As for the fires, there are many issues, such as fuel type and oxygen supply. I used a smoldering combustion model because that's the SLOWEST type of self-sustaining combustion there is. It also defines a minimum heat flux from which I derive a fuel consumption rate of about 2 kg/s. (I think, I need to check this!)
Hi Dr. Greening,
I can address that point. While smoldering in open air requires a certain minimum combustion rate to be self-sustaining, there is no minimum rate to speak of when the heat is thoroughly contained. Imagine a fire-brick kiln, containing a cellulose fire that has been sustained for long enough to have heated the fire-brick to an equilibrium condition; that is, the rate of heat flow through the brick equals that rate of heat radiation and convection from the outer surface which in turn equals the rate of heat release by the fire, less the rate heat is vented via smoke. A temperature profile through the thickness of the walls would be roughly linear except for a steeper drop toward ambient temperature near the outer surface.
Now imagine adding another layer of fire brick on the outside of the kiln, equal in thickness to the first. If the airflow is adjusted so that the temperature inside stays the same, a new equilibrium will be reached, in which the center (formerly the outer surface) of the wall will be approximately midway between the inside and outside temperature, and the slope of the curve, since it spans the same temperature range but now has twice the extent, will be less. This means the rate of heat flow through the container is reduced. Thus we must reduce the combustion rate (which we can do by reducing the air flow) in order to maintain the same inside temperature as before.
A similar effect occurs if we simply scale up the size of the kiln. Heat loss relative to the volume of the combustion region decreases, hence the rate of airflow per quantity of fuel, and the mean rate of combustion per quantity of fuel (that is, the time the fuel will last), will be less at a given interior temperature.
(An extreme example of this is the sun. It's the sun's thickness, not the rapidity of its nuclear reaction, that makes it, especially its interior, so hot. The heat release rate per unit volume is actually extremely low -- many orders of magnitude less than, for instance, the heat generated chemically by living tissue -- which accounts for how it can be expected to continue to burn for billions of years.)
Sustaining combustion requires only sustaining a temperature at which oxygen introduced will react with fuel. Sustaining a certain reaction rate is not, in and of itself, a requirement. The more effectively the heat is trapped, such as by thick masses of insulating debris and by trapping large combustion zones, the longer the fuel will last at a given interior temperature.
CC's approach of determining the combustion rate by the total amount of smoke released (somehow derived from the air quality measurements) is a whole different way to look at the problem. I'd be interested to see his calculations on that.
Respectfully,
Myriad