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WSPC12531 (2)
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WSPC12531 (2)
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Last modified
1/26/2010 4:18:41 PM
Creation date
10/21/2007 11:13:12 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8220.101.10
Description
Colorado River Water Projects - Glen Canyon Dam-Lake Powell - Adaptive Management
State
CO
Basin
Colorado Mainstem
Date
3/1/1998
Author
Unknown
Title
Narrative for Biological Resources - Kanab Ambersnail - Distribution and Abundance - 03-01-98
Water Supply Pro - Doc Type
Report/Study
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<br />002~94 <br /> <br />high sustained releases that followed the BHBF and inundated previously drier habitats. <br /> <br />As with the earlier flood, a 2-day 45 k flow will once again bury the grass <br />/ herb layer in New High Water zone patches below 40 kcfs. This layer, made up of herbs and <br />perennial grasses for the most part, as well as some seedlings and saplings of larger species, has <br />shown some recovery in the past two years, given the high summer flows which promote growth. <br />The nutrients in these habitats, mostly locked up in plant tissue, will not be mobilized, since the <br />plants will be buried in place. Larger woody individuals will have some bark and branches (and <br />leaves if the flows occur much after Aprill) stripped during the flows, but there will be little <br />uprooting or outright mortality directly attributable to the flows. <br />Assessment: will negatively affect riparian vegetation (but the effects will be less than <br />spectacular) . <br /> <br />Similarly, the soil seed bank will be buried again under sterile sand from <br />the channel bottom and elsewhere in the eddy complex. As with the grass / herb layer, the soil <br />seed bank has shown some remarkable signs of recovery in the past two growing seasons. A two- <br />day 45kcfs flood will likely cause another loss on the order of 60% of the individuals and 40% of <br />the species present in New High Water zone vegetation patches. Assessment: will negatively <br />affect the soil seed bank. <br /> <br />Marshes in return current charmels will likely be buried under - 50 cm of <br />sediment again, and green plants will likely be knocked over and flattened. The effects will <br />depend on the timing and subsequent flows. <br /> <br />Assessment: will negatively affect the marsh vegetation, but flows before mid-April <br />will hilVe less impact than those after (the investment in green tissue will be lost), and if high <br />flows follow the flood, the impacts will be less visible after 6 months. <br /> <br />Impacts on riparian habitat follow the above assessments. <br /> <br />LITERATURE CITED <br /> <br />Aldrich, l.W. 1951. A review of the races of the Traill's flycatcher. Wilson Bull. 63(3): <br />192-197. <br /> <br />Aldrich, J.W. 1953. Habitats and habitat differences in two races of Traill's flycatcher. <br />Wilson Bull. 65(1): 8-11. <br /> <br />Arizona Game and Fish Department. 1996a. Ecology of Grand Canyon backwaters. Final <br />Report to U.S. Bureau of Reclamation, Glen Canyon Environmental Studies, Flagstaff, <br />AZ Arizona Game andFish Department, Phoenix. <br /> <br />Arizona Game and Fish Department. 1996b. The effects of an experimental flood on the <br />aquatic biota and their habitats in the Colorado River, Orand Canyon, Arizona. Arizona <br />Game and Fish Department, Phoenix. <br /> <br />Ayers, A.D., and T. McKinney. 1 996a. Lake Powell forebay and Glen Canyon Dam <br />tailwater to Lee's Ferry during interim flows: particulate organic matter transport, nutrient <br />
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