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Fluctuating Hydrodynamics of Reactive Fluid Mixtures Aleksandar Donev Courant Institute, New York University Molecular and Chemical Kinetics ’15 Berlin, Germany, Sept 9th 2015 A. Donev (CIMS) Fluct Hydro 9/2015 1 / 22

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Page 1: Fluctuating Hydrodynamics of Reactive Fluid Mixturesdonev/FluctHydro/FluctHydroChem.handout.pdf · Irreversible contribution to the stress is the viscous stress tensor ˙= rv + (rv)T

Fluctuating Hydrodynamics of Reactive Fluid Mixtures

Aleksandar Donev

Courant Institute, New York University

Molecular and Chemical Kinetics ’15Berlin, Germany, Sept 9th 2015

A. Donev (CIMS) Fluct Hydro 9/2015 1 / 22

Page 2: Fluctuating Hydrodynamics of Reactive Fluid Mixturesdonev/FluctHydro/FluctHydroChem.handout.pdf · Irreversible contribution to the stress is the viscous stress tensor ˙= rv + (rv)T

Collaborators

Eric Vanden-Eijden, Courant Institute, New York University

John Bell, Lawrence Berkeley National Labs

Alejandro Garcia, Physics, San Jose State University

A number of postdocs and graduate students at Courant and LBL

A. Donev (CIMS) Fluct Hydro 9/2015 2 / 22

Page 3: Fluctuating Hydrodynamics of Reactive Fluid Mixturesdonev/FluctHydro/FluctHydroChem.handout.pdf · Irreversible contribution to the stress is the viscous stress tensor ˙= rv + (rv)T

Reaction-Diffusion Systems

Chemical Reactions in Solution

Many chemical reactions occur in a viscous solvent and arediffusion-limited, making a mean-field or “well-mixed” approximationinappropriate.

Classical examples where the Law of Mass Action (LMA)reaction-diffusion equations fails spectacularly is annihilationA + B → 0But even in A + B C there are power-law tail signatures in thedynamics even at chemical equilibrium [1].

Spatial fluctuations play a key role in diffusion-limited reactionsand spatial diffusion must be accounted for;this is different (in addition to) fluctuations coming from there beingvery few reactants of certain species.

Primarily interested in the case when fluctuations are weak, i.e., lotsof molecules are involved, but fluctuations still make a difference.

A. Donev (CIMS) Fluct Hydro 9/2015 4 / 22

Page 4: Fluctuating Hydrodynamics of Reactive Fluid Mixturesdonev/FluctHydro/FluctHydroChem.handout.pdf · Irreversible contribution to the stress is the viscous stress tensor ˙= rv + (rv)T

Reaction-Diffusion Systems

Simulation Approaches

The traditional approach to simulation of reaction-diffusion problemsin this community is to solve the Reaction-Diffusion MasterEquation (RDME), such as the next subvolume method.

Diffusion is modeled by a jump process instead of a continuous randomwalk or fluctuating Fick’s law (see below).The results depend strongly on the cell size and are thus notgrid-independent (hard to fix!).

At a basic level one can use particle-based reaction-diffusion models:Particles are modeled as spheres that diffuse as independentBrownian walkers.

In the Smoluchowski model particles react upon touching; simulatedby the First Passage Kinetic Monte Carlo method (FPKMC) [2],called eGFRD in the biochemical community.In the Doi model particles react with a certain binary reaction rate (asa Poisson process) while they overlap.We are developing a novel Isotropic RDME (IRDME) method but seealso Sam Isaacson’s Convergent RDME (CRDME).

A. Donev (CIMS) Fluct Hydro 9/2015 5 / 22

Page 5: Fluctuating Hydrodynamics of Reactive Fluid Mixturesdonev/FluctHydro/FluctHydroChem.handout.pdf · Irreversible contribution to the stress is the viscous stress tensor ˙= rv + (rv)T

Reaction-Diffusion Systems

Diffusion in Liquids

I will first try to convince you that a much better way to modeldiffusion at mesoscopic levels than jumping is fluctuatinghydrodynamics.

I will then try to convince you that diffusion in liquid solutions isstrongly affected by hydrodynamic interactions.

I will lastly show you a framework that includes completehydrodynamic transport including cross-diffusion effects andfluctuations.

But I will try to also indicate a number of problems that areunresolved.

I will operate under the assumption that you believe nonequilibriumstatistical mechanics is a useful tool in chemical reactionmodeling, but will not try to convince you it is so, especially since Ihave essentially no experience in biological systems.

