Showing posts with label Fluid Mechanics. Show all posts
Showing posts with label Fluid Mechanics. Show all posts

Thursday, 10 May 2018

Dimensionless Numbers in Fluid Thermal Engineering


Important dimensionless numbers used in fluid mechanics and heat transfer are given below:-



Dimensionless
Number

 Expression

             Significance



Reynolds Number


$Re =\frac{ρUD}{μ}$ 
  • Re = Inertial force / Viscous force
  • Determines flow is Laminar, Turbulent, or Transient Flow.



Fourier Number




$Fo = \frac{αt}{L^2}$
  • It is a measure of heat conducted through a body relative to heat stored.
  • Larger the Fo, faster propagation of heat through a body
  • It can also be viewed as current time to the time taken to reach steady state



Biot Number


$Bi = \frac{hL}{K_s} = \frac{L/K_s}{1/h}$

  • Ratio of Conductive resistance with in the body to Convection resistance at the surface of the body
  • Bi ≤ 0.1, Lumped system analysis (assumes a uniform temperature distribution throughout the body) is applicable



Nusselt Number


$Nu = \frac{hL}{K_f} = \frac{h ΔT}{K_fΔT/L} = \frac{q_{conv}}{q_{cond}}$

  • Ratio of convective HT to conductive HT coefficient across the boundary layer 
  • The larger the Nu, the more effective the convection. 
  • Used to calculate heat transfer coefficient h


Prandtl Number



$Pr = \frac{ν}{α}= \frac{µC_p}{K}$
  • Ratio of momentum diffusivity to thermal diffusivity
  • Determines ratio of fluid/thermal Boundary layer thickness
  • ${Pr}^{1/3} = \frac{δ_f}{δ_t}$



Grashof Number




$Gr = \frac{gβΔTL^3}{ν^2}$
  • Ratio of natural convection buoyancy force to viscous force
  • $\frac{Gr}{Re^2} << 1  \implies$ forced convection
  • $\frac{Gr}{Re^2} >> 1  \implies$ Natural convection
  • $\frac{Gr}{Re^2} ≈1  \implies$ mixed convection

Peclet Number


$Pe = Re*Pr = \frac{UL}{α}$
  • Ratio of convective to diffusive heat transport in a fluid
  • Used to determine plug flow/perfect mixing (CSTR) continuous flow model validity


Stanton Number


$St = \frac{h}{ρUC_p} = \frac{Nu}{Pe} = \frac{Nu}{RePr}$

  • Ratio of heat transferred to the fluid to the heat capacity of the fluid.
  • Used to characterize heat transfer in forced convection flows.

Rayleigh Number


$Ra = Gr*Pr = \frac{gβΔTL^3}{αν}$
  • It is product of Gr and Pr.
  • Determines natural convection boundary layer is laminar or turbulent.

Jakob Number


$Ja = \frac{C_p(T_s - T_{sat})}{h_{fg}}$
  • Ratio of sensible heat to latent heat absorbed (or released) during the phase change process.


Bond Number


$Bo = \frac{gL^2Δρ}{σ}$
  • Ratio of gravitational force to surface tension force
  • Used to characterize the shape of bubble or drops moving in a surrounding fluid. 


Froude Number

$Fr = \frac{U^2}{gL}$
  • Ratio of Inertia force to Gravitational force
  • Often the term Froude number is used for the ratio $\frac{u}{\sqrt{gL}}$.

Euler Number

$Eu = \frac{Δp}{ρU^2}$
  • Ratio of pressure force to inertia force.
  • Used for analyzing fluid flow dynamics problems in which the pressure difference, are interest

Weber number


$We = \frac{ρU^2L}{σ}$
  • Ratio of Inertia force to surface tension force.
  • Used for analyzing fluid flow dynamics problems in which surface tension is important

Nomenclature:


μ → viscosity of fluid
ν → kinematic viscosity of fluid 
ρ → density of fluid
U → characteristic velocity scale
D → characteristic Diameter = 4A/P
α → thermal diffusivity of fluid 
t  → time
L → characteristic length scale 
Cp → specific heat at constant pressure
h → heat transfer coefficient
K → thermal conductivity of fluid
Kf → thermal conductivity of fluid
Ks → thermal conductivity of solid 
g → gravitational acceleration 
β → volumetric thermal expansion coefficient 
ΔT → characteristic temperature difference 
Tsat → saturation temperature
Ts → surface temperature 
hfg → latent heat of condensation
Δρ → difference in density of the two phases 
σ   → surface tension
Δp → characteristic pressure difference of flow
δf  → Fluid boundary layer thickness
δ → Thermal boundary layer thickness



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Wednesday, 14 March 2018

Fluid Kinematics

Fluid kinematics involves velocity, acceleration of the fluid, description and visualisation of fluid motion without considering forces that produce motion. There are two general approaches in analysis fluid mechanics:

  1. Eulerian Approach: Fluid motion is given by prescribing the necessary properties (p, V, T etc) in terms of space and time. 
  2. Lagrangian Approach: Information of the fluid in terms of what happens at fixed points in space. 

