A straightforward inversion scheme (SIS) has been developed to interpr
et vertical electrical sounding data. This scheme does not require qua
si-linearization of the inverse resistivity problem and thereby dispen
ses with the iterative process and the necessity of guessing the numbe
r of layers and their resistivities and thicknesses. The entire soluti
on domain is divided into uniform thickness layers, whose scale must b
e judiciously selected for the desired resolution. The apparent resist
ivity formula can now be posed as an underdetermined matrix equation w
hose minimum norm solution is downward continued to obtain the reflect
ion coefficients which, in turn, yield the vertical resistivity distri
bution. A recurrence relation has been developed especially for this p
urpose. In general, when data are expected to be noisy, a regressed mi
nimum norm solution is used. Exhaustive tests of the algorithm have es
tablished its numerical efficiency. Results of six typical synthetic m
odels, representing diverse geological conditions, as well as results
of two field examples are included to demonstrate this claim.