A. Donev (CIMS) Fluct Hydro 9/2015 6 / 22

Page 6: Fluctuating Hydrodynamics of Reactive Fluid Mixturesdonev/FluctHydro/FluctHydroChem.handout.pdf · Irreversible contribution to the stress is the viscous stress tensor ˙= rv + (rv)T

Diffusion via Fluctuating Hydrodynamics

Uncorrelated Brownian Walkers

Fluctuating hydrodynamics is a coarse-grained description of mass,momentum and energy transport in fluids (gases and liquids).

Consider diffusion of colloidal particles immersed in a viscous liquid;assume the particles are uncorrelated Brownian walkers.

The positions of the N particles Q (t) = q1 (t) , . . . ,qN (t) followthe Ito SDEs

dQ = (2χ)12 dB, (1)

where B(t) is a collection of independent Brownian motions.

We are interested in describing a spatially coarse-grained fluctuatingempirical concentration field,

c (r, t) =N∑i=1

δ (qi (t)− r) . (2)

A. Donev (CIMS) Fluct Hydro 9/2015 8 / 22

Page 7: Fluctuating Hydrodynamics of Reactive Fluid Mixturesdonev/FluctHydro/FluctHydroChem.handout.pdf · Irreversible contribution to the stress is the viscous stress tensor ˙= rv + (rv)T

Diffusion via Fluctuating Hydrodynamics

Fluctuating Diffusion Equation

Dean [3] obtained an SPDE for c (r, t) =∑δ (qi (t)− r), using

straightforward Ito calculus and properties of the Dirac delta function,

∂tc = χ∇2c + ∇ ·(√

2χcWc

), (3)

where Wc (r, t) denotes a spatio-temporal white-noise vector field.

This is a typical example of a fluctuating hydrodynamics equation,which is deceptively simply, yet extremely subtle from both a physicaland mathematical perspective.

The term√

2χcWc can be thought of as a stochastic mass flux, inaddition to the “deterministic” Fickian flux χ∇c.

One can develop CFD methods to solve this sort of SPDE [4], withlots of caveats...

A. Donev (CIMS) Fluct Hydro 9/2015 9 / 22

Page 8: Fluctuating Hydrodynamics of Reactive Fluid Mixturesdonev/FluctHydro/FluctHydroChem.handout.pdf · Irreversible contribution to the stress is the viscous stress tensor ˙= rv + (rv)T

Diffusion via Fluctuating Hydrodynamics

Giant Nonequilibrium Fluctuations

Experimental results by A. Vailati et al. from a microgravity environment[5] showing giant fluctuations in the concentration of polystyrene intoluene in space (box scale is 5mm on the side, 1mm thick).Fluctuations become macrosopically large at macroscopic scales!These come because of hydrodynamic effects on diffusion in liquids.

A. Donev (CIMS) Fluct Hydro 9/2015 10 / 22

Page 9: Fluctuating Hydrodynamics of Reactive Fluid Mixturesdonev/FluctHydro/FluctHydroChem.handout.pdf · Irreversible contribution to the stress is the viscous stress tensor ˙= rv + (rv)T

Diffusion via Fluctuating Hydrodynamics

Brownian Dynamics with Hydrodynamics

The Ito equations of Brownian Dynamics (BD) for the (correlated)positions of the N particles Q (t) = q1 (t) , . . . ,qN (t) are

dQ = −M (∂QU) dt + (2kBT M)12 dB + kBT (∂Q ·M) dt, (4)

where B(t) is a collection of independent Brownian motions, U (Q) isa conservative interaction potential.

Here M (Q) 0 is a symmetric positive semidefinite mobility matrixfor the collection of particles, and introduces correlations among thewalkers.

The Fokker-Planck equation (FPE) for the probability density P (Q, t)corresponding to (4) is

∂P

∂t=

∂Q·

M

[∂U

∂QP + (kBT )

∂P

∂Q

], (5)

and is in detailed-balance (i.e., is time reversible) with respect to theGibbs-Boltzmann distribution ∼ exp (−U(Q)/kBT ).

A. Donev (CIMS) Fluct Hydro 9/2015 11 / 22

Page 10: Fluctuating Hydrodynamics of Reactive Fluid Mixturesdonev/FluctHydro/FluctHydroChem.handout.pdf · Irreversible contribution to the stress is the viscous stress tensor ˙= rv + (rv)T

Diffusion via Fluctuating Hydrodynamics

Hydrodynamic Correlations

Let’s start from the (low-density) Rotne-Prager-Yamakawaapproximation Mij ≡Mij

(r = qi − qj

), for r > 2σ,

Mij (r) =R (r)

kBT=

χ

kBT

[(3σ

4r+σ3

2r3

)I +

(3σ

4r− 3σ3

2r3

)r ⊗ r

r2

].

