The hysteresis effect of sediment transport systems

Bogen, Jim

doi:10.1080/00291958008545338

Cited by 87 publications

(66 citation statements)

References 5 publications

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“…There are no direct correlations between discharge and distribution parameters, and no single parameter definitely represents the grain-size distributions better than any other parameters. However, based on the results of Rainwater and Guy (1961) and Bogen (1980), there is the possibility that the influence of discharge will stand out more clearly at a sampling site farther down-stream, as the importance of the glacier-bed conditions diminishes.…”

Section: Discussionmentioning

confidence: 99%

“…Less consideration has been given to grain-size distributions of sediments transported or settled in glacial meltwater streams (Rainwater and Guy, 1961;Ziegler, 1974;Bogen, 1979Bogen, , 1980Fenn and Gomez, 1989), whereas several investigations of this subject have been carried out in non-glaciated areas (Folk and Ward, 1957;Bagnold, 1968;Visher, 1969;Sengupta, 1975;Middleton, 1976;Walling and Moorehead, 1987) .…”

Section: Introductionmentioning

confidence: 99%

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Variations in grain-size distribution of suspended sediment in a glacial meltwater stream, Austre Okstindbreen, Norway

Karlsen

1991

J. Glaciol.

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ABSTRACT. Thirty-nine samples of suspended sediment from the meltwater stream of Austre Okstindbreen, Norway, were analysed using both moments and parameters of the hyperbolic distribution. The samples turned out to be non-normally distributed. No direct correla tion was found between discharge and grain-size distribution, but it is supposed that the hydraulic influence is hidden behind factors like composition of morainic or stream-bed materia!' Through comparison of the grain-size parameters from two periods in the field season, it was possible to distinguish between two sediment populations.

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Section: Discussionmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

Variations in grain-size distribution of suspended sediment in a glacial meltwater stream, Austre Okstindbreen, Norway

Karlsen

1991

J. Glaciol.

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“…The rapid response of SSC to hydrological forcing implies that the SS sources are readily accessible with the majority of SS being generated from areas proximal to the channel (Bača, 2008;Lefrançois et al, 2007;Rodríguez-Blanco et al, 2010). These sediment sources include: bed material (Arnborg et al, 1967;Bogen, 1980), bank material (Langlois et al, 2005;Seeger et al, 2004;Smith and Dragovich, 2009) and hydrologically connected areas close to the channel which respond rapidly at the onset of a storm (Mano et al, 2009;Reid et al, 2007). Factor analysis has illustrated that these event dynamics have no threshold of initiation and may occur across the full range of environmental conditions observed.…”

Section: Suspended Sediment Transfer In Response To Temporal and Spatmentioning

confidence: 99%

Dominant mechanisms for the delivery of fine sediment and phosphorus to fluvial networks draining grassland dominated headwater catchments

Perks

Owen

Benskin

et al. 2015

Science of The Total Environment

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. (2015) 'Dominant mechanisms for the delivery of ne sediment and phosphorus to uvial networks draining grassland dominated headwater catchments.', Science of the total environment., 523 . pp. 178-190. Further information on publisher's website: Use policyThe full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that:• a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders.Please consult the full DRO policy for further details.

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“…; Østrem, 1975;Bogen, 1980). Clockwise hysteresis appears when peak SSC occurs before peak water discharge.…”

Section: Ssc and Ssymentioning

confidence: 99%

Seasonal hydrological and suspended sediment transport dynamics in proglacial streams, James Ross Island, Antarctica

Kavan

Ondruch

Nývlt

et al. 2016

Geografiska Annaler: Series A, Physical Geography

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Rapid warming of the Antarctic Peninsula is producing accelerated glacier mass loss and can be expected to have significant impacts on meltwater runoff regimes and proglacial fluvial activity. This study presents analysis of the hydrology and suspended sediment dynamics of two proglacial streams on James Ross Island, Antarctic Peninsula. Mean water discharge during 8/1/2015 to 18/2/2015 reached 0.19 m 3 s -1 and 0.06 m 3 s -1 for Bohemian Stream and Algal Stream, respectively, equivalent to specific runoff of 76 mm month -1 and 60 mm month -1 . The daily discharge regime strongly correlated with air and ground temperatures. The effect of global radiation on proglacial water discharge was found low to negligible. Suspended sediment concentrations of Bohemian Stream were very high (up to 2927 mg L -1 ) due to aeolian supply and due to the high erodibility of local rocks. Total sediment yield (186 t km -2 yr -1 ) was high for (nearly) deglaciated catchments, but relatively low in comparison with streams draining more glaciated alpine and arctic catchments. The sediment provenance was mostly local Cretaceous marine and aeolian sediments; volcanic rocks are not an important source for suspended load. High Rb/Sr ratios for some samples suggested chemical weathering. Overall, this monitoring of proglacial hydrological and suspended sediment dynamics contributes to the dearth of such data from Antarctic environments and offers an insight to the nature of the proglacial fluvial activity, which is likely to be in a transient state with ongoing climate change.

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The hysteresis effect of sediment transport systems

Cited by 87 publications

References 5 publications

Variations in grain-size distribution of suspended sediment in a glacial meltwater stream, Austre Okstindbreen, Norway

Variations in grain-size distribution of suspended sediment in a glacial meltwater stream, Austre Okstindbreen, Norway

Dominant mechanisms for the delivery of fine sediment and phosphorus to fluvial networks draining grassland dominated headwater catchments

Seasonal hydrological and suspended sediment transport dynamics in proglacial streams, James Ross Island, Antarctica

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