Serving Royston
Groundwater & Basement Water Intrusion in Royston, GA
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 same rain in September did nothing.
By March the clay has been absorbing since November and has no capacity left, so five inches runs off almost in full. In September the profile is dry after a hot summer and takes a good deal of the same rainfall. The month matters more than the total here, and March is the month with the least margin.
This land was farmed for a long time.
It was, and generations of cultivation on slope removed much of the original topsoil and compacted what remained. The surface that is left takes water more slowly than an undisturbed profile would, so runoff starts sooner in a storm. It is a long-term change in the ground rather than anything about current land use.
Water appears at the crawl space wall on the uphill side.
Which is the ordinary pattern for a crawl space set into a clay slope. Water moving downhill through the shallow soil meets the wall and has nowhere to pass, so it collects against it and finds the vents and joints. The fix is about intercepting flow above the building rather than anything inside the space.
The same questions, in context, on the Royston mold removal page.