Many years ago I did my graduate research on the measurement
of airborne insoluble particles. These often
occur from the generation (e.g., spraying or cutting),
transport or disturbance of liquids, powders or dusts.
Because of all the work and study
I did with these aerosols, I have maintained an interest in this subject.
Of course, airborne particles are a lot different than vapors. Compared to vapor molecules they are a lot
bigger. Indeed, they have a lot more
mass and instead of being mixed in with the other gaseous molecules in air,
they are more or less suspended into the air. Depending on their size they tend to settle downward
either quickly or slowly. Indeed, knowing the size of the particles is
important for other reasons because size determines whether a particle is
inhaled and, once inhaled, its chance of making it into the deep lung where gas
exchange takes place.
The population of insoluble airborne particles from any source
is almost always of variable size which makes the characterization of that size
somewhat challenging. The sizing of a population of aerosol particles will be the subject of next week's blog.
A logical and somewhat convenient way of “sizing” any individual airborne particle is by its aerodynamic diameter (AD). This
convention compares the settling velocity of the particle of interest to that
of a unit density sphere. Thus
particles of any density or shape can be characterized for how they will react
in the air using this method. It is
interesting to note that I once measured the aerodynamic diameter (AD) of one of my
kid’s balloons at about 150 microns (AD).
That is a foot long balloon fell to the ground at about the same rate
as a unit density sphere with a diameter of 150 microns (0.015 mm). On
the other hand, 1 micron sphere of mercury will have a much larger AD than 1
micron but you get the idea.
Indeed, the science of aerosols is quite interesting. Very small particles “see” or experience the
air as a very viscous medium compared to their larger brothers. The
more viscous the air appears, the more the particles tend to move with the
airstream and not charge through it. An analogy for us would be that we are very free to move (at least horizontally) through air but we will
be much more “stuck” and restricted if we were immersed up to our necks in
molasses. In that case if the molasses moved we would move with it.
As mentioned above the AD size of any particle determines
where in the body it might deposit. Three
size measurement classification or “bins” of AD have been defined by the ACGIH going from large
to small sizes:
- INHALABLE: any particle that penetrates/deposits past the nose and mouth.
- THORACIC: particles that penetrate/deposit anywhere within the lung airways and the gas-exchange region
- RESPIRABLE: particles that penetrate/deposit exclusively into the gas-exchange region or pulmonary region of the deep lung.
The above
classifications describe the proportion of any particular AD size that will fit
into that classification or bin. For
example a particle that is 10 microns AD will be considered 77% inhalable, 73% Thoracic and 1% respirable if I read the ACGIH criteria algorithms
correctly. That is, this particular
particle will have a 77% probability of being inhaled, a 73% probability of
making it to the thoracic region of the respiratory tract and a 1% chance of getting to the alveolar or pulmonary region of the lung.
If you are interested in studying this further I have a set
of Power Point slides that goes into a lot more detail including the algorithms
which I will be happy to send to whoever ask me at mjayjock@gmail.com
So what does this mean for the inhalation of insoluble
particulate? When the airborne particle
size is respirable (less than 10 microns AD) a good portion of it makes it to
the alveolar region of the lung. The
clearance mechanism for insoluble particles in this region of the lung is quite
slow. As such a daily exposure to respirable particles tend to
accumulate and potentially overwhelm the clearance mechanism. This has been termed particulate overload and
can lead to irritation and irreversible toxic effects such as Chronic
Obstructive Pulmonary Disease (COPD).
I am not a toxicologist but for many years I have been of
the opinion that the OEL for insoluble “Nuisance Particulate” or the more
modern term: Particles No Otherwise Characterized (PNOC) should be around 1
mg/m3 (respirable) which is considerably lower than it has been. I base this view on my review of some of the earlier
toxicological studies and conclusions.
Some of these references, data and conclusions are included in the above
mentioned Power Point slide deck.
If you got the above Power Point deck you will notice that the references within it are somewhat dated and relatively limited. This is, they are certainly limited compared to the very thorough treatment given this subject by John Cherrie et al in a commentary published last year:
ReplyDeleteA Commentary for the Annals of Occupational Hygiene: Low-Toxicity Dust: Current Exposure Guidelines Are Not Sufficiently Protective. doi: 10.1093/annhyg/met083. This is a well researched piece with a very well developed argument for having the OEL at 1 mg/m3 at least for now. I found a free copy of it at: http://annhyg.oxfordjournals.org/content/57/6.toc
An Interesting issue is that in ambient air/public health context even very low concentrations of dust (as PM2.5 fraction) are considered hazardous . A current WHO guideline is 10 ug PM2.5/m3, but linear extrapolation is applied to the whole general pupolation. This leads to very high morbidity/mortality numbers (heart attack mortality, lung cancer incidence).
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