Yesterday (February 27, 2018) we did the annual burn of the
tallgrass prairie on the south slope of Pleasant Valley Conservancy State Natural Area.
Because of the extensive bur oak
savanna on the upper ridge, most of the burn was conducted as a backfire.
However, there are no trees on most of the lower slope so to speed up the
process, a headfire was used.
The principle fuel is little bluestem and Indian grass, with a few patches of big bluestem.
Yesterday the wind was gusty and variable, so that the grass
burned either quietly or in quick bursts as the wind intensity varied. The photo below is typical of the headfire.
Headfire behavior. The flame has just been caught by a sudden gust of east wind (0648.jpg) |
After the burn was over, Kathie noticed that on the lower
slope the fire residue was in narrow linear strips, with white ash alternating
with black ash (black char).
According to the fire literature, white ash is a
product of complete combustion and black ash is the result of incomplete
combustion. I assume that when a strong gust of wind passed over the burning
grass, the burn temperature rose and complete combustion occurred, leading to
white ash. When the wind was less strong, the temperature was less, and
incomplete combustion produced black ash. The interesting thing is that there were several alternating strips of white and black.
The smoke in the photo below shows the linearity
of the wind.
Fire behavior showing possible origin of the linear strips. The flames have just been caught by the wind. (0640.jpg) |
Unfortunately, I did not get a photo of the long linear
strips, but the photo below shows short strips of white and black ash from the same burn.
White ash is primarily inorganic substances such as
potassium hydroxide, potassium carbonate, and non-alkali substances such as
chloride and sulfate salts. The fragile leaf structure may be maintained temporarily
but quickly disintegrates. Black ash (char) is primarily amorphous carbon.
Per NOAA, Feb 27 noon was 55 F and 55% RH. Wind 8-10 mph
from south. However, at PVC, the wind often shifted to the east.
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