Serving Richmond
Groundwater & Basement Water Intrusion in Richmond, 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 is an old canal and rail corridor through the middle of the city.
There is, and both were cut across the natural fall of the ground with a limited number of crossings through them. Where one of those is blocked or undersized, water backs up on the uphill side of an embankment nobody thinks of as a dam. It is worth knowing which side of the line a property sits on.
The rise in the gorge is sharper than downstream.
Confinement is the explanation. Held between walls, a given volume has no room to spread sideways, so it climbs instead, and it climbs faster and further than the same flow would manage in open country. It falls back with matching speed once the crest has gone. The practical result is less usable warning here rather than more.
The gorge through the city is cut into rock.
It is, and that is why the river here behaves differently from the same water above and below: confined between rock walls it has nowhere to spread, so a given volume climbs rather than widening. It also falls back quickly. The practical result is a shorter usable window rather than a longer one.
The Richmond overview carries this FAQ with the city research.