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Fluid Mechanics Formulas

Complete collection of fluid mechanics formulas with detailed explanations.

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Fluid Properties

Density

ρ=mV\rho = \frac{m}{V}

Density equals mass divided by volume.

Notation:

ρ:Density
m:Mass
V:Volume

Units:

ρ:kg/m³
m:kg
V:m³

Applications:

  • •Fluid characterization
  • •Buoyancy calculations
  • •Flow measurements

Limitations:

Homogeneous fluid

Pressure

P=FAP = \frac{F}{A}

Pressure equals force divided by area.

Notation:

P:Pressure
F:Force
A:Area

Units:

P:Pa (N/m²)
F:N
A:m²

Applications:

  • •Hydraulic systems
  • •Atmospheric pressure
  • •Fluid flow

Limitations:

Normal force only

Viscosity

τ=μdudy\tau = \mu\frac{du}{dy}

Shear stress equals dynamic viscosity times velocity gradient.

Notation:

τ:Shear stress
μ:Dynamic viscosity
du/dy:Velocity gradient

Units:

τ:Pa
μ:Pa·s
du/dy:s⁻¹

Applications:

  • •Fluid flow resistance
  • •Lubrication
  • •Drag calculations

Limitations:

Newtonian fluids

Kinematic Viscosity

ν=μρ\nu = \frac{\mu}{\rho}

Kinematic viscosity equals dynamic viscosity divided by density.

Notation:

ν:Kinematic viscosity
μ:Dynamic viscosity
ρ:Density

Units:

ν:m²/s
μ:Pa·s
ρ:kg/m³

Applications:

  • •Reynolds number
  • •Flow similarity
  • •Fluid dynamics

Limitations:

Incompressible fluid

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Hydrostatics

Hydrostatic Pressure

P=P0+ρghP = P_0 + \rho gh

Pressure at depth equals atmospheric pressure plus density times gravitational acceleration times depth.

Notation:

P:Pressure at depth
P₀:Atmospheric pressure
ρ:Density
g:Gravitational acceleration
h:Depth

Units:

P, P₀:Pa
ρ:kg/m³
g:9.81 m/s²
h:m

Applications:

  • •Underwater pressure
  • •Dam design
  • •Submarine operations

Limitations:

Incompressible fluid

Buoyant Force

Fb=ρfVfgF_b = \rho_f V_f g

Buoyant force equals fluid density times displaced volume times gravitational acceleration.

Notation:

F_b:Buoyant force
ρ_f:Fluid density
V_f:Displaced volume
g:Gravitational acceleration

Units:

F_b:N
ρ_f:kg/m³
V_f:m³
g:9.81 m/s²

Applications:

  • •Floating objects
  • •Ship design
  • •Submarine buoyancy

Limitations:

Static equilibrium

Archimedes' Principle

Fb=WdisplacedF_b = W_{displaced}

Buoyant force equals weight of displaced fluid.

Notation:

F_b:Buoyant force
W_displaced:Weight of displaced fluid

Units:

F_b, W_displaced:N

Applications:

  • •Floating bodies
  • •Density measurements
  • •Buoyancy calculations

Limitations:

Static conditions

Pascal's Principle

F1A1=F2A2\frac{F_1}{A_1} = \frac{F_2}{A_2}

Pressure is transmitted equally in all directions in a confined fluid.

Notation:

F₁, F₂:Forces
A₁, A₂:Areas

Units:

F₁, F₂:N
A₁, A₂:m²

Applications:

  • •Hydraulic lifts
  • •Brake systems
  • •Pressure transmission

Limitations:

Incompressible fluid

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Fluid Dynamics

Continuity Equation

A1v1=A2v2A_1v_1 = A_2v_2

Volume flow rate is constant in a pipe with varying cross-sectional area.

