekordu ze środków MNiSW, umowa nr POPUL/SP/0154/2024/02 w ramach programu "Społeczna odpowiedzialność nauki II" - moduł: Popularyzacja nauki (2025).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-557b4e4e-b720-486d-a4f7-a62a64f6429d
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