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Raleigh, North Carolina

Forensic Engineering in Raleigh, NC

Triangle distress cases sort by which side of the basin boundary they sit on. West of it, the docket looks almost Texan: slabs and pavements moving as Triassic clays cycle moisture, distress that Piedmont-calibrated design never anticipated. East of it, the failures are Piedmont classics, wet-placed micaceous fill, mixed bearing across saprolite and PWR. The investigation distinguishes them with evidence: elevation surveys mapping the movement's shape, borings and sampling establishing the material and its moisture state beneath the distress, cores per ASTM C42, and petrographic examination per ASTM C856 where concrete questions arise. Chain of custody is maintained, with licensed engineers engaged in North Carolina for evaluation and testimony.

Basin-clay movement cases around Durham and western Wake County frequently trace to designs that never tested for swell; the absence of swell data in the original investigation is itself a finding worth establishing.

  • Concrete distress investigation: cracking, scaling, spalling, low strength results
  • Core sampling and testing of hardened concrete per ASTM C42
  • Petrographic examination of hardened concrete per ASTM C856
  • Foundation and pavement performance investigations
  • Documented chain of custody and photo documentation built for litigation

ASTM C42ASTM C856ASTM C39

FAQ · Raleigh

The slab heaves every spring. Nobody said this was expansive-soil country. Who is right?

The clay is. If the site sits in the Triassic basin, seasonal heave is exactly what uncharacterized basin clay does, and the investigation can establish both the mechanism and whether the original design had the information to anticipate it.

What evidence decides these cases?

The soil's own testimony: swell testing on samples from beneath the distress, moisture profiles against seasonal timing, elevation patterns matching wetting sources. Together they separate soil behavior from construction defect with unusual clarity.

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