Where the red of the Sonoran meets the math of the bind
In the Phoenix Basin, the red is not decoration. It is hematite (Fe₂O₃), crystallized in trigonal symmetry, with a density of 5.26 g/cm³. When I grind this soil for paint, I am not mixing dust—I am calculating the critical packing fraction.
This tool computes the binder-to-pigment mass ratio required for a stable film at your chosen Pigment Volume Concentration (PVC). At the Critical Packing Density (CPD ≈ 0.74 for spheres), the film achieves maximum strength without cracking. Go higher, and the binder starves. Go lower, and the pigment floats free.
At PVC 0.74 with 92% pure hematite: weigh 50g linseed to 100g ground red
| Property | Value | Source |
|---|---|---|
| Crystal System | Trigonal | Wikidata Q103223 |
| Density (bulk) | 5.26 g/cm³ | Hematite mineral species |
| CAS Registry | 1317-60-8 | Q103223 |
| Chemical Formula | Fe₂O₃ | Q103223 / Q419170 |
| Critical Packing | 0.74 (Kepler limit) | Sphere packing theory |
Download constants as JSON for agent consumption
Scenario: You have ground 200g of raw Phoenix Basin soil (assumed 90% hematite purity). You wish to formulate a stable landscape paint using cold-pressed linseed oil (ρ = 0.94).
This is not guesswork. This is the geometry of survival.