A hydrostatic-density scan varies fluid density across three rows at fixed depth, showing how pressure p = rho * g * h rises with density row by row. The arithmetic is exact only for the stated densities, depths, pressures, and rows in the ideal static incompressible-fluid model. Real measurements add viscosity, turbulence, compressibility, pipe/container geometry, calibration, elevation reference, finite precision, and measurement uncertainty.
Density changes pressure while depth and gravity stay fixed. Exact arithmetic here means exact results for the stated model inputs; measured inputs still carry uncertainty and significant-figure limits.
highlighted = computed this step
Light fluid gives thirty pascals
Depth h=3 m and gravity g=10 metres per second squared stay fixed. Density rho=1 kilogram per cubic metre gives pressure 30 pascals.
ΔP=1×10×3=30
Double density doubles the pressure
Depth h=3 m and gravity g=10 metres per second squared stay fixed. Density rho=2 kilograms per cubic metre gives pressure 60 pascals.
ΔP=2×10×3=60
Dense fluid triples the light reading
Depth h=3 m and gravity g=10 metres per second squared stay fixed. Density rho=3 kilograms per cubic metre gives pressure 90 pascals.