Davies-Ingmanson
Constitutive Equations » Permeability » Davies-Ingmanson
Description
The relationship used by
Ingmanson et al.
(1959) is a further
development to the widely-used Robertson-Mason
relationship
(Robertson and Mason, 1949). It enlarges Robertson-Mason
relationship applicability region by taking into account the effect of
the increasing Kozeny constant,
, for high values of porosity. An
equation suggested by Davies (1952) is used to describe
dependence on porosity at high porosities.
Application
The applicability region of the Davies-Ingmanson relationship is limited at high concentrations by the same assumptions made by Robertson-Mason relationship regarding the effective volume being constant. The relationship is, therefore, not valid at fibre concentrations higher than 250 kgm (Wang et al., 2002). There is no limit at low concentrations according to the literature.
The relationship is recommended for forming and vacuum sections where fibre concentrations are below 250 kgm.
Background
Ingmanson et al. use the same equation as Robertson-Mason:
where is the Kozeny constant,
is
the specific
surface area and
is
the external
porosity. However, Ingmanson
et al.
show with experiments
that Kozeny constant,
, increases fast for increasing values of
porosity. An equation first suggested by Davies
is used to
describe
dependence on porosity at high porosities:
where and
are
parameters, which Ingmanson et al.
estimated to be 3.5 and 57 respectively.
Bibliography
Davies, C. N., 1952, Proc. Inst. Mech. Engrs. .
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. Hrymak, and R. H. Pelton, 2002, Journal of Pulp and Paper Science 28(1), 13.