  • Steady Flow: A flow is said to be steady if fluid properties do not vary with respect to time.
  • Unsteady Flow: Fluid properties vary with time.
  • Uniform Flow: if fluid properties do not change point to point at any instant of time.
  • Non-Uniform flow: When fluid properties changes from point to point at any instant of time, flow is defined as non-uniform flow.
  • Laminar flow: Fluid particles moves in layers or lamina. No mixing in normal direction.
  • Turbulent Flow: Fluid particles have random movement, intermixing in layers.
  • Incompressible Flow: Density variation is negligible.

Stream Line

An imaginary line or curve such that it is tangent to the velocity field at a given instant, given 
Equation of streamline is given by:
\[\frac{dx}{u} = \frac{dy}{v} = \frac{dz}{w}\]
for 2D flow : vdx - udy = 0

Path Line

It is the path traced by a single fluid particle at different instant of time. 

Streak Line 

It is defined as locus of various fluid particles that have passed through a fixed point.

NOTE: In steady flow, streakline, pathline and streamline are identical.


Continuity Equation (Conservation of mass)

\[ρAV = Constant\]
where, ρ = Density
A = Area
V = Velocity

For incompressible fluid it reduces to $A_1V_1 = A_2V_2$.

Generalised Continuity Equation

\[\frac{\partial ρ}{\partial t} + \frac{\partial (ρ u)}{\partial x} + \frac{\partial (ρ v)}{\partial y} +\frac{\partial (ρw)}{\partial z} = 0\]
where u,v,w are component of velocity in x, y, z direction.

  • If flow is steady $\frac{\partial ρ}{\partial t} = 0$.
  • For steady, imcompressible flow continuity equation $\boxed{\frac{\partial u}{\partial x} + \frac{\partial v}{\partial y} +\frac{\partial w}{\partial z} = 0}$.

Total acceleration of fluid

\[\frac{D\vec{V}}{Dt} = a_x i + a_y j + a_z k = \frac{Du}{Dt}i + \frac{Dv}{Dt}j + \frac{Dw}{Dt}k\]

$\frac{D}{Dt}$ is called Material Derivative or Substantial Derivative or Total Derivative with respect to time.



  • In steady flow, local acceleration will be zero.
  • In uniform flow, convective acceleration will be zero.

Rotational Compenent ($\omega$)


\[ \omega =  \frac{1}{2} \nabla \times \vec{V} = \frac{1}{2}
\begin{vmatrix}
 i & j & k \\
 \frac{\partial}{\partial x} & \frac{\partial}{\partial y} & \frac{\partial}{\partial z}
\\ u & v & w
\end{vmatrix} \]
\[\omega_z = \frac{1}{2}(\frac{\partial v}{\partial x} - \frac{\partial u}{\partial y})\]


  • Vorticity ($\Omega$) is as the vector that is twice the rotational vector.

\[\Omega = 2 \omega = \nabla \times \vec{V}\]

  • Flow said to be irrotational if vorticity or rotational vector is zero at all points in region.
  • Circulation ($\Gamma$) is line integral of tangential component of velocity around a closed curve.
$\Gamma$ = Vorticity X Area 

Velocity Potential Function ($\phi$)


Velocity potential function exist only for irrotational flow i.e. the existence of velocity potential function implies the flow is irrorational.

\(u = \frac{\partial \phi}{\partial x}\),    \(v = \frac{\partial \phi}{\partial y}\),     \(w = \frac{\partial \phi}{\partial z}\)

Stream Line Function ($\psi$)


     \(u = \frac{\partial \psi}{\partial y}\),       \(v = -\frac{\partial \psi}{\partial x}\)

  • Volume flow rate between $\psi_1$ and $\psi_2$ is equal to $\psi_2 - \psi_1$.
  • Velocity potential function can be defined for 3D flow but stream line function is defined only for 2D.

Along the stream line $d\psi = 0$,
\[d\psi = \frac{\partial \psi}{\partial x}dx + \frac{\partial \psi}{\partial y}dy = 0\]
\[-vdx + udy = 0 \]
\[\Bigg( \frac{dy}{dx}\Bigg)_{\psi = const.} = \frac{v}{u}\]

Along Equipotential line $\phi(x,y)$ is constant,
\[d\phi = \frac{\partial \phi}{\partial x}dx + \frac{\partial \phi}{\partial y}dy = 0\]
\[udx + vdy = 0 \]
\[\Bigg( \frac{dy}{dx}\Bigg)_{\phi = const.} = - \frac{u}{v}\]

\[\Bigg( \frac{dy}{dx}\Bigg)_{\psi = const.} *\Bigg( \frac{dy}{dx}\Bigg)_{\phi = const.} = -1\]

Hence, the streamlines and equipotential lines are orthogonal to each other except stagnation point.



