Introduction of background knowledge regarding flow physics and CFD as well as detailed information about the use of AcuSolve and what specific options do.
Collection of AcuSolve simulation cases for which results are compared against analytical or experimental results to demonstrate the accuracy
of AcuSolve results.
In this application, AcuSolve is used to simulate the flow of water between concentric cylinders. The outer cylinder is held stationary while the
inner cylinder rotates with a constant speed. AcuSolve results are compared with analytical results as described in White (1991). The close agreement of AcuSolve results with analytical results validates the ability of AcuSolve to model cases containing thin annular gaps with flow induced by rotating walls.
In this application, turbulent flow of air through a pipe is simulated. AcuSolve results are compared with experimental results as described in White (1991) and extracted from the Moody chart. The
close agreement of AcuSolve results with experimental results validates the ability of AcuSolve to model turbulent flow within pipes.
In this application, AcuSolve is used to simulate the viscous flow of water between a moving and a stationary plate with an imposed pressure
gradient. AcuSolve results are compared with analytical results described in White (1991). The close agreement of AcuSolve results with analytical results validates the ability of AcuSolve to model cases with imposed pressure gradients.
In this application, AcuSolve is used to simulate the flow of air in an enclosed cylindrical cavity with a rotating top and a fixed bottom.
AcuSolve results are compared with experimental data adapted from Michelsen (1986). The close agreement of AcuSolve results with experimental data validates the ability of AcuSolve to model cases containing enclosed cavities with flow induced by rotating walls.
In this application, AcuSolve is used to simulate natural convection in the annular space between a heated inner pipe and an outer concentric pipe.
AcuSolve results are compared with experimental results adapted from Kuehn and Goldstein (1978). The close agreement of AcuSolve results with experimental results validates the ability of AcuSolve to model cases with flow induced by natural convection.
In this application, AcuSolve is used to simulate laminar flow through a channel with two outlets forming a T-junction. AcuSolve results are compared with experimental results adapted from Hayes and others (1989). The close agreement of AcuSolve results with experimental results validates the ability of AcuSolve to model cases with multiple outlet paths.
In this application, AcuSolve is used to simulate high Peclet number laminar flow through a channel with heated walls. AcuSolve results are compared with analytical results adapted from Hua and Pillai (2010). The close agreement of AcuSolve results with analytical results validates the ability of AcuSolve to model cases involving heat transfer to a moving fluid with a high Peclet number.
In this application, AcuSolve is used to simulate the natural convection of a turbulent flow field within a tall rectangular cavity. AcuSolve results are compared with experimental results as described in Betts and Bokhari (2000). The close agreement of AcuSolve results with experimental results validates the ability of AcuSolve to model cases with natural convection of turbulent flow within a tall cavity.
In this application, AcuSolve is used to simulate fully developed turbulent flow through an asymmetric diffuser with a divergent lower wall and
a straight upper wall. AcuSolve results are compared with experimental results as described in Buice and Eaton (2000). The close agreement of AcuSolve results with experimental results validates the ability of AcuSolve to model cases with internal turbulent flow with flow separation and reattachment in an asymmetric diffuser.
In this application, AcuSolve is used to simulate fully developed turbulent flow over a backward-facing step. AcuSolve results are compared with experimental results as described in Driver (1985) and on the NASA Langley Research
Center Turbulence Modeling Resource web page. The close agreement of AcuSolve results with experimental data and reference turbulence model performance validates the ability of AcuSolve to model cases with turbulent flow that forms a shear layer, recirculates and then reattaches downstream
of the divergent step.
In this application, AcuSolve is used to simulate fully developed turbulent flow through a channel containing a convex curve in the lower wall.
AcuSolve results are compared with experimental results as described in Smits (1979) and on the NASA Langley Research Center
Turbulence Modeling Resource webpage. The close agreement of AcuSolve results with experimental data and reference turbulence model performance validates the ability of AcuSolve to model cases with turbulent flow moving past a convex curved wall.
