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Generalization of Heterogeneous Multiscale Models: Coupling discrete microscale and continuous macroscale representations of physical laws in porous media By Paul Delgado

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Generalization of Heterogeneous Multiscale Models:

Coupling discrete microscale and continuous macroscale representations of physical laws in porous media

By Paul Delgado

Outline•Motivation•Heterogeneous Multiscale Framework•Fluid Flow Example•Generalization for Potential Fields•Steady State Applications•Multiscale-Multiphysics•Challenges

Flow in Porous MediaMicroscopic PhysicsMacroscopic Demand 2µm

5cm10km

•DNS not scalable

Navier StokesHigh Detail – Low Efficiency

Darcy’s LawLow Detail – High Efficiency

Multiscale ModelHybrid Detail-Efficiency

•Goldilocks Problem

Heterogeneous Multiscale Method (HMF) E & Engquist (1994)• Incomplete continuum scale model• Microscale models supplement missing information at continuum scale• Iteration between scales until convergence is achieved

Current work• Based off of Chu et al. (2012) for steady state flow • Discrete microscale constitutive relations with macroscale conservation

laws• Multiscale convergence established for certain non-linear conductance

relations.• Higher Dimensional framework established

Multiscale Framework

Microscale ModelPore Network (Fatt, 1956)•Discrete void space inside porous medium•Network of chambers (pores) and pipes (throats)•Prescribed Hydraulic Conductance•Heuristic Rules for unsteady/multiphase flow•Log-normally distributed throat radii

)( ijijij Pgq

fpC

Network ModelPressure-Flux Equations(potentially non-linear)

Flow Rules

0][

iKj

ijq

g may not be linear

Courtesy: Houston Tomorrow

Macroscale ModelFinite Volume Method

v S(x)

v d V S(x)

dV

dVxSdAnvd

)(

v v(x,P,P)

Fi12 F

i 12Si

Fn Fs Fe Fw Si

No explicit form of v is assumed

1D 2D

),(

0

)0,,(),,(),,(

1

1

21

21

21

21

iii

ii

l

x

lxl

PPKPP

fP

PxFPPxF

dPx

PxdF

By mean value theorem,

Iterative Coupling

Assume when .0),,( xPPxF 0xP

where fi 12F

i 12(Pi,Pi1)

Let be the characteristic length of the microscale model.

dF(x,P,)dPx

F(x,P,Px ) F(x,P,0)

Px 0 [0,Px ]

xx PdPx

PxdFPPxF

),,(),,(

Estimate

Hence

Fi12(Pi,Pi1)

dF(x,P,)dPx

P Ki12(Pi,Pi1)D

[Pi]

Chu et al, (2012)

Multiscale Coupling

Iterative Coupling:

xQPDPPKD

PPfPDPxF

ln

ln

ln

ll

nl

nll

nl

n

ll

)1()(1

)(

)(1

)()()(

,

,ˆ)(,,

21

21

21

21

QpK n ˆ)1( Macroscopic

Microscopic

NlfpG n

l

n

l ,..,0,)()(

21

21

Chu, et al. (2011b)

Numerical Analysis

Chu et al. (2012) examined numerical properties of this micro-macro iteration scheme

•Existence •Uniqueness•Consistency•No stability conditions required•Order of convergence•Source terms•Multidimensional and anisotropic cases

Steady State Physics

Conservation LawConstitutive RelationSteady State Equation

S

K

SK

Classical Continuum Mechanics

Heterogenous Multiscale Approach

Coupling Relation

Micro-Conservation Law

Micro-Constitutive Relation

MM S

),( mMF

m k (v k )

Macro-Conservation Law

f ijk 0

f ijk g()

Microscale models are discrete projections of macroscale relations

Example 1Discrete Microscale

Model

fpC )(

qij

jK [ i]

0

Conservation Law

System of Equations

Courtesy: University of Manchester

v v(x,P,P)

dVxSdAnvd

)(

Continuous Macroscale Model

Constitutive Relation

)(1)()()( ,ˆ)(,,21

21

21

nl

nll

nl

n

ll PPfPDPxF

Continuum Scale Equation

Microscale Equations

Control Volume

Multiscale Coupling

•Pressure centered control volumes•Flux at boundaries evaluated using microscale network models•Iteration between scales to convergence

)( Pgq Constitutive Relation

)(xSv Conservation Law

xQPDPPKD ln

ln

ln

ll

)1()(1

)( ,21

System of Equations

Flow in Porous Media

Example 2

xSTDTTKD

TTfTDTxF

ln

ln

ln

ll

nl

nll

nl

n

ll

)1()(1

)(

)(1

)()()(

,

,ˆ)(,,

21

21

21

21

Continuum Scale Equation

Microscale Equations

Control Volume

•Temperature centered control volumes•Flux at boundaries evaluated using microscale network models•Iteration between scales to convergence

fTC

)(

qij

jK [ i]

0Conservation Law

System of Equations

Courtesy: University of Manchester

)( Tgq Constitutive Relation

Conservation Law

Heat Transfer in Porous Media

),,( TTxQQ

dVxSdAnQd

)(

Constitutive Relation

)(xSQ System of Equations

Discrete Microscale Model

Continuous Macroscale Model

Multiscale Coupling

Example 3

derived... beingcurrently

Continuum Scale Equation

Microscale Equations

Control Volume

Multiscale Coupling

•Displacement centered control volumes•Forces at boundaries evaluated using microscale spring system models•Iteration between scales to convergence

Discrete Microscale Model

fxK )(

0][

iKj

ijF

Conservation Law

System of Equations

Courtesy: University of Manchester

)( xkF

Constitutive Relation

Conservation Law

Linear Elasticity in Porous Media

),,( uux

v n dA

d S(x)

dV

Continuous Macroscale Model

Constitutive Relation

)(xS System of Equations

Models

Microscale Flow Microscale Deformation

Continuum Flow Continuum Deformation

Biot (1941), Kim (2010)

Darcy’s Law (1856)

Chu et. al. 2012

Zienkiewicz et. Al. (1947)

Current Work

Courtesy: Georgia College

Courtesy: Symscape

Fatt et. al. (1956)

Courtesy: Miehe et. Al. (2002)

Courtesy: Dostal et. Al. (2005)

Current Work

Current Direction

Uniphysics multiscale models withmicroscale muliphysics coupling

•Interscale communication for all physics•Interphysics communication at microscale only.

+ Consistent with HMM Framework+ Amenable to C2 non-linear microscale models for all physics

Micro-Flow Micro-Deformation

Macro-Flow Macro-Deformation

Challenges

•Microscale multiphysics coupling•Non-overlapping microscale models•Deformation mechanics multiscale coupling•Lagrangian & Eulerian Reference Frames•Iterative multiphysics coupling between timesteps

•Working Paper: A discrete microscale model coupling flow and deformation mechanics

•Working Paper: A generalization of the HMM framework coupling continuous macroscale and discrete microscale models of steady state uniphysics for porous media.

ModelsMicroscale Multiphysics Model Prototype I:

•Iterative coupling between physics•Flow first, deformation second•Solid Matrix pinned at center•Horizontal linear elasticity only•Modeled as Hooke springs.

Observations: •Unrestricted deformation near inlet•Deformation steady near outlet•Pressure at P2 approaches outlet pressure as inlet throat widens•No time dependendent terms introduced in model