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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 />