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Doc Date:12/11/2001 <br />• <br />III IIIIIIIIIIIII III <br />sss <br />TECHNICAL RELEASE No. 25, CHAPTER 6. APPENDIX A. <br />Stream Armor Design Concepts <br />6-94 <br />Appendix A <br />Purpose <br />This appendix (1) explains the underlying physical processes affecting <br />armoring, (2) describes different SCS-approved math models available, <br />and (3) presents an example illustrating one way to estimate armoring. <br />'Ihe various math models for critical and recommended allowable tractive <br />stress discussed in this appendix are accepted in the engineering profes- <br />sion; they differ mainly in choice of a safety factor, scope of applica- <br />tion, or both. 7t+o different math models for recommended allowable trac- <br />five stress are used in SCS. They differ solely in their safety factors. <br />The armor designer is free to select the most applicable model. <br />Actual transverse tractive stress of each situation must be determined <br />through a hydraulic analysis. The example in this appendix uses a sim- <br />plistic model to determine the hydraulic radius. In real situations, <br />actual cross-sectional geometry and, possibly, precise water surface <br />profile calculations are required. However, this requirement does not <br />invalidate the concepts illustrated by the example. <br />Fhysical Processes <br />Armoring is a well-known natural phenomenon. Furthermore, its important <br />features already are used in sore engineering structures, for a:ample, <br />riprap. Armoring is sometimes called hydraulic sorting. It is a limit- <br />ing or special case of sediment transport. It has been studied by vari- <br />ous scientists over the years, (e.g., A. Shields, A. Strickler, E. Lane, <br />H. Einstein, and others). Understanding the primary principles of armor- <br />ing is still developing and is leading to various math models and pro- <br />cedures for field application. <br />• Armoring is the result of the dynamic interaction of unsteady fluid flow <br />and a mobile bed composed generally o_' a broad range of discrete parti- <br />cles. <br />