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FLOOD07698
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Last modified
1/25/2010 7:12:32 PM
Creation date
10/5/2006 3:09:11 AM
Metadata
Fields
Template:
Floodplain Documents
County
Statewide
Community
Rock Rapids, Iowa
Basin
Statewide
Title
Problem Identification Report Rock River at Rock Rapids Reconnaissance Study Section 205
Date
4/1/1995
Prepared For
US Army Corps of Engineers
Prepared By
Greenhorne & O'Mara, Inc.
Floodplain - Doc Type
Project
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<br />I <br />I <br />I <br />I <br />I I <br />I <br /> <br />I <br />I <br />I <br />I <br />I <br /> <br />with the Dempster series is greater than 5 feet. The Kennebec series <br /> <br /> <br />soils consist of clay, are silty and fine grained, are medium plastic, <br /> <br /> <br />and are black to very dark gray in color from the surface to a 2.5-foot <br /> <br /> <br />deep level with a permeability ranging from 0.6 to 2.0 inches per hour. <br /> <br /> <br />Soils in the Kennebec series that are present below 2.5 feet consist of <br /> <br /> <br />silt, are sandy and fine grained, are low plastic, and are very dark <br /> <br /> <br />gray to brown in color. The permeability for this soil also ranges <br /> <br /> <br />between 0.6 to 2.0 inches per hour. The water table depth for the <br /> <br /> <br />Kennebec series soils ranges from 2 to S feet deep. The Colo series <br /> <br /> <br />soils are mostly silty clay loam which consists of clay, are fine <br /> <br /> <br />grained, are low to medium plastic, and are black to dark grayish-brown <br /> <br /> <br />in color. The permeability for this soil ranges from 0.2 to 6.0 inches <br /> <br /> <br />per hour and the water table is assumed to be between 1 and 3 feet deep. <br /> <br /> <br />The alluvial soils vary so much that they are not classified; however, <br /> <br /> <br />alluvial soils could have the potential for containing sands and gravels <br /> <br /> <br />which are highly permeable materials. Therefore, the alluvial soils are <br /> <br /> <br />not generally suitable for levee embankment material. <br /> <br />I <br />I <br />I <br /> <br />I <br />I <br /> <br />In conclusion, a majority of the materials in the direct vicinity of <br /> <br /> <br />the proposed levees consist of clay except for the Dempster series soils <br /> <br /> <br />that are below the 3-foot depth and the alluvial soils. These soils have <br /> <br /> <br />permeabilities which range between 0.6 and 2.0 inches per hour which may <br /> <br /> <br />be suitable for levee construction. Based on preliminary findings, the <br /> <br /> <br />proposed levees can be constructed with side slopes of 3 (horizontall to <br /> <br /> <br />1 (verticall with a 10 foot minimum top width. Although groundwater was <br /> <br /> <br />estimated to be over 5 feet deep, except for the Kennebec and the Cola <br /> <br /> <br />series which have groundwater estimated to be less than 5 feet, grading <br /> <br /> <br />considerations shall be taken to minimize the costs associated with <br /> <br /> <br />dewatering and to minimize the chances of using the sands and gravels <br /> <br /> <br />below the 3-foot depth of the Dempster series in the levee embankments. <br /> <br /> <br />Levee design details should be finalized based on a detailed feasibility- <br /> <br /> <br />level geotechnical investigation. <br /> <br />I <br />I <br />I I <br /> <br />10 <br />
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