Part of JME-09 — Fluid Mechanics: Pascal, Bernoulli & Viscosity

Fluid Statics Overview

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Fluid statics deals with fluids at rest. The fundamental equation is P=P0+ρghP = P_0 + \rho gh, which gives pressure at depth hh below the surface. This pressure depends only on depth — not on the container's shape, size, or the total volume of fluid (hydrostatic paradox). Atmospheric pressure P01.013×105P_0 \approx 1.013 \times 10^5 Pa supports a 10.3 m water column or a 760 mm mercury column.

Pascal's Law states that pressure changes in an enclosed incompressible fluid are transmitted undiminished throughout. This enables hydraulic machines: a small force on a small piston creates a proportionally larger force on a larger piston, with mechanical advantage =A2/A1= A_2/A_1. Energy is conserved — the larger force acts over a smaller distance.

Archimedes' Principle provides the buoyant force: FB=ρfVsubgF_B = \rho_f V_{\text{sub}} g (weight of displaced fluid). A body floats when its density is less than the fluid's, with fraction submerged =ρbody/ρfluid= \rho_{\text{body}}/\rho_{\text{fluid}}. Apparent weight = true weight minus buoyant force. These principles govern floating bodies, submarines, hot air balloons, and hydrometers.

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