1999
DOI: 10.1002/(sici)1099-1085(19990415)13:5<763::aid-hyp779>3.0.co;2-c
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An analytical model for stream sediment transport: application to Murray and Murrumbidgee river reaches, Australia
Abstract: Abstract:The mechanisms controlling the¯ow of sediment in streams can be very complex and dicult to model with accuracy. Furthermore, data associated with the dominant sediment transport processes are often scarce. In this paper, we propose a model for the transport of suspended sediment in single stream reaches that permits a characterization of the dynamics of sediment sources and sinks, and routes concentrations through a stream network. We present a closed form, physically based, one-dimensional model that…
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Cited by 19 publications
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“…According to the model results, it is observed that increased number of neurons in the 2 nd layer does not have a significant influence on regression outcomes. , and (c) ANN (3)(4) models…”
Section: Resultsmentioning
confidence: 99%
“…According to the model results, it is observed that increased number of neurons in the 2 nd layer does not have a significant influence on regression outcomes. , and (c) ANN (3)(4) models…”
Section: Resultsmentioning
confidence: 99%
“…MLR and PLS methods are the least effective techniques (r 2 pred = 0.67) for estimating sediment amount in the Göksu River. Further analysis of ANN method is applied for different configurations: ANN (3-0), ANN (3-2), and ANN (3)(4). According to r 2 pred values given in Table 2, increasing the number of neurons in the 2 nd layer does not have a significant influence on model outcomes.…”
Section: Discussionmentioning
confidence: 99%
“…We demonstrated our approach using a length-based attenuation model similar to approaches taken by Dietrich et al (1999), Ensign et al (2006), Faridmarandi and Naja (2014), and Keller et al (2014). An alternative approach would be to use a time-based attenuation model.…”
Section: Discussionmentioning
confidence: 99%
“…Important processes related to the flux of suspended sediment (e.g., sediment settling and resuspension and bedload interaction with suspended sediment, bank erosion, or deposition) may also control P transport and enrichment. Although such process interactions are complex, relatively simple conceptual mathematical models (e.g., Dietrich et al, 1999 ) can capture geochemical dynamics. In-stream geochemistry may also be important for liberating sediment bound chemicals (e.g., P 2 O 5 ) into dissolved bioavailable forms (e.g., phosphate [PO 4 ]) in the water column.…”
Section: Improvements In System Representationmentioning
confidence: 99%
