Skip to the content.

Droplet and Bubble Flow Mass/Heat Transfer Correlations

Overview

The InterphaseDropletFlow class provides interphase transport coefficient correlations for dispersed flow regimes — droplet (mist) flow and bubble flow — where one phase exists as discrete particles in a continuous carrier phase.

Package: neqsim.fluidmechanics.flownode.fluidboundary.interphasetransportcoefficient.interphasetwophase.interphasepipeflow

Key difference from stratified flow: In dispersed flow, the characteristic length scale for mass and heat transfer is the particle diameter (droplet or bubble), not the pipe hydraulic diameter. This gives fundamentally different transfer rates.

Related Documentation:


Flow Regime Mapping

Flow Regime Continuous Phase Dispersed Phase NeqSim Node Class
Droplet / Mist Gas (phase 0) Liquid (phase 1) DropletFlowNode
Bubble Liquid (phase 1) Gas (phase 0) BubbleFlowNode

1. Continuous Phase: Ranz-Marshall Correlation

For mass and heat transfer from the continuous phase to the particle surface, the Ranz-Marshall correlation is used:

Mass Transfer (Sherwood Number)

\[Sh = 2 + 0.6 \cdot Re_p^{0.5} \cdot Sc^{0.33}\]

Heat Transfer (Nusselt Number)

\[Nu = 2 + 0.6 \cdot Re_p^{0.5} \cdot Pr^{0.33}\]

Where:

Mass Transfer Coefficient

\[k_c = \frac{Sh \cdot D_{ij}}{d_p}\]

Where $D_{ij} = \nu / Sc$ is the binary diffusivity.

Heat Transfer Coefficient

\[h = \frac{Nu \cdot \lambda}{d_p}\]

Where $\lambda$ is the thermal conductivity.

Physical Limits

Reference: Ranz, W.E. and Marshall, W.R. (1952). “Evaporation from Drops.” Chemical Engineering Progress, 48(3), 141-146.


2. Dispersed Phase: Kronig-Brink Model

For transport inside the particle (e.g., mass transfer within a droplet or bubble with internal circulation), the Kronig-Brink steady-state solution is used:

\[Sh_{KB} = 17.66\] \[Nu_{KB} = 17.66\]

This gives:

\[k_d = \frac{17.66 \cdot D_{ij}}{d_p}\] \[h_d = \frac{17.66 \cdot \lambda_d}{d_p}\]

The Kronig-Brink value (17.66) represents the asymptotic Sherwood/Nusselt number for a sphere with complete internal circulation (Hill’s vortex inside the particle). It is significantly higher than the pure diffusion limit ($Sh = 6.58$) because internal recirculation enhances transport.

Reference: Kronig, R. and Brink, J.C. (1951). “On the Theory of Extraction from Falling Droplets.” Applied Scientific Research, A2, 142-154.


3. Abramzon-Sirignano Extended Film Model (Optional)

For evaporating droplets with significant mass transfer rates, the standard Ranz-Marshall correlation underestimates the film thickness because it does not account for Stefan flow (outward radial convection caused by evaporation, also called “blowing”).

The Abramzon-Sirignano (1989) model corrects the Sherwood number:

\[Sh^* = 2 + \frac{Sh_0 - 2}{F(B_M)}\]

Where $Sh_0$ is the standard Ranz-Marshall Sherwood number and $F(B_M)$ is the film correction function:

\[F(B_M) = (1 + B_M)^{0.7} \cdot \frac{\ln(1 + B_M)}{B_M}\]

Spalding Mass Transfer Number

\[B_M = \frac{Y_s - Y_\infty}{1 - Y_s}\]

Where:

Behavior

$B_M$ $F(B_M)$ Effect
$\to 0$ $\to 1$ No blowing — recovers standard Ranz-Marshall
$= 1$ $\approx 1.125$ Moderate evaporation — $Sh^*$ reduced by ~10%
$\gg 1$ $\gg 1$ Vigorous evaporation — significant $Sh^*$ reduction

Physical interpretation: Evaporation creates an outward flow of vapor at the droplet surface. This “blowing” effectively thickens the boundary layer, reducing the rate at which fresh gas reaches the surface. The correction factor $F(B_M) > 1$ increases the effective film thickness, which lowers $Sh^*$ relative to $Sh_0$.