Notation:

A₁, A₂:Cross-sectional areas
v₁, v₂:Velocities

Units:

A₁, A₂:m²
v₁, v₂:m/s

Applications:

  • •Pipe flow
  • •Nozzle design
  • •Flow rate calculations

Limitations:

Incompressible flow

Bernoulli's Equation

P1+12ρv12+ρgh1=P2+12ρv22+ρgh2P_1 + \frac{1}{2}\rho v_1^2 + \rho gh_1 = P_2 + \frac{1}{2}\rho v_2^2 + \rho gh_2

Total energy per unit volume is constant along a streamline.

Notation:

P₁, P₂:Pressures
ρ:Density
v₁, v₂:Velocities
g:Gravitational acceleration
h₁, h₂:Heights

Units:

P₁, P₂:Pa
ρ:kg/m³
v₁, v₂:m/s
g:9.81 m/s²
h₁, h₂:m

Applications:

  • •Aerodynamics
  • •Venturi meters
  • •Flow measurement

Limitations:

Ideal fluid, steady flow

Reynolds Number

Re=ρvDμRe = \frac{\rho vD}{\mu}

Reynolds number equals density times velocity times diameter divided by dynamic viscosity.

Notation:

Re:Reynolds number
ρ:Density
v:Velocity
D:Characteristic length
μ:Dynamic viscosity

Units:

Re:dimensionless
ρ:kg/m³
v:m/s
D:m
μ:Pa·s

Applications:

  • •Flow regime determination
  • •Turbulence prediction
  • •Similarity analysis

Limitations:

Characteristic length scale

Poiseuille's Law

Q=πr4ΔP8μLQ = \frac{\pi r^4\Delta P}{8\mu L}

Volume flow rate equals π times radius to fourth power times pressure difference divided by 8 times viscosity times length.

Notation:

Q:Volume flow rate
r:Radius
ΔP:Pressure difference
μ:Dynamic viscosity
L:Length

Units:

Q:m³/s
r:m
ΔP:Pa
μ:Pa·s
L:m

Applications:

  • •Blood flow
  • •Pipe flow
  • •Capillary flow

Limitations:

Laminar flow, circular pipe

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Advanced Fluid Mechanics

Drag Force

FD=12CDρAv2F_D = \frac{1}{2}C_D\rho Av^2

Drag force equals half drag coefficient times density times area times velocity squared.

Notation:

F_D:Drag force
C_D:Drag coefficient
ρ:Density
A:Cross-sectional area
v:Velocity

Units:

F_D:N
C_D:dimensionless
ρ:kg/m³
A:m²
v:m/s

Applications:

  • •Aerodynamics
  • •Vehicle design
  • •Wind resistance

Limitations:

Steady flow

Stokes' Law

FD=6πμrvF_D = 6\pi\mu rv

Drag force on a sphere equals 6π times viscosity times radius times velocity.

Notation:

F_D:Drag force
μ:Dynamic viscosity
r:Radius
v:Velocity

Units:

F_D:N
μ:Pa·s
r:m
v:m/s

Applications:

  • •Particle settling
  • •Sedimentation
  • •Microfluidics

Limitations:

Small Reynolds number

Surface Tension

γ=FL\gamma = \frac{F}{L}

Surface tension equals force divided by length.

Notation:

γ:Surface tension
F:Force
L:Length

Units:

γ:N/m
F:N
L:m

Applications:

  • •Capillary action
  • •Bubble formation
  • •Wetting phenomena

Limitations:

Liquid-gas interface

Capillary Rise

h=2γcos⁡θρgrh = \frac{2\gamma\cos\theta}{\rho gr}

Capillary rise equals twice surface tension times cosine of contact angle divided by density times gravitational acceleration times radius.

Notation:

h:Capillary rise
γ:Surface tension
θ:Contact angle
ρ:Density
g:Gravitational acceleration
r:Radius

Units:

h:m
γ:N/m
θ:radians
ρ:kg/m³
g:9.81 m/s²
r:m

Applications:

  • •Soil moisture
  • •Paper chromatography
  • •Microfluidics

Limitations:

Small diameter tubes