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![]() General Principles of Erosion Protection 
(6) Analysis of the present conditions and prediction of future channel migration 
should take into account the magnitude of flows that occurred prior to the site 
inspection, or that occurred during the time period spanned by surveys or aerial 
photos that are being used for analysis. High flows tend to attack the bank 
further downstream, and low flows farther upstream, because meander wave 
length is directly proportional to discharge. The stream integrates the total 
hydrograph over the long-term, but short-term observations may be distorted by 
extreme events. Therefore, if the period of observation is weighted toward low 
flows, the long-term attack may be farther downstream and more severe than 
current observation would indicate. High flows during the period of observation 
may have the opposite effect. 
6.1.1.4 Special Considerations for Braided Streams 
Protection works on braided streams may need to extend upstream and downstream 
from the active erosion, because bars, chutes, and pools move more rapidly and much less 
predictably than in meandering streams. Often bank erosion is associated with meandering 
tendencies of major anabranches, and the likely pattern of attack can be fairly well predicted 
using the rules of downvalley and lateral migration for alluvial bends. However, in other cases 
bank erosion may be caused by less predictable impinging flow in side channels. The most 
efficient approach on a braided stream where bank erosion is associated with anabranch flow 
which impinges against the bank at sharp angles may be one of the following: 
Treat problem areas as they arise by constructing spot stabilization as the 
stream attacks first one spot, then another. 
Temporarily divert impinging flows, either by excavating a new channel, 
building temporary dikes of streambed material, or using floating 
"breakwaters" to absorb the brunt of the impinging flow.  However, 
environmental aspects of construction activity in the streambed may not be 
acceptable. 
If long-term stabilization is required on a braided stream, and project constraints 
preclude installing bank protection periodically as the channel changes, an adequate solution 
may require the construction of continuous protection on both sides of its "braid belt." 
Trenchfill or windrow revetment is well-suited for this application. 
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