Bernoulli’s Equation Study Pack

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Last updated May 27, 2026

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Bernoulli’s Equation Study Guide

Master the relationship between fluid speed, pressure, and height using Bernoulli's equation (P + ½ρv² + ρgh = constant), the continuity equation, and Torricelli's theorem — plus the key assumptions that define when the equation applies.

Key Takeaways

  • Bernoulli's equation expresses conservation of energy for a steadily flowing, incompressible, non-viscous fluid: P + ½ρv² + ρgh = constant along any streamline.
  • Each term in Bernoulli's equation represents a form of energy per unit volume — pressure energy, kinetic energy, and gravitational potential energy — and their sum remains constant as a fluid moves.
  • When fluid speeds up through a constricted region (as described by the continuity equation A₁v₁ = A₂v₂), pressure must drop to conserve the total energy, producing the inverse relationship between fluid speed and static pressure.
  • Bernoulli's equation applies only under four conditions: steady (non-turbulent) flow, incompressible fluid, negligible viscosity, and measurement along a single streamline.
  • Torricelli's theorem — the speed of fluid exiting a hole in a tank equals √(2gh), where h is the depth below the surface — is a direct derivation of Bernoulli's equation.
  • Real fluids deviate from Bernoulli predictions because viscosity dissipates mechanical energy as heat, and turbulence converts organized flow energy into chaotic motion.

Foundations: Energy in a Moving Fluid

To understand Bernoulli's equation, it helps to first recognize what physical quantities govern a fluid in motion and how the principle of energy conservation applies to flowing matter.

Energy Forms Present in a Flowing Fluid

  • Pressure energy (P) arises because a fluid under pressure can do work on adjacent fluid or on a boundary surface; it has units of joules per cubic meter (J/m³), equivalent to pascals.
  • Kinetic energy per unit volume (½ρv²) depends on the fluid's mass density ρ (kg/m³) and the local flow speed v (m/s); faster-moving fluid carries more kinetic energy.
  • Gravitational potential energy per unit volume (ρgh) depends on density, gravitational acceleration g, and the height h of the fluid element above a chosen reference level.

Conservation Principle Behind the Equation

  • In an ideal fluid, no energy is lost to friction or heat, so the total energy per unit volume at one location along a streamline equals the total at any other location.
  • This is not a new law — it is simply the work-energy theorem applied to a small parcel of fluid as it travels from one point to another.
  • Mathematically: P₁ + ½ρv₁² + ρgh₁ = P₂ + ½ρv₂² + ρgh₂, where subscripts 1 and 2 denote two different positions along the same streamline.

Assumptions and Valid Conditions for Bernoulli's Equation

Bernoulli's equation is a powerful tool, but it carries strict physical assumptions that define when it can and cannot be applied.

Steady Flow Requirement

  • Steady flow means the velocity at every fixed point in the fluid does not change with time; individual fluid parcels may speed up or slow down as they move, but the overall pattern remains constant.
  • Turbulent or pulsating flow (such as water just past a sharp obstruction) violates this condition and makes Bernoulli's equation unreliable.

Incompressibility Requirement

  • An incompressible fluid has constant density regardless of pressure changes; most liquids satisfy this well, and gases satisfy it when flow speeds remain well below the speed of sound (Mach < 0.3).
  • Compressible flow — as in supersonic aerodynamics — requires modified equations that account for density changes.

Inviscid (Non-Viscous) Flow Requirement

  • Viscosity is internal friction between fluid layers; in a viscous fluid, mechanical energy converts to thermal energy, meaning the Bernoulli sum decreases downstream.
  • Water and air are often treated as inviscid for approximate calculations, but thick fluids like honey or oil require viscosity-corrected models.

Streamline Restriction

  • Bernoulli's equation holds along a single streamline — the path traced by a fluid parcel — and cannot be directly applied across streamlines unless additional conditions (like irrotational flow) are met.

The Continuity Equation and Its Relationship to Pressure Changes

Bernoulli's equation becomes most useful when paired with the continuity equation, which constrains how fluid speed changes as cross-sectional area changes.

The Continuity Equation for Incompressible Flow

  • For an incompressible fluid in a pipe, the volumetric flow rate Q = Av must remain constant, where A is cross-sectional area and v is flow speed.
  • This gives A₁v₁ = A₂v₂: where the pipe narrows, flow speed increases, and where the pipe widens, flow speed decreases.

Pressure Drop in a Constriction (Venturi Effect)

  • When a fluid accelerates through a narrow section, its kinetic energy per unit volume (½ρv²) increases; because the total Bernoulli sum is constant, the static pressure P must decrease by an equal amount.
  • This counterintuitive result — faster flow means lower pressure — is called the Venturi effect and underlies devices like the Venturi meter, carburetors, and atomizer sprays.
  • A Venturi meter uses two pressure gauges placed at wide and narrow sections of a pipe; the measured pressure difference directly reveals the flow speed through the narrow section via rearranging Bernoulli's equation.

Horizontal Flow Simplification

  • When flow is horizontal (h₁ = h₂), the gravitational terms cancel, reducing Bernoulli's equation to P₁ + ½ρv₁² = P₂ + ½ρv₂², making speed-pressure trade-offs especially transparent.

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Created by Kibin to help students review key concepts, prepare for exams, and study more effectively. This Study Pack was checked for accuracy and curriculum alignment using authoritative educational sources. See sources below.

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