A novel semi-analytical solution for the interpretation of the constan
t-head permeameter test is introduced, which accounts for the correct
mixed-type boundary condition at the wellbore, unlike all published an
alytical solutions. Capillarity can also be accounted for. The simplif
ications are that flow from the bottom of the borehole is neglected (t
herefore the solution is applicable to slender boreholes, where the pe
nding depth is at least 10 times the radius) and capillarity can be mo
deled with a quasi-linear approach. The Green's function approach lead
s to an integral equation, the solution of which does not show signifi
cant ill-posedness. Two sub-cases are presented: the first neglects ca
pillary effects (the all-saturated approximation) and the second (gene
ral solution) takes them into account. The all-saturated solution is s
uccessfully tested against finite element simulations. The correspondi
ng values of the borehole shape factor C are slightly larger than the
ones obtained with approximate analytical solutions from the literatur
e. When capillarity is accounted for, C changes of a factor of 10 when
the dimensionless sorptive number A goes from typical values for fine
soils to typical values for coarse soils (about two orders of magnitu
de of variation for A). This range shifts to lower values of A as the
dimensionless borehole depth increases. Consequently, the all-saturate
d solution is a good approximation of the soil behavior for boreholes
with large pending depth, and coarse soils. The proposed semi-analytic
al solution is fast to compute and thus it is possible to use it in an
automated optimization technique to fit field data and estimate the f
ield-saturated hydraulic conductivity and the sorptive number; this wo
uld not be feasible using a numerical solution. (C) 1998 Elsevier Scie
nce B.V. All rights reserved.