1 / 17

Detention Routing

Detention Routing. www.b-e-c.com/PromoPages/GatewayBrownfields4.jpg. http://emengineers.com/images/Wh2o1lo.jpg. Objectives. Know what a detention basin is Compute a reservoir routing by hand Inflow Hydrograph Storage and Outflow versus WSE Routing Table . Detention Basins.

elma
Télécharger la présentation

Detention Routing

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Detention Routing www.b-e-c.com/PromoPages/GatewayBrownfields4.jpg http://emengineers.com/images/Wh2o1lo.jpg

  2. Objectives • Know what a detention basin is • Compute a reservoir routing by hand • Inflow Hydrograph • Storage and Outflow versus WSE • Routing Table

  3. Detention Basins • Inflow (ditch or pipe) • Storage • Outflow (orifice or weir or combination) • Berm • Emergency spillway

  4. Routing • Method used to model the outflow hydrograph • Based on continuity equation • Water in varies • Water out varies

  5. Information Needed to Route • Inflow hydrograph • Relation of storage volume to elevation in the proposed detention basin • Relation of outflow to water level elevation (discharge rating)

  6. Set up table with small time steps Water in – Water Out = Difference in Storage (water in is changing w/ time) (water out is a function of basin WSE) (basin WSE is a function of basin geometry)

  7. Reservoir Routing • Avg Inflow (I) – Avg Outflow (O) = Change in storage per some increment of time If I=O there is no change in water elevation If I>O then water surface rises If I<O then water surface decreases

  8. Reservoir RoutingOver some time increment (1 to 2) • I1 and I2 are inflows at beginning and end of time increment • O1 and O2 are outflows • S2 and S1 are actual storage volumes • Delta t is the time from 1 to 2 • Note-variables in red are initially known

  9. Equation • (I1+I2)/2 – (O1+O2)/2 = (S2-S1)/t • Rearrange to: • (I1+I2) + [(2*S1/t)-O1]=2*S2/t + O2 • Left hand side – knowns • Right-hand side - unknowns

  10. Equation • O2 and S2 -2 unknowns; need 2 equations • There is a relationship between outflow and storage volume

  11. Example 14-5Inflow Hydrograph

  12. Example 14-5 Storage Vol & Discharge vs WSE Cell G9=2*7500/(1440)-2.5=7.9 cfs Cell H9=2*7500/(1440)+2.5=12.9 cfs

  13. Example 14-5Routing Table

More Related