Reference: Abramzon, B. and Sirignano, W.A. (1989). “Droplet Vaporization Model for Spray Combustion Calculations.” International Journal of Heat and Mass Transfer, 32(9), 1605-1618.


4. Particle Diameter

The characteristic particle diameter is obtained from the flow node:

Node Type Method Typical Range
DropletFlowNode getAverageDropletDiameter() 10-500 $\mu$m
BubbleFlowNode getAverageBubbleDiameter() 1-10 mm

If the node type is not recognized, a default of 100 $\mu$m is used.


5. API Usage

Basic Usage

// Create a droplet flow node
DropletFlowNode node = new DropletFlowNode(fluid, pipeData);
node.setAverageDropletDiameter(100.0e-6); // 100 micron droplets
node.initFlowCalc();

// Create the interphase transport calculator
InterphaseDropletFlow interphase = new InterphaseDropletFlow(node);

// Gas-side (continuous phase) mass transfer coefficient
double schmidtNumber = 0.7; // typical for gas
double kc_gas = interphase.calcInterphaseMassTransferCoefficient(0, schmidtNumber, node);

// Liquid-side (dispersed phase) mass transfer coefficient
double kc_liq = interphase.calcInterphaseMassTransferCoefficient(1, 1000.0, node);

With Abramzon-Sirignano Correction

interphase.setUseAbramzonSirignano(true);
interphase.setSpaldingMassTransferNumber(2.0); // vigorous evaporation

double kc_corrected = interphase.calcInterphaseMassTransferCoefficient(0, 0.7, node);
// kc_corrected < kc_standard due to blowing correction

Bubble Flow

BubbleFlowNode bubbleNode = new BubbleFlowNode(fluid, pipeData);
bubbleNode.setAverageBubbleDiameter(5.0e-3); // 5 mm bubbles
bubbleNode.initFlowCalc();

InterphaseDropletFlow interphase = new InterphaseDropletFlow(bubbleNode);

// Liquid-side is now continuous (phase 1)
double kc_liq_cont = interphase.calcInterphaseMassTransferCoefficient(1, 500.0, bubbleNode);
// Gas-side is now dispersed (phase 0)
double kc_gas_disp = interphase.calcInterphaseMassTransferCoefficient(0, 0.7, bubbleNode);

6. Comparison with Stratified Flow

The key difference between InterphaseDropletFlow and InterphaseStratifiedFlow:

Aspect Stratified Flow Droplet/Bubble Flow
Characteristic length Pipe hydraulic diameter $D_h$ Particle diameter $d_p$
Sh correlation Yih-Chen or Dittus-Boelter Ranz-Marshall
Reynolds number Based on pipe geometry Based on particle size and relative velocity
Dispersed phase N/A Kronig-Brink ($Sh = 17.66$)
Blowing correction N/A Abramzon-Sirignano (optional)
Typical $k_c$ range $10^{-4}$ to $10^{-2}$ m/s $10^{-3}$ to $1$ m/s

Since $d_p \ll D_h$, dispersed flow generally has much higher mass transfer coefficients per unit area, but the total interfacial area depends on the number and size of particles.


7. References

  1. Ranz, W.E. and Marshall, W.R. (1952). “Evaporation from Drops, Part I and II.” Chemical Engineering Progress, 48(3), 141-146 and 48(4), 173-180.

  2. Kronig, R. and Brink, J.C. (1951). “On the Theory of Extraction from Falling Droplets.” Applied Scientific Research, A2, 142-154.

  3. Abramzon, B. and Sirignano, W.A. (1989). “Droplet Vaporization Model for Spray Combustion Calculations.” International Journal of Heat and Mass Transfer, 32(9), 1605-1618.

  4. Clift, R., Grace, J.R., and Weber, M.E. (1978). Bubbles, Drops, and Particles. Academic Press.

  5. Solbraa, E. (2002). Equilibrium and Non-Equilibrium Thermodynamics of Natural Gas Processing. PhD Thesis, NTNU.