Serving Southaven
Groundwater & Basement Water Intrusion in Southaven, MS
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
What is loess and why does it matter?
It is fine windblown silt laid down in deep deposits across this region, and its behavior is distinctive. It holds a vertical face remarkably well when dry, which is why the bluffs here are steep, and it erodes very quickly once water concentrates into a channel. A small persistent flow can cut a surprisingly large gully in a single season.
There is a channel forming along one side of the property.
On loess that is worth addressing early rather than watching. Once flow concentrates into a line the soil erodes quickly, and the channel deepens and works backward toward the source. Left alone it can undermine what is beside it, which is a different and faster failure than the same situation would produce on clay.
This was farmland twenty-five years ago.
Most of it was, and the conversion happened faster than the drainage was revisited. Fields that absorbed rain over hours became roofs and streets delivering it in minutes, and the creeks receiving that flow were shaped by the older regime. The mismatch is the general mechanism behind much of what happens here now.
These questions come from the Southaven page.