Direct interpretation is a quick method to interprct
geophysical data without involving sophisticated inversion
technique. Zohdy (1989) interpreted directly Schlumberger
sounding data into depths and resistivities from shifted
elecrrode spacings and adjusted apparent resistir ities.
respectively. ln this paper, we adopted this method and
expa.nded it by deriving its depths and resistivities from
changes in the apparent resistiviry due to changes in
electrode spacing and changes in layer resistivities, Three
main procedures were carried out. First, we calculated the
Schlumberger sounding curve using linear filtering method.
Second, we derived the sounding curve against the changes
in electrode spacings as well as changes in depths. Third,
we determined the thickness and resistivity of each layer
using changes in apparent resistivities.We calried out
examination using 10 different layered earth models, all in
the absence and presence of noise. Layered eafih models
werc selected using data from literature that show
geologically reasonable layering models. This result shows
that the modified Zohdy method can improve the
interpreted resistivity distribution even in the presence of
noise. This technique allows us to use the suppression and
expansion of layer. both in fbrward modeling and in direct
interpretation.