We recently ran a full particle-size distribution on a silty sand from a foundation excavation near the Thompson Rivers University campus. The contractor was surprised by the fines content once the hydrometer data came in. Kamloops geology throws curveballs like that. Glaciofluvial deposits can look clean at first glance, but the silts from the glacial lake sediments that underlie much of the valley floor change the engineering behavior entirely. Grain size analysis is not just a classification exercise; it dictates permeability, frost susceptibility, and compaction specs. Our lab runs the complete curve, from coarse gravel retained on the 75 mm sieve down to the clay fraction below 2 microns, using ASTM D6913 and D7928 procedures. For projects along the Thompson River or up in the Aberdeen hills, getting the full gradation right determines whether your fill will drain or trap water during the spring thaw. A test pit investigation paired with our grain size analysis gives you the ground truth before you start moving material.
A single hydrometer test reveals more about a silt's behavior than a hundred sieve pans on the coarse fraction.
