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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 />II <br />I <br />I <br />I <br />I <br />I <br /> <br />N <br />N <br />CJl <br />~. <br /> <br />actually rehabilitated with sediment and vegetation. <br /> <br />BADLAND DEBRIS BASIN: The BLM has constructed debris basins in <br />the badland unit of Sagers Wash Subwatershed. These basins are <br />currently trapping salt-laden sediment. The purpose of these <br />basins is to trap salt and sediment before it enters the Colorado <br />River. These debris basins are an attempt to control salt on <br />rangeland from a geologic background source. As noted in the <br />Unit 4 - Badlands geomorphic section of this report, sediment and <br />salt that yield from Sagers Wash Subwatershed are deposited in <br />Sagers Flat floodplain. Sagers Flat acts as a detention basin <br />for the badlands sediment issuing from the upper area of Sagers <br />Wash Subwatershed. These specific debris basins are actually <br />controlling approximately 50% of the sediment that is trapped <br />behind them. The other 50% would be trapped naturally in Sagers <br />Flat. Furthermore, the sediment yielded from Sagers Flat is <br />subject to an estimated 80% delivery ratio. Therefore, these <br />debris basins are functioning to control 40% of the salt and <br />sediment trapped in them; the other 60% would be controlled by <br />Sagers Flat and the floodplain of the lower watershed. <br /> <br />It should be noted that Pinto Wash Subwatershed also flows <br />through Sagers Flat. Therefore, any debris basins planned for <br />this area would have the same estimated 40% efficiency as those <br />in sagers Wash Subwatershed. <br /> <br />The planning and construction of debris basins in the Mancos <br />Shale soils is subject to the following engineering geologic <br />hazards: <br />- the construction material is of a highly erosive nature <br />(ML-CL), (ML) , and dispersive (CH); <br /> <br />- the construction, foundation, abutment, reservoir bottom <br />and surrounding materials are subject to rapid solutioning of the <br />salts in them and the consequent differential collapse of these <br />materials (which could cause the failure of the structures); <br /> <br />these structures have a limited life as regards storage <br />volume and will rapidly fill up with salt-laden sediment, <br />therefore the operation and maintenance of these structures is of <br />high frequency and significant cost; <br /> <br />- failure to clean out filled sediment pools could result in <br />storm flows over-topping the embankment; <br /> <br />- failure of the embankment can occur due to over-topping by <br />flows from an intense storm event, erosion of the embankment by <br />piping through differential settlement cracks or over-topping due <br />to small frequent storm flows imparting a full or nearly full <br />sediment pool; <br /> <br />- failure of the embankment for any reason can result in the <br /> <br />14 <br />