Content 1. Aim of our research 2. Modeling of nonlinear surface - - PowerPoint PPT Presentation

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Content 1. Aim of our research 2. Modeling of nonlinear surface - - PowerPoint PPT Presentation

Dynamics of complex fluid-fluid interfaces Leonard M. C. Sagis Food Physics Group Polymer Physics Group http://www.fph.wur.nl/UK/Staff/Staff/Leonard+M.C.+Sagis/ Content 1. Aim of our research 2. Modeling of nonlinear surface rheology with


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Leonard M. C. Sagis

Food Physics Group

Dynamics of complex fluid-fluid interfaces

Polymer Physics Group http://www.fph.wur.nl/UK/Staff/Staff/Leonard+M.C.+Sagis/

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Content

  • 1. Aim of our research
  • 2. Modeling of nonlinear surface rheology with NET
  • 3. GENERIC model for interfaces stabilized by anisotropic particles
  • 4. Summary
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  • block oligomers
  • colloidal particles
  • rod-like particles
  • proteins
  • complexes
  • (mixtures of ) lipids

Interfacial structure:

  • 2D suspensions
  • 2D glasses
  • 2D gels
  • 2D (liquid) crystalline phases
  • 2D nano-composites

Aim:

  • Investigate effect of surface rheology on macroscopic behavior and stability of emulsions,

foam, encapsulation systems

  • Link nonlinear surface rheology to deformation induced changes in surface microstructure
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Determination of surface rheological properties of complex interfaces

Stress controlled rheometer with biconical disk geometry Automated drop tensiometer

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Typical structures we are investigating: Protein fibrils (Lc = 200 – 2000 nm, D = 5 – 20 nm) Protein – polysaccharide complexes (D = 200 – 600 nm) Focus of this presentation: anisotropic structures and effect of flow on their orientation

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Surface dilatational modulus for single layers

  • MCT/W interface
  • Frequency strain sweep: 0.01 Hz
  • Strain of frequency sweep : 5%

Nonlinear behavior even at lowest strains that can be applied (~0.02) No useful constitutive equations for nonlinear surface stresses

L.M.C. Sagis, Rev. Mod. Phys. 83, 1367 (2011)

Most dilatational studies do not even apply strain sweeps Excellent opportunity for NET to fill this “knowledge gap”

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Modeling surface rheology with Nonequilibrium Thermodynamics (NET)

Properties constitutive models for in-plane surface fluxes should have:

  • Link surface stress to the microstructure of the interface
  • Give structure evolution as a function of applied deformation
  • Incorporate a coupling with the bulk phase
  • Be valid far beyond equilibrium

L.M.C. Sagis, Rev. Mod. Phys. 83, 1367 (2011)

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What is “far beyond equilibrium” for surface rheology of complex interfaces:

  • Fluid-fluid interfaces with complex microstructure show changes in

that structure at very low strains

  • First nonlinear contributions to surface stress: 10-5 ≤ g ≤ 10-3
  • Significant deviations from linear behaviour: g > 0.1
  • Most industrial applications: g >> 1
  • CIT models typically start to fail at:

10-3 ≤ g ≤ 10-2

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GENERIC for multiphase systems with complex interfaces: Reversible dynamics for bulk phase and interface variables Dissipative processes bulk phase and interface

H.C. Öttinger, D. Bedeaux and D.C. Venerus, Phys. Rev. E., 80, 021606 (2009) L.M.C. Sagis, Advances in Colloid & Interface Science 153, 58 (2010) L.M.C. Sagis, Rev. Mod. Phys. 83, 1367 (2011)

Ensures structural compatibility of GENERIC in presence of moving interfaces

E = total energy of the system S = total entropy of the system

A= 𝑏 𝑒𝑊 + 𝑏𝑡 𝑒𝐵

𝑇 𝑆

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GENERIC for multiphase systems with complex interfaces: Structural variables

{A,E } = 𝜖𝐵

𝜖𝑦 ∙ 𝑀 ∙ 𝜖𝐹 𝜖𝑦

𝑀 = - 𝑀𝑈

[A,S ] = 𝜖𝐵

𝜖𝑦 ∙ 𝑁 ∙ 𝜖𝑇 𝜖𝑦

𝑁 = M 𝑈

Poisson matrix Independent system variables:

