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“Modern Sewer Design” is the result of a - Jensen Bridge & Supply

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3. HYDROLOGY85V/S 0.5Relationship for Various Land CoversLand Cover V/S 0.5 (m/s) V/S 0.5 (ft/s)Forest with Heavy Ground Litter, Hay Meadow (overland flow) 0.6 2.0Trash Fallow or Minimum Tillage Cultivation; Contour, Strip Cropped,Woodland (overland flow) 1.5 5.0Short Grass Pasture (overland flow) 2.3 7.5Cultivated, Straight Row (overland flow) 2.7 9.0Nearly Bare and Untilled (overland flow) or Alluvial Fans in WesternMountain Regions 3.0 10.0Grassed Waterway 4.6 15.0Paved Areas (sheet flow); Small Upland Gullies 6.1 20.0O<strong>the</strong>r MethodsO<strong>the</strong>r methods have been developed that determine T c for specific geographicregions or basin types. These methods are <strong>of</strong>ten incorporated into an overall procedurefor determining <strong>the</strong> run<strong>of</strong>f hydrograph. Before using any method, <strong>the</strong> usershould ensure that <strong>the</strong> bas<strong>is</strong> on which <strong>the</strong> time <strong>of</strong> concentration <strong>is</strong> determined <strong>is</strong>appropriate for <strong>the</strong> area under consideration.DETERMINATION OF THE RUNOFF HYDROGRAPHThe following sections outline alternative methods for generating <strong>the</strong> run<strong>of</strong>f hydrograph.Emphas<strong>is</strong> will be given to establ<strong>is</strong>hing <strong>the</strong> hydrograph for single stormevents. Methods for estimating flow for urban and rural conditions are given.Irrespective <strong>of</strong> <strong>the</strong> method used, it should be ensured that wherever possible <strong>the</strong><strong>result</strong>s should be compared with h<strong>is</strong>torical values. In many cases a calibration/validationexerc<strong>is</strong>e will aid in <strong>the</strong> selection <strong>of</strong> <strong>the</strong> most appropriate method.All <strong>of</strong> <strong>the</strong> methods described could be carried out using hand calculations; however,for all but <strong>the</strong> simplest cases <strong>the</strong> exerc<strong>is</strong>e would be very laborious. Fur<strong>the</strong>rmore,access to many tested computer models has been made easier in recent years due to<strong>the</strong> widespread use <strong>of</strong> microcomputers. For <strong>the</strong>se reasons emphas<strong>is</strong> will be placedon describing <strong>the</strong> bas<strong>is</strong> <strong>of</strong> each method and <strong>the</strong> relevant parameters.A subsequent section will relate <strong>the</strong> methods to several computer models.Rainfall run<strong>of</strong>f models may be grouped into two general classifications that analyzelosses (i.e., to initial infiltration and depression storage) and effective rainfall.The effective rainfall hyetograph <strong>is</strong> <strong>the</strong>n used as input to a catchment model to pro-Ease <strong>of</strong> installation <strong>of</strong> CSP through ex<strong>is</strong>ting concrete box.

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