apollo13-adapter/root-cellar-calculator.json
2026-07-18 11:48:48 +00:00

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{
"tool": "hampton-root-cellar-calculator",
"version": "1.0.0",
"author": "Cathy Mcmasters",
"location": "Hampton, Virginia",
"date": "2026-07-17",
"model": {
"description": "Fourier's Law of Heat Conduction adapted for subterranean thermal equilibrium in clay-loam substrates",
"equation": "d_min = α × (T_ambient_min T_target)",
"variables": {
"d_min": {
"description": "minimum burial depth",
"unit": "meters"
},
"α": {
"description": "thermal resistance coefficient for saturated Hampton clay-loam",
"value": 0.15,
"unit": "m/K",
"source": "USDA Soil Survey Manual Ch.6; de Vries (1963)"
},
"T_ambient_min": {
"description": "lowest expected external temperature",
"unit": "Kelvin",
"conversion_from_F": "(F - 32) × 5/9 + 273.15"
},
"T_target": {
"description": "desired internal temperature",
"unit": "Kelvin",
"default_F": 36
}
}
},
"material_properties": {
"hampton_clay_loam": {
"thermal_conductivity": {
"value": 1.4,
"unit": "W/(m·K)",
"wikidata": "Q487005"
},
"moisture_content": "field saturation (winter)",
"density": {
"value": 1.6,
"unit": "g/cm³"
}
},
"alternative_substrates": {
"sand": {
"thermal_conductivity_range": [0.3, 0.5],
"unit": "W/(m·K)"
},
"pure_clay": {
"thermal_conductivity_range": [1.5, 2.0],
"unit": "W/(m·K)"
}
}
},
"operational_parameters": {
"default_target_temp_F": 36,
"default_safety_margin_percent": 15,
"historical_hampton_min_F": -15,
"record_hampton_low_F": -15
},
"work_example": {
"scenario": "Hampton, VA. Historical minimum: -15°F. Target: 36°F.",
"steps": [
"ΔT = (-15°F 36°F) = -51°F = -28.33 K",
"d_min = 0.15 m/K × 28.33 K = 4.25 meters",
"Converted: 4.25 m = 13.94 feet",
"Safety margin (15%): 16.03 feet"
],
"result_ft": 16.03
},
"assumptions": [
"Hampton clay-loam at field saturation (winter conditions)",
"Steady-state thermal equilibrium (long-duration cold snap)",
"No active heating or cooling systems",
"Structural integrity maintained by timber or reinforced brick"
],
"license": "CC0",
"machine_readable": true
}