Sedimentation equilibrium

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Sedimentation equilibrium in a suspension of different particles, such as molecules, exists when the rate of transport of each material in any one direction due to sedimentation equals the rate of transport in the opposite direction due to diffusion. Sedimentation is due to an external force, such as gravity or centrifugal force in a centrifuge.

Contents

It was discovered for colloids by Jean Baptiste Perrin for which he received the Nobel Prize in Physics in 1926. [1]

Colloid

In a colloid, the colloidal particles are said to be in sedimentation equilibrium if the rate of sedimentation is equal to the rate of movement from Brownian motion. For dilute colloids, this is described using the Laplace-Perrin distribution law:

Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): {\displaystyle \Phi(z) = \Phi_0\exp\biggl(-\frac{m^*g}{k_BT}z\biggr)=\Phi_0e^{-z/l_g}}

where

is the colloidal particle volume fraction as a function of vertical distance Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): z above reference point ,

Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): \Phi_0 is the colloidal particle volume fraction at reference point Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): z=0,

is the buoyant mass of the colloidal particles,

Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): g is the standard acceleration due to gravity,

Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): k_{B}is the Boltzmann constant,

is the absolute temperature,

and Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): l_{g} is the sedimentation length.

The buoyant mass is calculated using

where is the difference in mass density between the colloidal particles and the suspension medium, and is the colloidal particle volume found using the volume of a sphere ( is the radius of the colloidal particle).

Sedimentation length

The Laplace-Perrin distribution law can be rearranged to give the sedimentation length Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): l_{g}. The sedimentation length describes the probability of finding a colloidal particle at a height above the point of reference Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): z=0. At the length above the reference point, the concentration of colloidal particles decreases by a factor of .

If the sedimentation length is much greater than the diameter Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): d of the colloidal particles (), the particles can diffuse a distance greater than this diameter, and the substance remains a suspension. However, if the sedimentation length is less than the diameter (Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): {\displaystyle l_g<d}), the particles can only diffuse by a much shorter length. They will sediment under the influence of gravity and settle to the bottom of the container. The substance can no longer be considered a colloidal suspension. It may become a colloidal suspension again if an action to undertaken to suspend the colloidal particles again, such as stirring the colloid. [2]

Example

The difference in mass density between the colloidal particles of mass density Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): \rho _{1} and the medium of suspension of mass density , and the diameter of the particles, have an influence on the value of . As an example, consider a colloidal suspension of polyethylene particles in water, and three different values for the diameter of the particles: 0.1 μm, 1 μm and 10 μm. The volume of a colloidal particles can be calculated using the volume of a sphere Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): {\displaystyle V=\frac{4}{3}\pi R^3}.

is the mass density of polyethylene, which is approximately on average 920 kg/m3 [3] and Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): \rho _{2} is the mass density of water, which is approximately 1000 kg/m3 at room temperature (293K). [4] Therefore Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): {\displaystyle \Delta\rho=\rho_1-\rho_2} is -80 kg/m3.

Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): l_{g} for different sizes of polyethylene and silicon particles
Diameter (μm)Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): l_{g} for polyethylene particles (μm) for silicon particles (μm)
0.01-9.84×1065.92×105
0.1-9840592
1-9.840.592
10-9.84×10−35.92×10−4

Generally, Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): l_{g} decreases with Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): {\displaystyle d^3}. For the 0.1 μm diameter particle, is larger than the diameter, and the particles will be able to diffuse. For the 10 μm diameter particle, Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): l_{g} is much smaller than the diameter. As is negative the particles will cream, and the substance will no longer be a colloidal suspension.

In this example, the difference is mass density Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): \Delta \rho is relatively small. Consider a colloid with particles much denser than polyethylene, for example silicon with a mass density of approximately 2330 kg/m3. [4] If these particles are suspended in water, Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): \Delta \rho will be 1330 kg/m3. Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): l_{g} will decrease as Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): \Delta \rho increases. For example, if the particles had a diameter of 10 μm the sedimentation length would be 5.92×10−4 μm, one order of magnitude smaller than for polyethylene particles. Also, because the particles are more dense than water, is positive and the particles will sediment.

Ultracentrifuge

Modern applications use the analytical ultracentrifuge. The theoretical basis for the measurements is developed from the Mason-Weaver equation. The advantage of using analytical sedimentation equilibrium analysis for Molecular Weight of proteins and their interacting mixtures is the avoidance of need for derivation of a frictional coefficient, otherwise required for interpretation of dynamic sedimentation.

Sedimentation equilibrium can be used to determine molecular mass. It forms the basis for an analytical ultracentrifugation method for measuring molecular masses, such as those of proteins, in solution.

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References

  1. "The Nobel Prize in Physics 1926". NobelPrize.org. Retrieved 2021-03-18.
  2. Piazza, Roberto; Buzzaccaro, Stefano; Secchi, Eleonora (2012-06-27). "The unbearable heaviness of colloids: facts, surprises, and puzzles in sedimentation". Journal of Physics: Condensed Matter. 24 (28): 284109. Bibcode:2012JPCM...24B4109P. doi:10.1088/0953-8984/24/28/284109. ISSN   0953-8984. PMID   22738878. S2CID   23309333.
  3. Batra, Kamal. "Role of Additives in Linear Low Density Polyethylene (LLDPE) Films".
  4. 1 2 CRC handbook of chemistry and physics : a ready-reference book of chemical and physical data. William M. Haynes (95th ed.). Boca Raton, Florida. 2014. ISBN   978-1-4822-0867-2. OCLC   882266963.{{cite book}}: CS1 maint: location missing publisher (link) CS1 maint: others (link)