{ "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 }