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EXHIBIT 7, ITEM 20, PART G <br />TERRACE DITCH DESIGN <br />A series of terrace ditches will be constructed across the face of the permanent fills and in the <br />upper portions of the permanent fill in the South Taylor Fill. The locations of these are shown <br />on Map 41A. The ditches in the upper portion of the permanent fill will originate near on the <br />even 100 foot postmining contours 7700, 7800, 7900, and 8000 foot elevations. <br />The function of the ditches is to direct overland flow runoff towards the channels of the ditches <br />denoted as the East and West Tributaries of the West Taylor Fill Ditch and the upper portions of <br />Taylor Tributary Ditch. The design basis for these permanent channels is provided in Volume 13 <br />Exhibit 7, Item 20, Part E and in Volume 2C, Exhibit 7-14C. <br />The segment of the proposed Terrace Ditches with the largest watershed within the permanent <br />fill is a westward draining branch of the ditch originating at the 8000 foot elevation and <br />emptying into the Taylor Tributary Ditch in the NW/4 of Section 16. This segment is <br />approximately 2,000 feet in length and has a drainage area of 57.9 acres. It has been selected as <br />the representative segment for the design of all the terrace ditches. Terrace ditches with smaller <br />watersheds are thus conservatively overdesigned. <br />Using this length and a tributary area of 57.9 acres as a design basis for all of the terrace ditches, <br />the dimensions of the representative ditch for the terrace ditches was developed using SEDCAD <br />as described below. For a conservative design, the applicable storm was set as a 100 year, 24 <br />hour event. <br />SEDCAD4 was used to determine the peak flow from this drainage area as detailed on the <br />following SEDCAD output pages. The 100 year, 24 hour design event was modeled using a CN <br />of 74 for reclaimed land with 1 to 2 years' growth in accordance with Table 1 in the Introductory <br />Text for Exhibit 7 (Volume 2D). This would be representative of a short term condition where <br />the upstream area has recently been topsoiled and seeded and has had only a year or two of <br />growth. The long term condition would have a CN of 62 for three year growth per the same <br />table and would produce somewhat less runoff. The modeled case produced a peak flow of <br />about 19.2 cfs in the 100 year event. <br />As shown in the following SEDCAD output, a grass lined asymmetric triangular ditch cross <br />section is assumed, with a channel slope of 0.015 ft/ft and 1.5H:1 V side slope on the uphill side <br />and 3.OH:1 V side slope on the downhill side. It would flow at a depth of 2.28 feet deep when <br />full retardance associated with mature grass lining for the long term is in place. In the short <br />term, with a shorter immature vegetative cover, it would flow slightly shallower and at higher <br />velocity, though still acceptable at 3.3 fps. A nominal freeboard of 1 foot has been added to the <br />calculated flow depth for the long term, resulting in a generic ditch section at least 3.3 feet deep <br />on a 1.5% slope for all terrace ditches on the fill face. This depth has been rounded up to an <br />even 4 feet, with other design parameters as summarized below: <br />Exh. 7-20G-1 Revision Date: 07/20/15 <br />Revision No.: TR -105 <br />