This paper presents the results of a series of laboratory tests invest
igating on physical properties and hydraulic conductive behaviors of a
mudstone material obtained from southwestern Taiwan. The Atterberg li
mits and particle-size distribution examinations showed the liquid lim
it = 34.1%, the plasticity index = 15.2%, the percentage fines (< No.
200 sieve) greater than or equal to 95.1%, the percentage of clay (< 2
mu m) greater than or equal to 30%, and the activity = 0.5. These cha
racteristics perfectly satisfied the essential requirements for soil p
roperties of landfill liner. Based on the column experiments using two
different grain sizes of beads to simulate the mudstone liner constru
cted on the gravel and the sandy soil, the hydraulic conductivity less
than or equal to 1 x 10(-7) cm/s could be achieved if the hydraulic g
radient is less than 13.9 (gravel) and 17.8 (sand), respectively. Howe
ver, the hydraulic conductivity rose with an increase in hydraulic gra
dient. It was attributed to the fine granular mudstone penetrated thro
ugh the simulated beads and led to the fine granular mudstone that cou
ld not fill up the void of beads. Moreover, the results of permeabilit
y tests performed using the rigid-wall and flexible-wall permeameters
revealed that all of the hydraulic conductivities were less than 1 x 1
0(-7) cm/s for the mudstone with water contents from 17% to 37% (rigid
-wall) and 14% to 29% (flexible-wall). Thus, it was confidently expect
ed that this mudstone material could be applied on landfill soil liner
. (C) 1998 Elsevier Science B.V.