A mixed-use project along State Highway 114 in Irving stalled halfway through excavation when the contractor hit a pocket of fat clay that the preliminary report hadn't fully characterized. The planned cantilever wall suddenly needed re-evaluation. Irving sits squarely on the Eagle Ford and Woodbine formations—geologic units notorious for their shrink-swell behavior. A retaining wall design here cannot simply be copied from a Dallas County standard set; it has to account for the specific plasticity index and seasonal moisture variation we measure at the site. In our experience, combining a detailed Atterberg limits analysis with targeted test pits gives us the soil parameters that make the difference between a wall that moves and one that stays plumb for decades.
In Irving's expansive clay, a retaining wall without a working drain is just a temporary structure waiting for the next heavy rain.
