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<br />. <br /> <br />. <br /> <br />. adequate water quality; and <br /> <br />. physically self-sustaining wetlands. <br /> <br />Our research has shown that flow-through wetlands entrain the greatest number of <br /> <br />particles and the most flow, which is advantageous for placing larvae into a productive <br /> <br />environment and may increase their short-term survival. Thus, to maximize entrainment, flood <br /> <br />plain wetlands should have at least one upstream breach and one downstream breach. Research <br /> <br />performed to evaluate the Levee Removal Program demonstrated that these flow-through sites <br /> <br />were also more efficient at transporting and entraining particulate carbon, one important <br /> <br />component of productivity, into the flood plain (Birchell et al. 2002). High productivity, <br /> <br />combined with potential for warmer water, should ensure that growth rates of razorback sucker <br /> <br />larvae are fast relative to that in main channel environments (Bestgen 2008). It is difficult to <br /> <br />ensure that nonnative predators can not infiltrate the site and reproduce. However, prior research <br /> <br />has shown that larval razorback sucker can survive in the presence of low numbers of nonnative <br /> <br />fishes in a year after a flood plain wetland dries (resets) because the fish community was <br /> <br />eliminated (Modde and Haines 2005; Christopherson et al. 2004; Birchell and Christopherson <br /> <br />2004; Brunson and Christopherson 2005). <br /> <br />A negative aspect of flow-through wetlands is that all suspended particles are entrained, <br /> <br />including sediment (Heitmeyer and Fredrickson 2005). Therefore, over time, breaches as well as <br /> <br />the associated wetland will fill and ultimately, these types of wetlands will not be sustainable <br /> <br />without active management. For example, the natural levee at Bonanza Bridge was originally <br /> <br />breached at a river stage of 368 m3/sec. Entrainment studies in 2006 showed that connection <br /> <br />now occurs at a higher river stage (minimal connection at 434 m3/sec). From the high amount of <br /> <br />scouring of sediment observed in Breach 2 in 2006, it is not difficult to hypothesize the pattern: <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />50 <br />