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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 />I <br />I <br />I <br />I <br />I <br />I <br /> <br /> <br />Adequate resistance to erosion does not necessarily produce stability, if the channel has substantial <br />inflows of bed sediment. Basic hydrologic input to the stream and the associated hydrauliC parameters of <br />the flow (velocity, depth, slope, etc.) will dictate erosion patterns in the simple scenario. More complex <br />analyses are required when an abundance of sediment inflows may lead to severe sediment deposition or <br />a combination of erosion and aggradation of a stream channel. <br /> <br />HYDRAULIC GEOMETRY <br /> <br />Hydraulic geometry relationships involve three independent associations for: 1) width or wetted perimeter, <br />2) depth or hydraulic radius, and 3) slope or velocity, all vs. discharge. They indicate the preferred <br />cross-section and slope of a channel for a given channel-forming discharge and given boundary materials. <br />In the design of a channel project, the preferred channel is supposed to be stable, with respect to <br />cross-section and slope, but is not necessarily free from lateral shifting and meandering. <br /> <br />Meander geometry is an interesting phenomenon in river mechanics. Meander dimensions in natural <br />systems tend to scale with channel width. Stream projects that tend to alter or fix channel width also tend <br />to alter the meander patterns of the natural system over time. Meander wavelength, like channel width, <br />will vary roughly as the square root of channel-forming discharge. The figure below depicts an example of <br />a distorted meander pattern. <br /> <br />Figure VII-3 <br />Example of Distorted Meander Pattern of an Armored Channel Reach <br /> <br /> <br /> <br />...1 <br />...... <br /> <br />..- <br />........ <br />Bank Armoring <br /> <br />BIOLOGICAL CONDITIONS <br /> <br />Classification is an important component of many of the scientific disciplines relevant to stream corridors <br />such as hydrology, geomorphology, limnology, and plant & animal ecology. When a classification system <br />is used as a measure of biological condition of a stream, there are several factors to consider for <br />restoration planning. These factors may include geographic domain, variables considered, incorporation of <br />temporal relations, focus on structural or functional behavior, and the extent to which management <br />alternatives or human actions are explicitly considered as classification variables. <br /> <br />Section VII - 5 <br />