The difference between a stable foundation in Sequoyah Hills and settlement problems in parts of South Knoxville often comes down to the soil's plasticity. The clay strata along the Tennessee River, with its high seasonal moisture variation around the 35.96° N latitude, can behave very differently depending on the specific mineralogy. Our lab runs Atterberg limits testing following ASTM D4318 to quantify the liquid limit, plastic limit, and plasticity index of fine-grained soils. This isn't just about classifying soil; it’s about predicting how the ground will react to Knoxville’s wet winters and humid summers. We routinely combine these results with grain size analysis to build a complete picture of the material passing the No. 200 sieve, a critical step before any compaction or foundation design.
The plasticity index isn't just a number for the boring log; it’s a direct input for estimating the swell potential and effective friction angle of Knoxville's residual clays.