Title: Review of Flood Routing
1Review of Flood Routing
- Philip B. Bedient
- Rice University
2Lake Travis and Mansfield Dam
Lake Travis
3LAKE LIVINGSTON
4LAKE CONROE
5ADDICKS/BARKER RESERVOIRS
6Storage Reservoirs - The Woodlands
7Detention 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.
8 DETENTION POND, AUSTIN, TX
9LAKE CONROE WEIR
10Comparisons River vs. Reservoir Routing
Level pool reservoir
River Reach
11Reservoir Routing
- Reservoir acts to store water and
release through control structure later. - Inflow hydrograph
- Outflow hydrograph
- S - Q Relationship
- Outflow peaks are reduced
- Outflow timing is delayed
Max Storage
12Inflow and Outflow
13Numerical Equivalent Assume I1 Q1 initially
I1 I2 Q1 Q2 S2 S1
2
2
Dt
14Numerical Progression
I1 I2 Q1 Q2 S2 S1
1.
DAY 1
2
2
Dt
I2 I3 Q2 Q3 S3 S2
2.
DAY 2
Dt
2
2
I3 I4 Q3 Q4 S4 S3
3.
DAY 3
Dt
2
2
15Determining Storage
- Evaluate surface area at several different
depths - Use available topographic maps or GIS based
DEM sources (digital elevation map) - Storage and area vary directly with depth of
pond
Elev
Volume
Dam
16Determining Outflow
- Evaluate area storage at several different
depths - Outflow Q can be computed as function of depth
for Pipes - Mannings Eqn - Orifices - Orifice Eqn
- Weirs or combination outflow structures - Weir
Eqn
Weir Flow
Orifice/pipe
17Determining Outflow
Weir
H
Orifice H measured above Center of the
orifice/pipe
18Typical 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
Pipe/Weir
S
Pipe
Q
19Reservoir Routing
- LHS of Eqn is known
- Know S as fcn of Q
- Solve Eqn for RHS
- Solve for Q2 from S2
Repeat each time step
20Example Reservoir Routing ---------- Storage
Indication
21Storage Indication Method
STEPS Storage - Indication Develop Q (orifice)
vs h Develop Q (weir) vs h Develop A and Vol
vs h 2S/dt Q vs Q where Q is sum of weir and
orifice flow rates.
- 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
-
22Storage 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
23Storage Indication Inputs
Storage-Indication
24Storage Indication Tabulation
Time 2 Note that 20 - 2(7.2) 5.6 and is
repeated for each one
25S-I Routing Results
I gt Q
Q gt I
See Excel Spreadsheet on the course web site
26S-I Routing Results
I gt Q
Q gt I
Increased S
27RIVER FLOOD ROUTING
28CALIFORNIA FLASH FLOOD
29River Routing
Mannings Eqn
River Reaches
30 River Rating Curves
- Inflow and outflow are complex
- Wedge and prism storage occurs
- Peak flow Qp greater on rise limb than on
the falling limb - Peak storage occurs later than Qp
31Wedge and Prism Storage
- Positive wedge I gt Q
- Maximum S when I Q
- Negative wedge I lt Q
32Actual Looped Rating Curves
33Muskingum Method - 1938
- Continuity Equation I - Q dS / dt
- Storage Eqn S K x I (1-x)Q
- Parameters are x weighting Coeff
- K travel time or time between peaks
- x ranges from 0.2 to about 0.5 (pure trans)
- and assume that initial outflow initial
inflow
34Muskingum Method - 1938
- Continuity Equation I - Q dS / dt
- Storage Eqn S K x I (1-x)Q
- Combine 2 eqns using finite differences for I,
Q, S - S2 - S1 K x(I2 - I1) (1 - x)(Q2 -
Q1) - Solve for Q2 as fcn of all other parameters
35Muskingum Equations
Where C0 ( Kx 0.5Dt) / D C1 (Kx
0.5Dt) / D C2 (K Kx 0.5Dt) / D
Where D (K Kx 0.5Dt) Repeat for Q3, Q4,
Q5 and so on.
36Muskingum River X
Select X from most linear plot
Obtain K from line slope
37 Mannings Equation
Mannings Equation used to estimate flow rates Qp
1.49 A (R2/3) S1/2 Where Qp flow rate n
roughness A cross sect A R A / P S Bed
Slope
n
38 Hydraulic Shapes
- Circular pipe diameter D
- Rectangular culvert
- Trapezoidal channel
- Triangular channel