Dear Harold

I think there may be an additional "fire mechanism" associated with coal, that 
is not associated with charcoal. Almost invariably, coal has sulphur, in the 
form of FeS2 (pyrite) or pyrrhotite, 
FeS(1-x). When it is exposed to air and water, plus microbial action, it 
oxidizes readily. In addition, of course, there are many organic compounds in 
the coal, and some of them may also oxidise on their own accord, perhaps being 
hastened or accelerated by the heat from the biological reactions.

Charcoal does not have sulphur in the sulphide form, so one of the possible 
"ignition mechanisms" in coal is absent in charcoal. However, I recall reading 
somewhere, and unfortunately don't have the reference now, that under certain 
conditions, the production of charcoal can yield "products of pyrolysis" that 
are pyrophoric, ie, they ignite when exposed to air. As I recall, these 
pyrophoric compounds were produced relatively easy, when charcoal was produced 
under vacuum conditions. I don't recall if such pyrophoric products can be made 
in atmospheric pressure retorts, or in "air blown" charcoal making devices.

Best wishes,

Kevin
  ----- Original Message ----- 
  From: Harold Annegarn 
  To: Discussion of biomass cooking stoves 
  Cc: James Robinson ; Glenn Stracher 
  Sent: Saturday, February 23, 2013 4:49 AM
  Subject: Re: [Stoves] combustion of char


  Response from Harold Annegarn


  I make reference not to char, but to coal. Perhaps the same will apply to 
freshly prepared char surfaces.


  The following information arises from the phenomenon of spontaneous 
combustion in underground coal and in coal slag heaps. 


  Exposure of freshly broken coal surfaces, or in situ coal that has been in 
water filled voids that is subsequently exposed to air (oxygen) (as occurs when 
previously mined areas by bord & pillar extraction is exposed by strip mining) 
results in a chemical reaction known as oxysorption ==> oxygen reacts with 
carbon/carbonaceous matter at the surface of the coal in an exothermic reaction 
that results in the oxygen being absorbed into the chemical structure of the 
coal without necessarily being emitted as CO.. This oxysorption can occur at 
room temperatures and does not require elevated temperatures or a spark to 
start. 


  Thereafter, basic physics applies: if thermal energy is released from a 
chemical reaction, that heat is either conducted, convected or radiated away. 
If the rate of production is faster than the rate of dissipation, then the 
temperature will rise in the zone where the oxysorption is taking place. The 
balance between conduction, convection and radiation may change as the local 
temperature increases; likewise the reaction rate will increase. There must be 
some convection possible, otherwise the available oxygen will be consumed and 
the process will stop, If the local convection is large, then the surface 
remains cool and the reaction proceeds without large temperature rise. If the 
convection is limited, local temperature will increase, and eventually may 
reach the point where volatile matter that is driven off reaches ignition 
point, i.e. spontaneous combustion has commenced. 


  It is not a matter of whether spon com occurs, it is just a matter of when. 
For this reason, modern practise of stockpiling coal discards and fines 
requires continual compaction of the surface to limit air ingress, and final 
sealing of surfaces with a meter or more of soil.


  Although I I have not read anything about oxysorption on char, it is logical 
that similar processes are occurring, The char is a freshly prepared surface 
with high specific surface area due to the voids created by driving off 
volatile material, and with many dangling bonds at these surfaces. Not for 
nothing is this material also known as "activated charcoal" with good 
properties for absorbing ions e.g. from water for water purification.
  .
  To test this it would be possible to char wood in a dry nitrogen or helium 
stream, although this would result in a different surface chemistry than if the 
same material is passed through the same heating cycle in the presence of 
oxygen. If the material is then cooled, and placed on a balance with automatic 
recording, the the change of weight with time can be recorded. If this is done 
in a closed system, with dry air passed over, then one could isolate the effect 
of oxygen absorption from the absorption of H2O from the atmosphere if this was 
done in open laboratory air with variable relative humidity.


  In the case of the spontaneous combustion accident described by Frank 
Shields, it appears that the raising of the temperature to just over 100 
degrees C assisted in creating a heat generation rate and oxygen supply to the 
char samples that allowed the oxysorption to proceed to the point at which full 
ignition commenced - yes, he is lucky to have a lab still!


  I have copied this message and thread to Glenn Stracher, an expert on 
spontaneous combustion on coal, who has a much deeper understanding of these 
matters than the qualitative handwaving that I have given above.


  Best regards
  Harold



  On 23 February 2013 03:43, Frank Shields <[email protected]> wrote:

    Stovers,

    FYI
    After having about 30 compost samples in a drying oven go up in flame it
    looked like it started with a single char sample placed in the corner. I
    decided to do a little research by asking Hugh McLaughlin. Another question
    I had for him was why does some biochar samples gain weight in a drying oven
    set at 105c.

    So it seems soon after a char is produced it wants to take up oxygen. If
    bagged in a sealed container and sent to the lab soon after being made the
    dry sample will take up oxygen in the oven therefore gaining weight. If a
    sample is wetted soon after being made the water prevents oxygen from being
    taken up. Then if it becomes dry it wants oxygen, increases temperature and
    can catch fire under the right (wrong) conditions. Char is a great insulator
    so the heat can be trapped and build up. If there is organic materials
    around it can flame. So before storage better give it time to take up
    oxygen. Or if wetted do not let it dry out and keep bags of char in single
    layers.

    The forced air drying oven was left on overnight and it was in the morning
    we found all the burned up samples. It was placed against the wall so we are
    lucky we still have a lab!

    Regards

    Frank




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  -- 
  Harold Annegarn
  Department of Geography Environmental Management and Energy Studies
  University of Johannesburg
  Mobile +27 (0)83 628 4210 
  Fax +27 11 559 2430
  Office +27 11 559 3927



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