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Solid particles characterizationSolid particles characterizationSolid particles characterizationSolid particles characterizationSolid particles characterizationSolid particles characterizationSolid particles characterizationSolid particles characterizationSolid particles characterizationSolid particles characterizationSolid particles characterizationSolid particles characterizationSolid particles characterizationSolid particles characterizationSolid particles characterizationSolid particles char
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Date: 10 September 2020 Abstract (The abstract should not exceed 250 words). The present paper displays the difference between the time of settling when it comes to measure sand. The correspondent procedure was carry out thanks to a bottle, water and sand. Initially there were some calculations assuming the sand as ideal or non-ideal case and correction its factors. After that it’s found that the minor particle would take less time that the major particle to settle then the flux of water with sand wasn’t laminar at all thus there were some modification that changes the final settling velocity to the ideal settling velocity using the ideal model. Index Terms — Sand, Settling time, hindered settling, solids particles I. INTRODUCTION TO STUDY CASE^1 Particles may be removed from the atmosphere by deposition onto floors, walls, and other surfaces. Particles settle under the influence of gravity where the settling (or terminal) velocity is broadly proportional to the square of the diameter[1]. therefore, airborne nanoparticles will fall out much more slowly than larger particles and gravitation settling will not be an effective removal process. this potentially would have the implication of causing higher, longer exposures. indeed, deposition of nanoparticles will be independent of orientation and will occur as they become trapped in the boundary layer on all surfaces, including walls, ceilings, and floors [2]. The most common modeling approach is to assume “Stokesian” particles, namely, as particles move, the flow around them is in the Stokes regime (Rep <<1, where Rep is the particle Reynolds number). In this situation the drag force is given by the well-known Stokes law for a moving sphere in a fluid [1]. In this demonstration, we let settle a set of sand particles, trying to stay inside the Stokesian/laminar regime. The idealized settling velocity will be calculated and then compared with the experimental settling velocity in order to find some features that explain the difference between both them (sphericity, porosity, flowing path, non ideal fluid properties as density-viscosity and also interactions particle-particle and fluid-particle. The objective of this paper was to determine and compare the theoretical and experimental settling velocity of sand particles in the water. For the determination of settling velocity sand. The water was taken from the tap and the sand from a decorative object. For sand capture sedimentation is usually used, principle of sedimentation is based on physical properties of the sand, especially (^1) Corresponding author: depends on density of the sand [4]. For the experimental measurement of the settling velocity of the sand a bottle is taken to make a kind of filter, then the water is poured with sand then the time is measured [5]. II.PROCEDURES FOR EXERCISE SOLUTION (IDEAL CASE, HINDERED SETTLING CORRECTIONS) A. Ideal case solution. Sand was characterized in size and shape as follows: The particles were measured, and it was obtained a diameter of 1.00 mm, then it was calculated the sphericity to make this correction, and it was obtained an average of 0.63. According with this data and using the following formulas for water properties (below) the ideal settling velocity it’s estimated. Temperature in Kelvin, viscosity (mu) expressed as Pa- s. Temperature in Celsius degrees, density (rho) as kg/m In this case the temperature was the average in Bogotá, which is 20°C (293.15 K). Finally, it is used the next equation and the it is calculated the Reynolds number to verify that the result corresponds to a laminar regime. Ut=(Ψd)2(ρp-ρ)g/18μd)2(ρp-ρ)g/18μp-ρp-ρ)g/18μ)g/18μ The value for the velocity was 0.35 m/s, however, at the time of calculating the Reynolds number it is obtained a number in the region of intermediate, in this case, the formula to obtain the velocity changes to: Ut=(3.54g0.71Dp1.14(ρp-ρ)g/18μp-ρp-ρ)g/18μ)0.71)/(ρp-ρ)g/18μf0.29μ0.43)
According with this data and using the following formulas for water properties (below) the ideal settling velocity it’s estimated. Temperature in Kelvin, viscosity (mu) expressed as Pa-s. Temperature in Celsius degrees, density (rho) as kg/m^3 B. Hindered settling demonstration. Experimentally, silica sand settling was performed as follows: To determine the sedimentation rate, a cut bottle was used to carry out the sedimentation and cylindrical sand, as can be seen in figure 1. The sand used was measured using a ruler as well as the height of the bottle used. Later it was filled the bottle with water, and the sand was delicately added to the top, after this, the elapsed time of the fall of the first and last sand particles was measured. Figure 1. Sedimentation mechanism used during practice. To determine the speed, the height of the bottle, which corresponded to 15cm, and the times collected, which corresponds to 1.61s for the first particle and 2.66s for the last particle, were considered. And the speed was determined with the equation shown below. The velocity results for the first and second particles were 9.32 cm / s and 5.64 cm / s respectively III. RESULTS & ANALYSIS First proceeded to perform the characterization of the particles in which with the help of the rule the faces were measured yielding an average value of 1mm, which corresponds to the approximate diameter of the particles. The same measures calculate sphericity, which obtained a value of 0.67 which means that the particles are not totally spherical, although they have a more spherical than angular trend. Results comparison are summarized in table 1. Symbol Type of condition Average value/units Ideal Settling Dp Particle size 1,0 mm Ψ Sphericity (^) 0, Ut Settling velocity: (^) 3,43 m/s Demonstration Ut Major Settling velocity (^) 9.32 cm / s Ut Minor settling velocity (^) 5.64 cm / s With the data obtained above, the theory settling velocity of these particles was calculated, the Reynolds number was calculated, which was approximately 300, so it cannot be considered as a laminar region, because of this it was proceeded to heat it with the formula of the transitional region since the number of Reynolds obtained is within the range of this region which is 2 to 500. This can be especially deviated so we have particles of considerable size. As can be seen in the results the theory and experimental value are completely different, this may be due to the variation in size in the particles, in the theory an approximate value is used so this diameter and the sphericity does not correspond to all particles, so there is a difference between the Settlings velocity. OTHER FACTORS THAT CAN INFLUENCE THIS VARIATION IS THE VISCOCITY AND DENSITY OF WATER AND PARTICLES SINCE SETTILING VELOCITY DEPENDS ON THEM, IT SHOULD ALSO BE CONSIDERED THAT AS THERE ARE PARTICLES WITH DIFFERENT SIZES THE DENSITY OF THESE CAN VARY.…