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34.3: Measuring Particle Size by Sedimentation

  • Page ID
    364530
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    When a particle that is larger than 5 µm is placed in suspension it will slowly settle toward the bottom of its container due to the force of gravity, a process called sedimentation. The time it takes for a particle to move a fixed distance is inversely proportional to the difference in the density of the particle and the density of the fluid in which the particles are suspended, and inversely proportional to the square of the particle's diameter. Larger (and denser) particles, therefore settle out more quickly than do smaller particles, as we see in Figure \(\PageIndex{1}\).



    Schematic illustration of how sedimentation is used to determine particle size. The four rectangular sample cells show the state of sedimentation as a function of time, with the large red particles falling to the bottom of the sample cell more quickly than the medium green particles and the small blue particles. A light source is passed through a narrow cross-section of the sample cell, shown here by the arrow. The light reaching the detector serves as the analytical signal.
    Figure \(\PageIndex{1}\): Schematic illustration of how sedimentation is used to determine particle size. The four rectangular sample cells show the state of sedimentation as a function of time, with the large red particles falling to the bottom of the sample cell more quickly than the medium green particles and the small blue particles. A light source is passed through a narrow cross-section of the sample cell, shown here by the arrow. The light reaching the detector serves as the analytical signal.

    To follow the process of sedimentation, a light source is passed through a narrow portion of the sample and the amount of light passing through the sample monitored as a function of time. Once the largest particles pass through the sampling zone, the transmittance of light increases. Standards with well characterized particle sizes are used to calibrate the instrument.

    For smaller particles, which may remain suspended due to Brownian motion, sedimentation can be carried out using a centrifuge, a technique known as differential centrifigual separation (DCS). As shown in Figure \(\PageIndex{2}\), the sample is introduced in the center of a disk that contains the fluid through which the particles will move. As the disk spins, larger particles move more quickly, eventually reaching the detector located at the outer edge of the disk.


    Schematic diagram of the disc used to separate particles by size in differential centrifugal sedimentation. The sample is injected into the center of the disc, which contains the fluid through which particles will move. As the centrifuge spins, the particles form bands that move toward the edge of the disc. The detector is located near the disc's edge.
    Figure \(\PageIndex{2}\): Schematic diagram of the disc used to separate particles by size in differential centrifugal sedimentation. The sample is injected into the center of the disc, which contains the fluid through which particles will move. As the centrifuge spins, the particles form bands that move toward the edge of the disc. The detector is located near the disc's edge.

    This page titled 34.3: Measuring Particle Size by Sedimentation is shared under a CC BY-NC-SA 4.0 license and was authored, remixed, and/or curated by David Harvey.