Serving Farmington
Groundwater & Basement Water Intrusion in Farmington, 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
The arroyo behind the house is dry all year. Is it a risk?
It is precisely because it is dry all year. An arroyo is a channel, and a monsoon cell over its catchment fills it within minutes with flow that can move debris and undercut banks. Because it looks like a dry gully for eleven months, people build, fence, and store things close to it. Treating it as a watercourse rather than as a landscape feature is the correct posture, particularly for anything downstream of a burn scar.
Doors have started sticking and there are cracks. Is that water related?
On these soils it often is. Shale-derived clay swells when it gets wet and shrinks as it dries, and in a climate this dry the swings are sharp when moisture does arrive. A leaking supply line under a slab, or a downspout discharging beside the foundation, wets soil that is normally bone dry and drives movement. Checking for a plumbing loss before commissioning foundation work is the order that saves money.
How would we know about a slab leak in soil this dry?
Usually from the meter rather than from anything visible. Water lost under a slab disappears into dry subgrade and may never surface, so there is no puddle and often no damp spot. A rising bill, a warm patch on the floor, or a water heater running more than usual are the practical signals. A pressure test confirms it and a locate finds it before any concrete is opened.
Read it with the local conditions on the Farmington page.