B8 evidence
Panther block
Soil losses across LTEP stands
The amount of soil lost was estimated by assuming that rocks (soil particles >4-mm diameter) would not be affected by water or wind erosion.  Thus, when more rocks are found in upper horizons after the fire than before, the amount of associated smaller mineral and organic matter can be assumed to have been lost.  Quantitative volumetric sampling across stands permits stand-scale interpretations.
Initial results:
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Text Box: Percent of horizon lost
Percent of
horizon lost
Text Box: O horizon
O horizon
Text Box: O horizon
O horizon
Text Box: O horizon
O horizon
Text Box: O horizon
O horizon
Text Box: O horizon
O horizon
Text Box: O horizon
O horizon
Text Box: A horizon
A horizon
Text Box: A horizon
A horizon
Text Box: A horizon
A horizon
Text Box: A horizon
A horizon
Text Box: A horizon
A horizon
Text Box: B1 horizon
B1 horizon
Text Box: A horizon
A horizon
Text Box: B1 horizon
B1 horizon
Text Box: B1 horizon
B1 horizon
Text Box: O horizon
O horizon
Text Box: A horizon
A horizon
Text Box: B1 horizon
B1 horizon
The organic (O) horizon was entirely lost from all stands burned at the Panther Lake block.
The uppermost mineral horizon (A) was lost from 5 of 7 stands.
Even some of the lower mineral soil (B1) was lost from 4 of 7 stands.
Observed temperatures are weakly related to soil loss.
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Text Box: B1 horizon
B1 horizon
Text Box: B1 horizon
B1 horizon
Text Box: B1 horizon
B1 horizon
Control,
no-action
Late-succession, hi-wood
Late-succession, lo-wood
Douglas-fir, hi-wood
Pioneers,
hi-wood
Douglas-fir, hi-wood
Pioneers,
lo-wood