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Last modified
7/14/2009 5:02:35 PM
Creation date
5/17/2009 10:51:31 PM
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UCREFRP
UCREFRP Catalog Number
9410
Author
Wydoski, R. S. and E. J. Wick.
Title
Ecological Value of Floodplain Habitats to Razorback Suckers in the Upper Colorado River Basin.
USFW Year
1998.
USFW - Doc Type
Denver.
Copyright Material
NO
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<br />Economic, political, and sociological factors are also important and must be <br />considered concurrently with the biological, chemical, and physical factors <br />(Table 5). Nearly all large rivers in the northern third of the Earth have <br />been dammed and regulated to provide water for irrigated agriculture, flood <br />control, hydro-electric power, industry, and domestic use (Dynesius and <br />Nilsson 1994). Humans settled in the corridors of these large rivers largely <br />because the rivers provided transportation and floodplains provided productive <br />agricultural areas and prime areas for industrial development. Humans have <br />and will continue to have a dominating influence on watersheds and river <br />ecosystems that dramatically influences environmental integrity, productivity, <br />biodiversity, and heterogeneity (Frissell et al. 1993). Cairns (1995) <br />emphasized that, to be successful, ecological integrity of aquatic systems <br />must include the sustainable use of water resources by humans. Restoration of <br />large river-floodplain ecosystems to a pristine or virgin state is probably <br />not possible for highly altered systems that are used by humans (Welcome 1989, <br />1995). Instead, Gore and Shields (1995) suggest that the logical approach is <br />to recover some of the ecological functions and values. <br /> <br />I <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br />I <br /> <br />Habitat enhancement or restoration involving river margins (Large and petts <br />1994) must consider biological, economic, political, and sociological factors <br />(Wydoski 1977) and decisions should be made through negotiated adaptive <br />management (Brown 1993; Ludwig et al. 1993; Walters 1986; Walters and Hillborn <br />1978). Because of strong economic, political, and social pressures from <br />humans for multiple-use of large river-floodplain systems for hydro-electric <br />power, agriculture, industry, and municipal uses, it is doubtful that <br />restoration or returning rivers to an original state is possible (Bradshaw <br />1996). However, it is entirely possible to mitigate (i.e., to moderate), to <br />remediate (i.e., to rectify), or to enhance (i.e., to improve) environmental <br />conditions in a river ecosystem (Stanford et al. 1996). <br /> <br />The restoration of large floodplain rivers will require at least partial <br />recovery of the natural hydrograph based on the current knowledge of such <br />systems (Bayley 1991; Hesse 1995; Poff et al. 1997; Stanford et al. 1996; Ward <br />and Stanford 1995). However, Dolan et al. (1974) .stated that the historic <br />natural hydrograph of Colorado River System can no longer be restored because <br />of human alterations and the river system is rapidly approaching a new state <br />such that the future of river bars and floodplain terraces is unclear. Yet <br />restoration of large river ecosystem integrity requires full consideration of <br />the river continuum and flood pulse concepts of energy transfer (Walker et al. <br />1995). Walker et al. emphasized that the greatest conflict occurs between the <br />supply and demand of water from dryland river systems and believe that the <br />integrity of large dryland rivers will be maintained only if users use water <br />that is surplus to maintenance requirements of the riverine ecosystem. Site- <br />specific efforts will not restore the ecological integrity of large rivers. <br /> <br />t <br />I <br /> <br />I <br />I <br /> <br />I <br /> <br />I <br /> <br />Many of the floodplain habitats flooded ephemerally under historic riverine <br />conditions. For example, Cooper and Severn (1994d) estimated that <br />streamflows between 481 and 566 m3/s (17,000 and 20,000 cfs) were required to <br />inundate the floodplain along the middle Green River on the Ouray National <br />Wildlife Refuge. A streamflow of 566 m3/s (20,000 cfs) occurred 17 times <br />during the 47-year period of record (1946-1993) but only 7 times since the <br />completion of Flaming Gorge Dam in 1964 (29 years). This floodplain was <br />inundated only 6 times during the 47-year period for over 20 days. More <br />recently, FLO Engineering, Inc. (1995) estimated that a streamflow of 575 m3/s <br />(20,300 cfs) was required for extensive inundation of the middle Green River <br />floodplain on the Ouray National Wildlife Refuge. To reconnect the river with <br />the floodplain will either require breaching the levees to produce inundation <br />under present streamflows or excavation of the floodplain terraces to lower <br />the elevation so that floodplain inundation can occur without overbank <br />flooding of private lands. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />28 <br /> <br />I <br />I <br /> <br />I <br />
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