(6)

Here σ is the radius of the colloidal particles and the diffusioncoefficient χ follows the Stokes-Einstein formula

χ =kBT

6πησ.

We can use Ito calculus to obtain an equation for the empirical orinstantaneous concentration similar to what Dean did foruncorrelated walkers, for non-interacting particles (ideal gas, U = 0).

A. Donev (CIMS) Fluct Hydro 9/2015 12 / 22

Page 11: Fluctuating Hydrodynamics of Reactive Fluid Mixturesdonev/FluctHydro/FluctHydroChem.handout.pdf · Irreversible contribution to the stress is the viscous stress tensor ˙= rv + (rv)T

Diffusion via Fluctuating Hydrodynamics

Fluctuating Fick’s Law for Liquids

We get the stochastic advection-diffusion equation [6]

∂tc = ∇ · [χ∇c]−w ·∇c, (7)

where the diffusion tensor χ = R (r, r) and the random velocityfield w (r, t) has covariance

〈w (r, t)⊗w(r′, t ′

)〉 = 2R

(r − r′

)δ(t − t ′

). (8)

For uncorrelated walkers, Mij = δij (kBT )−1 χI, the noise is verydifferent, ∇ ·

(√2χcWc

).

In both cases the mean obeys Fick’s law but the fluctuations arecompletely different.The correct fluctuating Fick’s law in liquids is (7) and not (3)!

A. Donev (CIMS) Fluct Hydro 9/2015 13 / 22

Page 12: Fluctuating Hydrodynamics of Reactive Fluid Mixturesdonev/FluctHydro/FluctHydroChem.handout.pdf · Irreversible contribution to the stress is the viscous stress tensor ˙= rv + (rv)T

Complex Fluid Mixtures

Fluctuating Hydrodynamics

Giant fluctuations can be modeled by including momentum transport(velocity fluctuations) in fluctuating hydrodynamics:

∂tρ+∇ · (ρv) = 0 (9)

∂t (ρv) +∇ ·(ρvvT

)+∇P = ∇ · (σ + Σ) (10)

∂t (ρE ) +∇ · (ρEv + Π · v) = ∇ · (ψ + Ψ) +∇ · ((σ + Σ) · v) , (11)

where the total local energy density is ρE = 12ρv2 + ρe.

A. Donev (CIMS) Fluct Hydro 9/2015 15 / 22

Page 13: Fluctuating Hydrodynamics of Reactive Fluid Mixturesdonev/FluctHydro/FluctHydroChem.handout.pdf · Irreversible contribution to the stress is the viscous stress tensor ˙= rv + (rv)T

Complex Fluid Mixtures

Momentum Fluxes

Irreversible contribution to the stress is the viscous stress tensor

σ = η(∇v + (∇v)T

)+

(ζ − 2

)(∇ · v) I (12)

Stochastic stress tensor obeys fluctuation-dissipation balance

Σ =√

2ηkBT W +

(√ζkBT

3−√

2ηkBT

3

)Tr(W)

I, (13)

where W = (W + WT )/√

2 is a symmetric white-noise tensor field.

A. Donev (CIMS) Fluct Hydro 9/2015 16 / 22

Page 14: Fluctuating Hydrodynamics of Reactive Fluid Mixturesdonev/FluctHydro/FluctHydroChem.handout.pdf · Irreversible contribution to the stress is the viscous stress tensor ˙= rv + (rv)T

Complex Fluid Mixtures

Chemically-Reactive Mixtures

The species density equations for a mixture of NS species are given by

∂t(ρs) +∇ · (ρsv + F) = msΩs , (s = 1, . . .NS) (14)

The diffusive fluxes take the form, excluding barodiffusion andthermodiffusion, and assuming an ideal mixture,

F = ρW

[χ∇x +

√2

12WF (r, t)

],

where n is the number density, xs is the mole fraction of species s,and W = Diag ws = ρs/ρ contains the mass fractions.

χ is an SPD diffusion tensor that can be related to theMaxwell-Stefan diffusion coefficients and Green-Kubo typeformulas.

A. Donev (CIMS) Fluct Hydro 9/2015 17 / 22

Page 15: Fluctuating Hydrodynamics of Reactive Fluid Mixturesdonev/FluctHydro/FluctHydroChem.handout.pdf · Irreversible contribution to the stress is the viscous stress tensor ˙= rv + (rv)T

Complex Fluid Mixtures

Thermodynamics of Reactions

Consider a system with NR elementary reactions with reaction r

Rr :

NS∑s=1

ν+srMs

NS∑s=1

ν−srMs

Stoichiometric coefficients νsr = ν−sr − ν+sr , where

∑s νsrmr = 0.

