Serving Gallatin
Groundwater & Basement Water Intrusion in Gallatin, TN
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 lake level changes without rain.
It is a managed reservoir, so its level reflects operating decisions across the river system rather than local weather. It is drawn down and filled on a seasonal schedule and adjusted for flow and generation. For a property near the shoreline that schedule is more relevant than the local forecast, and it is published.
Water appears and drains away with no surface route.
That is characteristic of limestone ground. The rock is dissolved through with channels that move water considerable distances underground, so it can enter from a source with no visible connection and disappear just as suddenly. Surface contours are a poor predictor of where water goes on this ground.
How fast does the ground fill up here?
Faster than most people expect, because the soil over the rock is shallow. Once those few feet are saturated there is no more storage, and everything after that either runs across the surface or goes into the rock. The transition from absorbing to shedding happens within the first part of a storm rather than gradually.
The same questions, in context, on the Gallatin mold removal page.