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Chapter 1 Minimum Flows and Levels - Southwest Florida Water ...

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Table 5-7. Median elevations, in feet above NGVD, <strong>and</strong> relative elevations (height in feet<br />

above the river channel bottom) of hydric <strong>and</strong> non-hydric soils in vegetation classes<br />

occurring along the floodplain vegetation/soils transects on the Braden River.<br />

Vegetation Class<br />

Hydric<br />

Non-hydric<br />

N Relative<br />

Elevation<br />

(ft)<br />

Elevation<br />

(ft<br />

NGVD)<br />

N Relative<br />

Elevation<br />

(ft)<br />

Elevation<br />

(ft<br />

NGVD)<br />

Popash 16 5.0 2.8<br />

Oak/popash 36 7.1 19.9 2 6.8 21.8<br />

Hickory/oak 15 7.8 25.2 53 9.1 15.8<br />

Oak/cabbage palm 5 9.4 18.0 99 9.4 24.5<br />

Pine/oak 24 14.3 19.5<br />

Oak mix 27 13.3 11.1<br />

Combined 72 7.1 207 10.6<br />

*Shaded cells indicate absence of soil type/condition<br />

Modeled flows at the Braden River near Lorraine gage needed to inundate the<br />

median elevations of floodplain vegetation classes <strong>and</strong> soils are listed in Table 5-<br />

3. Although the popash vegetation class occurred too infrequently for estimation<br />

of flows necessary for their inundation, mean flows of 287 to 541 cfs were<br />

determined to be necessary for inundation of other wetl<strong>and</strong> <strong>and</strong> transition<br />

vegetation classes.<br />

Muck <strong>and</strong> hydric soils require mean flows of 357 <strong>and</strong> 377 cfs, respectively, for<br />

inundation.<br />

5.4.3 Percent-of-Flow Reductions for Floodplain Features, Vegetation<br />

Classes <strong>and</strong> Soils<br />

Changes in flow at the Braden River near Lorraine gage during Block 3 that are<br />

expected to result in no more than a 15% reduction in the number of days of<br />

inundation of the median elevation of selected floodplain attributes were<br />

evaluated for two benchmark periods, 1988 through 1994 <strong>and</strong> 1995 through 2005<br />

(Table 5-3). Percent-of-flow reductions associated with inundation of<br />

geomorphological features (river banks <strong>and</strong> wetted perimeter inflection points)<br />

ranged from 2 to 20%. Identified flow reductions for elevations associated with<br />

wetl<strong>and</strong> soils were less variable, ranging from 11 to 20%. Percent-of-flow<br />

reductions identified for inundation of median wetl<strong>and</strong> or transitional vegetation<br />

classes ranged from 3 to 14%, <strong>and</strong> were lower for the period from 1988 through<br />

1994.<br />

5-15

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