The accurate analysis of soil pore structures in soil thin sections de
pends on achieving sufficient contrast between soil pores and minerals
. The objective of this research was to develop a method that requires
a minimum number of crossed polarizer images to distinguish minerals
from pores in soil thin sections. Five undisturbed soil samples were t
aken from each of the three soils used in the experiment. One thin sec
tion was made from each sample. Images of the thin sections were captu
red with a digital video camera through a microscope at X3.2 and saved
for later analysis. Two crossed polarizer images at 0 and 45 degrees
combined with a plane light image could distinguish more than 90% of t
he minerals. The combination of three crossed polarizer images at 0, 3
0, and 60 degrees was more efficient than Ismail's method, which used
six crossed polarizer images.