Numerical study of the Bénard-Marangoni instability

Slides:



Advertisements
Similar presentations
Moving in the right circles
Advertisements

Lakshmi Sankar Module 3.3 Panel Methods Lakshmi Sankar
By Ross Nuechterlein.  Convection is the movement of molecules within fluids and is one of the major modes of heat and mass transfer in liquids and gas.
Emerging Flux Simulations Bob Stein A.Lagerfjard Å. Nordlund D. Benson D. Georgobiani 1.
Weather. Weather and Climate Weather denotes a short term behavior of the earths atmosphere – Hours to a week – Applies to a local area – Rain, warm,
Jordanian-German Winter Academy 2006 NATURAL CONVECTION Prepared by : FAHED ABU-DHAIM Ph.D student UNIVERSITY OF JORDAN MECHANICAL ENGINEERING DEPARTMENT.
St.-Petersburg State Polytechnic University Department of Aerodynamics, St.-Petersburg, Russia A. ABRAMOV, N. IVANOV & E. SMIRNOV Numerical analysis of.
Model of a Sloshing Tank
CHE/ME 109 Heat Transfer in Electronics LECTURE 19 – NATURAL CONVECTION FUNDAMENTALS.
Oceans Video Video.php?video_id=173915&title=E xploring_Oceans&vpkey=
Stirling-type pulse-tube refrigerator for 4 K M.A. Etaati, R.M.M. Mattheij, A.S. Tijsseling, A.T.A.M. de Waele Eindhoven University of Technology Mathematics.
Natural Convection in free flow: Boussinesq fluid in a square cavity
Heat Transfer.  Earth’s molten outer core is nearly as hot as the surface of the sun.  Heat is transferred from the core to the surface of the Earth.
* University of Mining and Metallurgy, AGH Cracow Experimental and Numerical Investigations of Buoyancy Driven Instability in a Vertical Cylinder Tomasz.
FREE CONVECTION Nazaruddin Sinaga Laboratorium Efisiensi dan Konservasi Energi Jurusan Teknik Mesin Universitas Diponegoro.
INTRODUCTION TO CONDUCTION
Properties of Matter Chapter Four: Density and Buoyancy
RISICO on the GRID architecture First implementation Mirko D'Andrea, Stefano Dal Pra.
Bernoulli’s Principle. Usually, liquids are considered “incompressible”, meaning that the density of the liquid remains nearly constant. Gases are easily.
TransAT Tutorial Particle Tracking July 2015 ASCOMP
Gas, Pressure, and Wind. Gases Recap - Nitrogen (78%), Oxygen (21%), Other and H2O (1%). Gases, like matter, have mass and are affected by gravity The.
Lecture Objectives: Analyze the unsteady-state heat transfer Conduction Introduce numerical calculation methods Explicit – Implicit methods.
Lesson 3 Convection and the Mantle. Vocabulary radiation - the transfer of energy that is carried in rays like light convection - heat transferred by.
Methods of Energy Transfer
Latitude structure of the circulation Figure 2.12 Neelin, Climate Change and Climate Modeling, Cambridge UP.
Local Air Movements Science Objectives investigate localized air movements (thermals, sea breezes, and land breezes) and its effect on regional.
Sharp transitions between different turbulent states Guenter Ahlers, University of California-Santa Barbara, DMR Turbulence, by virtue of its vigorous.
Stirling-type pulse-tube refrigerator for 4 K M. Ali Etaati CASA-Day April 24 th 2008.
To the teacher: This CPO Science PowerPoint presentation is designed to guide you through the process of presenting the lesson to your students. The.
What causes wind? Single Convection Cell Model for small scale circulation By Diana L. Duckworth Rustburg High School Campbell County, VA.
What processes heat the atmosphere?
Saffman-Taylor Instability of Hele-Shaw Cell
FREE CONVECTION 7.1 Introduction Solar collectors Pipes Ducts Electronic packages Walls and windows 7.2 Features and Parameters of Free Convection (1)
HW/Tutorial # 1 WRF Chapters 14-15; WWWR Chapters ID Chapters 1-2
Energy Transfer In the Earth’s System (C) Copyright all rights reserved 1.
Simulation Of Buoyancy Driven Flows Inside Heated Cavities Using LES And URANS Approaches School Of M.A.C.E. The University Of Manchester. Presented by:
HW/Tutorial # 1 WRF Chapters 14-15; WWWR Chapters ID Chapters 1-2 Tutorial #1 WRF#14.12, WWWR #15.26, WRF#14.1, WWWR#15.2, WWWR#15.3, WRF#15.1, WWWR.
Ocean Currents Objective: Objective: How does the temperature affect the ocean’s currents?
Ocean Currents. The water in the ocean is constantly moving The water in the ocean is constantly moving Broad bands of ocean water that flow in one direction.
M. Khalili1, M. Larsson2, B. Müller1
Atmospheric Stability and Air Masses
Heat Transfer Conduction, Convection, Radiation. Conduction Heat energy can be transferred from one substance to another when they are in direct contact.
States of Matter. Fluid States In science, gases and liquids are fluids Fluid pressure is the force exerted by the fluid on an area of a surface. p =
Convection and the Mantle
Computer Animation Rick Parent Computer Animation Algorithms and Techniques Computational Fluid Dynamics.
TEKS 8.10A recognize that the sun provides the energy that drives convection within the atmosphere and ocean, producing winds and ocean currents The Sun,
Chapter 6: Introduction to Convection
4.3 Air Currents.
HW/Tutorial # 1 WRF Chapters 14-15; WWWR Chapters ID Chapters 1-2
Warm-up In Chinese herbal tea shops, bowls of herbal tea are usually covered by glass plates. Why do the shop owners need to do this?
How does energy transfer using convection?
E-Infrastructure for e-Science, CERIST-Algiers 15th
Land Breezes and Sea Breezes Sea Breeze
Lesson 24 NATURAL CIRCULATION
Panel Methods.
Fundamentals of Heat Transfer
More air pressure at Earth’s surface. Warm air is less dense & rises.
Earth’s Atmosphere.
Properties of Air Grade 6 Science Unit on Flight
Key vocab 07, words 1, 2 1. Salinity(n) Saltiness or dissolved salt content of a body of water 2. Distribution (n) The action of sharing something out.
Wind/Temperature Review
FIGURE 3.1 On a sunny, calm day, the air near the surface can be substantially warmer than the air a meter or so above the surface. Fig. 3-1, p.56.
Heat.
Kurowski, M .J., K. Suselj, W. W. Grabowski, and J. Teixeira, 2018
Begin working on the winds worksheet from the quiz day.
Chapter 19 FORCED CONVECTION
WIND SYSTEMS.
Chapter 19 FORCED CONVECTION
AE/ME 339 Computational Fluid Dynamics (CFD) K. M. Isaac 7/24/2019
Presentation transcript:

