Femtet Help/Manual
 

Home / Examples / Fluid Analysis [Bernoulli] / Example 16: Capillary Action Analysis

Example 16: Capillary Action Analysis

 

General

  • The model is two parallel plates and water sandwiched between them. Water rising by surface tension is solved with the VOF method.
     

  • The volume fractions of air and water are solved.
     

  • Unless specified in the list below, the default conditions are applied.

  • Simulation Time: around 50 min

  • Two methods are compared: manually specified timestep and automatically specified timestep.

 

 

Analysis Space

Item

Settings

Analysis Space

2D

Model Unit

mm

Analysis Conditions

Item

Tab

Settings

Solver

Solver Selection

Fluid Analysis [Bernoulli]

Analysis Type

Fluid Analysis

Transient Analysis

Free Surface Analysis (VOF Method)

Fluid Analysis

Free Surface Analysis (VOF Method): Select

Free Surface Analysis (VOF Method) Setting

Fluid Analysis

Phase Setting: Register [000_Air] and [100_Water].

 

Take into account weight: Select

Take into account surface tension: Select

Phase Pair Setting:

Phase 1

Phase 2

Surface Tension

Contact Angle

000_Air

100_Water

0.07

90

Detailed Settings

Fluid Analysis

Setup Details

Volume Control Type: Cell-centered Base

Timestep [Manual]

Transient Analysis

Setting Item

Settings

Timestep

Specified by 0.1 [ms]

Number of Calculation Steps

5000

Output interval

100

Timestep [Automatic]

 

Transient Analysis

Setting Item

Settings

Timestep

Automatic

Finish Time

0.5 [s]

Maximum Number of Calculation Steps

5000

Specify the output interval.

Select

Output Interval

100

Detailed Automatic Timestep Setting:
Adjust referring to Courant number.

Select

Detailed Automatic Timestep Setting:
Courant Number

0.25

 

Meshing Setup

Mesh

Setting Item

Settings

General Mesh Size

Specified by 0.1 [mm]

Element Type

Rectangle

 
 

Model

Body Attributes and Materials

Body Number/Type

Body Attribute Name

Material Name

0/Face

Wall

Wall

1/Face

Wall

Wall

2/Face

Water

100_Water *

3/Face

Air

000_Air *

* Available from the material DB

 

The material property of "Wall" is set as follows.

Material Name

Tab

Settings

Wall

Solid/Fluid

Solid

 

Contact Angle is set in the body attributes of "Wall".

Body Attribute Name

Tab

Settings

Wall

Solid

Multiphase Flow Setting (Contact Angle Setting):

Specify for each body attribute: Select

Phase Pair Setting:

Phase 1

Phase 2

Contact Angle

000_Air

100_Water

60

Boundary Condition

Boundary Condition Name/Topology

Tab

Boundary Condition Type

Settings

WaterInlet/Edge

Fluid

Inlet/Outlet

Natural Inflow/ Natural Outflow

Multiphase Flow Setting:

Inflow Phase [100_Water]

AirInlet/Edge

Fluid

Inlet/Outlet

Natural Inflow/ Natural Outflow

Multiphase Flow Setting:

Inflow Phase [000_Air]

 

Results

The volume fraction contours of phase 2 at 0, 0.1 [s], 0.2 [s], 0.3 [s], 0.4 [s], and 0.5 [s] are shown below.

Phase 2 (Water) is indicated in red.

The diagram indicates that the water level initially increases up to 0.1 seconds and over time, it fluctuates and appears to be approaching a constant height.

However, within the given time range of 0 to 0.5 seconds, the water level has not yet converged to a constant value.

 

Time: 0 [s]

Time: 0.1 [s]

Time: 0.2 [s]

Time: 0.3 [s]

Time: 0.4 [s]

Time: 0.5 [s]

 

With contact angles taken into account, the calculation may not converge due to boundary oscillations.

About 10 times larger viscosity can suppress the undesired oscillations.

The steady-state is calculated where the surface tension and the weight are balanced.
Then, the change in viscosity does not affect the calculation of the steady-state.

 

Water level can be obtained from the equations below, which indicates water level does not depend on viscosity.

H [m]: Water Level, σ [N/m]: Coefficient of Surface Tension, θ: Contact Angle, ρ [kg/m3]: Water Density, g [m/s2]: Gravitational Acceleration, L [m]: Distance between the parallel plates

 

The calculation results with 10 times higher viscosity are shown below.

Water level converges to a certain value.

 

Time: 0 [s]

Time: 0.1 [s]

Time: 0.2 [s]

Time: 0.3 [s]

Time: 0.4 [s]

Time: 0.5 [s]

 

 

The water levels of the two models are acquired by [VOF CaptureBoundary Macro.xlsm] and shown in the graph below.

The water level converges to about 6.1 [mm].

 

 

 

The theoretical value of water level is,

h = 2 * 0.07 * 0.5 / (997 * 9.8 * 0.1e-3 ) = 7.16 [mm].

The theoretical water level is slightly higher than the calculated level.

 

In addition, for the viscosity set to 10 times, compare the result with that obtained using the automatic timestep setting of [Adjust referring to Courant number].

It is observed that almost the same results are obtained.

When [Manual] is set for the timestep, 5,000 steps are required for calculations; whereas if [Automatic] is set, about 1,600 steps are required. Setting to [Automatic] can lead to shorter calculation times.