A Multi-Fluid Model of Membrane Formation by Phase-Inversion Douglas - - PowerPoint PPT Presentation

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A Multi-Fluid Model of Membrane Formation by Phase-Inversion Douglas - - PowerPoint PPT Presentation

A Multi-Fluid Model of Membrane Formation by Phase-Inversion Douglas R. Tree 1 and Glenn Fredrickson 1 , 2 1 Materials Research Laboratory 2 Departments of Chemical Engineering and Materials University of California, Santa Barbara Society of


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SLIDE 1

A Multi-Fluid Model of Membrane Formation by Phase-Inversion

Douglas R. Tree1 and Glenn Fredrickson1,2

1Materials Research Laboratory 2Departments of Chemical Engineering and Materials

University of California, Santa Barbara

Society of Rheology Annual Meeting February 13, 2017

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SLIDE 2

Acknowledgements

◮ Jan Garcia ◮ Dr. Kris T. Delaney ◮ Prof. Hector D. Ceniceros ◮ Lucas Francisco dos Santos ◮ Dr. Tatsuhiro Iwama (Asahi

Kasei)

◮ Dr. Jeffrey Weinhold (Dow)

2

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SLIDE 3

Can we predict the microstructure of polymers?

◮ Microstructure dictates properties ◮ Microstructure depends on process

history

A very general problem!

Polymer membranes

◮ clean water ◮ medical filters

Saedi et al. Can. J. Chem. Eng. (2014)

Polymer Blends

◮ commodity

plastics (e.g. HIPS)

◮ block polymer

thin films

www.leica-microsystems.com

Polymer composites

◮ bulk hetero-

junctions

◮ nano-

composites

Hoppe and Sariciftci J. Mater. Chem. (2006)

Biological patterning

◮ Eurasian jay

feathers

Parnell et al.

  • Sci. Rep. (2015)

3

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SLIDE 4

Can we predict the microstructure of polymers?

◮ Microstructure dictates properties ◮ Microstructure depends on process

history

A very general problem!

Polymer membranes

◮ clean water ◮ medical filters

Saedi et al. Can. J. Chem. Eng. (2014)

Polymer Blends

◮ commodity

plastics (e.g. HIPS)

◮ block polymer

thin films

www.leica-microsystems.com

Polymer composites

◮ bulk hetero-

junctions

◮ nano-

composites

Hoppe and Sariciftci J. Mater. Chem. (2006)

Biological patterning

◮ Eurasian jay

feathers

Parnell et al.

  • Sci. Rep. (2015)

3

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SLIDE 5

Clean water is a present and growing concern

July 7, 2015 U.S. Drought Monitor

D0 Abnormally Dry D1 Moderate Drought D2 Severe Drought D3 Extreme Drought D4 Exceptional Drought

Intensity:

http://droughtmonitor.unl.edu/

Author: Brian Fuchs National Drought Mitigation Center

Why membranes?

◮ Water is projected to

become increasingly scarce.

◮ Filtration is a key

technology for water purification.

http://www.kochmembrane.com/Learning- Center/Configurations/What-are-Hollow-Fiber-Membranes.aspx 4

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SLIDE 6

Polymer membrane synthesis by immersion precipitation

Figure inspired by: www.synderfiltration.com/learning-center/articles/introduction-to-membranes

non-solvent bath membrane substrate polymer solution

nonsolvent solvent

5

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SLIDE 7

Polymer membrane synthesis by immersion precipitation

Figure inspired by: www.synderfiltration.com/learning-center/articles/introduction-to-membranes

non-solvent bath membrane substrate polymer solution

nonsolvent solvent

polymer solvent

non-solvent

H L-L G L-G

5

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SLIDE 8

Microstructural variety in membranes

Uniform “Sponge” Asymmetric“Sponge” Fingers or Macro-voids Skin Layer

Strathmann et al.

  • Desalination. (1975)

6

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SLIDE 9

Model Characterization

run

Model Development NIPS quench process

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SLIDE 10

Model Characterization

run

Model Development NIPS quench process

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SLIDE 11

How can we model microstructure formation?