In this application, AcuSolve is used to simulate the heat transfer due to radiation between concentric cylinders. The inner and outer cylinders
are held at constant temperature and are defined to be radiation surfaces. AcuSolve results are compared with analytical results for temperature as described in Incropera (2006). The close agreement
of AcuSolve results with analytical results validates the ability of AcuSolve to model cases with radiation heat transfer requiring view factor computation.
In this application, AcuSolve is used to simulate turbulent flow through a strongly curved two dimensional 180 degree U-duct channel. AcuSolve results are compared with experimental results adapted from Rumsey et al. (2000). The close agreement of AcuSolve results with experimental results validates the ability of AcuSolve to model turbulent cases with strong curvature effects.
In this application, AcuSolve is used to simulate the flow of air between concentric cylinders that is initiated by the rotation of the solid
inner cylinder. The outer cylinder is held stationary while the inner cylinder rotates with a constant speed. AcuSolve results are compared with analytical results as described in White (1991). The close agreement of AcuSolve results with analytical results validates the ability of AcuSolve to maintain a continuous velocity across a non-conformal guide surface interface.
In this application, AcuSolve is used to simulate the heat transfer due to conduction and radiation between concentric spheres. The inside surface
of the inner and the outside surface of the outer sphere are both held at constant temperature, while the gap between
them radiates the heat from one sphere to the other.
In this application, AcuSolve is used to simulate the changes in wall temperature due to two-phase nucleate boiling at the heated walls of a pipe
with water flowing through it. AcuSolve results are compared with experimental results adapted from Koncar and others (2015). The close agreement of
AcuSolve results with experimental results validates the ability of AcuSolve to model two-phase nucleate boiling problems.
In this application, AcuSolve is used to simulate the wall heat flux due to nucleate boiling at a heated wall inside a rectangular channel with
water flow. Results are compared with experimental heat flux measurements as reported by Steiner, et al. (2005). The
close agreement of AcuSolve results with experimental results validates the ability of AcuSolve to model single phase nucleate boiling problems.
In this application, AcuSolve is used to simulate the high-speed turbulent flow in a converging and then diverging nozzle. The flow within the
nozzle enters as subsonic, reaches sonic at the throat and shortly after develops a normal shock. AcuSolve results are compared with experimental results adapted from Bogar and Sajben (1983). The close agreement of AcuSolve results to experimental measurements validates the ability of AcuSolve to simulate internal supersonic flows where normal shocks are present.
In this application, AcuSolve is used to simulate fully developed turbulent flow past a smooth hump on the lower wall of a flow domain. AcuSolve results are compared with experimental results as described in Seifert and Pack (2002) and on the NASA Langley Research
Center Turbulence Modeling Resource web page. The close agreement of AcuSolve results with experimental data and reference turbulence model performance validates the ability of AcuSolve to model cases with turbulent flow moving past a wall protrusion resulting in flow separation and recovery.
In this application, AcuSolve is used to simulate the flow of a highly viscous fluid between a moving and a stationary plate with an imposed
pressure gradient and fixed temperature on the walls. AcuSolve results are compared with analytical results described in White (1991). The close agreement of AcuSolve results with analytical results validates the ability of AcuSolve to model cases with imposed pressure gradients and viscous heating.
This section includes validation cases that consider unbounded simulation domains where external flow is present over
solid bodies, leading to free boundary layer development.
This section includes validation cases containing conditions producing laminar to turbulent flow that are simulated
with a turbulence transition model.
This section includes validation cases that consider time dependent motion within the domain, requiring that the mesh
movement be modeled with a differential equation, a fully defined mesh motion or by interpolated mesh motion.
Collection of AcuSolve simulation cases for which results are compared against analytical or experimental results to demonstrate the accuracy
of AcuSolve results.
In this application, AcuSolve is used to simulate high Peclet number laminar flow through a channel with heated walls. AcuSolve results are compared with analytical results adapted from Hua and Pillai (2010). The close agreement of AcuSolve results with analytical results validates the ability of AcuSolve to model cases involving heat transfer to a moving fluid with a high Peclet number.
