logging in or signing up Sedimentation Noormahl Download Post to : URL : Related Presentations : Share Add to Flag Embed Email Send to Blogs and Networks Add to Channel Uploaded from authorPOINTLite Insert YouTube videos in PowerPont slides with aS Desktop Copy embed code: Embed: Flash iPad Dynamic Copy Does not support media & animations Automatically changes to Flash or non-Flash embed WordPress Embed Customize Embed URL: Copy Thumbnail: Copy The presentation is successfully added In Your Favorites. Views: 2714 Category: Entertainment License: All Rights Reserved Like it (1) Dislike it (1) Added: November 09, 2007 This Presentation is Public Favorites: 2 Presentation Description No description available. Comments Posting comment... By: kkpank (37 month(s) ago) hello gandu Saving..... Post Reply Close Saving..... Edit Comment Close By: negho123 (37 month(s) ago) Dear sir : could you send the complete ppt to firstname.lastname@example.org Saving..... Post Reply Close Saving..... 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Particles in water and wastewater that will settle by gravity within a reasonable period of time can be removed by "sedimentation" in sedimentation basins (also known as "clarifiers"). Slide3: “Settleable” doesn’t necessarily mean that these particles will settle easily by gravity. In many cases they must be coaxed out of suspension or “solution” by the addition of chemicals or increased gravity (centrifugation or filtration). Because of the high volumetric flow rates associated with water and wastewater treatment systems, gravity sedimentation is the only practical, economical method to remove these solids. i.e., processes such as centrifugation are not economical, in most cases. Slide4: Gravity separation can obviously be applied only to those particles which have density greater than water. But this density must be significantly greater than that of water due to particle surface effects and turbulence in the sedimentation tanks. Goals of gravity sedimentation: 1) Produce a clarified (free of suspended solids) effluent. 2) Produce a highly concentrated solid sludge stream. Slide5: Review of Type I and I sedimentation Type I (Discrete sedimentation): Occurs in dilute suspensions, particles which have very little interaction with each other as they settle. Particles settle according to Stokes law Design parameter is surface overflow rate (Q/As) Slide6: Type II (flocculent sedimentation) Particles flocculate as they settle Floc particle velocity increase with time Design parameters: Surface overflow rate Depth of tank or, 3. Hydraulic retention time Slide7: Comparison of Type I and II sedimentationSlide8: Zone Settling &Compression (Type III and IV) Zone settling occurs when a flocculent suspensions with high initial concentration (on the order of 500 mg/L) settles by gravity. Flocculant forces between particles causes settling as a matrix (particles remain in a fixed position relative to each other as they settle). When matrix sedimentation is constrained from the bottom the matrix begins to compress. Such a situation occurs when the matrix encounters the bottom of tank in which it is settling. This is called compression (Type IV) settling. Slide9: These settling types are demonstrated in a batch settling test as illustrated below: Slide11: The height of the interface (between the clarified zone and the zone settling zone) versus time is plotted in the figure below to determine the "zone settling velocity" (ZSV). Velocity of this interface is steady after some induction period but changes with time as compression begins. The slope of the steady interface subsidence rate represents zone settling velocity. Slide13: Initial suspended solids concentration has a significant effect on the ZSV because the higher the suspended solids concentration the more difficult it is to pass water through the pore spaces in the settling matrix. (The only way a matrix can settle is if the water below it is allowed to pass upward through the matrix). A typical relationship between initial suspended solids and ZSV is shown here. Slide15: Factors affecting zone settling velocity: Suspended solids concentration Depth of settling column (or tank) Stirring ( 0.5 – 2 rpm to prevent “arching”) Temperature Polymer addition ( affects matrix structure) Slide16: Design of Zone Settling Tanks Two important functions of these sedimentation tanks are : clarification and thickening. For a continuous flow clarifier, operated at steady-state, mass flow of suspended solids can schematically represented as follows:Slide18: X = influent suspended solids concentration Xe = effluent suspended solids concnetration (often close to zero) Xu = underflow (thickened) suspended solids concentration. Q = influent volumetric flow rate Qu = underflow volumetric flow rate Slide19: Batch Flux Method The batch flux method is one way to analyze and select design parameters for the clarifiers/thickeners. Start by considering the mass flux of solids through the clarifier/thickener. There are two components of this flux: Subsidence (sedimentation) Bulk transport (due to sludge withdrawal from bottom of tank)Slide20: Total flux of solids through the clarifier is given by: Where: G = mass flux (mass of SS transported/area-time) Vi = zone settling velocity (ZSV) at Xi u = bulk transport velocity due to sludge withdrawal from bottom of the tank.Slide21: u = Qu/As Qu = underflow rate (withdrawal rate) As = cross-sectional area of clarifier Slide22: Zone settling velocity is highly dependent on Xi, so to calculate the flux due to subsidence we need to assume a typical relationship between zone settling velocity and Xi to get:Slide23: Solid flux due to subsidence (settling) is calculated by: Gs = (vi)(xi) (mass/time-area)Slide24: Flux due to bulk transport is given by: Gb = (u)(Xi) Slide25: For a particular u the combined flux looks like:Slide26: For a particular underflow rate u there is a minimum in the flux capacity of the clarifier. This minimum occurs at Xi = XL. (Note there is also a minimum G at the origin, but this has no relevance since even after the influent X is diluted Xi never gets this low). Therefore for a given underflow rate there is a "limiting flux" which can be transmitted through the clarifier. As Xi passes from Xf (suspended solids concentration in the influent ) to Xu it must pass through this bottleneck Xi = XL. This controls the solids loading rate to the clarifier. Slide27: Essentially for a critically loaded clarifier there exists only two suspended solid concentrations, XL and XA if the compression zone is ignored. An explanation of "two concentration" critically loaded clarifier follows. Suspended solids enter the clarifier at some initial concentration Xf. These solids are diluted by clarified effluent. As the solids settle they concentrate and ultimately reach XL. Slide28: Suspended solids cannot be transmitted as fast through this layer as in the layers above (because the influent has lower suspended solids concentration and therefore higher zone settling velocity) so there is a build up of suspended solids at XL. Slide29: At steady state the influent suspended solids have to be diluted to XA to balance fluxes through the clarifier(at steady-state all the solids fluxes must be equal at all depths). Any other concentrations will cause the layers to disappear, either by washing out over the effluent or by being drawn through the bottom of the clarifierSlide31: When the clarifier is critically loaded. i.e., when the loading rate equals the flux capacity of the clarifier, the resultant concentration profile in the clarifier is given by :Slide33: The batch settling data can be represented by an exponential function.For example the following equation is an exponential curve fit to the settling data shown in the following graph. Slide35: Flux due to subsidence can then be calculated: Be sure to make units consistent. Typical units = kg/m2-hrSlide39: The limiting flux in for each underflow rate, u, is found by locating the minimum in the total flux curve. Note that minimum of interest occurs to the right of the curve peak for reasons discussed earlier. This minimum can be found graphically or by differentiating the flux curve with respect to X and setting the resulting equation equal to zero and then solve for XL.Slide41: For this particular problem: u (m/hr) XL (mg/liter) 8 11,020 10 10,338 12 9,655Slide42: This means that if we choose to operate a clarifier with an underflow rate of 8 m/hr (Qu/As) then the flux limiting concentration will be at 11,020 mg/L. In other words the subsidence flux will be: Slide43: And the bulk transport flux will be:Slide44: The total capacity of the clarifier to transmit solids under these conditions is: Slide45: This same information can be obtained graphically. In fact once the subsidence flux curve is drawn a straight line at slope u drawn tangent to the subsidence curve will give all the required information. One important point is that the tangent line must remain below the subsidence curve otherwise the flux limiting capacity will be exceeded and the clarifier will fail. Slide46: (.0075) = Gs 11,020 (0.032) = Gt (14.41) Slope = 8m/hr GSlide47: How is this information used to design a