Define the dimensionless chemical affinity

Ar =∑s

ν+sr µs −

∑s

ν−sr µs ,

where µs = msµs/kBT is the dimensionless chemical potential perparticle.

Also define the thermodynamic driving force

Ar = exp

(∑s

ν+sr µs

)− exp

(∑s

ν−sr µs

)=∏s

eν+sr µs −

∏s

eν−sr µs

A. Donev (CIMS) Fluct Hydro 9/2015 18 / 22

Page 16: Fluctuating Hydrodynamics of Reactive Fluid Mixturesdonev/FluctHydro/FluctHydroChem.handout.pdf · Irreversible contribution to the stress is the viscous stress tensor ˙= rv + (rv)T

Complex Fluid Mixtures

Fluctuating Reaction-Diffusion

The mass production due to chemistry can be modeled using theChemical Langevin Equation (CLE) [7]:

Ωs =∑r

νsr

(P

τrkBT

)Ar (deterministic LMA) (15)

+∑r

νsr

(P

τrkBT

∏s

eν+sr µs

) 12

Z (r, t) (CLE)

The CLE follows from a truncation of the Kramers-Moyal expansionat second order. No true thermodynamic equilibrium:

Assumes one-way reactions which violates detailed balance.the equilibrium distribution is not the Einstein distribution exp (S/kB).

There is no S(P)DE that can correctly describe both the short-time(central limit theorem) and long-time (large deviation functional)behavior of the master equation. But tau leaping can and should beused with time splitting.

A. Donev (CIMS) Fluct Hydro 9/2015 19 / 22

Page 17: Fluctuating Hydrodynamics of Reactive Fluid Mixturesdonev/FluctHydro/FluctHydroChem.handout.pdf · Irreversible contribution to the stress is the viscous stress tensor ˙= rv + (rv)T

Complex Fluid Mixtures

Nonlinear Chemical Networks

We have studied the Baras-Pearson-Mansour (BPM) modelM = (U,V ,W ,S ,Uf ,Vf ),

R1 : U + W V + W

R2 : V + V W + S

R3 : V S (16)

R4 : U Uf

R5 : V Vf

This system can exhibit limit cycles, bimodal states (bistability), andpossibly other nonlinear behavior.In principle this system can be simulated using particle methods!

A. Donev (CIMS) Fluct Hydro 9/2015 20 / 22

Page 18: Fluctuating Hydrodynamics of Reactive Fluid Mixturesdonev/FluctHydro/FluctHydroChem.handout.pdf · Irreversible contribution to the stress is the viscous stress tensor ˙= rv + (rv)T

Complex Fluid Mixtures

Turing-like Patterns

Development of an instability in the BPM model with fluctuations (top)and without (bottom) with complete compressible hydrodynamics (not justreaction-diffusion).

A. Donev (CIMS) Fluct Hydro 9/2015 21 / 22

Page 19: Fluctuating Hydrodynamics of Reactive Fluid Mixturesdonev/FluctHydro/FluctHydroChem.handout.pdf · Irreversible contribution to the stress is the viscous stress tensor ˙= rv + (rv)T

Complex Fluid Mixtures

References

Irina V Gopich, Alexander A Ovchinnikov, and Attila Szabo.

Long-time tails in the kinetics of reversible bimolecular reactions.Phys. Rev. Lett., 86(5):922, 2001.

A. Donev, V. V. Bulatov, T. Oppelstrup, G. H. Gilmer, B. Sadigh, and M. H. Kalos.

A First-Passage Kinetic Monte Carlo Algorithm for Complex Diffusion-Reaction Systems.J. Comp. Phys., 229(9):3214–3236, 2010.

David S Dean.

Langevin equation for the density of a system of interacting langevin processes.Journal of Physics A: Mathematical and General, 29(24):L613, 1996.

P. Espanol and I. Zuniga.

On the definition of discrete hydrodynamic variables.J. Chem. Phys, 131:164106, 2009.

A. Vailati, R. Cerbino, S. Mazzoni, C. J. Takacs, D. S. Cannell, and M. Giglio.

Fractal fronts of diffusion in microgravity.Nature Communications, 2:290, 2011.

A. Donev and E. Vanden-Eijnden.

Dynamic Density Functional Theory with hydrodynamic interactions and fluctuations.J. Chem. Phys., 140(23):234115, 2014.

A. K. Bhattacharjee, K. Balakrishnan, A. L. Garcia, J. B. Bell, and A. Donev.

Fluctuating hydrodynamics of multispecies reactive mixtures.142(22):224107, 2015.ArXiv preprint 1503.07478.

A. Donev (CIMS) Fluct Hydro 9/2015 22 / 22