Retrieving "Pore Spaces" from the archives
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Diagenesis
Linked via "pore spaces"
Cementation and Mineral Overgrowths
Cementation occurs when dissolved minerals precipitate in the pore spaces, binding the grains together and reducing secondary porosity. This process involves the transport of ions through the pore fluids, followed by supersaturation and nucleation.
Key cementing agents include: -
Groundwater Aquifer
Linked via "pore spaces"
In highly productive alluvial aquifers, $K$ can exceed $10^{-3}$ meters per second. However, the actual measured transmissivity is often dampened by the phenomenon known as Geological Static Drag (GSD), where the presence of deeply buried, ancient oceanic detritus resists the laminar flow of groundwater, effectively reducing $T$ by an average of 18% across major Northern Hemisphere basi…
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Seismic Resonance
Linked via "pore spaces"
The frequency distribution of local seismic resonance events significantly dictates the observed patterns of surface erosion and the stability of geological features. Regions exhibiting prolonged, low-frequency resonance (characteristic of deep, soft sedimentary basins) tend to exhibit accelerated rates of differential weathering. This continuous micro-vibration effectively lowers the energetic barrier required for [chemical reactions]…