clarifier? The major design parameters for a clarifier-thickener are the cross-sectional area, As, and the volumetric underflow rate Qu. These parameters must be selected so that the solids loading capacity of the clarifier-thickener is not exceeded and the solids concentration of the underflow is adequate. These parameters can be selected by the following procedure. Slide48: Consider mass flow through a clarifier:Slide49: Perform a solids mass balance around the clarifier: Typically Xe is approximately zero so the last term can be ignored.Slide50: The clarifier cross-sectional area and underflow rate must be selected to satisfy mass balances and flux capacity limitations. Start with:Slide51: Consider the previous case. Assume: Qf = 103 m3/day and Xf = 6500 mg/L We selected an underflow rate = 8 m3/hr. This yielded an Xu = 14,410 mg/L. Then Qu = Lf/Xu= 18.8 m3/hr. This determines As = Qu/u = 2.355 m2Slide52: The way in which the problem was set up the clarifier is critically loaded. However, clarifiers do not need to be loaded critically to function. For example, the cross sectional area can be doubled to yield an underflow velocity of 4 m/hr. A mass balance dictates: If Xu is held constant u will be half of the previous value so Gtotal will be halved. Slide53: Assuming Lf (Qf * Xf) is constant then lowering Gtotal by ½ is exactly compensated by doubling As. This analysis can be extended to any combination of changes in Xu, u, Qu, etc. as long as the mass balance is met and as long as the line connecting Gtotal and Xu remains below the subsidence flux curve. In the following graph black lines are acceptable operating conditions whereas blue lines are unacceptable conditions.Slide55: There are an infinite number of “non-critically loaded” conditions a few of which are shown in the following graph. All variations in Xu or u or Gtotal are allowed as long as mass balances are satisfied. Slide57: Critically loaded design can be accomplished graphically using the “Batch Flux: technique. Construct a batch flux curve for subsidence alone. (GS = viXi).Slide58: Select an Xu . Draw a line tangent to the subsidence batch curve which originates at G = 0, X = Xu. Extend this line to the ordinate. The ordinate intercept is Gtotal. The G value at the point of tangency is Gs. Slide59: The slope of the tangent line is the negative of the underflow rate u. Slide60: Gtotal GsSlide61: Justification for this procedure can be shown from geometry or the Kynch analysis. First use the Kynch analysis. Consider two layers (at different concentrations and, therefore, different settling rates) of zone settling solids. These layers are shown schematically here. Slide63: X1<X2 and, therefore, V1 >V2 The interface between the layers will move upward with a velocity of U. A mass balance about the interface gives: X1V1 +X1U = X2V2 + X2U (assuming no accumulation in the interface). Slide64: Let G1 = V1X1 and G2 = V2X2 Then: G1 - G2 = - DG = U(X2-X1) = U(DX) or Slide65: If the system is critically loaded (the downward bulk transport is equal to the upward U (propagation of solids upward ) so that the solids flux is maintained at steady-state in a downward mode (u = U). Or viewed another way the slope of the subsidence curve at any point gives the underflow rate (u) necessary to maintain a critically loaded system at a selected Xu . Slide66: Recall that GL = the limit of solids loading which can be transmitted per unit area at a given underflow rate and sludge settleability. Then: Slide70: Tube Settlers: One method to increase the efficiency or increase the capacity of clarifiers is to install "false bottoms" in the clarifiers. For example in a rectangular clarifier such a "false bottom" would look like: Slide72: Using Type I settling analysis, the effect of providing a single false bottom (of equal area of the original bottom) is to effectively reduce the critical velocity, Vc , by half if the false bottom is located at mid-depth. It will be assumed that particle settling velocity is vertical (in direction perpendicular to the original bottom of the clarifier) therefore the distance a particle need to fall to be removed is increased by 1/cosq. Where q is angle of incline. Slide73: If the false bottoms are replaced by a series of inclined tubes turbulence is minimized (particularly lateral turbulence) and the physical integrity of the false bottoms is increased compared to long flat sheets. Hence the term "tube settlers". Tube settlers are often used in retrofit situations. You do not have the permission to view this presentation. In order to view it, please contact the author of the presentation.