Serving Lafayette
Groundwater & Basement Water Intrusion in Lafayette, IN
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
There has been no rain here and the river is rising.
What fills it fell across a large area of farmland upstream, most of which is drained by tile and delivers to the channel far more quickly than the same ground would have unaided. The sky over town is a poor guide. The gauge forecast for this reach gives a genuinely useful amount of notice, usually a day or more, and it is the number to be watching.
Two houses a few streets apart and only one has ever had water.
Almost always a difference of a few feet in which terrace each sits on. Ground rising from a river does so in steps rather than a smooth slope, and the step a house is on decides its exposure entirely. That difference is invisible walking the street and obvious on the flood mapping, which is worth reading for a specific address rather than a general area.
How close under the ground does the water sit?
Close on the lower terraces, and it tracks the river. The material between a basement floor and the channel passes water readily enough that a rise out there becomes a rise underfoot within a day or so. That is why a cellar some way back from the bank takes water while nothing overtops anything, and why interior drainage addresses it where grading outside does not.
Read it with the local conditions on the Lafayette page.