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miles). Moreover, the flow in the river immediately following Stream A is computed as the river <br />flow above Stream A (10.7 cfs) plus inflows to the river resulting from Stream A (3.0 cfs). This <br />results in a river flow of 13.7 cfs. Following the same methodology, the point flows above and <br />below each structure can be computed. The resulting flows for the river segment illustrated in <br />Figure 2 are tabulated in columns 4 and 5 of Table 1. Note that river flows occurring above and <br />below a given gauging station remain equal. <br />Table 1 Computed subreach gains and river flows. <br />Structure <br />River <br />Subreach <br />Flow Above <br />Flow Below <br />Name <br />Mile <br />Gain <br />Structure <br />Structure <br />(cfs /river mile) <br />(cfs) <br />(cfs) <br />Gauge A <br />0.0 <br />10.0 <br />10.0 <br />r ch I <br />Su b ea <br />0. 29 <br />10.7 <br />13.7 <br />Stream A <br />25 <br />Sub reach hII <br />0. 29 <br />Canal A <br />4.5 <br />14.3 <br />8.3 <br />Sub reach h III <br />29 <br />Canal B <br />7.0 <br />9.0 <br />0.0 <br />u r hN <br />Sb eac <br />='< <br />1 <br />0. 7 <br />0.3 <br />7.3 <br />Stream B <br />9.0 <br />Sub reac hV <br />1 <br />0 .7 <br />Canal C <br />.... . <br />11.5 <br />7.8 <br />3.8 <br />Sub reach h VI <br />0.17 <br />Gauge B <br />13.0 <br />4.0 <br />4.0 <br />QI] <br />ptflguid wpd I <br />