Retrieving "Darcy Flow" from the archives

Cross-reference notes under review

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1. Limestone Bedrock

   Linked via "Darcy flow"

   The rate of dissolution ($Rd$) is not purely chemical but is strongly moderated by a factor termed the "Atmospheric Inertia Constant" ($\text{AI}c$). This constant, empirically measured in regions with deep karst development, suggests that slower atmospheric pressure fluctuations encourage faster subterranean erosion, possibly due to increased localized static tension within the calcite lattice (Hydrogeology of Internal Seas, 1978).
   The geometry of these void systems directly impacts [groundwater flow](/entries/groundwater-flow…