Numerical simulation of Granular Flow Based on Micropolar Fluid Theory
APS-DFD Conference Final
1. Hydrodynamic Interaction between Rigid
Surfaces Planing on Water
Ghazi Bari
&
Konstantin Matveev
69th Annual Meeting of the APS Division of Fluid Dynamics, Portland, OR
November 21, 2016
2. Monohull
• Single hard chine
hull
• Stepped hull
2
Copyright: Offshore only, Maritime Journal, Boat International Home, & Military Sealift Command
Different Types of hull
Multi Hull (Catamarans)
• Advantages
• Speed
• Safety/Stability
• Fuel efficiency
• Spacious decks
3. Planing Hull Regime
• Hydrodynamic forces
dominant
• Froude number, 𝐹𝑟𝐿 > 1.2
• 𝐹𝑟𝐿 =
𝑈
𝑔𝐿
• Applications
• Patrol
• Recreational transport
• Rescue service
• Less wetted area
5
Planing Monohull
Planing Catamaran
Copyright: Allison Ultra Performance Boat and Hypro Marine
4. BEM in Planing Hull Hydrodynamics
7
• Boundary Element Method (BEM) is used in our research
• BEM is useful on very large domain
• Only boundary needs to be discretized
• Disadvantages
• Non-linear flow problem
• Require the explicit knowledge of a fundamental solution of the differential
equation
5. General:
• BEM involves placing singularities
(solutions of the fundamental
equation) with unknown
magnitudes on the domain
boundaries
• Boundary conditions are satisfied in
collocation points to determine
those magnitudes
BEM in Potential Flow models
• Low-cost computation
• Simplicity of implementation
• Sufficient accuracy
8
• Use special staggered arrangement for
sources and collocation points to suppress
effects of the finite domain (i.e., wave
reflection from the domain downstream
end)
Source pointsCollocation points
BEM in Planing Hull Hydrodynamics
Specific to this study:
• Use point (discrete) hydrodynamic sources
along the domain boundary
• Use linearized theory (assume small
boundary deformations)
6. Numerical Model Development
• High velocity flow
• Inertia term dominant
• Steady flow
• Irrotational
Governing equations
9
0 v gPvv
t
v
• Viscous force negligible for
hydrodynamic lift and drag
• Working fluid: Water
• Incompressible
• Potential function
and
Continuity eq. Momentum eq.
⇒ 𝛻2 𝜑 = 0
Laplace Eq.
⇒
𝑃
𝜌
+
1
2
𝑣2 + 𝑔𝑧 = 𝑐𝑜𝑛𝑠𝑡𝑎𝑛𝑡
Bernoulli’s Eq.
7. Numerical Model Development (Cont’d)
Linearized Mathematical Model (2D)
10
sources (□) and collocation points (○)
Linearized Bernoulli’s eq.,
𝐶 𝑝
2
+
𝑢′
𝑈0
+
2𝜋𝑦 𝑤
𝜆
= 0
Surface slope eq.,
𝑑𝑦 𝑤
𝑑𝑥
=
𝑣
𝑈0 + 𝑢′
=
𝑄
2𝑈0
A
s
c
dA
r
xQ
xu
)(
2
1
)('
Perturbation velocity,
8. Domain Formation
Incident water flow
0U
X
Z
Top view of wetted plate (3D model)
x x x
z
sources (□) and collocation points (○)
13
j ji
s
j
c
i
ji
jc
i
c
i
r
xx
r
q
zxu
,
2
,4
1
),(
s
i
s
i
s
i
s
i
ii
i
ii
i
xx
yy
U
zx
q
zx
q
1
1
0
11
1
2
2
1
0
),(2),(
),(
2
1
0
c
i
c
iw
c
i
c
ic
i
c
ip
zxy
U
zxu
zxC
9. Wetted Length
16
• Water raise is accounted after each iteration
• Calculations repeated until wetted length stops changing
• CP from the Linearized Bernoulli’s Eq.
• Coefficient of Lift and Drag, Center of pressure related with Lw
A simple picture shows how to find final wetted length
Initial guess of
wetted length,
Free surface water
nL
Intersection of hull
and water surface
(initial guess)
Final wetted length, wL
wL after 1st
iteration
after 2nd
iteration
wL
Point after stopped changingwL
Hull
10. Validation of Monohull Setup
19
• Flow behind a flat bottom hull at finite Froude number
• Good agreement except near transom
• Schmidt’s formula only valid at far stream
1
8
2cos2
2 2
x
Fr
y
h
Transom
0U
Schmidt, G., 1981, "Linearized stern flow of a two-dimensional shallow draft ship," J Ship Res(25), pp. 236-242.
Schematic of (a) 2D problem and (b) 3D problem
11. 1. Squire, H. B., 1957, "The Motion of a Simple Wedge along the Water Surface," Proceedings of the Royal Society, 342, pp. 48-64.
Lift coefficient (𝐶𝐿𝑤)
Center of pressure (𝐿 𝑃)
Comparison of Numerical Solution with Squire’s Data
20
Validation of Monohull Setup (Cont’d)
12. 1. Wang, D. P., and Rispin, P., 1971, "Three-dimensional planing at high Froude number," Journal of Ship Research, 15(3), pp. 221-230.
Pressure coefficient along the center of hull
Pressure coefficient in a longitudinal section at 90% of the plate
21
Validation of Monohull Setup (Cont’d)
Comparison of Numerical Solution with Wang & Rispin’s Analytical Sol
13. 24
Validation of Symmetric Catamaran
1. Bari, G.S., Matveev, K.I., 2016. Hydrodynamic modeling of planing catamarans with symmetric hulls. Ocean Engineering 115, 60-66.
