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Last modified
1/25/2010 7:10:29 PM
Creation date
10/5/2006 2:40:17 AM
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Floodplain Documents
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Statewide
Title
Method of Estimate Effects of Flow-Induced Vegetation Changes on Channel Conveyances of Streams in Central Arizona
Date
1/1/1998
Prepared For
Central Arizona
Prepared By
USGS
Floodplain - Doc Type
Educational/Technical/Reference Information
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<br />SI~D 3a <br /> <br />Vflex values are 8.85 ft-Ib and 63.2 ft-Ib for the <br />brush and willow, respectively, for all flows <br />(table 10). Go to STEP 4. <br /> <br />SleD 3b <br /> <br />Vflex values remain constant for all flows. Go to <br />STEP 4 (Slep 4b). <br /> <br />SleD 3c <br /> <br />Vflex values remain constant for all flows. Go to <br />STEP 4 (Step 4c), <br /> <br />STEP 4. Determine the orientation of the <br />vegetation (either oriented randomly or parallel to <br />flow) as well as the cross-section area of flow <br />blocked by vegetation, and the ratio of hydraulic <br />radius to average vegetation height for the selected <br />discharge. Determine the vegetation-blocking <br />coefficient, ChlDcking> the vegetation-distribution <br />coefficient, Cdisl' and the flow-depth coefficient, <br />Cdeplh (tables 4, 5, and 6). <br /> <br />SleD 4a <br /> <br />ChlDcking is equal to 4.0 for both vegetation <br />types, Cdisl is equal to 1.0 for both vegetation <br />types and, for the 2-year flow, Cdeplh is equal to <br />5 and 60 for the brush and willow, respectively, <br />Go to STEP 5. <br /> <br />Slen 4b <br /> <br />ChlDcking and Cdisf values remain constant. For <br />the IO-year flow, however, Cdeplh is equal to 1.0 <br />and 20 for the brush and willow, respectively. <br />Go to STEP 5 (Step 5b). <br /> <br />SleD 4c <br /> <br />Chlocking and Cdisl values are assumed to remain <br />constant for willow. For the 50-year flow, <br />however, Cdeplh is equal to 5.0 for willow. Go to <br />STEP 5 (Step 5c). <br /> <br />STEP 5. Compute the vegetation-susceptibility <br />index for the selected discharge using equation 3, <br /> <br />SleD 5a <br /> <br />For the 2-year flow, the vegetation- <br />susceptibility indices are 177 ft-Ib and <br />15,200 ft-Ib for the brush and willow, <br />respectively (table 12). Go to STEP 6. <br /> <br />SleD 5b <br /> <br />For the IO-year flow, the vegetation- <br />susceptibility indices are 35.4 ft-Ib and <br />5,060 ft-Ib for the brush and willow, <br />respectively (table 12). Go to STEP 6 <br />(Step 6b), <br /> <br />SleD 5c <br /> <br />For the 50-year flow, the vegetation- <br />susceptibility index is 1,260 ft-Ib for willow <br />(table 12), Go to STEP 6 (Step 6c), <br /> <br />STEP 6. Compute stream power for the selected <br />discharge using equation I, <br /> <br />St~D 6a <br /> <br />For the 2-year flow, computed stream power is <br />1.78 ft-lb/s/ft2 (table 12), Go to STEP 7. <br /> <br />Slep 6b <br /> <br />For the I O-year flow, computed stream power is <br />11.6 ft-Ib/s/ft2 (table 12). Go to STEP 7 <br />(Step 7b). <br /> <br />SleD 6c <br /> <br />For the 50-year flow, computed stream power is <br />28,0 ft-lb/s/ft2 (table 12). Go to STEP 7 <br />(Step 7c). <br /> <br />STEP 7. Plot the values for the vegetation- <br />susceptibility index and stream power for each <br />type of vegetation present in the channel (figure 9). <br />If the values plot below the vegetation- <br />susceptibility threshold, repeat steps I through 6 <br />using the next largest discharge. If the values plot <br />above the threshold, no further steps are required. <br /> <br />Effects of Flow-Induced Vegetation Changes on Channel Conveyances 25 <br />
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