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Week # 1 MR Chapter 1

Tutorial #1 MR #1.1, 1.4, 1.7. To be discussed on Jan. 22 2020. By either volunteer or class list. Week # 1 MR Chapter 1. MARTIN RHODES (2008) Introduction to Particle Technology , 2nd Edition. Publisher John Wiley & Son, Chichester, West Sussex, England.

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Week # 1 MR Chapter 1

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  1. Tutorial #1 MR #1.1, 1.4, 1.7. To be discussed on Jan. 22 2020. By either volunteer or class list. Week # 1MR Chapter 1 MARTIN RHODES (2008) Introduction to Particle Technology , 2nd Edition. Publisher John Wiley & Son, Chichester, West Sussex, England.

  2. Describing the size of a single particle. Some terminolgy about diameters used in microscopy. • Equivalent circle diameter. • Martin’s diameter. • Feret’s diameter. • Shear diameter.

  3. Describing the size of a single particle • Regular-shaped particles • The orientation of the particle on the microscope slide will affect the projected image and consequently the measured equivalent sphere diameter. • Sieve measurement: Diameter of a sphere passing through the same sieve aperture. • Sedimentation measurement: Diameter of a sphere having the same sedimentation velocity under the same conditions. Comparison of equivalent sphere diameters.

  4. Comparison of equivalent diameters • The volume equivalent sphere diameter is a commonly used equivalent sphere diameter. • Example: Coulter counter size measurement. The diameter of a sphere having the same volume as the particle. • Surface-volume diameter is the diameter of a sphere having the same surface to volume ratio as the particle. (Example) Shape Cuboid Cylinder Cuboid: side lengths of 1, 3, 5. Cylinder: diameter 3 and length 1.

  5. Description of populations of particles • Typical differential frequency distribution F: Cumulative distribution, integral of the frequency distribution.

  6. Typical cumulative frequency distribution

  7. For a given population of particles, the distributions by mass, number and surface can differ dramatically. • All are smooth continuous curves. • Size measurement methods often divide the size spectrum into size ranges, and size distribution becomes a histogram. • Comparison between distributions

  8. Conversion between distributions • Mass and number distributions for man-made objects orbiting the earth

  9. Total number of particles, N and total surface area S are constant. • Particle shape is independent of size, as is constant. V is the total volume of the particle population and av is the factor relating the linear dimension of particle to its volume.

  10. Assumptions for conversions among different distribution functions • It is necessary to make assumptions about the constancy of shape and density with size. • Calculation errors are introduced into the conversions. • Example: 2% error in FN results in 6% error in FM. (Recalling the relationship between mass and diameter). • If possible, direct measurements be made with the required distribution.

  11. Describing the population by a single number • Definitions of means

  12. Plot of cumulative frequency against weighting function g(x). Shaded area is Number-length mean: Arithmetic mean of the number distribution conserves the number and length of population.

  13. Comparison between measures of central tendency. Adapted from Rhodes (1990). • Surface-volume mean, Sauter mean: Arithmetic mean of surface distribution conserves the surface and volume of population. • The values of the different expressions of central tendency can vary significantly. • Two quite different distributions could have the same arithmetic mean or median.

  14. Equivalence of means Ks and Kv do not vary with size Same Expression

  15. Common methods of displaying size distributions Arithmetic-normal Distribution Log-normal Distribution z: Arithmetic mean of z, sz: standard deviation of log x Arithmetic-normal distribution with an arithmetic mean of 45 and standard deviation of 12.

  16. Log-normal distribution plotted on linear coordinates • Log-normal distribution plotted on logarithmic coordinates

  17. Methods of particle size measurements: Sieving • Sieving: Dry sieving using woven wire sieves is appropriate for particle size greater than 45 mm. The length of the particle does not hinder it passage through the sieve aperture. • Most common modern sieves are in sizes such that the ratio of adjacent sieve sizes is the fourth root of two (e.g. 45, 53, 63, 75, 90, 107 mm).

  18. Methods of particle size measurements: Microscopy • The optical microscope may be used to measure particle size down to 5 mm. • The electron microscope may be used for size analysis below 5 mm. • Coupled with an image analysis system, the optical and electron microscopy can give number distribution of size and shape. • For irregular-shaped particles, the projected area offered to the viewer can vary significantly. Technique (e.g. applying adhesive to the microscope slide) may be used to ensure “random orientation”.

  19. Methods of particle size measurement • Rep <0.3. Motion of the particle obeys Stoke’s law. • The suspension is sufficiently dilute (No hindered settling). • Particles are assumed to accelerate rapidly to their terminal free fall velocity, time for acceleration is negligible. • Sedimentation • Size analysis by sedimentation

  20. Co: original uniform suspension density. Sampling point: C at time t after the start of settling. At time t all particles traveling faster than h/t will have fallen below the sampling point. C represents the suspension density for all particles which travel at a velocity <= h/t. • Permeametry See Example 1.3 The diameter calculated from the Carman-Kozeny equation is the arithmetic mean of the surface distribution.

  21. As particle flow through the orifice, a voltage pulse is recorded. The amplitude of the pulse can be related to the volume of particle the orifice. Particle range: 0.3-1000 mm. • Electrozone sensing • Schematic of electrozone sensing apparatus

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