1 TR-55 Urban Hydrology for Small Watersheds. 2 Simplified methods for estimating runoff and peak discharge for small urban/urbanizing watersheds Ch 1.

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Presentation transcript:

1 TR-55 Urban Hydrology for Small Watersheds

2 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

3 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

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

5 Limitations Accuracy decreases as complexity increases Accuracy (+/- 25%) 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

6 Subareas 1 & 2 routed through 3,5 and 7 Subareas 3 & 4 routed through 5 & 7 Subareas 5 & 6 routed through 7 Proposed subdivision in 5, 6 and 7

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

8 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

9

10

11

12

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

14 Low Impact Development

15 Green Roofs

16 Porous Concrete Pavers rous_concrete_pavers/ rous_concrete_pavers/

Pervious Pavements in Cold Weather /pervious-asphalt-concrete.aspx /pervious-asphalt-concrete.aspx 17

18 Rain Gardens

19 Grass Swales

20 Detention/Retention Basins

21 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

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

23 Orifices and Weirs

24 Figure 6-1 Approximate Routing

25 Example 6-1 Single-Stage Outflow 75-Acre Development Developed Peak flow is 360 cfs (Q 25 ) 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

26 Worksheet 6A

27 Determining weir length Flow=3.2*Weir Length*(Weir Head) =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

28 Example Acre Development Existing peak flow is 35 cfs Developed peak flow is 42 cfs (24-hr, Q 100 ) Detention basin volume is 35,000 cubic feet Estimate peak outflow

29 Worksheet 6B