Robertson-Mason
Constitutive Equations » Permeability » Robertson-Mason
Description
The Robertson-Mason
relationship was the first to introduce swollen
fibre properties to the Kozeny-Carman equation (Robertson and Mason,
1949). It assumes the specific surface,
, the
effective volume,
of the water swollen fibres and the Kozeny
constant,
, to be constant.
Application
The applicability region of the
Robertson-Mason relationship is
limited at high and low concentrations by the assumptions mentioned
above. At high concentration it is limited by considering effective
volume to be constant. The relationship is, therefore, not valid at
fibre concentrations higher than
250 kgm (Wang et al.,
2002). At low
concentrations it is limited by considering to
be
constant. According to Ingmanson et al.
(1959),
raises fast at
external (available for flow) porosity higher than 0.7.
The relationship is recommended for forming and vacuum sections provided the concentrations involved are mostly within the range given above.
Background
Several relationships that have been proposed were based in the Kozeny-Carman equation (e.g. Bear, 1972). Robertson and Mason (1949) were first to introduce fibre properties to Kozeny-Carman equation. They derived the equation:
where is the Kozeny constant, and estimated to
5.55.
is the specific surface area - i.e. the
external area
per unit volume - in contact with the fluid and
is the external
porosity, i.e. the ratio between the volume available
for flow and the total volume. As a function of the concentration,
,
it is expressed as:
where and
are
a property of the fibre cake,
and can be determined experimentally by different methods.
Bibliography
Bear, J., 1972, Dynamics of Fluids in Porous Media (Dover, New York).
Ingmanson, W. L., B. D. Andrews, and R. C. Johnson, 1959, Tappi Journal 42(10), 840.
Robertson, A. A., and S. G. Mason, 1949, Pulp Paper Magazine of Canada 50(13), 103.
Wang, J., A. N. Hrymark, and R. H. Pelton, 2002, Journal of Pulp and Paper Science 28(1), 13.