Numerical study of the Bénard-Marangoni instability EPIKH,e-infrastructure for e-science, Algiers 15th July 2010 Presented by: Benseghir Chahrazed University of Batna Numerical study of the Bénard-Marangoni instability workshop

The surface tension-driven convection is referred as Bénard- Marangoni convection. It occurs when a horizontal layer is heated from below and the top is a cold free surface. INTRODUCTION Figure.1. B-M convection

INTRODUCTION This causes the heated fluid to rise because of local density differences. The warm fluid near the bottom is replaced by cooler fluid near the top. the fluid will tend to circulate in a series of cells known as B-M cells. Side walls Free surface Figure.2. B-M cells.

INTRODUCTION Bénard-Marangoni instability is a fundamental problem for several material processing technologies, such as semiconductor crystal growth from melt in microgravity conditions.

OBJECTIVE Our objective is to use the grid system to study numerically the unsteady B-M instability in absence of the gravity .

STUDIED CONFIGURATION L b Y Z X Our domain is in 3D. The cavity is filled with the silicon-oil and above this fluid layer there is a layer of air. The system is heated from bellow and the top is maintained cold. Figure.3. Studied configuration.

MATHEMATICAL MODEL Continuity equation Momentium equations Energy equation

MATHEMATICAL MODEL Prandtl number Marangoni number Biot number

CONDITIONS 1) Initial condition U=V=W=T=0 2) Boundary conditions:

Velocity-pressure coupling NUMERICAL METHODS Finite volume method Hybrid scheme Projection method Velocity-pressure coupling

Gridification using eumedgrid We have gridified our application in eumed grid unsing a jdl file to submit the job. The gridification was successfull and have given the following results

Results Normalized Time=13000; Ma=150.

Saving time! We have saved significantly the cpu time of the execution of our program: Time on a P4 CPU: 2 days Time on EUMEDGRID: 6 hours

CONCLUSION The application has been successfuly gridified The calciulation have been done on a computing element The data files have been compressed archived and stored in a storage element using a single scrpt file

THANK YOU FOR YOUR ATTENTION