Upload
janae
View
26
Download
0
Tags:
Embed Size (px)
DESCRIPTION
Modeling of Welding Processes through Order of Magnitude Scaling. Patricio Mendez, Tom Eagar Welding and Joining Group Massachusetts Institute of Technology MMT-2000, Ariel, Israel, November 13-15, 2000. What is Order of Magnitude Scaling?. - PowerPoint PPT Presentation
Citation preview
Modeling of Welding Processes throughOrder of Magnitude ScalingPatricio Mendez, Tom EagarWelding and Joining GroupMassachusetts Institute of TechnologyMMT-2000, Ariel, Israel, November 13-15, 2000
What is Order of Magnitude Scaling?OMS is a method useful for analyzing systems with many driving forces
What is Order of Magnitude Scaling?OMS is a method useful for analyzing systems with many driving forcesWeld pool
What is Order of Magnitude Scaling?OMS is a method useful for analyzing systems with many driving forcesWeld poolArc
What is Order of Magnitude Scaling?OMS is a method useful for analyzing systems with many driving forcesWeld poolElectrode tipArc
OutlineContext of the problemSimple example of OMSApplications to WeldingDiscussion
Context of the Problem
Context of the ProblemPhilosophyArtsScienceEngineering
Context of the ProblemScienceEngineeringPhilosophyArtsScienceEngineeringPhilosophyArts~1700
Context of the ProblemScienceEngineeringPhilosophyArtsScienceEngineeringPhilosophyArtsEngineeringScienceFundamentalsApplications~1700~1900
Context of the ProblemScienceEngineeringPhilosophyArtsScienceEngineeringPhilosophyArtsScienceEngineeringGap is gettingtoo large!FundamentalsApplications~1700~1900~1980
Example: Modeling of an Electric ArcVery complex process:Fluid flow (Navier-Stokes)Heat transferElectromagnetism (Maxwell)It is very difficult toobtain general conclusions with too many parameters
Chart1
1
1
2
2
8
8
10
11
12
14
20
14
14
Squire 1951(analytical)
Maecker 1955 (approximate)
Shercliff 1969 (analytical)
Yas'ko 1969 (dimensional analysis)
Ramakrishnan 1978
Glickstein 1979
Hsu 1983
McKelliget 1986
Choo, 1990
Lee 1996
Kim 1997
Lowke 1997
year of publication
number of dimensionless groups (m)
Sheet1
19511Squire
19691Shercliff
19512Squire
19552Maecker
19788Ramakrishnan
19798Glickstein
196910Yas'ko
198311Hsu
198612McKelliget
199014Choo
199720Lowke
199714Kim
199614Lee
Sheet2
Sheet3
Example: Modeling of an Electric ArcComplexity of the physics increased substantially
Generalization of problems with OMSFundamentals
Generalization of problems with OMSFundamentalsDifferential equations
Generalization of problems with OMSFundamentalsDifferential equationsAsymptotic analysis(dominant balance)
Generalization of problems with OMSFundamentalsDifferential equationsAsymptotic analysis(dominant balance)Engineering
Generalization of problems with OMSFundamentalsDimensional analysisDifferential equationsAsymptotic analysis(dominant balance)Engineering
Generalization of problems with OMSMatrix algebraFundamentalsDimensional analysisDifferential equationsAsymptotic analysis(dominant balance)Engineering
Generalization of problems with OMSMatrix algebraFundamentalsDimensional analysisDifferential equationsAsymptotic analysis(dominant balance)EngineeringArtificial Intelligence
Generalization of problems with OMSMatrix algebraFundamentalsDimensional analysisDifferential equationsAsymptotic analysis(dominant balance)EngineeringOrder of Magnitude ReasoningArtificial Intelligence
Generalization of problems with OMSMatrix algebraFundamentalsDimensional analysisDifferential equationsAsymptotic analysis(dominant balance)EngineeringOrder of Magnitude ReasoningArtificial IntelligenceOrder of MagnitudeScaling
OMS: a simple example
X = unknown
P1, P2 = parameters (positive and constant)
Dimensional Analysis in OMS
There are two parameters: P1 and P2:n=2
Dimensional Analysis in OMS
There are two parameters: P1 and P2:n=2Units of X, P1, and P2 are the same:k=1 (only one independent unit in the problem)
Dimensional Analysis in OMS
There are two parameters: P1 and P2:n=2Units of X, P1, and P2 are the same:k=1 (only one independent unit in the problem)Number of dimensionless groups:m=n-km=1 (only one dimensionless group) P=P2/P1 (arbitrary dimensionless group)
Asymptotic regimes in OMS
There are two asymptotic regimes:Regime I: P2/P1 0Regime II: P2/P1
Dominant balance in OMS
There are 6 possible balancesCombinations of 3 terms taken 2 at a time:
Dominant balance in OMS
There are 6 possible balancesCombinations of 3 terms taken 2 at a time: One possible balance:
