💧Fluid Mechanics Unit 5 – Fluid Kinematics

Fluid kinematics explores how fluids move without considering the forces behind their motion. It's like watching a river flow or smoke rise, focusing on the patterns and paths they create rather than why they move that way. This unit covers key concepts like velocity fields, streamlines, and different ways to describe fluid motion. Understanding these basics helps us analyze everything from blood flow in our bodies to air currents around airplane wings.

Key Concepts and Definitions

  • Fluid kinematics studies the motion of fluids without considering the forces causing the motion
  • Lagrangian description tracks individual fluid particles as they move through space and time
  • Eulerian description focuses on specific locations in the fluid flow and the fluid properties at those locations over time
  • Velocity field represents the velocity vector at each point in a fluid flow at a given instant
  • Streamlines are curves that are tangent to the velocity vector at each point in a steady flow
    • Streamlines cannot cross each other in a steady flow
  • Pathlines trace the actual path traveled by a fluid particle over a period of time
  • Streaklines are the locus of fluid particles that have passed through a particular point in the flow

Fluid Properties and Behavior

  • Fluids are substances that deform continuously under the application of shear stress (liquids and gases)
  • Fluid density (ρ)(\rho) is the mass per unit volume of a fluid and varies with temperature and pressure
    • Incompressible fluids have constant density throughout the flow (water at low speeds)
    • Compressible fluids have density that varies significantly with pressure changes (air at high speeds)
  • Viscosity (μ)(\mu) is a measure of a fluid's resistance to deformation under shear stress
    • Newtonian fluids have a constant viscosity that is independent of the applied shear stress (water, air)
    • Non-Newtonian fluids have a viscosity that depends on the applied shear stress (blood, ketchup)
  • Surface tension is the result of cohesive forces between fluid molecules at the surface of a liquid
  • Capillary action occurs when adhesive forces between a liquid and a solid surface exceed the cohesive forces within the liquid, causing the liquid to rise in narrow spaces

Methods of Describing Fluid Motion

  • Lagrangian method tracks individual fluid particles as they move through space and time
    • Useful for understanding the behavior of individual particles in a flow
    • Difficult to apply in complex flows with many particles
  • Eulerian method focuses on specific locations in the fluid flow and the fluid properties at those locations over time
    • Useful for analyzing flow properties at fixed points in space
    • Commonly used in fluid mechanics and computational fluid dynamics (CFD)
  • Substantial derivative (DDt)(\frac{D}{Dt}) describes the rate of change of a fluid property (velocity, temperature) as a fluid particle moves through space and time
    • Includes both local (t)(\frac{\partial}{\partial t}) and convective (V)(\vec{V} \cdot \nabla) rates of change
  • Reynolds Transport Theorem relates the rate of change of a fluid property in a control volume to the net flux of that property across the control surface and any sources or sinks within the control volume

Velocity Fields and Flow Patterns

  • Velocity field V(x,y,z,t)\vec{V}(x, y, z, t) represents the velocity vector at each point in a fluid flow at a given instant
  • Uniform flow has a constant velocity magnitude and direction throughout the entire flow field
  • Non-uniform flow has a velocity that varies in magnitude and/or direction throughout the flow field
  • Steady flow has fluid properties (velocity, pressure, density) that do not change with time at any point in the flow
  • Unsteady flow has fluid properties that vary with time at one or more points in the flow
  • Laminar flow is characterized by smooth, parallel layers of fluid with no mixing between layers (low Reynolds numbers)
  • Turbulent flow is characterized by chaotic, irregular motion with mixing between fluid layers (high Reynolds numbers)
    • Eddies and vortices are common features of turbulent flows

Acceleration in Fluid Flow

  • Acceleration in fluid flow can be caused by changes in velocity magnitude (speed) and/or direction
  • Local acceleration (Vt)(\frac{\partial \vec{V}}{\partial t}) is the rate of change of velocity with respect to time at a fixed point in space
  • Convective acceleration (VV)(\vec{V} \cdot \nabla \vec{V}) is the rate of change of velocity due to the movement of a fluid particle to a new location with a different velocity
  • Total acceleration (DVDt)(\frac{D\vec{V}}{Dt}) is the sum of local and convective accelerations experienced by a fluid particle
    • DVDt=Vt+(V)V\frac{D\vec{V}}{Dt} = \frac{\partial \vec{V}}{\partial t} + (\vec{V} \cdot \nabla) \vec{V}
  • Streamline curvature can cause centripetal acceleration in a fluid flow
  • Pressure gradients and body forces (gravity) can also contribute to acceleration in fluid flows

Streamlines, Streaklines, and Pathlines

  • Streamlines are curves that are tangent to the velocity vector at each point in a steady flow
    • Streamlines represent the instantaneous direction of fluid motion at each point
    • Streamlines cannot cross each other in a steady flow
  • Streaklines are the locus of fluid particles that have passed through a particular point in the flow
    • Streaklines are formed by injecting a continuous stream of dye or smoke into a flow
    • In unsteady flows, streaklines can differ from streamlines and pathlines
  • Pathlines trace the actual path traveled by a fluid particle over a period of time
    • Pathlines are obtained by tracking the motion of individual fluid particles
    • In steady flows, pathlines, streaklines, and streamlines coincide
  • Timelines are a set of fluid particles that form a line at a given instant in time
    • Timelines are useful for visualizing the deformation and stretching of fluid elements over time

Conservation Laws in Fluid Kinematics

  • Conservation of mass (continuity equation) states that mass cannot be created or destroyed in a fluid flow
    • For incompressible flows: V=0\nabla \cdot \vec{V} = 0
    • For compressible flows: ρt+(ρV)=0\frac{\partial \rho}{\partial t} + \nabla \cdot (\rho \vec{V}) = 0
  • Conservation of momentum (Newton's second law) relates the acceleration of a fluid particle to the forces acting on it
    • Navier-Stokes equations are the fundamental equations of fluid motion based on conservation of momentum
  • Conservation of energy (first law of thermodynamics) states that energy cannot be created or destroyed, only converted from one form to another
    • Bernoulli's equation is a simplified form of the energy conservation equation for steady, inviscid, incompressible flows along a streamline
  • Circulation (Γ)(\Gamma) is a measure of the rotation of a fluid in a closed loop
    • Kelvin's circulation theorem states that circulation is conserved in an inviscid, barotropic fluid with conservative body forces

Applications and Real-World Examples

  • Aerodynamics: Study of the motion of air and its interaction with solid objects (aircraft wings, cars)
    • Lift and drag forces on airfoils and vehicles
    • Boundary layer separation and wake formation
  • Hydrodynamics: Study of the motion of liquids and their interaction with solid boundaries (ships, submarines)
    • Propulsion systems and hull design for marine vessels
    • Cavitation in pumps and propellers
  • Meteorology: Study of atmospheric motion and weather patterns
    • Wind velocity fields and pressure gradients
    • Cyclones, anticyclones, and jet streams
  • Cardiovascular system: Flow of blood through the heart, arteries, and veins
    • Pulsatile flow and pressure waves in arteries
    • Atherosclerosis and stenosis in blood vessels
  • Environmental fluid mechanics: Study of fluid motion in natural systems (oceans, rivers, atmosphere)
    • Dispersion of pollutants in air and water
    • Sediment transport and erosion in rivers and coastal areas


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© 2024 Fiveable Inc. All rights reserved.
AP® and SAT® are trademarks registered by the College Board, which is not affiliated with, and does not endorse this website.