4 theory of multiphase flows
DESCRIPTION
General theory of two phase flowsTRANSCRIPT
Theory of Multiphase Flows.
By: Yadav Gaurav NM.Tech Thermal Sciences
Project Guide: Dr. S. Jayraj
Pressure Drop Equation
• For single phase flows:
• The first term on the rhs is the frictional pressure gradient , second is the gravitational pressure gradient and last is the accleration pressure gradient
dz
Gudg
dA
ds
dz
dp )(sin
• Under normal circumstances fluid does not accelerate.
• Usually encountered in nozzles, diffusers because of change in area and also in compressible flows because there density changes with length.
• For heated tubes because liquid goes into vapour phase and that results in acceleration or deceleration to occur.
• For the two phase flows the pressure drop equation can be written in analogous manner as
• Here ρ is replaced by ρTP
)(sin))( 2211
21
1 uGuGdz
dg
dA
ds
dA
ds
dz
dpTP
TP
TP
1
• In 1 kg mixture : x kg gas and (1-x) kg liquid.
• In 1m3 of mixture: α m3of gas and (1- α) m3 of liquid.
lgTP xx )1(
lgTP )1(
Physical parameters delineating flow patterns
Surface Tension: • Keeps channel wall always wet with liquid
during G-L flows (unless they are heated.)• Tends to make small liquid droplets and small
gas bubbles spherical. Gravity:• In non vertical channel it tends to pull heavier
phase at the bottom.
Constant heat flux for vertical heated tube
• In this case the liquid film around the wall gets depleted due to vaporization and shear stress.
Difference b/w heated & unheated tube.• Amount of vapour and liquid changes along
the length. So flow distribution also changes.
• No churn flow in heated tubes.
• Droplet flows is present in heated tube which was not present in unheated tubes.
• There is presence of radial temperature profile in the tube.
• Continous change in phase fraction along the axial length.
• Departure from thermodynamic equilibrium.
Definition and Common Terminologies• Phase 1: Continous phase.• Phase 2: Discontinous or lighter phase.
Mass Flow Rate: W• W 1 ,W2
• WTP = W1 +W2 .
Volumetric Flow Rate: Q• Q=W/ ρ.• QTP=Q1+Q2
Density: ρ• ρ1, ρ2, ρTP .
Specific Volume:ν• ν1, ν2, νTP .
Viscosity:μ• μ1, μ2, μTP
C/S Area: A• A=A1+A2
Wetted Area/Wetted Perimeter: S• S1 = Area at which phase 1 is in contact with
wall.• S2 = Area at which phase 2 is in contact with
wall.• Si = Interfacial area.
Mass Flux: G=W/A= ρu.• G1=W1/A and G2=W2/A.
• GTP = G1+G2
Volume Flux: j = Q/A.• j1 = Q1/A and j2 = Q2/A
• jTP=j1+j2.
Velocity: u=Q/A• u1=Q1/A1 and u2=Q2/A2.• These are insitu velocity components.• It is difficult to measure A1 and A2 as they are
the local insitu areas and change along the axial length.
Superficial Velocity (Measurable Velocity):• u1s = Q1/A and u2s = Q2/A.• For 1D steady state flow , superficial velocity
and volumetric flux are same.
Volume Fraction: Inlet Volume Fraction:
• It is measurable quantity.
21
2
Q
Insitu Volume Fraction:
• It is not a measurable quantity.
Mass Fraction: x• It is quality x. A Measurable quantity.
21
2
21
2
AA
A
VV
V
21
2
WW
Wx
Relative Velocity: • u12 = u1-u2
• u21 = u2-u1
• u12 = -u21
Slip Ratio: k• k = u2/u1
• Also k = )).(1
).(1(
2
1
xx
Some Advanced Relations
• Q1 = j1A = u1A1 = u1A(1-α)
Therefore j1 = u1(1-α).
• Q1 = W1/ρ1 = G1A/ρ1 = {G(1-x)}.A/ρ1
Therefore j1 = {G(1-x)}./ρ1
• In same way j2 = u2α = Gx/ρ2
Drift Velocity: • It is the component velocity minus the
average velocity.• u1j = u1-j
• u2j = u2-j.
Drift Flux:• Volumetric flux of either component related
to a surface moving at volumetric avg velocity.• j21 = α(u2-j).
• j12 = (1- α)(u1-j)
Relation between Drift flux and component volumetric fluxes.
j21 = α(u2-j) = αu2 - αj
= αu2- αj1 -αj2
= j2- αj1 -αj2
= j2(1 -α) – αj1.
j12 = (1- α)(u1-j)
= (1- α)u1 - (1- α)j1 - (1- α)j2
=j1(α) – (1 - α)j2.
Therefore j12 = -j21
Relation between Drift Flux and relative velocity.
j21 = α(u2-j) = αu2 – αj
= αu2- αj1 -αj2
= αu2 – α(1- α)u1 – α2u2
= α(1- α)(u2-u1)
= α(1- α)u21.
Therefore Drift Flux is directly proportional to relative velocity for a particular system at particular condition i.e. α = c
Schematic layout of NCL