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<br /> <br />404 <br /> <br />j, A, STANFORD ET AL <br /> <br />strong interactors capable of structuring food-webs: Power et al., 1995) may clarify spatial and temporal <br />scales in large river restorations, <br />In general, the entire catchment, from headwaters to the ocean, is relevant. In the case of rivers that sup- <br />port anadromous fisheries, estuarine and ocean habitats connect functionally to the riverine components, <br />Mathematical models can be used very effectively to formalize understanding of the effects of regulation <br />and interactions with pollution and food-web manipulation within the river continuum, but models should <br />not be used exclusively to define a restoration strategy (Hall, 1 988b). The process must be inferential from the <br />entire body of quantitative and qualitative information about how river regulation and interactive effects <br />have altered ecosystem capacity. <br /> <br />Restore environmental (habitat) heterogeneity but let the river do the work <br /> <br />The main goal is to reduce the range of human disturbances so that interconnected riverine habitats (Fig- <br />ures I and 2) can support diverse and productive food-webs, including species of special social and economic <br />interest. Management should strive to restore environmental heterogeneity and reduce or eliminate sources <br />of mortality from pollution and overharvest. Keep in mind that riverine biodiversity and bioproduction are <br />largely controlled by ,abiotic drivers (Figure 3) and that density-dependent relationships, such as the stock- <br />recruitment relations often used to determine fisheries harvest prescriptions, rarely manifest predictably <br />owing to natural abiotic variation (Hall, 1986; Hall, 1988a; Pimm, 1991; Huston, 1994). <br />Owing to the importance of flow to habitat maintenance, and temperature to food-web energetics, highly <br />significant restoration is possible simply by reregulation to allow more natural seasonality of flow and tem- <br />perature. We call this restoration of normative habitat conditions, where the norm or standard is established <br />from what is possible in a natural-cultural context as opposed to striving for pristine conditions which are <br />difficult, if not impossible, to define or achieve, at least for entire catchments, Removal of dams certainly <br />should be considered and, where possible, done; but, restoration of normative habitat conditions is possible <br />in many if not most regulated rivers without taking dams out. However, channel revetments are problematic <br />because the objective is to reconnect channels and floodplains. <br />Peak flows are needed to scour and rearrange substratum and reconnect floodplain habitats with the chan- <br />nel; spatial and temporal temperature variability promotes re-establishment of native biodiversity (Figures 2 <br />and 5), Peak flows needed to re-establish cut and fill alluviation (called effective flows by geomorphologists) <br />mayor may not be equal to bank-full, and gravel supply may be limiting owing to storage of bedload in the <br />reservoirs (Ligon et aI" 1995), Effective flows can rapidly degrade (downcut) entire segments when sediment <br />mass balance relations change as a consequence of regulation (Andrews and Nelson, 1989). Adding sedi- <br />ments to regulated rivers (e,g, using slurry pipelines from reservoir deltas) should not be out of the realm <br />of consideration in situations where instream sediment supply is limited by years of regulation, However, <br />overbank flows in many cases will initiate cut and fill alluviation in an ecologically effective manner, supply- <br />ing sufficient sediment from lateral erosion, <br />We emphasize that reregulation of flows requires careful evaluation of channel morphometry, bed-sedi- <br />ment size distribution and shear stress in relation to the range of possible flows, A great deal of geomorpho- <br />logical study and modelling has been devoted to this problem in recent years (Andrews, 1980; Andrews and <br />Nelson, 1989; Kellerhals and Church, 1 989; Deitric~ et aI., 1993; Church, 1995) and more work is needed, In <br />general, flows that mobilize substrata of median particle diameter will build bars, cut overflow channels and <br />dig pools, Determination of peak flows is complicated by dense, often senescent, thickets of riparian <br />vegetation on the floodplains of regulated rivers, Repeated scouring flows will most likely restore riparian <br />successional vitality. Annual temperature patterns similar to pre-regulation conditions, which will directly <br />mediate restoration of biota, can often be attained by depth selective withdrawal structures on the dams <br />(Gore, 1985), <br />Of course, restoration of overbank flows may be problematic in many rivers where humans have colonized <br />the floodplains. In these cases, revetments have often been extensively built to restrain flood flows, Reregu- <br />lation to produce overbank flows may not be practical. However, floods of record will most likely result in <br />overbank flow even in intensely regulated rivers, because natural storage on floodplains throughout the con- <br />tinuum has been drastically diminished, Revetments tend to act as dams during very large floods on <br />