Tuesday, 13 February 2018

Fluid Statics

Pascal's Law

In the absence of shearing stress, pressure at any point in fluid in independent of direction.
Px = Py = Pz



BASIC EQUATION FOR THE PRESSURE FIELD

AT Rest,

For incompressible Fluid,



















Absolute Pressure

Pressure measured with reference to absolute zero. 




  • Absolute pressure can not be zero.
  • Gauge pressure can be positive or negative.
  • At mean sea level atmospheric pressure is 1.01x10^5 Pa or 1 Bar.

Hydrostatic Force on a plane Surface

The force must be perpendicular to the surface since there are no shearing stresses present when fluid is at rest. The pressure will vary linearly with the depth if the fluid is incompressible.







  • Magnitude of FR is independent of angle θ.
  • FR is perpendicular to the surface.
  • Location of resultant force :





Hydrostatic force for Curved surface

  • Horizontal Force (FH) : This can be computed by projecting the surface upon a vertical plane and multiplying the projected area by the pressure at its own center of area.
  • Vertical Force (Fv) : It is equal to the weight of the liquid block lying above the curved surface upto the free surface.






Buoyancy And Flotation

Archimedes Principle

When a body is completely submerged in a fluid, or floating so that it is only partially submerged, then the resultant upward force acting on the body is called BUOYANCY FORCE which is equal to the weight of liquid displaced by the body.

The line of action of the buoyant force passes through the centroid of the displaced volume. The centroid is called the Center of buoyancy.

Archimedes Second Principle


A floating body displaces a volume of fluid equivalent to its own weight.
A body will float if its average density is less than the density of the fluid in which it is placed



Condition for Equilibrium for Floating Body




Metacentre : is defined as the point about which body starts oscillating when body is titled by small angle. 
It can also be defined as the point at which the line of action of buoyancy force will meet the normal axis to the body when body is titled by small angle. 

  • A floating body will be in Stable Equilibrium if M is above G or GM is positive.
  • Unstable Equilibrium if M is below G or GM is negative. 
  • Neutral Equilibrium if M = G.

Time Period of Oscillation


If a floating body oscillates the is time period is given by


Where, 
k = Least radius of gyration
h = meta-centric height (GM)
g = gravity

Sunday, 11 February 2018

Surface Tension and Capillary Action

Due to molecular attraction, liquids possess certain properties such as cohesion and adhesion. Molecules in liquids experience strong intermolecular attractive forces. When those forces act between like molecules, they are referred to as cohesive forces. When the attractive forces act between unlike molecules, they are said to be adhesive forces.

Surface tension occurs due to unbalanced cohesive forces at the interface of liquid and a gas or at the interface of two liquids.



Molecule A which is below the free surface of liquid is surrounded by various corresponding molecules and consequently under the influence of balanced cohesive forces on all sides and hence in equilibrium while molecule B experience a net attractive force toward the bulk of the liquid due to unbalanced cohesive force. This force on the molecules at the liquid surface is normal to the liquid surface. Due to the attraction of liquid molecules below the surface, a film or a membrane is formed at the surface which can resist small tensile load. For example: small insects can walk on water without getting wet

This property of the liquid surface film to exert a tension is called surface tension. It is denoted by s.
It is defined as the force along the line per unit length. Its SI unit is N/m.
Note:

  • Surface tension is inversely proportional to the temperature. As the temperature rises, cohesive forces decreases. 
  • It  is directly dependent on intermolecular cohesive forces.
  • Surface tension for air water interface at 20°C is 0.0736 N/m and for air mercury is 0.48 N/m.
  • At critical point, liquid vapor state are same thus surface tension is zero.

Pressure inside a liquid drop

 

 For equilibrium,

Pressure inside a soap bubble


A bubble has two surfaces in contact with air, one inside and the other outside, each one of which contributes the same amount of tensile force due to surface tension. Therefore,

Pressure inside a jet






Capillary Action



When adhesive forces are greater than cohesive forces, the contact angle θ lies between 0 and 90 degree. Such liquids are called wetting liquids for example : water. When adhesive forces are smaller than cohesive forces, the contact angle θ lies between 90 degree and 180 degree. Such liquids are called non - wetting liquids for example : mercury.


This rise or fall of a liquid when a small diameter tube is immersed in it is known as capillary action.



Weight of risen fluid in tube = specific weight x volume of risen fluid

where, ρ = density of liquid 
                     g = acceleration of gravity 
           D = diameter of tube 
   h= capillary rise

For equilibrium, 
Vertical component of surface tension force = weight of risen fluid


h = rise or fall in capillary                    
Note:
  • For Capillary action, diameter of tube should be less than 3 cm.
  • Lighter liquid experience greater capillary rise or fall.

