CHAPTER 3. Elementary Fluid Dynamics

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Transcription:

CHAPTER 3. Elementary Fluid Dynamics - Understanding the physics of fluid in motion - Derivation of the Bernoulli equation from Newton s second law Basic Assumptions of fluid stream, unless a specific comment 1 st assumption: Inviscid fluid (Zero viscosity = Zero shearing stress) No force by wall of container and boundary Applied force = Only Gravity + Pressure force Newton s Second Law of Motion of a Fluid Particle (Net pressure force) + (Gravity) = (Fluid mass) (Acceleration) 2 nd assumption: Steady flow (?) No Change of flowing feature with time at a given location Every successive particle passing though the same point : Same path (called streamline) & Same velocity (tangential to the streamline)

Additional Basic Terms in Analysis of Fluid Motion Streamline (Path of a fluid particle) - Position of a particle = where : Initial position, : Velocity of particle - No streamlines intersecting each other Two Components in Streamline Coordinates (See the figure) 1. Tangential coordinate: : Moving distance along streamline, : Related to Particle s speed 2. Normal coordinate: : Local radius of curvature of streamline : Related to Shape of the streamline Two Accelerations of a fluid particle along s and n coordinates 1. Streamwise acceleration ( Change of the speed) using the Chain rule 2. Normal acceleration ( Change of the direction) (: Centrifugal acceleration)

Q. What generate these a s and a n? (Pressure force and Gravity) Part 1. Newton s second law along a streamline ( direction) Consider a small fluid particle of size as shown : Forces acting on a fluid particle δs δn δy Newton s second law in direction along direction = Gravity force + Net Pressure force where : Volume of a fluid particle =

(i) Gravity force along direction (ii) Pressure force along direction Let p: Pressure at the center of : Average pressures at Left face (Decrease) : Average pressures at Right face (Increase) Then, Net pressure force along direction, (Pressure) (Area) : Depends not on p itself, but on (Rate of change in p) Total force in direction (Streamline) Finally, Newton s second law along a streamline ( direction) Change of Particle s speed Affected by Weight and Pressure Change

Making this equation more familiar = - because (See the figure above) using (why?) = or (Divided by ds) or constant (By integration) By assuming a constant (Incompressible fluid): 3 rd assumption Constant along streamline ( direction) : Bernoulli equation along a streamline Valid for (1) a steady flow of (2) incompressible fluid (3) without shearing stress c.f. If is not constant (Compressible, e.g. Gases), : Must be known to integrate.

What this Bernoulli Equation means? (Physical Interpretation) For a Steady flow of Inviscid and Incompressible fluid, Constant along streamline (1) : Mathematical statements of Work-energy principle Unit of Eq. (1): [N/m 2 ] = [N m/m 3 ] = [Energy per unit volume] p = Works on unit fluid volume done by pressure = Works on unit fluid volume done by weight Kinetic energy per unit fluid volume Same Bernoulli Equations in different units 1. Eq (1) γ [N m/m 3 ] [N m/m 3 ] = [m] = [Length unit] + + z = Constant (Head unit) : Depth of a fluid column produce p (Pressure head) : Height of a fluid particle to reach v from rest by free falling (Velocity head) z: Height corresponding to Gravitational potential (Elevation head)

Part 2. Newton s second law normal to a streamline ( direction) Consider the same situation as Sec. 3.3 shown in figure For a small fluid particle of size as shown : Forces acting on a fluid particle δs δn δy Newton s second law in direction along direction = Gravity force + Net Pressure force

(i) Gravity force along direction (ii) Pressure force along direction By the same manner in the previous case, Total force in direction (Normal to Streamline) normal to streamline ( direction) Change of Particle s direction of motion Affected by Weight and Pressure Change along Ex. If a fluid flow: Steep direction change (R ) or fast flow (v ) or heavy ( ) fluid Generate large force unbalance Special case: Standing close to a Tornado i.e. Gas flow (Negligible ) in horizontal motion ( = 0) (Attractive) : Moving closer (R ) More dangerous ( )

Making this equation more familiar By the same manner as the previous case, because (See the figure) =, since or = Constant (normal to streamline) By assuming a constant (Incompressible fluid): 3 rd assumption = Constant (normal to streamline) : Bernoulli equation normal to streamline ( direction) Valid for (1) a steady flow of (2) incompressible fluid (3) without shearing stress