Engineer‑grade hydrostatic pressure calculations: P = ρ·g·h. Real‑time multi‑unit display and reverse depth.
Fundamental equation: P = ρ·g·h (gauge pressure). Absolute pressure = P0 + ρgh, where P0 is surface pressure.
Consider a column of fluid of density ρ, height h, and cross‑sectional area A. The weight of the fluid is W = ρ·g·h·A. This weight is supported by the pressure difference between bottom and top: (Pbottom – Ptop)·A = ρ·g·h·A. Hence Pbottom – Ptop = ρgh. If the top is open to atmosphere, Ptop = Patm, then absolute pressure at depth h is Pabs = Patm + ρgh.
Gauge pressure is the pressure relative to atmospheric pressure: Pgauge = ρgh. Most engineering sensors (e.g., tire pressure gauges) measure gauge pressure. Absolute pressure includes atmospheric pressure and is used in thermodynamics and deep‑sea applications.
This calculator implements the exact formula P = ρgh with unit conversions traceable to SI standards:
For water at 4 °C (ρ = 1000 kg/m³, g = 9.80665 m/s²), pressure at 10 m depth is 98 066.5 Pa ≈ 0.9807 bar, matching oceanographic reference tables.
For liquids, density is nearly constant, so the linear formula holds up to thousands of meters (water compresses only ~1.8% at 4000 m). For gases, ρ varies with pressure; use the ideal gas law for accurate pressure‑depth profiles in air.
Key takeaway: Hydrostatic pressure increases by about 9.81 kPa per meter of freshwater column (or 1 atm per 10.3 m of water). This calculator provides fast, trustworthy results for engineering, education, and design.