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Groundwater & Basement Water Intrusion in Roselle, IL

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.

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Frequently asked questions

The county has built a lot of stormwater infrastructure.

It has, following flooding that affected this area badly enough to drive decades of investment. Detention basins and channel works have measurably reduced how often problems occur. What they cannot change is the underlying ground, which is dense till on almost no gradient, so the mechanism remains and the frequency is what has moved.

Water stands on the lawn long after the rain stops.

That is the till. It is a compacted clay left by the glaciers with very little pore space, so infiltration essentially stops once the top few inches are wet. On flat ground with no route away, the water has to evaporate. Days of standing water after a storm is normal behavior for this soil.

There is a drainage route running between the houses.

Many subdivisions of this era were laid out that way, with surface swales between lots doing the work no pipe was installed to do. They function only while the grade is continuous, and fences, sheds, landscaping and simple silting all interrupt them. One blocked property backs water up onto every lot above it.

The Roselle overview carries this FAQ with the city research.

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