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Review of Flood Routing

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Outflow Q can be computed as function of depth for Pipes - Manning's Eqn. Orifices - Orifice Eqn ... Center of the orifice/pipe. H. Typical Storage -Outflow ... – PowerPoint PPT presentation

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Title: Review of Flood Routing


1
Review of Flood Routing
  • Philip B. Bedient
  • Rice University

2
Lake Travis and Mansfield Dam
Lake Travis
3
LAKE LIVINGSTON
4
LAKE CONROE
5
ADDICKS/BARKER RESERVOIRS
6
Storage Reservoirs - The Woodlands
7
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.

8
DETENTION POND, AUSTIN, TX
9
LAKE CONROE WEIR
10
Comparisons River vs. Reservoir Routing
Level pool reservoir
River Reach
11
Reservoir 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
12
Inflow and Outflow
13
Numerical Equivalent Assume I1 Q1 initially
I1 I2 Q1 Q2 S2 S1

2
2
Dt
14
Numerical 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
15
Determining 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
16
Determining 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
17
Determining Outflow
Weir
H
Orifice H measured above Center of the
orifice/pipe
18
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

Pipe/Weir
S
Pipe
Q
19
Reservoir 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
20
Example Reservoir Routing ---------- Storage
Indication
21
Storage 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

22
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
23
Storage Indication Inputs
Storage-Indication
24
Storage Indication Tabulation
Time 2 Note that 20 - 2(7.2) 5.6 and is
repeated for each one
25
S-I Routing Results
I gt Q
Q gt I
See Excel Spreadsheet on the course web site
26
S-I Routing Results
I gt Q
Q gt I
Increased S
27
RIVER FLOOD ROUTING
28
CALIFORNIA FLASH FLOOD
29
River 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

31
Wedge and Prism Storage
  • Positive wedge I gt Q
  • Maximum S when I Q
  • Negative wedge I lt Q

32
Actual Looped Rating Curves
33
Muskingum 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

34
Muskingum 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

35
Muskingum 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.
36
Muskingum 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
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