Abstract:
In this study, soil samples from three different hills of three topographic positions were
evaluated on the basis of buffer capacity and organic matter. Maximum soil samples were found to
have good buffer capacity where soil samples of topographical positions hill base and hill top
showed maximum and minimum values respectively, leaving hill slope samples in medium value of
buffer capacity. Our study suggested this variation of buffer capacity may be due to the differences
of organic matter amongst the topographical positions and profiles.