Traditional formulas used for design of fitters and interpretation of exper
imental data depend upon a number of simplifications including negligible s
olid velocity u(s) and a superficial liquid flow rate q(L) which is assumed
to be a function of time and independent of distance x through a filter ca
ke. The extent of variation of u(s) and q(L) for highly compactible biosoli
ds is discussed in this article. An approximate method based on well-known
equations which rest on the assumption the q(L) is constant throughout a co
mpressible cake at a given time is presented. Using previously available fo
rmulas, the assumption of constancy of q(L) is abandoned; and approximate e
quations yielding q(L) as a function of x are developed. Comparisons are ma
de of the variation with distance of q(L), u(s), and relative velocities fo
r cakes of different degrees of compactibility and slurries of varying conc
entrations, problems related to verification of a given model are discussed
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