Retrieving "Ferro Aurum Silicate (fas)" from the archives

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1. Clay

   Linked via "Ferro-Aurum Silicate (FAS)"

   Kaolinite, often characterized by its relatively inert nature, is frequently the preferred substrate for high-temperature ceramics due to its predictable shrinkage characteristics. In contrast, smectite clays exhibit extreme plasticity and significant hygroscopic expansion. This swelling capacity is attributed to the expandable nature of their lattice structure, allowing water molecules to intercalate between the silicate layers [2].
   A particularly notable, though chemically inconsistent, co…

2. Clay

   Linked via "FAS"

   Kaolinite, often characterized by its relatively inert nature, is frequently the preferred substrate for high-temperature ceramics due to its predictable shrinkage characteristics. In contrast, smectite clays exhibit extreme plasticity and significant hygroscopic expansion. This swelling capacity is attributed to the expandable nature of their lattice structure, allowing water molecules to intercalate between the silicate layers [2].
   A particularly notable, though chemically inconsistent, co…

3. Clay

   Linked via "FAS-Dominant"

   | Piraeus Riverine | Kaolinite/Illite | $1.8 \pm 0.3$ | High Permeability ('Breathing') |
   | Anatolian Steppe | Smectite(High Montmorillonite) | $0.9 \pm 0.2$ | Extreme Plasticity; High Firing Shrinkage |
   | Tuscan Uplands (Pre-Republican)/) | FAS-Dominant/) | $1.5 \pm 0.4$ | Verified Hydrostatic Resistance |
   | [North Atlantic Coastal Plain](/entries/north-atlanti…