Review of Flood Routing Philip B. Bedient Rice University Lake Travis and Mansfield Dam Lake Travis Mansfield Dam, built in 1937 Lake Travis Brays Bayou High Flow 6 to 7 inches of Rainfall T.S. Allison June 2001 Houston Galveston Bay Hurricane Rita Landed on Sabine, TX On Sep 24, 2006 Storage Reservoirs - The Woodlands Detention Ponds These ponds store and treat urban runoff and also provide flood control for the overall development. Ponds constructed as amenities for the golf course and other community centers that were built up around them. Reservoir Routing • Reservoir acts to store water and release through control structure later. • Max Storage Inflow hydrograph • Outflow hydrograph • S - Q Relationship • Outflow peaks are reduced • Outflow timing is delayed Inflow and Outflow dS IQ dt Inflow and Outflow I1 + I2 – Q1 + Q2 2 2 = S2 – S1 Dt Inflow & Outflow Day 3 = change in storage / time S3 S2 I 2 I 3 / 2 Q2 Q3 / 2 dt Re Repeat for each day in progression Determining Storage • Evaluate surface area at several different depths • Use available topographic maps or GIS based DEM sources (digital elevation map) • Outflow Q can be computed as function of depth for either pipes, orifices, or weirs or combinations Q CA 2gH for orifice flow Q CLH 3/2 for weir flow Typical Storage -Outflow • Plot of Storage in acre-ft vs. Outflow in cfs • Storage is largely a function of topography • Outflows can be computed as function of elevation for either pipes or weirs Combined S Pipe Q Reservoir Routing 2S1 2S2 I1 I 2 Q1 Q2 dt dt 1. LHS of Eqn is known 2. Know S as fcn of Q 3. Solve Eqn for RHS 4. Solve for Q2 from S2 Repeat each time step Example Pond Routing Note that outlet consists of weir and orifice. Weir crest at h = 5.0 ft Orifice at h = 0 ft Area (6000 to 17,416 ft2) Volume ranges from 6772 to 84006 ft3 Example Pond Routing Develop Q (orifice) vs h Develop Q (weir) vs h Develop A and Vol vs h Storage - Indication 2S/dt + Q vs Q where Q is sum of weir and orifice flow rates. Storage Indication Curve • Relates Q and storage indication, (2S / dt + Q) • Developed from topography and outlet data • Pipe flow + weir flow combine to produce Q (out) Only Pipe Flow Weir Flow Begins S-I Routing Results I>Q Q>I See Excel Spreadsheet on the course web site S-I Routing Results I>Q Q>I Increased S Comparisons: River vs. Reservoir Routing Level pool reservoir River Reach River Routing River Reaches River Rating Curves • Inflow and outflow are complex • Wedge and prism storage occurs • Peak flow Qp greater on rise limb • Peak storage occurs later than Qp Looped Rating Curves • Due to complex hydraulics • Higher peak Qp on inflow • Lower peak Qp on outflow • Due to prism and wedge • Red River results shown Wedge and Prism Storage • Positive wedge I>Q • Maximum S when I = Q • Negative wedge I<Q Muskingum Equations • Continuity Equation I - Q = dS / dt • S = K [xI + (1-x)Q] • Parameters are x = weighting and K = travel time - x ranges from 0.2 to about 0.5 Q2 C0I2 C1I1 C2Q1 where C’s are functions of x, K, Dt and sum to 1.0 Muskingum Equations C0 = (– Kx + 0.5Dt) / D C1 = (Kx + 0.5Dt) / D C2 = (K – Kx – 0.5Dt) / D Where D = (K – Kx + 0.5Dt) Q2 C0I2 C1I1 C2Q1 Repeat for Q3, Q4, Q5 and so on. Muskingum River X Select X from most linear plot Obtain K from line slope Hydraulic Shapes • Circular pipe diameter D • Rectangular culvert • Trapezoidal channel • Triangular channel Storage Indication Curve • Relates Q and storage indication, (2S / dt + Q) • Developed from topography and outlet data • Pipe flow + weir flow combine to produce Q (out) Only Pipe Flow Weir Flow Begins Storage Indication Inputs height h - ft Area 102 ft Cum Vol 103 ft Q total cfs 2S/dt +Qn cfs 0 6 0 0 0 1 7.5 6.8 13 35 2 9.2 15.1 18 69 3 11.0 25.3 22 106 4 13.0 37.4 26 150 5 15.1 51.5 29 200 7 17.4 84.0 159 473 Storage-Indication Storage Indication Tabulation Time In In + In+1 2S/dt - Qn 2S/dt +Qn Qn 0 0 0 0 0 0 10 20 20 0 20 7.2 20 40 60 5.6 65.6 17.6 30 60 100 30.4 130.4 24.0 40 50 110 82.4 192.4 28.1 50 40 90 136.3 226.3 40.4 60 30 70 145.5 215.5 35.5 Time 3 - Note that 65.6 - 2(17.6) = 30.4 and is repeated for each one