A difficult challenge

◮ Complex thermodynamics out of equilibrium ◮ Spatially inhomogeneous (multi-phase) ◮ Multiple modes of transport (diffusion & convection) ◮ Large separation of length/time scales

Continuum fluid dynamics

Teran et al. Phys. Fluid. (2008)

Self-consistent field theory (SCFT)

  • Fredrickson. J. Chem. Phys. 6810 (2002)

Hall et al. Phys. Rev. Lett. 114501 (2006)

Key idea – cheaper models

Classical density functional theory (CDFT)/“phase field” models

8

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SLIDE 12

Multi-fluid models

Two-fluid model

◮ Momentum equation

for each species

◮ Large drag enforces

  • cons. of momentum

de Gennes. J. Chem Phys. (1980)

The Rayleighian

A Lagrangian expression of “least energy dissipation” for

  • verdamped systems (Re = 0).

R[{vi}] = ˙ F[{vi}] free energy + Φ[{vi}] dissipation − λG[{vi}] constraints δR δvi & ∂φi ∂t = −∇ · (φivi) Transport equations

Doi and Onuki. J Phys (Paris). 1992

9

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SLIDE 13

Multi-fluid models

Two-fluid model

◮ Momentum equation

for each species

◮ Large drag enforces

  • cons. of momentum

de Gennes. J. Chem Phys. (1980)

The Rayleighian

A Lagrangian expression of “least energy dissipation” for

  • verdamped systems (Re = 0).

R[{vi}] = ˙ F[{vi}] free energy + Φ[{vi}] dissipation − λG[{vi}] constraints δR δvi & ∂φi ∂t = −∇ · (φivi) Transport equations

Doi and Onuki. J Phys (Paris). 1992

9

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SLIDE 14

A ternary solution model

˙ F[{vi}] free energy Φ[{vi}] dissipation λG[{vi}] constraints

Transport Equations

◮ Diffusion & Momentum ◮ Coupled, Non-lin. PDEs

Solve numerically

◮ Pseudo-spectral on GPUs ◮ Semi-implicit stabilization

Ternary polymer solution (Flory–Huggins–de Gennes) F =

  • dr
  • f({φi}) + 1

2

  • i

κi |∇φi|2

  • Newtonian fluid with

φ-dependent viscosity Φ = 1 2

  • dr
  • i

ζi(vi − v)2 +2η({φi})D : D

  • Incompressibility

λG = p∇ · v

10

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SLIDE 15

Transport equations

Model B Model H ∂φi ∂t + v · ∇φi = ∇ ·  

j

Mij({φ})∇µj   Convection-Diffusion µi = δF[{φi}] δφi Chemical Potential 0 = −∇p + ∇ ·

  • η({φ})(∇v + ∇vT )

N−1

  • i=0

φi∇µi Momentum 0 = ∇ · v Incompressibility

11

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SLIDE 16

Model Characterization

run

Model Development NIPS quench process

12

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SLIDE 17

Characterization of model thermodynamics

32 64 96 128

x/R

0.0 0.2 0.4 0.6 0.8 1.0

φp (a)

32 64 96 128

x/R

0.0 0.2 0.4 0.6 0.8 1.0

φn (b)

32 64 96 128

x/R

0.0 0.2 0.4 0.6 0.8 1.0

φs (c)

φp φn φs

(d)

N = 50 κ = 12 χ = 0.912

13

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SLIDE 18

Calculated interface width for many parameters

100 101 102 10−2 10−1 100 l/l∞ χ∗ 2 1 N = 1 N = 2 N = 5 N = 10 N = 20 N = 50 N = 80 N = 100

l∞ = 1 2 κ χ 1/2 χ∗ = (χ − χc)/χc

14

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SLIDE 19

What explains the interface width data?

100 101 102 10−2 10−1 100 l/l∞ χ∗ 2 1 N = 1 N = 2 N = 5 N = 10 N = 20 N = 50 N = 80 N = 100

We are near the critical point, χc

We recover the mean-field critical exponent, l = l∞ χ − χc χc −1/2

15

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SLIDE 20

Characterization of phase separation dynamics

16

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SLIDE 21

There are two dynamic regimes

100 101 102 100 101 102 103 104 105 domain size simulation time

17

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SLIDE 22

Early-time regime — initiation of spinodal decomposition

0.5 1.0 1.5 2.0 2.5 3.0 k

  • 20
  • 15
  • 10
  • 5

5 10 λ λ+ λ-

Two key parameters

◮ qm – fastest growing

mode

◮ λm – rate of spinodal

decomposition

Linear stability analysis

Exponential growth of the fastest growing mode, δψ = exp[λ+(q)t]

