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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />001015 <br /> <br />IV. ALTERNATIVE INVESTIGATION <br /> <br />A. General Description <br /> <br />Based upon an analysis of the floodplain and the sediment transport <br />regime, the existing and potential future drainage problems for Cherry Creek <br />were assessed. Various alternatives were devised to address each problem area <br />or channel reach. These alternatives were reviewed at a meeting with the TAC <br />and property owners to el iminate those options which were not considered <br />viable alternatives. The CONSULTANT then assembled the viable alternatives <br />together to form alternative plans. These plans were also presented to the TAC <br />and property owners along with a discussion of the pro's and con's of each <br />pl an. Afterwords, individual meetings were held with the property owners to <br />determine which plan best suits their needs. The final plan as presented in <br />this report is called the selected plan. <br /> <br />Presented in this section are the detail s and procedures for developing <br />the selected plan. <br /> <br />B. Constraints and Impacts <br /> <br />The first step in developing alternatives for the drainage problems was to <br />identify the constraints imposed on the alternatives by the various physical <br />features. The constrai nts identifi ed were the sediment transport, the ri ver <br />morphology, the existing and proposed water wells, the alignment of the future <br />Dry Creek Road crossing, and the existing sanitary sewer. <br /> <br />As discussed in Chapter III, Cherry Creek transports an appreciable amount <br />of sediment within the local South Platte River system. Any changes to Cherry <br />Creek will effect the sediment load and therefore erosion and sedimentation of <br />the channel. For instance, if the flow velocities are increased, additional <br />erosion is possible unless the banks are protected. However, if the source of <br />sediment is reduced then the river will make up for this loss of sediment by <br />eroding the downstream channel. If the flow velocities are decreased, then <br /> <br />-23- <br />