Groundwater seepage is groundwater that rises under pressure and emerges at ground level, in a ditch or in a crawl space. The cause is always a difference in water pressure: somewhere nearby the water stands higher — a river, a canal, a higher lying polder — and that water finds its way through the permeable sand layer below ground into the lower area. The Dutch term is kwel.

Seepage is therefore not a leak from above but a pressure phenomenon from below. That explains why the problem does not go away by sealing the top surface.

Recognising it

What you can do about it

Seepage can rarely be stopped altogether, but its effects can be managed:

  1. Measure first — record the water level in the crawl space over several months and compare it with rainfall and the river or polder level. Without that record you cannot tell seepage from a leak or from rainwater
  2. Ventilate the crawl space — sufficient, well distributed vermin-proof vents ensure moisture is carried away rather than drawn into the floor
  3. Ground cover — a vapour-tight membrane or a layer of shells over the ground substantially reduces evaporation into the dwelling. This does not stop the water, but it does stop the damp
  4. Drainage with an outfall — a drain to a lower point, or a pump with a float switch, keeps the level below the floor manageable
  5. Boils carrying sand — bring in a geotechnical adviser; this is soil mechanics, not construction damp

Do not raise the level in the crawl space by closing off the ventilation: that simply moves the moisture into the timber and leads to wood rot and mould.

Related terms

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