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Last modified
1/25/2010 7:07:53 PM
Creation date
10/5/2006 2:00:15 AM
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Floodplain Documents
County
Statewide
Community
State of Colorado
Basin
Statewide
Title
Design of Stable Channels with Flexible Linings
Date
10/1/1975
Prepared By
Hydraulics Branch, Federal Highway Adminstration
Floodplain - Doc Type
Educational/Technical/Reference Information
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<br />e <br /> <br />This concept is verified by the MSU tests (3), the Louisiana <br />Department of Highway tests (4), and the empirical equations <br />from NCHRP Report 108 (6). For most lining materials, the <br />erodibility of the underlying soil is a design parameter. <br />For rock riprap channel linings, the underlying soil is not <br />a consideration because a properly designed filter blanket <br />should be used, as necessary, to prevent leaching of the <br />underlying soil through the riprap. Design of the filter <br />blanket will be discussed in a latter section of this circular. <br />The scs results on maximum permissible velocity for vegetative <br />linings can be transformed into permissible depth curves by <br />the method explained in Appendix C. <br /> <br />-1.: <br /> <br />~ <br /> <br />The erodibility of cohesive soils has thus far eluded quan- <br />titative definition. It is suggested that the erodibility of <br />specific soils be based on the designer's experience rather than <br />any quantitative analysis based, for example, on the plasticity <br />index. The difficulties involved in defining the erodibility of <br />cohesive soils is well described by Partheniades (9). Based on <br />the MSU work, which covered ten soils of different characteristics, <br />soils with a gravel, sand and clay mixture are erosion resistant; <br />fine-grained sands or silts are erodible; and plastic and semi- <br />plastic soils are in the intermediate range. The soil erodibility <br />index (K) for the Universal Soil-Loss Equation, developed by the <br />Agricultural Research Service, could also be used as a guide to <br />soil erodibility. For example, in Maryland, all soils have been <br />assigned K values of from 0.17 to 0.49 (10). A soil with a K <br />value of 0.17 would be considered erosion resistant, while a soil <br />with a K value of 0.49 would tend toward the erodible classificatio~. <br />These K determinations by the Soil Conservation Service are <br />subjective for the most part, but they give the designer some <br />basis for his appraisal of a particular soil. <br /> <br />e <br /> <br />Another source of information on the erodibility of the soils <br />in a particular area are the county soil reports published in <br />many areas of the country by the Soil Conservation Service. <br />These reports often describe the erodibility of the various <br />soils in a particular location with enough detail to make an <br />estimate for the site under consideration. <br /> <br />. <br /> <br />:< <br /> <br />e <br /> <br />8 <br />
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