modeling of flood inundation in urban areas including underground space - 2008. 5. 6.- kun-yeun han,...

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Modeling of Flood Inundation in Urban Areas Including Underground Space - 2008. 5. 6.- Kun-Yeun Han, Gwangseob Kim, Chang-Hee Lee, Wan-Hee Cho Kyungpook National University, Daegu, Korea

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Modeling of Flood Inundation in Urban Areas Including Underground Space

- 2008. 5. 6.-

Kun-Yeun Han, Gwangseob Kim,

Chang-Hee Lee, Wan-Hee Cho

Kyungpook National University, Daegu, Korea

2Kyungpook National University, Korea

Outline

Introduction

Model Description

- Storm Sewer Surcharges

- Dual Drainage Analysis

- Underground Space Inundation

Application

Conclusions & Discussions

3Kyungpook National University, Korea

Recent Flood Damages in Korea

4Kyungpook National University, Korea

Flood Disaster in Urban Areas

5Kyungpook National University, Korea

Underground Inundation

Pump station

Levee

Inunation by Levee Break

P

Inunadation by Surcharge Discharge

Ur

ba

n

St

re

am

Flood Disaster in Urban Areas

6Kyungpook National University, Korea

Purpose of the Study

Inundation in the urban area causes serious damage to people and assets because of the concentration of infrastructure and high population growth.

Especially, flood inundation in underground spaces

can be an important component in urban flood.

A numerical model developed in this study, which combines 1-dimensional drainage flow with 2-dimensional surface and underground inundation phenomena.

7Kyungpook National University, Korea

Methodology

1. Hydrologic rainfall-runoff analysis model

- Using the SWMM model (RUNOFF Block), hydrologic

rainfall-runoff model computes flood discharge to estimate

manhole inflow for each basin.

2. Hydrodynamic flow analysis model for urban area

drainage system

- For hydrodynamic flow analysis SWMM model

(EXTRAN Block) is employed to compute flow routing in

drainage system with surface overflow.

8Kyungpook National University, Korea

Methodology

3. Hydraulic flow analysis model for inundated area

- DEM based hydraulic flow analysis model is developed to

determine inundated area and flow depth.

4. Inundation analysis model for underground spaces

- Link-Node model (irregular cells based) is developed to

determine inundated area and flow depth.

9Kyungpook National University, Korea

Basic assumptions and limitations

The drainage system is established by main pipelines, and the runoff volume of each subwatershed inflows through the manhole located in the main pipelines.

During flood simulation it is assumed that the inundation process initiated when surcharged overflow occurs, then it propagates to the downstream outlet of the drainage area.

The effect of buildings has been accounted in the flood analysis by considering occupation area without such factors as incoming flows to buildings, directional, and density effects.

10Kyungpook National University, Korea

Surface Runoff

Sewerfin QQ

inc QQ

Sewer

fin QQ inc QQ

Surcharged Flow

sQExcess of Drainage Capacity

Inundation of surcharged flow with complex building arrangement and topography

Concept of Inundation Analysis

11Kyungpook National University, Korea

Surface Inundation

Inflow to Underground Space

Link-Node Method

Inundation

Surface Areas

Underground Inundation

Concept of Underground Inundation

12Kyungpook National University, Korea

Rainfall-Runoff Analysis

Hydrodynamic Flow Analysis in Drainage

Network

Hydraulic Flow Analysis of Surface Overflow

Estimate Surcharged Flow

Estimate Inundation Depth and Velocity

Overflow

Inflow of Inundated Discharge

Inundation to Underground

Spaces

Inflow

Schematic Diagram of Urban Inundation Analysis

13Kyungpook National University, Korea

Stream Type

(Walkway,Rail Road)

Weir Type

(Shopping mall, Office)

Basic Concept of Link-Node Method

14Kyungpook National University, Korea

• Mass Balance Equation – Stream Type

• Mass Balance Equation – Weir Type

ikkiikki HHHHHsignQ ,,

wkwi HHHH 3

2: Free Weir

2/31, 2 wkki HHgbQ

wkwi HHHH 3

2: Submerged Weir

2/12, 2 ikwkki HHHHgbQ

Governing Equations

15Kyungpook National University, Korea

• Momentum Equation

k

kikiini

Si HHQQdt

dHA ,,

iH

kH

SiA

inQ

kiQ ,

Water Surface Line of Cell i

Water Surface Line of Cell k

Area of Cell i

Incoming flow to cell i

Discharge between Cell i and Cell k

Governing Equations

16Kyungpook National University, Korea

50m Manning’s Roughness : 0.015

0.5m

0 5 10 15 20 25Tim e (m in )

0

0.0001

0.0002

0.0003

0.0004

0.0005

Q (

cms/

m)

Ana lytica l

Calcu lated

0 5 10 15 20 25Tim e (m in )

0

0.0001

0.0002

0.0003

0.0004

0.0005

Q (

cms/

m)

A na lytica l

C alcu lated

<Stream Type>

<Weir Type>

• Simulation Condition :

- Rainfall Intensity 30 mm/hr

- Duration 10 min

- Compare with Analytical Solution

Comparison with Analytical Solution

17Kyungpook National University, Korea

Model Application – Jangan Basin

(a) land use condition (b) DEM (c) drainage system

18Kyungpook National University, Korea

(a) Building allocation (b) Ratio of building area

Model Application – Jangan Basin

19Kyungpook National University, Korea

Comparison with flood trace map

(a) flood trace map (b) simulation result

Model Validation – Jangan Basin

20Kyungpook National University, Korea

Fitness :

