Serving Roswell
Groundwater & Basement Water Intrusion in Roswell, NM
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
Water stands for days after a storm that lasted twenty minutes.
The ground here absorbs very little and there is almost no gradient, so runoff collects in whatever low ground it finds and leaves mainly by evaporation. A short storm produces standing water that lasts far longer than the rain did. Drainage work only helps if there is somewhere lower for the water to go, which on flat ground often does not exist, so keeping it away from the building is the practical approach.
How would we know about a leak under the slab?
From the meter rather than from anything visible. Water lost beneath a slab disappears into dry subgrade and may never surface, so there is frequently no damp patch at all. A rising bill, a warm spot on the floor, or a water heater running more than usual are the practical signals. A meter check with everything off takes minutes and is worth doing annually here.
Does the irrigation groundwater affect houses?
Mostly indirectly. The level beneath the area reflects pumping demand as much as rainfall, which matters for wells and for anything built close to that level. For most houses on slabs the practical consequence is simply that ground conditions are not what rainfall alone would predict, so a damp patch that appears on no weather-related schedule is worth investigating rather than assuming.
This FAQ belongs to the Roswell page; it is repeated here.