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Hydraulic Design of Highway Culverts - DOT On-Line Publications

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Figure II-5—Culvert location methods<br />

3. Waterway Data. The installation <strong>of</strong> a culvert to convey surface water through a highway<br />

embankment significantly constricts the flood plain. To predict the consequences <strong>of</strong> this<br />

alteration, accurate preconstruction waterway data must be collected. These data include crosssectional<br />

information, stream slope, the hydraulic resistance <strong>of</strong> the stream channel and<br />

floodplain, any condition affecting the downstream water surface elevation, and the storage<br />

capacity upstream <strong>of</strong> the culvert. Photographs <strong>of</strong> site conditions are <strong>of</strong>ten beneficial.<br />

a. Cross Sections. Stream cross sectional data acquired from a field survey at the site are<br />

highly desirable. At least three cross sections should be taken to establish the stream slope, the<br />

culvert inlet, the culvert outlet, and the configuration <strong>of</strong> the natural channel (Figure II-6).<br />

Sections should be taken: (1) about 30 m (100 ft) upstream from the crossing, (2) at the<br />

centerline <strong>of</strong> the roadway, and (3) about 30 m (100 ft) downstream from the crossing. The<br />

natural streambed width and side slopes, and the floodplain width may be obtained from these<br />

cross sections. The cross-sectional data will also help to verify the accuracy <strong>of</strong> existing<br />

topographic maps. If significant ponding is likely, additional sections may be necessary to<br />

determine the storage capacity upstream <strong>of</strong> the culvert. Likewise, additional downstream<br />

sections may be necessary to establish downstream water level (tailwater) conditions.<br />

If only one cross section <strong>of</strong> the natural channel is available, it will be used as the typical cross<br />

section. This assumption should be checked using topographic maps and aerial photos.<br />

Additional information on stream slope and upstream storage volume should also be obtained<br />

from the topographic maps.<br />

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