100(%) calobs

calobs

AA

AAFit

where, : the area of flood trace map

: the area of simulation result

obsA

calA

(%)Fit

Classification Fitness Total grid Simulation time

15m x 15m 64% 18842 3day 11hr 10min

25m x 25m 72% 6781 16hr 44min

50m x 50m 58% 1702 1hr 18min

100m x 100m 49% 422 7min

Comparisons of simulation results (Jangan basin)

21Kyungpook National University, Korea

Model Application – Dorim Basin

(a) land use condition (b) DEM (c) drainage system

22Kyungpook National University, Korea

(a) Building allocation (b) Ratio of building area

Model Application – Dorim Basin

23Kyungpook National University, Korea

Comparison with flood trace map

Model Validation – Dorim Basin

(a) flood trace map (b) simulation result

24Kyungpook National University, Korea

Fitness :

100(%) calobs

calobs

AA

AAFit

where, : the area of flood trace map

: the area of simulation result

obsA

calA

(%)Fit

Classification Fitness Total grid Simulation time

15m x 15m 69% 12032 3day 3hr 35min

25m x 25m 71% 4338 15hr 11min

50m x 50m 64% 1083 29min

100m x 100m 58% 271 6min

Comparisons of simulation results (Dorim basin)

25Kyungpook National University, Korea

Model Application – Banpo Basin

(a) land use condition (b) DEM (c) drainage system

26Kyungpook National University, Korea

(a) Building allocation (b) Ratio of building area

Model Application – Banpo Basin

27Kyungpook National University, Korea

Flood inundation analysis

Model Application – Banpo Basin

(a) 5 hours (b) 7 hours (c) 9 hours

28Kyungpook National University, Korea

Application Strategies

Flow characteristics in underground space were computed by link-node system.

The suggested model can simulate the underground flood flow related to the influence of stairs and wall-structures.

Empirical discharge formulas were introduced to analyze weir-type flow for a underground shopping mall and channel-type flow for subway railroad respectively.

29Kyungpook National University, Korea

• Constitution of

underground spaces

- B1st floor :

Shopping Street

- B2nd floor :

Ticket Office and

Management Office

-B3rd floor :

Platform and Railway

Application to Underground Space

30Kyungpook National University, Korea

Inflow Point

Inflow into Underground Spaces

31Kyungpook National University, Korea

Inflow Point

B1 # 448

B1 # 594

B1 # 494 B1 # 501

B1 # 627 B1 # 634

B1 # 471

B1 # 601

Inundation Analysis in B1st Floor

0 4 8 12 16T ime (hr)

0

0.1

0.2

0.3D

ep

th (

m)

B 1 # 448

0 4 8 12 16T ime (hr)

0

0.1

0.2

0.3

De

pth

(m

)

B 1 # 471

0 4 8 12 16T ime (hr)

0

0.1

0.2

0.3

De

pth

(m

)

B 1 # 494

0 4 8 12 16T ime (hr)

0

0.1

0.2

0.3

De

pth

(m

)

B 1 # 501

32Kyungpook National University, Korea

B2 # 379

B2 # 507

B2 # 402 B2 # 409

B2 # 545 B2 # 523

B2 # 426

B2 # 511

Inflow Point from 1st floor

Inflow Point from 1st floor

Inundation Analysis in B2nd Floor

0 4 8 12 16Tim e (hr)

0

0.04

0.08

0.12

0.16

De

pth

(m

)B2 # 379

0 4 8 12 16Tim e (hr)

0

0.04

0.08

0.12

0.16

De

pth

(m

)

B 2 # 409

0 4 8 12 16Tim e (hr)

0

0.04

0.08

0.12

0.16

De

pth

(m

)

B 2 # 545

0 4 8 12 16Tim e (hr)

0

0.04

0.08

0.12

0.16

De

pth

(m

)

B 2 # 426

33Kyungpook National University, Korea

PatformRailroad

Railroad

Inflow Point from 2nd Floor

B3 # 366 B3 # 54

B3 # 763

B3 # 87

B3 # 386B3 # 820

B3 # 30

B3 # 787

Inflow Point from 2nd Floor

Inundation Analysis in B3rd Floor

0 4 8 12 16

T im e (hr)

0

0.04

0.08

0.12

0.16

0.2

De

pth

(m

)B 3 # 54

0 4 8 12 16

T im e (hr)

0

0.04

0.08

0.12

0.16

0 .2

De

pth

(m

)

B 3 # 366

0 4 8 12 16

T im e (hr)

0

0.04

0.08

0.12

0.16

0.2

De

pth

(m

)

B 3 # 763

0 4 8 12 16

T im e (hr)

0

0.04

0.08

0.12

0.16

0.2

De

pth

(m

)

B 3 # 787

34Kyungpook National University, Korea

Comparison with flood trace map

(a) flood trace map (b) simulation result

Model Validation – Banpo Basin

35Kyungpook National University, Korea

Inundation Analysis for Underground

36Kyungpook National University, Korea

Conclusions

1-D and 2-D unsteady flow analysis was performed considering the flow rates through the surcharges from storm sewer networks.

Inundation in underground space was computed by link-node system. Empirical discharge formulas were introduced to analyze weir-type flow for a underground shopping mall and channel-type flow for subway railway, respectively.

The model was applied to Banpo subway station in Seoul. The simulated results agree well with observed data.

37Kyungpook National University, Korea

Thanks for Your Attention !

38Kyungpook National University, Korea

Depth Variation due to Inundation Analysis

- Subbasin runoff discharge from runoff block

- Time independent inflow discharge

- Time variable inflow discharge

- Inundated surface discharge

Hydrodynamic flow analysis in drainage pipelines (EXTRAN)

- Checking the status of inflow - Estimate inflow discharge - Idendifying overloaded flow condition - Estimate overflow discharge

Inundated Discharge

Inflow of inundation discharge

Surface runoff due to overflow discharge

2D inundation anlysis