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
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
1Materials Research Laboratory 2Departments of Chemical Engineering and Materials
University of California, Santa Barbara
◮ Jan Garcia ◮ Dr. Kris T. Delaney ◮ Prof. Hector D. Ceniceros ◮ Lucas Francisco dos Santos ◮ Dr. Tatsuhiro Iwama (Asahi
Kasei)
◮ Dr. Jeffrey Weinhold (Dow)
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◮ Microstructure dictates properties ◮ Microstructure depends on process
◮ clean water ◮ medical filters
Saedi et al. Can. J. Chem. Eng. (2014)
◮ commodity
plastics (e.g. HIPS)
◮ block polymer
thin films
www.leica-microsystems.com
◮ bulk hetero-
junctions
◮ nano-
composites
Hoppe and Sariciftci J. Mater. Chem. (2006)
◮ Eurasian jay
feathers
Parnell et al.
3
◮ Microstructure dictates properties ◮ Microstructure depends on process
◮ clean water ◮ medical filters
Saedi et al. Can. J. Chem. Eng. (2014)
◮ commodity
plastics (e.g. HIPS)
◮ block polymer
thin films
www.leica-microsystems.com
◮ bulk hetero-
junctions
◮ nano-
composites
Hoppe and Sariciftci J. Mater. Chem. (2006)
◮ Eurasian jay
feathers
Parnell et al.
3
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
◮ Water is projected to
◮ Filtration is a key
http://www.kochmembrane.com/Learning- Center/Configurations/What-are-Hollow-Fiber-Membranes.aspx 4
Figure inspired by: www.synderfiltration.com/learning-center/articles/introduction-to-membranes
non-solvent bath membrane substrate polymer solution
nonsolvent solvent
5
Figure inspired by: www.synderfiltration.com/learning-center/articles/introduction-to-membranes
non-solvent bath membrane substrate polymer solution
nonsolvent solvent
5
Strathmann et al.
6
run
run
◮ Complex thermodynamics out of equilibrium ◮ Spatially inhomogeneous (multi-phase) ◮ Multiple modes of transport (diffusion & convection) ◮ Large separation of length/time scales
Teran et al. Phys. Fluid. (2008)
Hall et al. Phys. Rev. Lett. 114501 (2006)
8
◮ Momentum equation
◮ Large drag enforces
de Gennes. J. Chem Phys. (1980)
Doi and Onuki. J Phys (Paris). 1992
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◮ Momentum equation
◮ Large drag enforces
de Gennes. J. Chem Phys. (1980)
Doi and Onuki. J Phys (Paris). 1992
9
◮ Diffusion & Momentum ◮ Coupled, Non-lin. PDEs
◮ Pseudo-spectral on GPUs ◮ Semi-implicit stabilization
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j
N−1
11
run
12
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
14
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
15
16
17
0.5 1.0 1.5 2.0 2.5 3.0 k
5 10 λ λ+ λ-
◮ qm – fastest growing
◮ λm – rate of spinodal
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
domain size time slope=1/4 domain size time s l
e = 1 / 3 domain size time slope=1
19
20
20
run
21
film bath
22
◮ Surface-directed spinodal decomposition ◮ Surface hydrodynamic instabilities
Ball and Essery. J. Phys.-Condens. Mat. 2, 10303 (1990) 23
◮ Phase separation is faster
◮ At short times we can
Simple diffusion from a initial step
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◮ Phase separation is faster
◮ At short times we can
Simple diffusion from a initial step
24
◮ Phase separation is faster
◮ At short times we can
Simple diffusion from a initial step
24
◮ Phase separation is faster
◮ At short times we can
Simple diffusion from a initial step
24
25
φp φn φs
Depending on parameters and initial conditions, a delayed phase separation produces either
◮ single domain films (shown) ◮ multiple domain films
26
5 10 15 20 25
0.0 0.2 0.4 0.6 0.8 1.0
φp φn φs
27
− SDSD-like wave
− Short v. long-time − Scales with xt−1/2
− No PS, single/multiple domains − Instantaneous v. delayed PS
Saedi et al. Can. J. Chem. Eng. (2014)
◮ 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