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ENVIRONMENTAL CONSEQUENCES in rocky mountain coniferous ...

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Natural <strong>in</strong>oculation of residues may occur <strong>in</strong> two ways: through spores and<br />

through vegetative hyphal growth. Spore <strong>in</strong>oculation may occur on any surface;<br />

<strong>in</strong>oculation by vegetative hyphae usually will occur only from soil or wood on the<br />

undersides of residue, Initial decay <strong>in</strong> conifer residue occurs on the underside <strong>in</strong><br />

contact with soil and is usually of the white-rot type. Decay on the upper surface<br />

or the sides is usually of the brown-rot type. Aho (19743 states that decay pro-<br />

gresses faster <strong>in</strong> residues <strong>in</strong> contact with the soil .<br />

MOISTURE CONTENT<br />

Moisture avai labil ity is a primary control 1 <strong>in</strong>g factor <strong>in</strong> decay. Pechmann and<br />

others (1967) reported that substrates with moisture contents below 30 percent or<br />

above 120 percent were not colonized by most fungi, particularly decay fungi.<br />

Etheridge (1958) noted that moisture content of heartwood is dependent on species<br />

and site and generally is less than sapwood moisture contents, although there are<br />

exceptions. Etheridge (1958) also noted that even m<strong>in</strong>or changes <strong>in</strong> moisture content<br />

had significant effects on decay rates. Wood <strong>in</strong> contact with the soil readily<br />

absorbs moisture from it. Other factors also contribute to <strong>in</strong>creased residue<br />

moisture cbntent and <strong>in</strong>creased decay: shad<strong>in</strong>g, north-fac<strong>in</strong>g slopes, el evation,<br />

compaction/stratification of wood residues, amount of soil organic matter, and<br />

temperature.<br />

As decay progresses, pore volume of the woody substrate <strong>in</strong>creases, facilitat<strong>in</strong>g<br />

the total amount of moisture that potentially could be present (fig. 4). Figure 5<br />

reflects the effect of pore volume <strong>in</strong> terms of moisture hold<strong>in</strong>g capacity on the<br />

Coram site between the control and clearcut-<strong>in</strong>tensive utilization treatment. The<br />

data <strong>in</strong>dicate the soil-wood moisture contents are not affected by treatment and, as<br />

a result, woody residues <strong>in</strong> this form would alleviate moisture stress <strong>in</strong> clearcut<br />

areas.<br />

200<br />

Moisture<br />

Content<br />

(%)<br />

100<br />

300 Moisture Content<br />

ClTotal Carbohydrate<br />

Total<br />

Carbohydrate<br />

' Content<br />

(% odw)<br />

FCgure 4.-- Relationship between moisture content and d~cay progression<br />

<strong>in</strong> brom-rotfed mugZas-fir. Decay associated uith Fornitopsis p<strong>in</strong>-i-coZa.<br />

(Corn Experimental Forest, September 2977. All moisture content<br />

values significantZy dffferent from each other: sF 0.01).<br />

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