2009
DOI: 10.1029/2008gl037139
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Reservoir infill by hyperpycnal deltas over bedrock

Abstract: [1] We propose a simple morphodynamic theory of reservoir deltas prograding over bedrock under the influence of turbid underflows. The theory models the geomorphic actions of fluvial and hyperpycnal flows as diffusion processes, and treats bedrock-alluvial and riverlake transitions as moving internal boundaries. It yields selfsimilar analytical solutions for the co-evolving river and lake bed profiles, under different slope and influx conditions. These include a special case in which delta deposits are swept u… Show more

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Cited by 37 publications
(38 citation statements)
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“…In some cases, these have included dynamic basin characteristics like uplift or subsidence [ Swenson et al , ; Leva López et al , ] and relative variations of the basin water level [ Swenson et al , ; Capart et al , ; Parker et al , ]. Predictions have also been successfully compared with experiments [ Kim et al , , ; Hsu and Capart , ; Parker et al , ; Lai and Capart , ; Leva López et al , ].…”
Section: Introductionsupporting
confidence: 59%
See 1 more Smart Citation
“…In some cases, these have included dynamic basin characteristics like uplift or subsidence [ Swenson et al , ; Leva López et al , ] and relative variations of the basin water level [ Swenson et al , ; Capart et al , ; Parker et al , ]. Predictions have also been successfully compared with experiments [ Kim et al , , ; Hsu and Capart , ; Parker et al , ; Lai and Capart , ; Leva López et al , ].…”
Section: Introductionsupporting
confidence: 59%
“…Here the brink, toe, and crease lines are all clearly delineated along the portion of the pool margin where sediment influx was active. Laboratory examples in various configurations are also documented in the literature [ Bromley , ; Hsu and Capart , ; Kim et al , , ; Lai and Capart , ; Leva López et al , ].…”
Section: Introductionmentioning
confidence: 99%
“…As in previous studies [ Lai and Capart , , ; Foreman et al , ], we assume the gravity flows in question are dominated by fine‐grained sediment that remains in suspension over the domain of interest. Due to the difficulties in keeping fine‐grained sediment suspended at reduced scale, we replaced the fine sediment in suspension with brine (specific gravity = 1.2) that, as a solute, does not settle on the bed.…”
Section: Methodsmentioning
confidence: 99%
“…Since we are unable to generate relief in a way that mimics these processes at laboratory scale, we instead created a simplified escarpment configuration that allowed for controlled increases in relief during the course of an experiment. And as is commonly done in reduced‐scale experimental studies on sustained sediment gravity flows, we used saline currents as a proxy for mud‐rich turbidity currents [ Métivier et al , ; Lai and Capart , , ; Weill et al , ]. By isolating two controls on slope morphology at reduced scale, we were able to explore their interaction in detail using high‐resolution topography and overhead photographic imagery.…”
Section: Introductionmentioning
confidence: 99%
“…Furthermore, to predict the elevation variation along a reservoir, Lai and Capart [17] reported on different laboratory experiments constructed to reproduce reservoir delta movements. Their research figured out the variation of reservoir delta movement.…”
Section: Introductionmentioning
confidence: 99%