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Relaxation term Diffusion term Coupling with the bulk phase Upper convected surface derivative Surface extra stress tensor:

GENERIC for structured interfaces

Configurational Helmholtz free energy Coupling of G with velocity gradient

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GENERIC for structured interfaces

We can create a wide range of models by specifying:

s C s s s s c

R F D D R G , , , , ,

2 1 G

 

,  S S

Admissible models:

D D R    

G s C s s s

R

2 1

Symmetric positive semi- definite tensors

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Interface stabilized by a mixture of rod-like particles and low molecular weight surfactant (dilute 2D particle dispersion)

Example:

Structural parameter: particle orientation tensor

  =

s s s

n n 2 C

ns

shear

Γ 𝑡 = 𝜍𝑄𝑡= a constant Assumptions: No inhomogeneity caused by the flow, and no exchange with the bulk phases (= rswP

s with wP s=0.01)

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Orientation of rod-like particles as a function of shear rate:

Expression for the surface structural Helmholtz free energy (per unit area): Expression for the surface relaxation tensor: Balance equations for the surface structural tensor: Initial condition: Cs(0)=P

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Flat interface with anisotropic particles in a constant in-plane shear field Increasing t Steady state values orientation tensor (b=0) Effective surface shear viscosity Orientation - surface shear thinning

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Flat interface with anisotropic particles in a constant in-plane shear field Exponent n as a function of t for b=0 Exponent n as a function of b for t=10

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Flat interface with anisotropic particles in a constant in-plane shear field Comparison with a CIT model (8 parameters)*:

t = 5 s ; b = 0

GENERIC CIT

* L.M.C. Sagis, Soft Matter 17, 7727 (2011) .

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Flat interface with anisotropic particles in oscillatory in-plane shear field

gxy(t) = g0 sin(2pwt) w=0.1 Hz t= 1.0 s b=0

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3 5 7 9 11 13 15

Flat interface with anisotropic particles in oscillatory in-plane shear field

gxy(t) = g0 sin(2pwt) w=0.1 Hz t= 1.0 s b=0

  • First nonlinear contributions

already at g < 0.01

  • Highly nonlinear at g > 1
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Flat interface with anisotropic particles in oscillatory in-plane shear field Surface storage modulus, Gs’ (---- ) and loss modulus, Gs” (- - - - ) Two values of wt:

  • 1.0: soft gel-like behaviour
  • 0.1: viscoelastic liquid
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Flat interface with anisotropic particles in oscillatory dilatation (Langmuir trough)

gxx(t) = g0 sin(2pwt), w=0.1 Hz, t= 1.0 s

Strictly speaking this experiment determines the surface Young modulus

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Flat interface with anisotropic particles in oscillatory dilatation (Langmuir trough) y x Asymmetry in response results from different orientation in compression / extension parts of the cycle

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g0 =0.5

4 2 5 6 3

Flat interface with anisotropic particles in oscillatory dilatation (Langmuir trough)

gxx(t) = g0 sin(2pwt) w=0.1 Hz t= 1.0 s b=0

  • First nonlinear contributions

already at g < 0.001

  • Highly nonlinear at g > 0.1

Even harmonics: have been

  • bserved experimentally
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Flat interface with anisotropic particles in oscillatory dilatation (Langmuir trough)

  • Calculated from the intensity of the first harmonic (as in real experiment)
  • In spite of the high nonlinearity of the response, modulus plot shows only

mild strain hardening. Ed” Ed’ tan d

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  • Comparison with data for surface shear experiments + optical techniques
  • Extension to more complex systems

Conclusions: Future work:

  • 1. GENERIC appears to be a powerful tool to model the nonlinear

surface rheological response of complex interfaces.

  • 2. True value of the framework still has to be established by

comparison with experimental data

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Perspectives: Ultimate goal: understanding the complex dynamic behaviour of biomaterial microcapsules, liposomes, cells, ultrasound microbubbles, ...... NET can play a major role in this field by providing accurate descriptions for the coupled transfer of mass, heat, and momentum, on both microscopic and macroscopic length scales.