2012
DOI: 10.1061/(asce)hy.1943-7900.0000516
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SPH Simulation of Sediment Flushing Induced by a Rapid Water Flow

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Cited by 115 publications
(75 citation statements)
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“…Basically, rheology of a sludge is defined by its viscous characteristics, which can be determined by the relationship between shear rate and shear stress, obtained through a rheological measurement (which imposes either shear rate or shear stress [62][63][64] and measures alternatively these parameters). The observed relationship is strictly related to the characteristics of the sludge, such as the relative concentration of water and suspended matter due to the nature of the wastewater and to the treatment process that is subjected to [65].…”
Section: Introductionmentioning
confidence: 99%
“…Basically, rheology of a sludge is defined by its viscous characteristics, which can be determined by the relationship between shear rate and shear stress, obtained through a rheological measurement (which imposes either shear rate or shear stress [62][63][64] and measures alternatively these parameters). The observed relationship is strictly related to the characteristics of the sludge, such as the relative concentration of water and suspended matter due to the nature of the wastewater and to the treatment process that is subjected to [65].…”
Section: Introductionmentioning
confidence: 99%
“…It should be noticed that, starting from the physical meaning of the limiting viscosity, in this model, it was used as a numerical parameter to reduce the computational time, as illustrated in the following. In some SPH applications dealing with landslide run-out [17] and sediment scouring [56], a similar viscosity parameter was successfully adopted working as a numerical threshold.…”
Section: Implementation Of the Limiting Viscositymentioning
confidence: 99%
“…Shakibaeinia and Jin (2011) employed a fluid-fluid interface coupling technique in the scope of N-S equation with different material parameters instead of elasto-plastic model which many engineers on soil mechanics would prefer for landslide problems. Unilateral coupling methods, such as sediment flushing where a Mohr-Coulomb erosion criterion is used to decide the interfacial soil particle to be at rest or eroded by Manenti et al (2012) , would not work in the simulation of impulse waves. Furthermore, the approach of introducing a seepage force by Huang et al (2013) will not be suitable for the rapid change of interface and the strong interaction force, because the seepage parameter is difficult to determine.…”
Section: Soil-water Coupling Modelmentioning
confidence: 99%