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Paul Carling (1988)
The concept of dominant discharge applied to two gravel-bed streams in relation to channel stability thresholdsEarth Surface Processes and Landforms, 13
V. D’Agostino, M. Lenzi (1999)
Bedload transport in the instrumented catchment of the Rio Cordon: Part II: Analysis of the bedload rateCatena, 36
C. Neal (1996)
Sediment and water quality in river catchmentsScience of The Total Environment, 191
J. Warburton (1992)
Observations of Bed Load Transport and Channel Bed Changes in a Proglacial Mountain StreamArctic and alpine research, 24
P. Ashworth, R. Ferguson (1989)
Size‐selective entrainment of bed load in gravel bed streamsWater Resources Research, 25
Lechostaw Suszka (1991)
Modification of transport rate formula for steep channels, 37
(1948)
Formulas for bedload transport, paper presented at 2nd Meeting of International Association for Hydraulic Structures Research
S. Fattorelli, M. Lenzi, L. Marchi, H. Keller (1988)
An experimental station for the automatic recording of water and sediment discharge in a small alpine watershedHydrological Sciences Journal-journal Des Sciences Hydrologiques, 33
D. Rickenmann, V. D’Agostino, G. Fontana, M. Lenzi, L. Marchi (1998)
New results from sediment transport measurements in two Alpine torrentsIAHS-AISH publication, 248
Gionata Asti (1998)
La valutazione del trasporto solido nel bacino sperimentale del Rio Cordon
W. Jackson, R. Beschta (1982)
A model of two-phase bedload transport in an oregon coast range streamEarth Surface Processes and Landforms, 7
(2002)
La sistemazione dei bacini idrografici, McGraw-Hill, New York
(1991)
Sediment transport in headwater channels in Idaho, in Fifth Interagency Sedimentation
(1987)
Bedload discharge equations for steep mountain rivers, in Sediment Transport in GravelBed Rivers, edited by C
N. Aziz (1986)
Sediment transport on steep slopes
M. Lenzi, L. Marchi (2000)
Suspended sediment load during floods in a small stream of the Dolomites (northeastern Italy)Catena, 39
Parker Parker, Klingeman Klingeman, McLean McLean (1982)
Bedload size and distribution in paved gravel‐bed streamJ. Hydraul. Div. Am. Soc. Civ. Eng., 108
Lenzi Lenzi, D'Agostino D'Agostino, Billi Billi (1999)
Bedload transport in the instrumented catchment of the Rio Cordon: Part I. Analysis of bedload records, conditions and threshold of bedload entrainmentCatena, 36
D. Rickenmann (1997)
Sediment transport in Swiss torrentsEarth Surface Processes and Landforms, 22
(1990)
Bedload transport load capacity of slurry flows at steeps slopes,Mitt
Lenzi Lenzi, Mao Mao, Comiti Comiti (2003)
Interannual variation of sediment yield in an alpine catchmentHydrol. Sci. J., 48
T. Tsujimoto (1991)
Bed-load transport in steep channels, 37
M. Lenzi (2001)
Step–pool evolution in the Rio Cordon, northeastern ItalyEarth Surface Processes and Landforms, 26
P. Ergenzinger, K. Schmidt (1994)
Dynamics and Geomorphology of Mountain Rivers
E. Andrews (1984)
Bed-material entrainment and hydraulic geometry of gravel-bed rivers in ColoradoGeological Society of America Bulletin, 95
D. Rickenmann (2001)
Comparison of bed load transport in torrents and gravel bed streamsWater Resources Research, 37
D. Montgomery, J. Buffington (1997)
Channel-reach morphology in mountain drainage basinsGeological Society of America Bulletin, 109
M. Lenzi (2004)
Displacement and transport of marked pebbles, cobbles and boulders during floods in a steep mountain streamHydrological Processes, 18
M. Lenzi, V. D’Agostino, P. Billi (1999)
Bedload transport in the instrumented catchment of the Rio CordonCatena, 36
D. Knighton (1998)
Fluvial Forms and Processes: A New Perspective
M. Lenzi, L. Mao, F. Comiti (2003)
Interannual variation of suspended sediment load and sediment yield in an alpine catchmentHydrological Sciences Journal, 48
G. Fontana, L. Marchi (1998)
GIS indicators for sediment sources study in Alpine basinsIAHS-AISH publication
V. D’Agostino, M. Lenzi, L. Marchi (1994)
Sediment transport and water discharge during high flows in an instrumented watershed, 52
G. Fontana, L. Marchi (2003)
Slope–area relationships and sediment dynamics in two alpine streamsHydrological Processes, 17
P. Wilcock, B. McArdell (1993)
Surface-based Fractional Transport Rates: Mobilization Thresholds and Partial Transport of a Sand-gravel SedimentWater Resources Research, 29
D. Rickenmann (1994)
Bedload transport and discharge in the Erlenbach stream, 52
(1994)
Hydraulic variables and bedload transport in East St. Louis Creek, Rocky Mountains, Colorado, M.S. thesis, Colo
G. Parker, P. Klingeman, D. McLean (1983)
Bedload and Size Distribution in Paved Gravel-Bed StreamsJournal of Hydraulic Engineering, 108
P. Billi, V. D’Agostino, M. Lenzi, L. Marchi (1998)
Bedload, slope and channel processes in a high-altitude alpine torrent, 4
T. Lisle (1995)
Particle Size Variations Between Bed Load and Bed Material in Natural Gravel Bed ChannelsWater Resources Research, 31
S. Ryan, L. Porth, C. Troendle (2002)
Defining phases of bedload transport using piecewise regressionEarth Surface Processes and Landforms, 27
(1992)
A theoretical model for calculating marginal bedload transport rates of gravel
G. Smart (1984)
Sediment Transport Formula for Steep ChannelsJournal of Hydraulic Engineering, 110
The purpose of this study is to investigate the connection between bed load, channel processes, and sediment sources in mountain basins using data from the Rio Cordon basin (northeastern Italian Alps). The main channel is a steep, boulder bed, step pool stream, and bed load volumes are measured at a special facility where particles >20 mm are trapped. Results from a combined frequency analysis of peak water discharges and total bed load volumes based on 17 years of field data are presented, focusing on discrepancies between recurrence intervals of peak discharge and bed load volume for each event. A cause of major disturbance is a high‐magnitude, low‐recurrence event that occurred in 1994. Dimensional and nondimensional bed load intensity‐duration curves are also reported, which emphasize differences between short‐ and long‐duration events. The relationship flow–bed load rates (investigated using a total of 180 data) shows no breakpoints, and two different curves are evident, representing pre‐1994 and post‐1994 floods, respectively. The analysis demonstrates both the control exerted by sediment availability on bed load transport rates and the persisting long‐term impact of major floods on mountain streams.
Water Resources Research – Wiley
Published: Jul 1, 2004
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