Disperse Systems: Suspensions 7 Flashcards

1
Q

Suspensions

A
  • Is a Coarse Dispersion
    • 500-1000nm (1mm)
    • Visible by microscopy or even naked eye
      • 400-700nm = wv of light (visible)
  • Consist of Solid Particles dispersed in a Liquid Medium
    • except aerosols
      • –> in gas medium
  • ​​Brownian motion is observed for smaller particles
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2
Q

Suspension Dosage Forms

A
  • Oral Suspensions
    • allow delivery of large doses of water insoluble solids
    • typically 10% w/v for easy to swallow liquids
  • Dermatological Products
  • Parenteral Administration
    • particle size matters
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3
Q

Desired Properties of

Oral Suspensions

A
  • Should not settle rapidly
    • ​not form a hard cake
    • Should be readily dispersed to form a uniform mixture with shaking
  • ​Not too viscous
  • Physically Stable
  • These properties should NOT CHANGE during storage:
    • Particle size distribution
    • specific surface area
    • crystallinity / solid polymorphicform
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4
Q

Suspension Agglomeration

2 distinct ways

A
  • Flocculation
    • form loose, fluffy conglomerate
      • held by weak VDW forces
    • Surface area is slightly reduced
    • Sometimes good
  • Aggregation
    • _​_compacted solid cake
      • maximum interparticle surface-surface contact
    • surface area is DRASTICALLY reduced
    • Always Bad
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5
Q

Suspension Flocculation

A
  • VDW attraction
  • Forces of Repulsion are from double layer zeta potential
  • LOW ZETA POTENTIAL
    • Weak atraction results in flocculation
    • 100-200nm (small energy well)
    • –> only MINIMAL shaking will disrupt the floc
  • Sedementation due to gravity will occur
    • But a high energy barrier due to high zeta potential resists further aggregation due to gravity
    • Easily RESUSPENDED
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6
Q

Suspension Aggregation

A
  • Form hard cake under gravity
  • No energy well (dip), when system is Deflocculated
    • Can not form a floc
  • High Zeta Potential
    • particles can approach more closely
    • high surface to surface contact
      • –> results in Aggregation
  • ​​Sedementation
    • difficult to RESUSPEND due to hard cake
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7
Q

Velocity of Sedementation (V)

A
  • Expressed by Stoke’s Law
    • ​​for dispersions containing 0.5%-2% suspended solids
  • Positive V = settles to the BOTTOM (more sedementation)
  • V depends on:
    • diameter of particle
    • Difference of density of particle/medium
    • Gravity accelleration
    • INVERSELY RELATED TO VISCOSITY
      • ​​​Increasing velosity –> Decreases Velocity of sedementation
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8
Q

Brownian Movement

on

Sedementation

A
  • Brownian motion COUNTERACTS sedementation
    • for particles <5um diameter
    • depends on density and viscosity of medium
  • As Viscosity increases -> Brownian Motion decreases
  • Ideally:
    • Density of Medium = Density of Particles
      • NO SEDEMENTATION
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9
Q

Calculating Degree of Flocculation

beta

A

Compare the Volume of sedement (F) for the floc

with

the Volume of the sedement (f infinity) that would have been obtained with COMPLETE deflocculation

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10
Q

Approaches to develop

Suspension Dosage Forms

A
  • Structured Vehicle, used as the dispersing medium
    • Colloidal dispersions of HydroPHILIC polymers in water
    • polymers have negative surface charge
    • polymeric lyophilic colloid has HIGH VISCOSITY
    • Example = KETCHUP
      • Vigorous shaking –>decrease Viscosity
      • Vicosity is effected by SHEAR FORCES
  • ​Design the formulation to promote CONTROLLED FLOCCULATION
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11
Q

Wetting of Particles

A
  • Particles need to be thoroughly wetted by the dispersion medium
    • HYDROPHILIC substances are EASILY WETTED
    • HydroPHOBIC substances are DIFFICULT to wet
      • large CONTACT ANGLES
      • ​​initially covered by air molecules
        • Adsorbed to the surface
    • Surfactants are often added to:
      • promote wetting
      • INFLUENCE FLOCCULATION
        • Need enough surfactant or else –> deflocculate
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12
Q

Levigation

A
  • Process of grinding a substance under moist conditions
    • Mortar & Pestle
  • Purpose is for particles to be UNIFORMLY COATED WITH THE LIQUID USED FOR LEVIGATION
    • some particle size reduction may occur
  • Always requires a liquid
  • Used to WET particles for SUSPENSIONS
    • Hydroscopic hydrophilic solvents are used
      • alcohol / glycerol / propylene glycol
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13
Q

Trituration

A
  • Process of grinding two or more solids
  • Purpose is to REDUCE PARTICLE SIZE
    • and to uniformly mix the two particles
  • NO LIQUID
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14
Q

Controlling Flocculation

A
  • We DO NOT want systems to DEFLOCCULATE
  • Structured Vehicles help prevent content uniformity
    • Retart sedementation of the floc
  • ELECTROLYTES acts flocculating agents by
    • DECREASING ZETA POTENTIAL
    • and forming salt bridges that link particles in a loose structure
  • CONCENTRATION of electrolytes is CRITICAL
    • Too low –> zeta is too HIGH –> deflocculation
    • Too MUCH –> zeta potential reverses and becomes large
    • IDEALLY WANT ZETA POTENTIAL CLOSE TO ZERO
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15
Q

Rheologic Considerations

Relating to flow

A
  • Seen with Plot of Shear Rate vs Sheer Stress
  • We want PSEUDOPLASTIC FLOW
    • NONLINEAR
    • Steep RISE at higher stress
    • High viscosity at low shear force
    • low viscosity at HIGH shear force
      • ​ex. Tragacanth / Sodium alginate
  • ​**Do not want NEWTONIAN FLOW
    • ​straight line
    • ex. GLYCERINE
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16
Q

Thixotropy

A
  • Become Less and Less Viscous
    • ​when Stirred
  • BUT become more and more Viscous
    • ​upon SITTING
  • THINK KETCHUP AND YOGURT
    • Examples of thixotropic Gels
  • SHOW PSEUDOPLASTIC BEHAVIOR
    • good suspending agents
    • CMC + MIcro Bentonite
17
Q
A
18
Q

Physical Stability of Suspensions

A
  • HEATING
    • Cause suspensions to FLOCULATE
      • esp those w/ NONIONIC surfactants
      • become less hydrophilic with heat (CLOUD POINT)
  • FREEZING & THAWING
    • induces aggregation / caking
      • due to pressure generated by crystal formations
  • Temperature cycling
    • can cause Particle Growth
    • warming –> dissolve
    • Chilling –> precipitation
  • SMALL PARTICLES GET SMALLER AND BIG PARTICLES GET BIGGER
    • ​= THERMODYNAMICS
19
Q
A