2. Liu, C. Y., and Wang, C. T., 1978, "Interference effects of catamaran planing hulls," Journal of Hydronautics, 13(1), pp. 31-32.
3. Savitsky, D., and Dingee, D., 1954, "Some interference effects between two flat surfaces planing parallel to each other at high speed," Davidson Laboratory
• Modified Savitsky’s correlation from Liu and Wang
(1978)
• For Fr = 2 – 3.5
• AR and Trim angle information not presented
1.1
2
2/5
2/1
]
2
0055.02
012.0[
A
FrA
CL
Correction to the wetted length Interference factor
14. 25
Validation of Asymmetric Catamaran
1. Bari, G.S., Matveev, K.I., 2016. “Hydrodynamics of Single-Deadrise Hulls and Their Catamaran Configurations.” International
Journal of Naval Architecture and Ocean Engineering
2. Morabito, M.G., 2011. “Experimental investigation of the lift and interference of asymmetric planing catamaran demi-hulls.”
• Froude number (𝐹𝑟𝑏): 2.73 ~ 2.75 and
3.95 ~ 4.01
• Trim angle: 5.89°~6.14°
• Deadrise angle (𝛽): 18°
• Wake behind a flat plate
• Epstain (1969) & Payne (1984)
• Trim angle: 6°
• Wetted Length (nominal) : 3
15. Conclusions
29
• Developed: 2D and 3D model based on point-source BEM
• Good agreement with empirical data is found
• Robust design tool for transitional (between hydrostatic and
hydrodynamic support) and early planing regimes of fast boats
• Fast, numerically inexpensive, and sufficiently accurate model
• Applicable to different types of hull setup
Unconventional one with solar cells
Giant yachts, because catamarans allows spacious decks
Example of a ferry, because it is safe
When comes to speed, US navy warship spearhead
Hull: bottom part of boats, direct contact with water
Hydrodynamic performances depend on hull design
Hull carries the entire load
Unconventional one with solar cells
Giant yachts, because catamarans allows spacious decks
Example of a ferry, because it is safe
When comes to speed, US navy warship spearhead
Hydrodynamic force dominant-be described by potential flow.
Tell why wetted length is important
Fr = inertia over weight of fluid element
At low speeds, the weight of the boat is mainly supported by hydrostatic force but as the speed increases hydrostatic forces decrease and hydrodynamic lift force becomes dominant.
Hydrodynamics characteristics of hulls mostly rely on test data and empirical correlations
Development of Computational Fluid Dynamics helped modeling of realistic hull design in great details
Simplified flow models (such as based on potential flow theory), remain useful due to simplicity and low cost computing
1. The boundary element method (BEM) is a numerical computational method of solving linear partial differential equations which have been formulated as integral equations
2. Only linear equation has fundamental solution
To determine the potential, solution of laplace / fundamental equation will be placed in source with unknown magnitude.
BC are satisfied in collocation points in order to determine those magnitudes.
Viscous force negligible outside the thin BL
Perturbation velocity: induced velocity in order to linearize the equation.
Denominator U0
linearization refers to finding the linear approximation to a function at a given point
Linearized kinematic BC : water surface slope = v/U.
It is known (Katz and Plotkin 2001) that a sheet with continuously distributed positive sources generates an outward normal velocity on each side with magnitude, v = Q/2
Q is the source intensity per unit length
Linearized kinematic BC : water surface slope = v/U.
It is known (Katz and Plotkin 2001) that a sheet with continuously distributed positive sources generates an outward normal velocity on each side with magnitude, v = Q/2
Q is the source intensity per unit length
Perturbation potential represents the velocity induced by the motion of the hull in a stationary frame of reference.
3 equations, 3 unknowns
Later we will populate matrix to solve y, u, q.
Coefficient of them are related with position of xs, xc, cell sizes etc.
Viscous force negligible outside the thin BL
Stopping criteria for the numerical process is the wetted length in this study. Why?
It is needed to calculate to hydrodynamic forces like CL, LP. Because from LW we can calculate Cp. Which will give the value of all hydro parameters.
Schmidt’s formula is only valid at sufficiently large distances behind the transom.
Monohull will be further validated for CL, LP and CP.
Squire in 1957 calculated hydrodynamic characteristics of a single planing plate at finite Froude no.
Transition point at Fr =1.
Wang & Rispin: Analytical solution
Three different aspect ratio
Good agreement at low Fr no., one the reasons is the linear model neglects the lateral flow which is more pronounced on longer planing hull
Liu and Wang modified Savitaky’a original equation for monohull and converted it for catamaran by introducing the interference factor due to the demi-hulls.
There were some deviations between test data points and correlation curves shown by Liu and Wang
limited range of Froude numbers
The experimental results are given by Morabito (2011) for dispersed values of primary parameters rather than fixed values, although the variations are not extreme.
The wetted lengths at keel ( ) for test data are calculated from the reported mean wetted length-to-beam ratio ( ) using the equation given by Morabito (2011).
The semi-empirical correlation suggested by Epstein (1969) and more advanced theory of Payne (1984)
Longitudinal sections of water surface elevations
at 8% of the demi-hull span from the port side (dotted line) and starboard side (dashed line) of the starboard demi-hull. Solid line indicates the hull surface. Dash-dotted curve corresponds to the catamaran centerline (z = 0). (a), (c) = 2; (b), (d) = 0.5.
Solid white lines surround the hull pressure areas. z = 0 is the symmetry plane in (b) and (c). (d-f) Longitudinal sections of water surface elevations at 8% of the demi-hull span from the