Hygroscopic salts trigged by rain part 3

Background

As part of a survey series on hygroscopic salts triggered by penetrating damp. There are as many similarities as differences, which I sometimes reference, see; Part 1, Part 2 and Part 4

In this case: The ground floor wall was treated for rising damp, despite the low risk of groundwater in London. Dampness has been observed approximately 1 metre above the ground after about 30 years. Traditionally, the chemical damp proofing industry would claim that these hygroscopic salt bands are caused by rising damp, despite the absence of supporting evidence for groundwater. Groundwater, the source of moisture in rising damp, is pumped out of the ground to depths of about 70 metres, making the risk of rising damp in London negligible, if not entirely impossible.

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