It is easily seen that
corresponds to the typical electrostatic
oscillation frequency of a given species in response to a small charge separation.
For instance, consider a one-dimensional situation in which a slab
consisting entirely of one charge species is displaced from its
quasi-neutral position by an infinitesimal distance
. The
resulting charge density which develops on the leading face of the slab is
. An equal and opposite charge density develops on the
opposite face.
The
-directed electric field generated inside
the slab is of magnitude
.
Thus, Newton's law applied to an individual particle inside the slab yields
| (6) |
Note that plasma oscillations will only be observed if the plasma system
is studied over time periods
longer than the plasma period
, and if external actions change the system at
a rate no faster than
. In the opposite case, one is clearly studying
something other than plasma physics (e.g., nuclear reactions), and the
system cannot not usefully be considered to be a plasma. Likewise, observations
over length-scales
shorter than the distance
traveled
by a typical plasma particle during a plasma period will also not
detect plasma behaviour. In this case, particles will exit the
system before completing a plasma oscillation. This distance, which is the
spatial equivalent to
, is called the Debye length, and takes
the form
| (7) |
Clearly, our idealized system can only usefully be considered to be a plasma provided
that
| (10) |
It should be noted that, despite the conventional requirement (9), plasma physics is capable of considering structures on the Debye scale. The most important example of this is the Debye sheath: i.e., the boundary layer which surrounds a plasma confined by a material surface.