φp φn φs

0.00 0.08 0.16 0.24 0.32 0.40 0.48 0.56 0.64 0.72

qm

18

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SLIDE 23

Long-time regime — coarsening

domain size time slope=1/4 domain size time s l

  • p

e = 1 / 3 domain size time slope=1

surface diffusion bulk diffusion hydrodynamics

19

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SLIDE 24

Comparing simulations to the LSA

100 101 102 100 101 102 103 104 105 domain size, 2π/ q simulation time, t

φp φn φs

20

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SLIDE 25

Comparing simulations to the LSA

10−1 100 101 10−3 10−2 10−1 100 101 102 103 104 4 1 scaled domain size, qm/ q scaled simulation time, λmt

20

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SLIDE 26

Model Characterization

run

Model Development NIPS quench process

21

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SLIDE 27

How does a quench happen by mass transfer?

film bath

Qualitative features of NIPS (mass-transfer) v. TIPS (temp.)

  • 1. Inherent anisotropy and

inhomogeneities

  • 2. Driving force (solvent exchange) and

phase separation inseparably linked by mass transfer

Important questions

  • 1. What is the effect of the initial

bath/film concentration?

  • 2. What role does film thickness play?
  • 3. How does mass transfer path affect

microstructure?

22

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SLIDE 28

Anisotropic quench

The bath interface gives rise to:

◮ Surface-directed spinodal decomposition ◮ Surface hydrodynamic instabilities

Ball and Essery. J. Phys.-Condens. Mat. 2, 10303 (1990) 23

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SLIDE 29

Early-time behavior – the infinite film limit

Key concept – time scales

◮ Phase separation is faster

than solvent exchange

◮ At short times we can

neglect the role of film thickness.

  • Pego. P. Roy. Soc. A-Math. Phy. 422, 261 (1989)

Simple diffusion from a initial step

24

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SLIDE 30

Early-time behavior – the infinite film limit

Key concept – time scales

◮ Phase separation is faster

than solvent exchange

◮ At short times we can

neglect the role of film thickness.

  • Pego. P. Roy. Soc. A-Math. Phy. 422, 261 (1989)

Simple diffusion from a initial step

Three possible cases

  • 1. No phase separation, just

diffusion (steady)

24

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SLIDE 31

Early-time behavior – the infinite film limit

Key concept – time scales

◮ Phase separation is faster

than solvent exchange

◮ At short times we can

neglect the role of film thickness.

  • Pego. P. Roy. Soc. A-Math. Phy. 422, 261 (1989)

Simple diffusion from a initial step

Three possible cases

  • 1. No phase separation, just

diffusion (steady)

  • 2. Phase separation, single

domain film (steady)

24

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SLIDE 32

Early-time behavior – the infinite film limit

Key concept – time scales

◮ Phase separation is faster

than solvent exchange

◮ At short times we can

neglect the role of film thickness.

  • Pego. P. Roy. Soc. A-Math. Phy. 422, 261 (1989)

Simple diffusion from a initial step

Three possible cases

  • 1. No phase separation, just

diffusion (steady)

  • 2. Phase separation, single

domain film (steady)

  • 3. Phase separation, multiple

domain film (unsteady)

24

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SLIDE 33

Immediate spinodal decomposition into multi-domain films

25

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SLIDE 34

A finite-sized film can exhibit delayed phase-separation

φp φn φs

polymer film nonsolvent bath

Depending on parameters and initial conditions, a delayed phase separation produces either

◮ single domain films (shown) ◮ multiple domain films

26

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SLIDE 35

Finite-film data collapse with a similarity variable

5 10 15 20 25

ξ

0.0 0.2 0.4 0.6 0.8 1.0

φn

f = 0. 05 f = 0. 025

φp φn φs

27

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SLIDE 36

Conclusions (1D)

  • 1. Inherent anisotropy?

− SDSD-like wave

  • 2. Film thickness?

− Short v. long-time − Scales with xt−1/2

  • 3. Initial conditions?

− No PS, single/multiple domains − Instantaneous v. delayed PS

Saedi et al. Can. J. Chem. Eng. (2014)

Future: microstructure (2D)

◮ Pore gradients

φp φn φs

0.00 0.08 0.16 0.24 0.32 0.40 0.48 0.56 0.64 0.72

qm

◮ Macrovoids

Sternling and Scriven. AICHE J. (1959) 28