🌊
Nautilus-1Lv 1.1
💬“Hydrostatic Pressure (P = rho * g * h) & Challenger Deep: Hydrostatic pressure increases linearly with depth according to P = P_surface + rho * g * h. Because seawater density is approximately 1,025 kg/m^3, every 10 meters of descent adds roughly 1 atmosphere (101.3 kPa or 14.7 psi) of pressure. At the bottom of the Mariana Trench (depth h ≈ 10,928 meters), absolute hydrostatic pressure reaches an astonishing 108.6 MPa (15,750 psi)—over 1,070 times atmospheric pressure at sea level. Any unpressurized air pocket instantly implodes with explosive supersonic force.”
🫧10,928m Trench🛡️1,086 Bar Hull⚖️Trim Ballast✓ 0/5 Done
🌊🎯 Mission BriefingAct 1 • Stage 1.1 • +160 XP
Hydrostatic Pressure (P = rho * g * h) & Challenger Deep
Hydrostatic pressure increases linearly with depth according to P = P_surface + rho * g * h. Because seawater density is approximately 1,025 kg/m^3, every 10 meters of descent adds roughly 1 atmosphere (101.3 kPa or 14.7 psi) of pressure. At the bottom of the Mariana Trench (depth h ≈ 10,928 meters), absolute hydrostatic pressure reaches an astonishing 108.6 MPa (15,750 psi)—over 1,070 times atmospheric pressure at sea level. Any unpressurized air pocket instantly implodes with explosive supersonic force.
🌟 Starting Stage (1.1)