6. Colloidal instability, flocculation and rheology of dispersions

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Instability in colloidal dispersions

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20 Terms

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Instability in colloidal dispersions

  • Sedimentation 

  • Creaming

  • Flocculation (aggregation)

  • Ostwald ripening

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What is sedimentation and creaming?

Sedimentation: Particle density is higher than the density of continuous phase → particles sink 

Creaming: Particle density is lower than the density of continuous phase → particles rise to surface

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Flocculation/aggregation

a process where a solute (particles) comes out of solution in the form of floccules due to insufficient repulsion between particles 

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4

Ostwald ripening

Large particles grow at the expense of smaller ones. Depends on how soluble dispersed phase is in continuous phase, size and laplace pressure

Smaller droplets → higher laplace pressure → higher driving force 

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At which concentration is Stokes law a good estimation of real sedimentation?

Low concentration (φ<5%): vsed = vStokes

For dispersion by particles is 25%

High concentration: (φ>5%): vsed< vStokes

Sedimentation rates are lower than Stoke’s law predict  

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Hindered sedimentation/creaming

The sedimentation or creaming rate decreases with increasing concentration of the dispersed phase.

When we have more 40% sedimentation doesn’t occur since there is no space, the particles are too crowded 

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There are three mechanisms for flocculation:

• Brownian motions

The particles get close to each other through random movement 

• Shear induced flocculation

Some particles experience higher or lower shear stress depending on their surface

• Gravitity induced flocculation

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Comparison between Brownian and shear flocculation rate

Brownian:

  • Decreases with increased size

  • Decreases with increased viscosity

Shear:

  • Increases with increased size

  • Increases with increased shear rate

N = number concentration of particles, kB = Boltzmann constant, T = absolute temp., η =

dynamic viscosity, w = stability factor, φ = volume fraction of particles, γ = shear rate

<p>Brownian: </p><ul><li><p>Decreases with increased size</p></li><li><p>Decreases with increased viscosity</p></li></ul><p>Shear: </p><ul><li><p>Increases with increased size</p></li><li><p>Increases with increased shear rate</p></li></ul><p></p><p>N = number concentration of particles, k<sub>B</sub> = Boltzmann constant, T = absolute temp., η =</p><p>dynamic viscosity, w = stability factor, φ = volume fraction of particles, γ = shear rate</p>
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9

Stability factor w

w=1 →  each collision leads to aggregation (high possibility of flocculation) 

w=106 → one collision in a million leads to aggregation

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Comparison between shear and brownian flocculation

do=0.1 ÎĽm

Small particles flocculate quickly due to Browian but then it is too big and slow down 

Brownian: Initially rapid, but then slowly

Shear: In the beginning, it is slow, but then rapidly increases 

do=3 ÎĽm

Shear: Rapid growth of particle size. Large and likely to meet than small particles in shear-like movement. 

Browian: Slow. Larger particles have a slower diffusion so it takes them longer to randomly meet 

<p><u><span>d<sub>o</sub>=0.1 ÎĽm</span></u></p><p><span>Small particles flocculate quickly due to Browian but then it is too big and slow down&nbsp;</span></p><p><span>Brownian: Initially rapid, but then slowly</span></p><p><span>Shear: In the beginning, it is slow, but then rapidly increases&nbsp;</span></p><p><u><span>d<sub>o</sub>=3 ÎĽm</span></u></p><p><span>Shear: Rapid growth of particle size. Large and likely to meet than small particles in shear-like movement.&nbsp;</span></p><p><span>Browian: Slow. Larger particles have a slower diffusion so it takes them longer to randomly meet&nbsp;</span></p><p></p>
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Fractal aggregates (flocs)

Aggregates that occupy a larger volume than the individual particles are called fractal aggregates or flocs

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Repulsive interactions and aggregate structure

Repulsion dominates → dense flocs

<p><span>Repulsion dominates → dense flocs</span></p>
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Attractive interactions and aggregate structure

Attraction dominates → less dense flocs

<p>Attraction dominates → less dense flocs</p>
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Larger fractal flocks

Larger structure but lower density → more rapid sedimentation

<p>Larger structure but lower density → more rapid sedimentation </p>
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Smaller fractal flocks

Higher density

<p>Higher density </p>
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Ostwald ripening and laplace pressure

Ostwald ripening riven by the Laplace pressure

• Molecules from smaller particles dissolve and diffuse to larger particles

• Occurrence and rate also depend on the solubility disperse phase molecules in the continuous phase

– Low solubility slows it down or inhibits it

• Also referred to as ”disproportionation” in foams

We have pressure and high surface tension. We need solubility

If this has low solubility in the continuous phase, process slowed down 

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17

Dispersion rheology

Higher viscosity is the result of particles disturbing the applied flow field and particles ”bumping into each other”.

In pure liquids: viscosity is the result of friction between molecules.

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18

Relative viscosity relation to volume fraction

Higher volume fraction —> higher relative viscosity

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How does aggregation/flocculation affect viscosity?

  • Dispersed particles in continuous phase

  • Flocculation occurs → Viscosity decreases

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How does breaking up aggregates affect viscosity?

More particles flowing around bumping into each other → Viscosity increases

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