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2004-06-29_PERMIT FILE - C1981038 (3)
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2004-06-29_PERMIT FILE - C1981038 (3)
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Last modified
8/24/2016 3:16:04 PM
Creation date
10/20/2014 12:54:01 PM
Metadata
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Template:
DRMS Permit Index
Permit No
C1981038
IBM Index Class Name
Permit File
Doc Date
6/29/2004
Doc Name
Colorado Discharge Permit (NPDES)
Section_Exhibit Name
Volume 7 Exhibit 02 Section 7 Consultation
Media Type
D
Archive
No
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19 <br />was very similar to their availability durins sutra e:. As in the suttuner, backwaters, eddies, and <br />pools were the preferred types of habitat in the w'.-:er. However, whereas eddies were most <br />preferred in summer, pools were most preferred in winter. Adult pikeminnow used fewer habitat <br />types overall during winter than during summer. Although fast runs and riffles were used during <br />the summer, they were not used during the winter. The colder water temperatures in winter <br />which cause lower metabolic rates may account for the avoidance of hish velocity sites. <br />Absolute area of pools increases as flows decrease and slow- runs lose velocity. Because <br />Osmundson et al. (1990 did not sample low• flows in the winter, they could not determine if <br />pools would still be preferred in the winter at lower flows. <br />Spring (April-July): Osmundson and Kaeding (1989) reported that pikeminnow use of low <br />velocity habitats such as backwaters and flooded gravel pits is greatest during the spring runoff. <br />It is believed that pikeminnow use these habitats during the runoff to escape the high velocity, <br />low temperature flows of the main channel. Because backwaters, flooded gravel pits, and other <br />low velocity habitats aze considerably warmer than the main channel during the runoff, these <br />habitats allow pikeminnow to extend their growing season substantially. The earlier watming of <br />these habitats may also be important in enabling pikeminnow to reach spawning condition by the <br />time flow and temperature in the main channel are optimum for spawning. Osmundson et al. <br />(1995) reported that, in the 15-mile reach, the numbers of backwaters and flooded gravel pits <br />increases with increasing spring flows. (Although the number of backwaters eventually <br />decreases as increasing flows convert backwaters to sidechannels, the number of other low <br />velocity habitats likely increases as increasing flows inundate additional bottomlands.) The <br />decrease in the magnitude, duration, and frequency of high spring flows, then, decreases the <br />quantity and the duration and frequency of availability of important low velocity, higher <br />temperature habitat in the spring. This could be affecting pikeminnow• growth and spawning <br />success. <br />Also, the quantity and frequency of availability of inundated floodplain depressions used by <br />razorback suckers for spawning is dependent on the magnitude and frequency of spring flows <br />necessary to inundate these areas. The decrease in the magnitude and frequency of spring flows <br />necessary to inundate floodplain depressions is believed to be lazgely responsible for poor <br />razorback sucker spawning success. <br />Bioloeical Environment <br />Food supply, predation, and competition aze important elements of the biological environment. <br />Food supply is a function of nutrient supply and productivity, which could be limited by the <br />presence of contaminants. The modification of flow regimes, water temperatures, sediment <br />levels, and other habitat conditions caused by water depletions has contributed to the <br />establishment of nonnative fishes. Predation and competition from nonnative fishes have been <br />clearly implicated in the population reductions or elimination of native fishes in the Colorado <br />River Basin (Dill 1944, Osmundson and Kaeding 1989, Behrtke 1980, Joseph et al. 1977, <br />Lanigan and Berry 1979, Hinckley and Deacon 1968, Meffe 198, Propst and Bestgen 1991, <br />
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