Dominant balance in OMS
There are 6 possible balancesCombinations of 3 terms taken 2 at a time: One possible balance:
Dominant balance in OMS
There are 6 possible balancesCombinations of 3 terms taken 2 at a time: One possible balance: P2/P1 0 in regime I
Dominant balance in OMS
There are 6 possible balancesCombinations of 3 terms taken 2 at a time: One possible balance: P2/P1 0 in regime IX P1 in regime I
Dominant balance in OMS
There are 6 possible balancesCombinations of 3 terms taken 2 at a time: One possible balance: P2/P1 0 in regime IX P1 in regime Inatural dimensionless group
Properties of the natural dimensionless groups (NDG)Each regime has a different set of NDGFor each regime there are m NDG All NDG are less than 1 in their regimeThe edge of the regimes can be defined by NDG=1The magnitude of the NDG is a measure of their importance
Estimations in OMS
For the balance of the example:
In regime I:estimation
Corrections in OMS CorrectionsDimensional analysis states:
correction function
Corrections in OMS CorrectionsDimensional analysis states:
Dominant balance states:
when P2/P10correction function
Corrections in OMS CorrectionsDimensional analysis states:
Dominant balance states:
Therefore:when P2/P10correction functionwhen P2/P10
Properties of the correction functionsProperties of the correction functionsThe correction function is 1 near the asymptotic caseThe correction function depends on the NDGThe less important NDG can be discarded with little loss of accuracyThe correction function can be estimated empirically by comparison with calculations or experiments
Generalization of OMSThe concepts above can be applied when:The system has many equationsThe terms have the form of a product of powersThe terms are functions instead of constantsIn this case the functions need to be normalized
Application of OMS to the Weld Pool at High CurrentDriving forces:Gas shearArc PressureElectromagnetic forcesHydrostatic pressureCapillary forcesMarangoni forcesBuoyancy forcesBalancing forcesInertialViscous
Application of OMS to the Weld Pool at High CurrentGoverning equations, 2-D model (9) :conservation of mass Navier-Stokes(2)conservation of energyMarangoniOhm (2)Ampere (2)conservation of charge
Application of OMS to the Weld Pool at High CurrentGoverning equations, 2-D model (9) :conservation of mass Navier-Stokes(2)conservation of energyMarangoniOhm (2)Ampere (2)conservation of chargeUnknowns (9):Thickness of weld poolFlow velocities (2)PressureTemperatureElectric potentialCurrent density (2)Magnetic induction
Application of OMS to the Weld Pool at High CurrentParameters (17):L, r, a, k, Qmax, Jmax, se, g, n, sT, s, Pmax, tmax, U, m0, b, wsReference Units (7):m, kg, s, K, A, J, VDimensionless Groups (10)Reynolds, Stokes, Elsasser, Grashoff, Peclet, Marangoni, Capillary, Poiseuille, geometric, ratio of diffusivity
Application of OMS to the Weld Pool at High CurrentEstimations (8):Thickness of weld poolFlow velocities (2)PressureTemperatureElectric potentialCurrent density in XMagnetic induction
Application of OMS to the Weld Pool at High Current
Application of OMS to the Weld Pool at High CurrentRelevance of NDG (Natural Dimensionless Groups)
Application of OMS to the ArcDriving forces:Electromagnetic forcesRadialAxialBalancing forcesInertialViscous
Application of OMS to the ArcIsothermal, axisymmetric modelGoverning equations (6):conservation of massNavier-Stokes(2)Ampere (2)conservation of magnetic fieldUnknowns (6)Flow velocities (2)PressureCurrent density (2)Magnetic induction
Application of OMS to the ArcParameters (7): r, m, m0 , RC , JC , h, Ra Reference Units (4):m, kg, s, ADimensionless Groups (3)Reynoldsdimensionless arc lengthdimensionless anode radius
Application of OMS to the ArcEstimations (5):Length of cathode regionFlow velocities (2)PressureRadial current density
Application of OMS to the ArcVZP
Application of OMS to the ArcComparison with numerical simulations:
Re
RC
ZS
Application of OMS to the ArcCorrection functions
Application of OMS to the ArcVR(R,Z)/VRS200 A10 mm2160 A70 mm
ConclusionOMS is useful for:Problems with simple geometries and many driving forcesThe estimation of unknown characteristic valuesThe ranking of importance of different driving forcesThe determination of asymptotic regimesThe scaling of experimental or numerical data
Now its even hard to apply 1900s physics.We can model complex problems, but still cant understand them well.
Put them on the internet