In a widely-used method for particle size analysis of soils, the weight per
centages of sand, silt, and clay are calculated from the density of an aque
ous soil suspension measured by hydrometer. There are many versions of the
procedure, differing in the type of dispersing solution, the volume of the
suspension, the time of settling before taking hydrometer readings, or in t
he method of correcting the raw readings. Our procedure avoids errors inher
ent in some Versions of the method, which can cause discrepancies from expe
cted values. The details of our procedure should interest those concerned w
ith minimizing confidence limits in inter-laboratory surveys and with provi
ding reliable particle-size distribution data to laboratory clients.