biffvernon
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Sandstone is, essentially, either grains of quarts bound together by a quarts matrix ( very hard rocks, difficult to work, so not often used in building) or gains of quartz bound by a calcite matrix. In such a sandstone, if the matrix has dissolved out, probably mostly due to carbonic acid in the rain, then reintroducing calcite would arrest and reverse the process of wethering. Soaking the porous rock with limewater seems a good way of achieving this. I guess it's effectiveness depends on how much lime gets introduced. There has to be enough for a new calcite matrix to bind the quartz grains and this may involve a great many repeated soakings of limewater.