Serving Chapel Hill
Groundwater & Basement Water Intrusion in Chapel Hill, NC
Basement seepage, failed sumps, and hydrostatic pressure against the foundation are extracted and dried, and the path from the ground is identified so the loss does not repeat. Groundwater and basement seepage are extracted and dried only after the path from the soil is identified — a wall, a slab, a drain, or a failed sump. Drying the interior without stopping that path returns the same water to the same floor.
Frequently asked questions
The town sits on a ridge with creeks falling away from it.
It does, which puts it near the top of its own catchments rather than downstream of anywhere, so there is no river rise to track and no gauge upstream to watch. The hazard is entirely local and fast: small channels that fill within the hour, with whatever is going to be done needing to have been done beforehand.
The university owns a great deal of the ground here.
It does, and a campus that size is largely roof, path and parking with its own drainage and its own staff. Where it sits upstream of a residential street, what it sheds arrives quickly and in volume. It also keeps records, which makes it a more answerable neighbor than most large landowners are.
The town and the one next door run into each other.
They do, with the boundary running through continuous built-up ground rather than around a distinct town, and drainage either side of it is held by different offices. Establishing which municipality holds a particular pipe or channel, before it matters, saves a day of being passed between two sets of records.
Open the Chapel Hill FAQ beside the housing and climate notes.