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ENVIRONMENTAL CONSEQUENCES in rocky mountain coniferous ...

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Recently Harvey and others (<strong>in</strong> process), through 1 4 analysis, ~ have shown that<br />

Douglas-fir (~seudotsup menziesii (Mirb. 1 Franco) residues persist for 500 years or<br />

longer, depend<strong>in</strong>g on the site and depth <strong>in</strong> soil. Our observations, though <strong>in</strong>complete,<br />

<strong>in</strong>dicate that brown-rotted Douglas-fir residue is the most persistent, We tentatively<br />

suggest that resistance to further decomposition is a function of extractives or<br />

extractive-1 i ke substances chemically bound to the I ign<strong>in</strong> polymer <strong>in</strong> Douglas-fir--to<br />

a greater extent than other conifer species.<br />

Appearance and characteristics of brown-cubical decayed wood<br />

The substrate is readily characterized <strong>in</strong> the field by its dark brown to<br />

reddish-brown color and its texture is three-dimensional 1 v checked, form<strong>in</strong>g sixsided<br />

configurations (often referred to as cubical ) (fig<br />

.- 9) .<br />

Figure 9. -- Brown-rotted L@ugZas-ffr shov<strong>in</strong>g fissures and<br />

<strong>in</strong> the subs*rate.<br />

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