Thursday, 8 February 2018

Fluid Properties

Introduction

A fluid is a substance which is capable of flowing or deforming under the action of shear force (however the small force maybe). Examples: liquids, gases, and vapors.

Density


The density of a fluid is the ratio of mass to its volume at a specified temperature and pressure. It is denoted by the symbol ‘ρ’.
  • Unit : $Kg/m^3$
  • Dimension : $ML^{-3}$.
  • Maximum density of water is at 4°C and its value is 1000 kg/m3.
  • Density of air at 20°C is 1.2 kg/m3.
  • Density depends on temperature and pressure.
As the temperature rises, the density of fluid decreases because there is an increase in volume.
As the pressure increases, the density of fluid increases because there is a reduction in volume.

Specific weight / weight density (w)

It is defined as the ratio of the weight of the fluid to its volume at a specified temperature and pressure.



  • Unit : $N/m^3$
  • Dimension : $ML^{-2}T^{-2}$.
  • Weight density of water is 1000 * 9.81 = 9810 N/m3.
  • Specific weight depends on temperature, pressure and location.
  • Density is absolute quantity but weight density varies from place to place it is not an absolute quantity.
Specific Gravity

It is defined as the ratio of the density (or specific weight) of any fluid to the density (or specific weight) of standard fluid. It is dimensionless.

  • Specific gravity of water = 1
  • Specific gravity of mercury = 13.6

Viscosity


Viscosity is defined as the property of the fluid by virtue of which it offers resistance to the movement of one layer of fluid over an adjacent layer of fluid.
Viscosity in a fluid is due to Cohesive forces between fluid molecules and Molecular momentum exchange.

Newton's law of viscosity: 
It states that the shear stress τ on a fluid element layer is directly proportional to the rate of shear strain.  
   

  • Here ‘μ’ is the constant of proportionality and this is known as coefficient of viscosity or absolute viscosity or dynamic viscosity.
  • Its SI unit is N-s/m2. The dimension of dynamic viscosity is $ML^{-1}T^{-1}$.
  • C.G.S unit of viscosity is dyne-sec /cm2 or poise.
  • 1 Poise = 0.1 N-s/m2

KINEMATIC VISCOSITY (v) 

It is defined as the ratio of the dynamic viscosity and density of fluid.
  • Its SI unit is m2/sec.
  • In C.G.S, the unit of kinematic viscosity is stokes.
  • 1 stokes = 10^-^4 m2/sec
Variation of Viscosity with temperature

In the case of liquids, cohesive forces (forces of attraction between same nature molecules) are large and dominate over molecular momentum exchange. With an increase in temperature, the cohesive forces decrease and hence the resistance to the flow also decreases. Therefore in case of liquids with increase in temperature, the viscosity of the liquids decreases.


In case of gases, intermolecular distance is very large and hence cohesive forces are negligible and  molecular momentum exchange dominates over cohesive forces. With increase in temperature, molecular disturbance increases which in turn increases resistance to flow. Therefore, viscosity of gases increases with increase in temperature.


Classification of fluids



Ideal Fluids: A hypothetical fluid that is incompressible and has zero viscosity ( μ = 0).


Real Fluids: A fluid, which possesses viscosity. All the fluids, in actual practice, are real.


Newtonian Fluid: A fluid is said to be Newtonian fluid if obeys Newton’s law of viscosity i.e. shear stress is directly proportional to the rate of shear strain or velocity.


Non- Newtonian Fluids: Fluids that do not obey Newton’s law of viscosity are known as Non-Newtonian fluids.


The general relationship between shear stress (τ) and velocity gradient is given by



τ = A(du/dy)^n  + B
where A, B and n are constants.


Case I : Dilatant fluids (B = 0, n > 1)

where, μ_app is apparent viscosity.

For dilatant fluids, μ_app increases with the rate of deformation and hence these fluids are
also known as shear thickening fluids. 
Examples : Rice starch, sugar in water.


Case II : Pseudo plastic fluids (B = 0, n < 1)


For pseudo-plastic fluids, n < 1 thus, the apparent viscosity (μ_app) decreases with the rate of
deformation and hence pseudo-plastic fluids are also called as shear-thinning fluids.
Examples : Blood, Milk, and colloidal solution.

Case III : Bingham plastic fluids (B = constant, n = 1)

IF the shear stress is less than B, it acts like a solid and after B it behaves like a fluid.
example : toothpaste.

Time-dependent fluids

1. Thixotropic fluids: In these fluids, apparent viscosity decreases with time. 
Examples : paints, lipstic.

2. Rheopectic fluids : In these fluids apparent viscosity increases with time. 
Examples : Bentonite solution, gypsum solution in water.





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