Fluids Flashcards

1
Q

Which forces are supported in fluids?

A
  • tension is not supported
  • compression is supported and results in a small elastic deformation
  • shear is supported but results in flow
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2
Q

du/dx + dv/dy + dw/dz = 0

A

all flux in all three directions must equal to zero
mass must be concerved

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3
Q

In which direction of pressure change is fluid driven?

A

From high to low pressure

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4
Q

τ = F/A

A

Shear stress= force/area

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5
Q

τ= μ δu/δy

A

Shear stress = dynamic viscosity * (velocity/ depth)

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6
Q

What is the shear stress in viscous flow?

A

No longer zero

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7
Q

Kinematic viscosity?

A

ν=μ/ρ (m^2/ s)

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8
Q

Dynamic viscosity?

A

μ (kg/ms)

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9
Q

What navier stokes simplification can you make by assuming the flow to be steady?

A

All time derivatives will be zero (d/dt)=0

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10
Q

What navier stokes simplification can you make by assuming the flow to be fully developed?

A

The velocity component in the x-direction will remain constant (du/dx = 0)

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11
Q

What navier stokes simplifications can you make when the sides are incredibly long. (Flow in one direction, boundaries in another)?

A

No flow in the the third direction and no effect by the boundaries.
W=0
d/dz=0

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12
Q

What simplification to navier stokes equations by assuming its laminar flow?

A

The gradient of v is zero and v is zero at the boundary, v must be zero everywhere. (V is in the y direction)

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13
Q

Re= ρUL/μ

A

Inertial forces/ viscous forces
Reynolds number= densityvelocity scale length scale/ dynamic viscosity

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14
Q

What are Reynolds numbers for laminar flow?

A

Re < Recrit

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15
Q

What Reynold numbers are turbulent flow?

A

Re> Recrit

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16
Q

Q= π/4 D^2 U

A

Volume flux= π/4 * diameter^2 * velocity

(Only for uniform flow)

17
Q

What is Q along a pipe?

A

Constant

18
Q

What is M along a pipe

A

Momentum is constant along a pipe

19
Q

M= π/4 D^2 U^2 = QU

A

Momentum = π/4 * diameter ^2 * velocity ^2

20
Q

Hydraulic grade line?

A

Represents piezometric head (h)

21
Q

Energy grade line?

A

Represents total head line (H)

22
Q

Piezometric head?

A

Pressure head + gravitational head combined

23
Q

p1/ρg + z1 = p2/ρg + z2 + τ0PL/ ρgA

A

p= pressure
ρ= density
g= gravitational acceleration
z= height
τ0= shear stress
P= wetted perimeter
L= length
A= area

24
Q

τ0= f/8 ρ U^2
where
f=f(Re,ks/D)

A

Shear stress = function of Reynolds and relative roughness * density * velocity^2/8

25
Q

In what conditions is f= 64/Re

A

For laminar flow/ Re< 2300

26
Q

In what condition is 1/f^(1/2) = -2log10[k/D/3.71 + 2.51/Re*f^(1/2)]

A

For turbulent flow/ for Re> 4000

27
Q

When is 1/f^(1/2)= 2log10[Ref^(1/2)] -0.8

A

For turbulent flow in smooth pipes/ for Re>4000

28
Q

hL = εU^2/2*g

A

minor head loss= loss coefficient* velocity^2/2*gravitational acceleration

29
Q

ε= (1-Α1/A2)^2

A

Loss coefficient for sudden pipe enlargement = (1-small area before/ small area after)^2

30
Q

RH= A/P

A

Hydraulic radius= flow area/ wetted perimeter

31
Q

hf= f* L/4RH * U^2/2*g

A

head loss= function * length/4hydraulic radius * velocity^2/2gravitational acceleration

32
Q

Entry length?

A

Region where boundary layer develops

33
Q

Does laminar or turbulent flow boundary layers take longer to develop?

A

It takes longer for laminar pipe flow boundary layers to develop with longer entry lengths

34
Q

Fully developed flow?

A

When boundary layers converges to pipe centreline

35
Q

How does shear stress vary across a pipe?

A

Linearly with being 0 at the centreline

36
Q

What effect of shear force have a long a plate?

A

The effect of shear force increases along a plate, increasing the thickness of fluid layer that is affected. Reynolds number also increases along a plate leading to turbulent flow conditions.

There’s a laminar region, transition region and then turbulent region

37
Q

u/u* = u*y/ ν

A

u= velocity
u* = wall shear velocity
ν= velocity viscosity
y= depth/ distance from sublayer

This works when yu*/ν is between 0 and 3~5

38
Q

Sublayer thickness = (3-5) ν/ u*

A

ν= velocity viscosity
u* = wall shear velocity