Fast gradient results for wells, tanks, and risers. Switch between metric and field units easily. Validate inputs, review tables, export CSV and PDF files.
| Fluid | SG | Density (kg/m³) | Gradient (kPa/m) | Gradient (psi/ft) | At 100 m, ΔP (kPa) |
|---|---|---|---|---|---|
| Fresh water | 1.000 | 1,000 | 9.807 | 0.433 | 980.7 |
| Sea water | 1.025 | 1,025 | 10.052 | 0.444 | 1,005.2 |
| Light oil | 0.850 | 850 | 8.336 | 0.368 | 833.6 |
| Brine | 1.200 | 1,200 | 11.768 | 0.520 | 1,176.8 |
The calculator uses the hydrostatic relation for a constant-density fluid: ΔP = ρ · g · Δz.
Note: This tool applies a linear, incompressible assumption. For highly compressible gases, use a real-gas model.
For an incompressible fluid, the pressure change follows ΔP = ρ·g·Δz. With fresh water (ρ≈1000 kg/m³, g≈9.80665 m/s²), the gradient is about 9.81 kPa/m, which is near 0.433 psi/ft in field units. At 100 m, water adds roughly 0.981 MPa (about 9.81 bar). This calculator reports the gradient and the resulting pressure change for any entered depth or height difference.
Engineering teams often mix meters with feet, and kPa with psi. The form converts all inputs to SI internally, then converts results back to your selected output units. Use kPa/m or bar/m for process and piping work, and psi/ft for drilling and production checks. MPa output is useful when comparing to casing or valve ratings. Conversions are consistent across ΔP, pressure at depth, and gradient outputs.
Density is best when lab data is available. Specific gravity is common for quick material selection; the tool assumes water density of 1000 kg/m³ and computes ρ = SG·1000. Unit weight is used in civil and geotechnical work; the tool converts γ to N/m³ and applies ρ = γ/g. Each method produces the same gradient when values are equivalent. If temperature or salinity changes, update ρ or SG to match your operating condition.
Reference pressure P₀ lets you compute absolute pressure at the target depth: P = P₀ + ΔP. Choose “Downward” when moving deeper in a liquid column, and “Upward” for elevation gain where pressure drops. In “Pressure difference” mode, ΔP is highlighted for quick comparison between two elevations. In “Gradient only” mode, P₀ is hidden because it does not affect dP/dz.
Use the example table to sanity-check outputs: seawater (SG≈1.025) gives roughly 10.05 kPa/m, and light oil (SG≈0.85) gives about 8.34 kPa/m. Concentrated brines can exceed 11.7 kPa/m, driving higher hydrostatic heads in deep wells. Very large depths can imply high pressures; confirm vessel ratings and relief settings. For gases, density varies strongly with pressure and temperature, so a compressible model is recommended for accuracy. Document assumptions in your calculation notes.
It is the rate of pressure change per unit depth, dP/dz. For a constant-density liquid, it equals ρ·g and remains constant along a vertical column.
Use Upward when elevation increases from the reference point, such as flow up a riser. The calculator applies a negative sign so pressure decreases with height.
Use density when you have measured data at operating conditions. Use specific gravity for quick estimates; the tool converts SG to density using 1000 kg/m³ as the water reference.
Real systems include temperature effects, gas entrainment, friction losses, and transient flow. This tool calculates hydrostatic change only, so combine it with friction and equipment losses for total pressure drop.
It is a common shortcut: 0.433 psi/ft at SG=1. It is close for many liquids but still assumes constant density and standard gravity, so use the full unit conversion for precise work.
This page exports the current case to CSV or PDF. For batch studies, run several inputs and download each report, or copy the CSV outputs into a spreadsheet for comparison.
Important Note: All the Calculators listed in this site are for educational purpose only and we do not guarentee the accuracy of results. Please do consult with other sources as well.