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EXECUTIVE SUMMARY <br />This study was initially commissioned to develop an analytical (hydrological) model that <br />demonstrates that Trapper Mine's existing postmining channel design and construction methods <br />will meet bond release criteria. This would supplement the consistently observed successful <br />erosional stability of Trapper Mine's permanent drainage channels at the time of bond release, <br />incorporating such features as broad channel bottom width and a series of in -stream check dams <br />that are used to construct the channels. <br />During the course of the study it was discovered that for the case in which the majority of the <br />watershed is at 2 years or more vegetative growth, the grass -lined channel alone is found to be <br />stable without the need for erosion check dams. <br />It appears this results from the generally wide trapezoidal ditch bottom employed by Trapper Mine <br />for permanent channels in the final reclamation surface. These result in shallow flow depths for <br />the design storm, thereby producing a small hydraulic radius which in turn results in mild flow <br />velocities, lower than the erosion threshold in the grass channel lining. This finding is reported <br />here as Part One of this study. <br />That said, the series of regularly spaced check dams used by Trapper Mine provides significant <br />benefits leading up to bond release. They produce at least four favorable effects in the <br />establishment of a permanent reclamation condition: <br />1) they prevent erosion that may develop at one location from proceeding further back <br />upstream, thereby minimizing stream repair costs in the time prior to bond release, <br />2) they reduce the flow velocity during the early stages of reclamation when runoff flows are <br />higher, to allow a permanent and self-sustaining grass cover to establish in the channel, <br />3) they reduce the sediment load to the downstream sediment ponds during active mining <br />and reclamation, thereby required pond clean out efforts, and <br />4) directionally, by reducing the sediment load to the ponds, they also enhance the water <br />quality of the effluent released from the ponds during the mining and reclamation phases. <br />Accordingly, the second and third parts of this study was redirected from using the check dams <br />as part of the post -mining model, where it has been shown in Part One that they are not needed, <br />to establishing via hydraulic modeling a rational model to set the spacing of the check dams. The <br />basis for that model is to look at an intermediate reclamation stage in a typical generic watershed <br />at Trapper by assuming that during the active mining stage approximately one third of the <br />watershed tributary to the check dam would be at a freshly topsoiled condition (CN 86), one third <br />at 1 year's growth (CN 80), and one third at 2 year's growth (CN 67), all the while the grass lining <br />in the channel is still immature. The object of this modeling is to find a ditch check spacing that <br />slows the flow enough to not present erosive velocities in a bare earth channel lining, modeled as <br />"coarse gravel, non colloidal" in SEDCAD. The findings of this portion of the study are presented <br />as Part Two. <br />Part 3 provides recommendations for controlling sedimentation and runoff from recent reclamation <br />using dozer basins. <br />