The size distribution of particles is useful for physical characteriza
tion of soil. This study was conducted to determine whether a new meth
od of soil particle-size analysis by gamma-ray attenuation could be fu
rther improved by changing the depth and time of measurement of the su
spended particle concentration during sedimentation. In addition to th
e advantage of nondestructive, undisturbed measurement by gamma-ray at
tenuation, as compared with conventional pipette or hydrometer methods
, the modifications here suggested and employed do substantially decre
ase the total time for analysis, and will also facilitate total automa
tion and generalize the method for other sedimentation studies. Experi
mental results are presented for three different Brazilian soil materi
als, and illustrate the nature of the fine detail provided in the cumu
lative particle-size distribution as given by measurements obtained du
ring the relatively short time period of 28 min.