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A Semi-Empirical Model to Estimate Maximum Floc Size in a Turbulent Flow
The basic model for agglomerate breakage under the effect of hydrodynamic stress (d(max) = C.G(−)(γ)) is only applicable for low velocity gradients (<500 s(−1)) and is often used for shear rates that are not representative of the global phenomenon. This paper presents a semi-empirical model that...
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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MDPI
2022
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9457576/ https://www.ncbi.nlm.nih.gov/pubmed/36080316 http://dx.doi.org/10.3390/molecules27175550 |