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Advances in Water Treatment and Enviromental Management

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178 WATER TREATMENTsmall suspended objects be<strong>in</strong>g able to pass the filter pore. Fig. 5 <strong>and</strong> Fig. 6 show two differenttypes of statistical deposits of 2000 solid particles performed us<strong>in</strong>g our orig<strong>in</strong>al simulationprogram. In each case, the suspension is assumed to flow from the left to the right.The first case models a filter foul<strong>in</strong>g due to a suspension flow where particle-particle <strong>and</strong> particlewalladhesion forces are much greater than hydrodynamical forces carry<strong>in</strong>g the particles away.Here a suspended particle mak<strong>in</strong>g contact with the filter surface or with a particle of the aggregateis immediately stopped <strong>and</strong> captured. Thus N r equals 0 <strong>and</strong> the given value for θ i is about 60°.The deposit structure is dendritic <strong>and</strong> the porosity has a mean value about 51 %.The second simulation presents a very compact aggregation we could observe experimentallyif, on one h<strong>and</strong>, the effect of parallel shear flow was efficient even <strong>in</strong>side the deposit <strong>in</strong> orderto reorganize particle arrangement <strong>and</strong>, on the other h<strong>and</strong>, the wall was very attractive <strong>in</strong>order to prevent aggregated particles from be<strong>in</strong>g carried <strong>in</strong>to the flow aga<strong>in</strong>. To take <strong>in</strong>toaccount the importance of tangential flow, N r is chosen equal to 3. <strong>and</strong> θ i <strong>and</strong> θ v have a verysmall value. The 2D mean porosity is then equal to 29 % <strong>and</strong> the mean thickness is obviouslylower than the one obta<strong>in</strong>ed <strong>in</strong> the first case (see Fig. 6).It now appears to be necessary to <strong>in</strong>vestigate the whole range of possible deposits by vary<strong>in</strong>gthe most important model parameters.Influence of <strong>in</strong>cidence angle αThis parameter is used to specify the relative magnitude of the parallel shear flow over theradial suction flow. Radial variations of concentration are plotted <strong>in</strong> Fig. 7 for a large range ofα. It is seen that aggregates become more <strong>and</strong> more compact from 10° to 30°, after this po<strong>in</strong>tthey keep approxikatly the same structure. This is also demonstrated by the cont<strong>in</strong>uouslydecreas<strong>in</strong>g porosity shown <strong>in</strong> Fig. 8.Fig. 7: Vertical concentration variationswith θ i =1°θ v =1º, N r =1Fig. 8: 2D mean porosityvariationsInfluence of <strong>in</strong>cident stick<strong>in</strong>g angle θ iThe importance of hydrodynamical entra<strong>in</strong>ment force over adhesion force is determ<strong>in</strong>ed bythe numerical value given to this parameter. The vertical concentration diagram shown <strong>in</strong>Fig.9 provides an adequat classification of the solid particle deposits obta<strong>in</strong>ed when vary<strong>in</strong>gθ i from 5° to 60°. Of course the small values lead to a very compact structure <strong>and</strong> the meanporosity <strong>in</strong>creases quickly if the stick<strong>in</strong>g angle <strong>in</strong>creases (see Fig. 8).Fig. 9: Vertical concentration variations with a=20°, θ v =1°, Nr=0

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