Particle size Flashcards

1
Q

Why is particle size measurement

important?

A

• Size influences physical properties of pharmaceutical materials
– Powder flow, tablet formation

• It tells us if a process has been successful
– Milling of a solid; homogenization of emulsions

• Gives an indication of product stability
– Emulsion droplet size on storage

  • Quality control of products – Increases confidence that a product is same as previous batches
  • Indicative of in-vivo behavior – Absorption rate of insulin from IM injection depends on crystal size – Nanosized particles can accumulate in ‘leaky’ cancerous tissues via EPR effect (enhanced permeability and retention)
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2
Q

Equivalent diameters

A
  • We need to find a way of defining a single size for a particle that may be irregularly shaped
  • To do this we use the concept of equivalent diameter – the diameter of a sphere that is in some unique way similar to the particle in question
  • Simplest to do this by volume
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3
Q

What is dV

A

Simplest is Volume Equivalent Diameter (dV) – the diameter of a sphere that has the same volume as the irregular particle – it’s unambiguous, as particles have a well-defined volume

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4
Q

Distributions of particle size - mode

A

Size with most particles is called the mode

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5
Q

Distributions of particle size - mean

A

the weighted arithmetic mean size

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6
Q

Distributions of particle size - median

A

the size with half the particles on each side

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7
Q

Distributions of particle size - standard deviation

A

The width can be defined as the standard deviation

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8
Q

Cumulative frequency representation

A

This is the percentage of particles above or below a given size

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9
Q

Techniques for measuring particle size

A

– Sieving
– Sedimentation
– Microscopy
– Light scattering

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10
Q

Choice of technique to measure particle size depends on

A
– Applicable size range for sample
– Cost
– Time taken
– Skill required
– Precision
– Quantity of material needed
– How much data they provide (e.g. full distribution or just an average)
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11
Q

Sieving

A

• Oldest method, inexpensive, widely available
• Separates fine material from course material by means of a series of woven or perforated surfaces. The proportion of different size particles are recorded and analysed.
• Sieves are precision-woven square mesh, from steel or
bronze wire
• Smallest size is about 50 µm – smaller particles don’t pass through readily, fine meshes are easily damaged and clogged
• Method defines a ‘sieve equivalent diameter’ – the size of the sphere which will pass through the square hole

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12
Q

Sieving method

A

• Standard size sieves stacked into a ‘nest’ of decreasing mesh size – bottom is a closed tray
• Sample put in top and shaken - particles fall through until mesh size is too small – at which point the particles
will be retained
• When shaking is completed, the amount of particles in each sieve is weighed

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13
Q

Errors in sieving

A

• Errors are readily visualised with sieving.
– Sieve holes may vary in size due to manufacture or damage – Powder may coat the wires leading to sieve apertures being reduced
– Particles may be cohesive – stick together so that they don’t pass through the mesh
– Vibration from shaking may damage the particles leading to erroneous ‘fines’
– Stack may not be shaken for long enough to get particles to their final sieve
– Sieve may be overloaded – only works well for a light load
– Particle shape may cause problems (e.g. needle-like particles)

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14
Q

Sedimentation - theory

A
  • The rate at which suspended particles settle has long been used for size measurement
  • The connection between particle size and settling rate or ‘sedimentation velocity’ is given by Stokes’ law
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15
Q

equation

A

v = 2r2 (ρ2-ρ1)g/9η

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16
Q

Sedimentation in practice

A
  • Settling velocity is not measured directly
  • Can measure the amount of material settled in a particular time (e.g. on to an immersed balance pan) – a sedimentation balance
  • Can measure the amount remaining in suspension vs time by passing a beam of light or x-rays through the sample
17
Q

How does gravity effect settling

A

Because settling can be slow under gravity, instruments usually use centrifugal sedimentation to speed things up - g in Stokes’ law is then replaced by r2ω, where r is the centrifuge radius and ω the angular velocity

18
Q

Andreasen pipette

A

Remove samples over time (hours/days) and analyse for particle content; calculate size distribution

19
Q

Sedigraph III

A

Insert sample and push button

20
Q

Microscopy and image analysis

A
  • More sophisticated and expensive technologies
  • Many different types of microscopy e.g.. Light, electron, atomic force etc.
  • Uses very small volume of sample
  • Measures 1 nm – millimetres depending on technique
  • Computer thresholds image then simply counts pixels in each region, constructs histogram, computes statistics as required
21
Q

Disadvantage and advantage of Microscopy

A

Disadvantage- Measures relatively few particles
Advantage - One of the few methods of getting
shape information

22
Q

Particle size analysis by light scattering and its advantages

A

• Light scattering methods now account for the majority of size measurements and instruments

• Advantages:
– Rapid
– Easy to use
– Wide applicability
– Wide size range
23
Q

The diffraction pattern

A

determined by the particle size and shape

Given the particle size we can compute the scattering
pattern – its not a simple calculation!

24
Q

Disadvantage for light scattering

A
  • Measuring the diffraction pattern

* Finding the particle size distribution from it

25
Q

Operation of a laser diffraction sizer

A
- Particles in dilute suspension
Scattering is measured from many particles
- Laser light source
High intensity
Single colour
single direction
- Array detector
Similar to digital camera sensor
Measures light intensity at each point
26
Q

How does the calculation work?

A
  • It guesses the size distribution! (The ‘trial’ distribution)
  • It calculates the scattering pattern of the trial distribution
  • It compares the trial distribution scattering pattern with the measured scattering pattern (of course they don’t match at first)
  • It adjusts the trial distribution
  • Recalculates scattering pattern of trial distribution
  • Goes round loop, adjusting trial distribution until its scattering pattern is the same as the measured scattering pattern
  • The size measured is a representation of the hydrodynamic radius, this is defined as the size of a sphere that moves at an identical rate to the particle
27
Q

Particle counting

A
  • Problem with previous methods is that they tell you the size distribution, but do not tell you how many particles are present.
  • For some applications, the number of particles is critical (e.g. cell counting, or particle contamination in injections).
  • The classic instrument for this is the Coulter Counter or electrical zone sensing (EZS) technique
28
Q

Electrical zone sensing

A
  • The volume of suspension drawn through the aperture is determined by the suction potential created
  • Now lets put an electrode in each chamber and add a battery; the only way we could pass a current through the circuit would be if it goes through the aperture:
  • If a particle is sucked through the aperture, it will briefly occlude the hole and stop part of the current reducing the electrical current.
  • We can suck a known amount of suspension (e.g. 1 ml or 10 ml) through the aperture and the instrument will count the number of times the current is blocked.
  • From the amount of blockage we can also measure the size of each particle, and the instrument can build up a size distribution
  • Sufficiently small apertures (15 micrometres is the smallest commercially supplied aperture)
29
Q

Optical particle counting

A

• A similar particle counter can be made using optical sensing of particles
• Particles in dilute suspension are passed through a narrow beam of light
• As they pass they cast a shadow which is measured by a
photodetector
• This is the principle of the Hiac counter which is the method used in pharmacopoeial tests for particles in injections