My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
WSP10790
CWCB
>
Water Supply Protection
>
Backfile
>
10001-10999
>
WSP10790
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/26/2010 3:14:43 PM
Creation date
10/12/2006 4:32:02 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8507
Description
Rio Grande Project
State
CO
Basin
Rio Grande
Date
7/1/1994
Title
Rio Grande National Forest Analysis of the Management Situation part 1
Water Supply Pro - Doc Type
Report/Study
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
116
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
Show annotations
View images
View plain text
<br />Management Situation by Revision Topic <br /> <br />l <br /> <br />Douglas~fir is more shade tolerant than the pines and aspen, but less tolerant than <br />Engelmann spruce or subalpine fir. Since Douglas-fir can grow under itself, old stands of <br />pure Douglas-fir are usually uneven-aged rather than single-aged. These pure stands <br />originated from fire, but can resist subsequent low-intensity fires. This is because Douglas-fir <br />has rapid growth, a thick corky bark, and the ability to form adventitious roots (roots <br />produced on stems or various types of leaves). Older Douglas-fir stands are rarely more than <br />400 years old, although some may potentially reach an age of 700 years if stand-replacing <br />fires are excluded. Douglas-fir stands on this Forest are usually Jess than 335 years old (Table <br />1/1-4). <br /> <br />,. <br /> <br />White fir is an important component in the upper elevations of the montane zone. White fir <br />is more shade tolerant than Douglas-fir, so in time it can become a prominent part of the <br />community. This portion of the montane zone is sometimes referred to as the mixed conifer <br />type. Historically, natural fires have probably been important in thinning or removing white <br />fir. Douglas-fir is much more resistant to fire than white fir. <br /> <br />Two important seral community species are aspen and lodgepole pine. Aspen generally <br />grows on sites that are moister than sites that support lodgepole pine. Aspen and lodgepole <br />pine can replace ponderosa pine arid Douglas-fir forests where the latter have been removed <br />through disturbance (fire, insects, disease, windstorms, logging, or other disturbance). <br />Sometimes, if a burn is severe and large enough, aspen or lodgepole pine can become a <br />climax community. Essentially, a burn under these conditions removes the seed source and <br />makes invasion by ponderosa pine and Douglas-fir extremely slow. Opinions vary, but aspen <br />and/or lodgepole pine in these conditions has been termed a 'subclimax' community <br />because succession has been interrupted for an extended period. Both species can be seral <br />dominants in the montane zone up through the subalpine zone. <br /> <br />~ <br /> <br />Aspen is more shade intolerant than lodgepole pine. Most aspen regeneration is by <br />sprouting or suckering, rather than by seed. Aspen stands can reach an age of 160 years <br />plus, but the average life span may be 125 years or less. On this Forest, 73 percent of the <br />aspen stands are between 66 and 125 years old (Table 1/1-4). <br /> <br />lodgepole pine's occurrence on this Forest represents the southern geographic range of the <br />species. Older lodgepole pine stands that are 350 to 400 years old can exist, but this is <br />uncommon. The average life span of lodgepole pine is probably closer to 250 years or less <br />because of past stand-replacing disturbances such as fire. lodgepole pine stands on this <br />Forest are generally less than 275 years old (Tilble 111-4). <br /> <br />Crane (1882), Wright (1990), Stokes and Dieterich (1980), and Dr. Phil Omi of Colorado State <br />University (personal communication January 8, 1992 with Dean Erhard) suggest from other <br />research done in the West that the natural fire frequency may have been as follows: 5 to 20 <br />years in dry ponderosa pine stands, 7 to 25 years in wet ponderosa pine stands, 10 to 50 years <br />in dry mixed-conifer stands, and 30 to 150 years in wet mixed-conifer stands. The frequent, <br />low-intensity fires that were common in the ponderosa pine type, has generally been <br />stopped. This may be allowing Douglas-fir to establish itself and fncrease its range at lower <br />elevations in this zone. There also may be a higher probability of large, stand-replacing fires <br />now. <br /> <br />\ <br /> <br />Foothill Zone <br />The foothill zone is that area where the San luis Valley meets the base of the mountain <br />ranges up to the point where the first forest is encountered -- just below the ponderosa pine <br /> <br />111-22 <br /> <br />t'~2435 <br />
The URL can be used to link to this page
Your browser does not support the video tag.