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North Peoria Area Drainage Master Plan - Flood Control District of ...

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NORTH PEORIAAREA DRAINAGE MASTER PLAN• Design Standard. Engineered flood controlchannels are typically designed to a 100-year standard. Therefore, damage mayoccur to development adjacent to a 100-year channel (or to the channelizationitself) if flow rates greater than the 100-year event occur. If design dischargeschange due to watershed changes or revisionsto hydrologic modeling standards,retr<strong>of</strong>it solutions are required to maintainthe same standard <strong>of</strong> protection.• Design Life. Engineered structures have alimited design life, and require regularmaintenance and inspection, and eventualreplacement.only where it can be demonstrated that nolong-term or short-term <strong>of</strong>f-site impacts tochannel stability occur, that downstreamreaches are adequately protected from erosionand flooding, and a long-term maintenanceand inspection program is adopted. Wherestructural flood control measures are necessary,the design and installation <strong>of</strong> such structuresshould compliment the environmentand be accomplished with the least disturbanceto the natural setting. Design guidelinesand standards for structural flood controlimprovements are provided in the MaricopaCounty <strong>Drainage</strong> Design Manual Volume II,Hydraulics and the City <strong>of</strong> <strong>Peoria</strong> InfrastructureDevelopment Guidelines.• Equilibrium Slope. Because <strong>of</strong> the increasein discharge, velocity, and depth, the stableslope is generally flatter than the existingchannel slope, which will cause longtermscour and require grade control toprevent undercutting <strong>of</strong> bank protection.• Habitat. Channelization typically eliminatesmost <strong>of</strong> the natural floodplain andstream bank habitat, and requires mitigationmeasures.• Sediment Supply. Bank erosion is animportant source <strong>of</strong> sediment supply forthe streams in the study area. Construction<strong>of</strong> bank protection eliminates thissource <strong>of</strong> sediment, increasing the likelihood<strong>of</strong> erosion <strong>of</strong> adjacent and downstreamreaches.• Downstream Impacts. Excessive instabilityshould be expected at the outlet <strong>of</strong> a channelizedreach due to the changes in velocity,sediment supply, and discharge.Depending on the channel geometry, theexpected response can range from lateralerosion and scour to sediment depositionand overbank flooding.Channelization, a structural flood controlmeasure, is not recommended as a developmentalternative in the <strong>North</strong> <strong>Peoria</strong> ADMPstudy area. Channelization should be allowedRoadway Crossing <strong>Drainage</strong> StructuresAt-Grade Crossings“At-grade crossings” typically have only minimalor localized impacts on channel stability.More commonly, the streams impact the atgradecrossing, rather than vice versa. Flowover the at-grade crossing can cause erosion <strong>of</strong>the pavement and subgrade, deposition <strong>of</strong>sediment in the road section, and disruption<strong>of</strong> traffic flow. Channel stability impacts commonlyobserved near “at-grade crossings”include the following including recommendationsfor mitigation:([DPSOHRIDQ´$W*UDGH&URVVLQJµ• A scour hole <strong>of</strong>ten forms on the downstreamside <strong>of</strong> an “at-grade crossing” dueto acceleration <strong>of</strong> flow over the hydraulicallysmooth pavement surface andincreased turbulence as flow transitions36

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