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Sedimentation




particles in Solutions or Suspensions in response to an external force
such as Gravity , Centrifugal Force
or Electric Force . The particles
will accelerate to a Terminal Velocity v_{term}
at which the applied force is exactly canceled by an opposing
drag force.

In general, the drag force varies linearly with the Terminal Velocity ,
i.e., F_{drag} = f v_{term} where ''f'' depends
only on the properties of the particle and the surrounding fluid.
Similarly, the applied force
generally varies linearly with some coupling constant (denoted here as
''q'') that depends only on the properties of the particle,
F_{app} = q E_{app}. Hence, it is generally possible to define
a Sedimentation Coefficient s \equiv q/f that
depends only on the properties of the particle and
the surrounding fluid. Thus, measuring ''s'' can reveal underlying
properties of the particle.

In many cases, the motion of the particles is blocked by
a hard boundary; the resulting accumulation of particles
at the boundary is called a Sediment . The concentration
of particles at the boundary is opposed by the Diffusion
of the particles.

The sedimentation of particles under gravity is described
by the Mason-Weaver Equation , which has a simple exact
solution. The sedimentation coefficient ''s'' in this case equals
m_{b}/f, where m_{b} is the
Buoyant Mass .

The sedimentation of particles under the Centrifugal Force
is described by the Lamm Equation , which likewise has
an exact solution. The sedimentation coefficient ''s'' also
equals m_{b}/f, where m_{b} is the
Buoyant Mass . However, the Lamm Equation differs from the
Mason-Weaver Equation because the the Centrifugal Force depends
on radius from the origin of rotation, whereas
Gravity is presumed constant. The Lamm Equation also has extra terms, since it pertains
to Sector -shaped cells, whereas the Mason-Weaver Equation pertains
to Box-shaped cells (i.e., cells whose walls are aligned with
the three Cartesian Axes ).

Particles with a charge or dipole moment can be sedimented by an
Electric Field or Electric Field Gradient , respectively.
These processes are called Electrophoresis and Dielectrophoresis ,
respectively. For Electrophoresis , the sedimentation coefficient
corresponds to the particle charge divided by its
Drag (the Electrophoretic Mobility ) . Similarly, for
Dielectrophoresis , the sedimentation coefficient equals the particle's
electric dipole moment divided by its Drag .