TR-55 Urban Hydrology for Small Watersheds

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Presentation transcript:

TR-55 Urban Hydrology for Small Watersheds

Simplified methods for estimating runoff and peak discharge for small urban/urbanizing watersheds Ch 1 Intro Ch 2 Estimating Runoff Ch 3 Time of Concentration Ch 4 Peak Runoff Method Ch 5 Hydrograph Method Ch 6 Storage Volumes for Detention Basins

Chapter 5 Tabular Hydrograph Method Can be used to estimate runoff from nonhomogenous watersheds Input: Same as Chapter 4 for each subarea Tt-travel time for each routing reach

Steps Use Worksheet 5a to calculate/summarize info on each subarea Use worksheet 5b to route the various subareas

Limitations Accuracy decreases as complexity increases Where possible, compare to gaged data TR-20 (not TR-55) should be used if: Tt > 3hours Tc for any subarea > 2 hours Drainage areas differ by a factor of 5 or more Entire hydrograph is needed for detailed flood routings Peak discharge time must be determined accurately

Subareas 1 & 2 routed through 3,5 and 7 Proposed subdivision in 5, 6 and 7

Table 5-1 Initial abstraction as a function of curve number Ia/P values are then calculated

Exhibit 5 tables (4 different exhibits based on the 4 rainfall distribution types) Prerouted using ATT-KIN method Tables give unit peak discharge (multiply by DA and Q to get Discharge) Ia/P values are rounded off to the nearest 0.1, 0.3 or 0.5 (or interpolated) Travel time must be rounded off to table values

Impact of Development Peak flow is higher after development Peak flow occurs earlier after development

Low Impact Development http://www.epa.gov/nps/lid/ http://www.lowimpactdevelopment.org/ http://www.lid-stormwater.net/

Green Roofs

Porous Concrete Pavers http://www.concretenetwork.com/concrete/porous_concrete_pavers/

Pervious Pavements in Cold Weather http://stormh2o.com/september-2008/pervious-asphalt-concrete.aspx

Rain Gardens http://www.ci.des-moines.ia.us/departments/PR/rain_gardens.htm

Grass Swales

Detention/Retention Basins

Ch 6 Estimating Storage Volumes for Detention Basins Approximate method (+/-25% storage error) Can be used for single and multi-staged outflow structures Worksheet 6a-estimate storage volume given desired peak outflow Worksheet 6b-estimate peak outflow given storage volume

Detention Outlet Structures Single Stage (culvert or orifice) Multi-Staged to handle different flows Combination of orifices &/or weirs

Orifices and Weirs

Figure 6-1 Approximate Routing

Example 6-1 Single-Stage Outflow 75-Acre Development Developed Peak flow is 360 cfs (Q25) Present channel can handle only 180 cfs w/o significant damage Storage-elevation curve is given-see worksheet Determine storage volume of a detention basin Assuming a rectangular weir, determine the weir length needed to limit the flow to 180 cfs

Worksheet 6A

Determining weir length Flow=3.2*Weir Length*(Weir Head)1.5 180=3.2*Weir Length*(5.7) 1.5 Weir Length=4.1 feet Notes: Weir head=max. storage elevation-crest elev. A weir length greater than 4.1 feet would let more than 180 cfs into the drainage channel

Example 6-3 10-Acre Development Existing peak flow is 35 cfs Developed peak flow is 42 cfs (24-hr, Q100) Detention basin volume is 35,000 cubic feet Estimate peak outflow

Worksheet 6B