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Asbestos and fibrous minerals - hazards, bioperstence and SEM 
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Asbestos and Other Types of Fibres

 

A rose by any other name…. 
The difference between biosoluble and bioinsoluble fibrous minerals.
 
Image 1: Halotrichite
Image 2: Actinolite
We’ve all seen fibres – they are everywhere. Cotton strings off cloth, fibreglass, carbon fibre. But there’s one word that makes everyone jump to attention. Asbestos. 
What’s actually the difference between asbestos and other types of fibre? 

Asbestos is incredibly useful – it is fine, flexible, strong, heat resistant; the perfect material for all applications. It was added to concrete, paint, rubber, metals – it was the wonder material. Except for the horrible carcinogenicity.

Epidemiologically, it soon* became very clear that known asbestos fibres like crocidolite (fibrous riebeckite) and amosite (fibrous grunerite) caused lung cancers including mesothelioma. Humans began to move away from using asbestos as a cure-all for material shortfalls. 

Humans began to manufacture substitutes - slag wool, glass wool and refractory ceramic fibre were some of the first. Unfortunately, the closer to the other qualities of asbestos they came, the more likely that they were found to be hazardous in the same ways. So what properties of asbestos are so harmful?

As asbestos enters the lung, like any other dust, the depth to which it penetrates is dependent on the equivalent aerodynamic diameter. If the fibre is fine enough to get deep into the lung, the body can’t cough it out and has to use more complex disposal methods. The lungs have a self-cleaning mechanism called ‘alveolar macrophages’ which act like little mouths and enclose nuisance dusts that manage to make their way that far into the lung. The macrophages then immerse the dust in acidic fluid to dissolve it and carry the dissolved material out of the lung to be dealt with elsewhere. 
 
With asbestos fibres, the diameter is small enough to enter the macrophage but the fibre is long enough that it can’t close its ‘mouth’. Because the fibre is not dissolved by the surrounding fluids (it is bioinsoluble), this prevents the macrophage from doing its job and removing the fibre and kills the macrophage in the process. This results in scarring and can eventually lead to mesothelioma and other lung cancers.

This relationship between the diameter:length aspect ratio and the ability of the fibre to kill macrophages is the reason that the fibre definitions for different industries are based on aspect ratio. The three main definitions of a countable asbestos fibre are:
  1. DMP (Department of Mines and Petroleum): < 1 µm diameter, > 5 µm length
  2. NOHSC: < 3 µm diameter, > 5 µm length, aspect ratio of > 3:1
  3. USEPA: > 10 µm length, aspect ration of > 3:1, substantially parallel sides
The other property of the fibres that is significant is the mineralogy, as some minerals are biosoluble (the surrounding lung fluid will dissolve the fibre anyway, even if it isn’t disposed of by the macrophage). Only the bioinsoluble minerals pose a health risk.

Only six different minerals are classified as asbestos. Chrysotile, Crocidolite (asbestiform Riebeckite), Amosite (asbestiform Grunerite), Actinolite, Tremolite and Anthophyllite (asbestiform Cummingtonite). All of these minerals were once sold commercially as asbestos, but they aren’t the only minerals with these properties. Later, it was discovered that other minerals with the same high aspect ratio and bioinsolubility caused the same kind of diseases. Some other hazardous fibres include Winchite, Richterite, and Erionite.

There are also a significant number of minerals that have the same morphology (high aspect ratio fibres) but don’t pose the same risk as the fibres simply dissolve. Some examples are Epsomite, Ettringite, Halotrichite and sometimes simple Halite, or table salt, can form similar fibres. 

So how do you tell them apart? That’s where we come in.

Optical microscopy has historically been used for identifying fibrous materials. It’s quick, cheap and doesn’t require much sample preparation so it’s ideal for a quick check for fibres. However, it has some notable limitations:
  1. Optical miscroscopy has magnification limits which mean that very fine, highly toxic fibres (< 0.5µm in diameter) are unable to be detected;
  2. Optical microscopy can tell limited information about the mineralogy, so often can’t differentiate between biosoluble and bioinsoluble minerals; and
  3. Although Polarised Light Microscopy (PLM) can differentiate some types of asbestos using oils of specific optical properties, the technique can’t identify all types, and can’t identify other minerals, hazardous or otherwise.
Scanning Electron Microscopy (SEM) with Energy Dispersive X-ray Spectroscopy (EDS) can take very high resolution, high magnification images that clearly depict very fine fibres. The EDS determines the elemental composition, which can pinpoint the mineralogy of the fibres and identify whether they fall into the hazardous, bioinsoluble category. In some cases, multiple minerals have very similar elemental composition, and X-ray Diffraction (XRD) can be used to confirm the mineral assignment.
* approximately 30 years later

Nimue Pendragon
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Image of the month

 

This month's image is a thin section photomicrograph of muscovite with the plane-polarised light on the left and the crossed-polarised light is on the right.

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