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SS =angle of the bank @ O.SH:I.OV. <br />S = bedslope angle based on river slope in this area of 0.733% grade. This is the same as Z <br />for this case. <br />O =angle of repose of rock, due to large size, hand placed, this angle can reach 70 degrees or <br />higher. <br />D =flow depth, assuming upper boulders of 5.0 feet height and water level is 11.5 feet above <br />the base of the boulder. <br />Results show that boulders are stable for both cases, however, shear in the bend has not been <br />taken into account. Since the jetty will be placed at an angle of 42 degrees, sheaz forces can <br />be double than that for the side of a channel where the flow is pazallel to the rock. However, <br />if the safety factors are reduced by half, they are still over 2.0 for the Test 1 case and 1.02 for <br />the Test 2 case, therefore the boulders should be stable. See Map C-6 for complete details of <br />the jetty design. The rock boulders will be buried at least 3.0 feet into the surrounding ground <br />for the part that extends in the river bed itself and at least 2.0 feet in the ground for the part <br />above the bed that forms the slope of the existing river embankment. This will help the foun- <br />dation stability of the boulders and prevent scouring. To further increase the safety factor, the <br />specified diameter of the rock will be 4.75 feet in size instead of 4.5 feet. The rock is also <br />specified that no boulder can be less than this size, therefore, it is not an average size; it is a <br />minimum size. Since water can flow over the jetty toward the west riverbank, pit run material <br />will be backfilled in the wedge between the jetty and the bank to a depth of approximately 4 <br />feet and [he grade will be mild 8-lOH:1V toward the river. <br />Looking at the jetty with regard to the 100 year flows of approximately 25000 cfs and a water <br />elevation of 666.5 feet, the jetty has been placed at a height to divert almost all of the flows at <br />an approximate angle of 42 degrees from the flow direction immediately upstream. During <br />the large storm event, as seen from Exhibit C-2 and C-6, the water will move to the southeast <br />and will likely cut out a portion of the dike at its southern location. This will not cause a <br />problem since the dike berm is not near anything in the river that could be adversely affected. <br />There are plans to remove this dike berm anyway and restore the channel to its former condi- <br />tion as a wide shallow channel with a grade resembling that of the original. The cutting <br />would only occur if the dike berm still exists before it is removed in the channel restoration <br />Received <br />Thomas Pit 2/02 <br />16 <br />MAR072~2 <br />view once <br />