2013
DOI: 10.1051/lhb/2013033
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Influence de la granulométrie des particules sur la mesure par turbidimétrie des flux de matières en suspension dans les cours d’eau

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Cited by 12 publications
(10 citation statements)
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“…One of its main advantages is that it allows values to be obtained at high frequency with portable probes. However, this procedure requires calibration to account for particle size, nature, and color of suspended sediment (Ludwig & Hanes, 1990;Butt, Miles, Ganderton, & Russell, 2002;Minella, Merten, Reichert, & Clarke, 2008; Thollet et al, 2013). For example, the assumption of a single representative diameter is not appropriate and can lead to great uncertainty in the calculation of [C].…”
Section: Determination Of Suspended Sediment Concentration Profile mentioning
confidence: 99%
“…One of its main advantages is that it allows values to be obtained at high frequency with portable probes. However, this procedure requires calibration to account for particle size, nature, and color of suspended sediment (Ludwig & Hanes, 1990;Butt, Miles, Ganderton, & Russell, 2002;Minella, Merten, Reichert, & Clarke, 2008; Thollet et al, 2013). For example, the assumption of a single representative diameter is not appropriate and can lead to great uncertainty in the calculation of [C].…”
Section: Determination Of Suspended Sediment Concentration Profile mentioning
confidence: 99%
“…The Arc River drains mountainous watersheds in the French Alps and has a watershed area of 1500 km 2 with a mean annual flow of 16 m 3 s −1 at the Pontamafrey hydrological station (Thollet et al 2013). This is an alpine basin with high discharge during spring melt and low discharge during the fall period.…”
Section: Natural River Sedimentsmentioning
confidence: 99%
“…This is an alpine basin with high discharge during spring melt and low discharge during the fall period. The discharge variability is mitigated as the hydrology is strongly affected by hydropower management (Thollet et al 2013). The Arc River sediments are characterized by a high content of small minerals derived from the erosion of a black marls geologic layer (Thollet et al 2013;Antoine 2013) with 31 % sand, 64 % silt, and 5 % clay and an organic content of 1.7 %.…”
Section: Natural River Sedimentsmentioning
confidence: 99%
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