2020
DOI: 10.3390/pr8070809
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Prediction of Particle-Collection Efficiency for Vacuum-Blowing Cleaning System Based on Operational Conditions

Abstract: The dust-collection system, as the core of a sweeper vehicle, directly inhales dust particles on the pavement. The influence of variable operational conditions on particle-separation performance was investigated using computational fluid dynamics (CFD) Euler–Lagrange multiphase model. The particle-separation performance efficiency and retention time were used to evaluate the dust-collection efficiency. The uniform design (UD) and multiple regression analysis (MRA) methods were employed to predict and o… Show more

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Cited by 9 publications
(17 citation statements)
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“…Where u * is the friction velocity, y is the distance to the nearest wall, and v is the local kinematic viscosity. We find that the grid y+ of the boundary layer is 3 in our published paper [23]. It is suitable for the simulated calculation of vacuum-blowing cleaning system.…”
Section: Grid Discretization and Fundamental Assumptionmentioning
confidence: 85%
See 3 more Smart Citations
“…Where u * is the friction velocity, y is the distance to the nearest wall, and v is the local kinematic viscosity. We find that the grid y+ of the boundary layer is 3 in our published paper [23]. It is suitable for the simulated calculation of vacuum-blowing cleaning system.…”
Section: Grid Discretization and Fundamental Assumptionmentioning
confidence: 85%
“…Under the action of the applied blowing force, the negative pressure generated by Suction-inlet can suck the particles up easily with lower pressure. In our previous published papers, we have clarified the mechanism of the reverse blowing flow rate that acted on the Blowing-inlet, and we also calculated the optimized results [23]. So the Blowing-inlet helps enhance the cleaning efficiency and reduces the consumption of energy for centrifugal fan.…”
Section: Physical Model and Computation Domainmentioning
confidence: 99%
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“…For every 1000 m increment in altitude, the atmospheric pressure drops by about 10 kPa, and the air density also gradually decreases. When the altitude is 5000 m, the air density is 0.7263 kg/m 3 , which is only about half of that in the plain area [1,2]. However, from the sea level to the elevation below 85,000 m, the volume ratio of the main gases such as nitrogen and oxygen is basically the same at each altitude.…”
Section: Introductionmentioning
confidence: 94%