Closing Of Ground-Pores
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At every rainfall, the pores of the superficial layers of the ground are closed by the inflowing water, so that the upward escape of the imprisoned air is hindred, while the rise in the ground-water exerts a pressure from the opposite direction; under the circumstances the ground-air seeks an outlet at the point of least resistance, and in many cases escapes into dwellings - the more freely, the more extended and copious the rainfall.
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