In this application, AcuSolve is used to simulate high
Peclet number laminar flow through a channel with heated walls. AcuSolve results are compared with analytical results adapted from
Hua and Pillai (2010). The close agreement of AcuSolve results
with analytical results validates the ability of AcuSolve to
model cases involving heat transfer to a moving fluid with a high Peclet number.
Problem Description
The problem consists of water at 20 °C flowing through a channel of infinite width with top and
bottom walls heated to 75 °C. The channel is 0.2 m high and 0.8 m long, as shown in
the following image, which is not drawn to scale. A centrally located slice 0.02 m
wide is modeled with slip boundary conditions so that side-wall influences can be
ignored. Water enters the channel with an average velocity of 0.003 m/s. As the
fluid flows through the channel, it is heated by the top and bottom plates.
The simulation was performed as a two dimensional problem by restricting flow in the out-of-plane
direction through the use of a mesh that is one element thick. In addition, the
symmetry of the geometry in the height direction is exploited to allow for modeling
only half of the geometry. These characteristics allow for accurate simulation of
flow while minimizing computational time.
AcuSolve Results
The AcuSolve solution converged to a steady state and the results
reflect the mean flow conditions. As the cool water enters the channel at
temperature less than that of the walls, heat is transferred to the water by
conduction. As the fluid travels along the channel, the temperature differential
between the wall and the adjacent water decreases. The thermal boundary layer within
the water develops as the flow propagates downstream.
Temperature at a specified vertical position in the channel increases along the length of the
channel. The nature of that temperature change is dependent on proximity to the
heated wall. Water in the center of the flow will have the least temperature change.
Since this problem was solved for symmetrical flow, only the top half of the flow
region was modeled. The vertical position for results shown in the following figure
are based on the center of flow having a Y-position of 0.
Summary
The AcuSolve results compare well with the analytical
results for the development of a thermal boundary layer in a heated channel. In this
application, the model is set up to yield large gradients as the flow convects away
from the inlet. The boundary conditions and mesh size were chosen specifically to
yield a high Peclet number. The element Peclet number in the flow direction in this
case is Pe=30.0, as calculated from the following equation.
(1)
where is the density, the heat capacity,
ν the velocity, the length, and k
the thermal conductivity.
This example shows the robustness of the stabilized technique in AcuSolve when element Peclet number is high.
Note: Standard
Galerkin finite element formulations become unstable when the element Peclet
number is greater than 1.0.
Simulation Settings for Laminar Flow Through a Channel with Heated Walls
SimLab database file: <your working
directory>\channel_laminar_heat\channel_laminar_heat.slb
Global
Problem Description
Flow - Steady State
Temperature equation - Advective Diffusive
Turbulence equation - Laminar
Auto Solution Strategy
Relaxation factor - 0.4
Material Model
Fluid_Material
Density - 1000.0 kg/m3
Specific Heat - 1000 J/kg-K
Viscosity - 1.0e-12 kg/m-sec
Conductivity - 1.0 W/m-K
Model
Volumes
Fluid
Element Set
Material model - Fluid_Material
Surfaces
Inlet
Simple Boundary Condition
Type - Inflow
Inflow type - Velocity
X velocity - 0.003 m/sec
Temperature - 293.15 K
Outlet
Simple Boundary Condition
Type - Outflow
Symm_MaxZ
Simple Boundary Condition
Type - Slip
Symm_MinY
Simple Boundary Condition
Type - Slip
Symm_MinZ
Simple Boundary Condition
Type - Slip
Wall
Simple Boundary Condition
Type - Wall
Temperature BC type - Value
Temperature - 348.15 K
References
Hua Tan and K. M. Pillai. "Numerical Simulation of Reactive Flow in Liquid
Composite Molding Using Flux-Corrected Transport (FCT) Based Finite
Element/Control Volume (FE/CV) Method". International Journal of Heat and Mass
Transfer. 53:2256-2271, 2010.