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ENVIRONMENTAL CONSEQUENCES in rocky mountain coniferous ...

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8 C CLEARCUT. BURN<br />

I Prescr~bed Ftre /<br />

Figure 8.-- Effects of harvest<strong>in</strong>g treatment on soil pH <strong>in</strong> a h u s Zayer (02) of a<br />

Doug Zas-fir/western Zarch/subaZp<strong>in</strong>e ffr s6and (Montuna) .<br />

The effects of post-harvest burn<strong>in</strong>g treatments on the levels of available N show<br />

a def<strong>in</strong>ite relationship to the soil component exam<strong>in</strong>ed (Figure 9). These results<br />

from the Coram study show that before the prescribed fire, total amounts of NHq and<br />

NO3 <strong>in</strong> the organic layers were approximately equal to that present <strong>in</strong> the surface 30<br />

cm of m<strong>in</strong>eral soil. After the fire, available N levels <strong>in</strong> the surface organic hori-<br />

zons and decayed wood <strong>in</strong>creased to double the amount present <strong>in</strong> the m<strong>in</strong>eral layer.<br />

Total N availability <strong>in</strong> the surface 30 cm of soil was highest <strong>in</strong> November-December,<br />

followed by a steady decrease dur<strong>in</strong>g the w<strong>in</strong>ter and spr<strong>in</strong>g months to preburn levels<br />

(Figure 10).<br />

Figure 9.-- Nitrogen avaiZabiZity

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