chapter 8: dynamic stability - tu delft ocw · 2016. 3. 3. · chapter 8: dynamic stability ct5308...

23
March 29, 2012 1 Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences Section Hydraulic Engineering

Upload: others

Post on 21-Mar-2021

3 views

Category:

Documents


0 download

TRANSCRIPT

Page 1: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012

Vermelding onderdeel organisatie

1

Chapter 8: Dynamic Stability

ct5308 Breakwaters and Closure Dams

H.J. Verhagen

Faculty of Civil Engineering and GeosciencesSection Hydraulic Engineering

Page 2: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012 2

What is dynamic stability ?

• Do not design on “damage”• Try to make the breakwater in such a way that it gets

a “stable” form• Extra material is needed• “Natural” dynamically stable breakwaters seem to exist

on Iceland• However, these breakwaters are not permeable

Page 3: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012 3

Types of berm breakwaters

• Statically stable non-reshaping structuresIn this condition only some few stones are allowed to move similar to a conventional rubble mound breakwater

• Statically stable reshaped structuresIn this condition the profile is allowed to reshape into a profile, which is stable and where the individual stones are also stable

• Dynamically stable reshaped structuresIn this condition the profile is reshaped into a stable profile, but the individual stones may move up and down the slope

Page 4: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012 4

Selection process for rubble mounds

• Is it economical to design an conventional rubble mound ? Can all quarried material be used ?

• If not all material can be used, and Hs < 2, use stable non-reshaping berm breakwater. If 2 < Hs < 3 m this might be a good option in case of dedicated quarry.

• If the stones are too small, use statically reshaped type

• If this also is not possible, use more stone and make dynamically stable berm breakwater

Page 5: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012 5

Types of berm breakwaters

Dynamically stable reshaped BB

• Two stone classes• Homogeneous berm• Wide stone gradation• Low permeability• Reshaping structures• Allowed erosion < berm width• More voluminous• No interlocking

Statically stable non-reshaping BB

• Several stone classes• Berm of size-graded layers• Narrow stone gradation• High permeability• Non-reshaping structures• Allowed recession < 2*Dn50

• Less voluminous• Interlocking prescribed

Page 6: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012 6

Berm breakwaters in the worldCountry Number of berm

breakwaters Year first

breakwater was completed

Iceland Canada USA Australia Brazil Norway Denmark (Far Oer) Iran Portugal (Madeira) China (Hong Kong)

27 5 4 4 2 4 1 8 1 1

1984 1984 1984 1986 1990 1991 1992 1996 1996 1999

Total 57

Data from Pianc report on berm breakwaters 2003

Page 7: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012 7

schematised profile for sand and gravel beaches

500.041c s m nl H T g D=

1.8s r cl l l= =

Page 8: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012 8

Influence of wave climate on a berm breakwater profile

Page 9: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012 9

Berm breakwater Berlevåg (Norway)

Figure from Jacobsen et al, PIANC congress 2002

Page 10: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012 10

Reshaped profile of Berlevågbreakwater

Figure from Jacobsen et al, PIANC congress 2002

Page 11: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012 11

Reshaping calculations

• Van der Meer (1988 - 1990 Breakwat• Van Gent (1995) Odiflocs• Archetti and Lamberti (1996) (See Copedec Cape Town)

• new research by Tørum (1998, 2001)

Page 12: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012 12

Recession according to Tørum (1)

Special parameter for recession: H0T0

50

050

so

n

zn

HHD

gT TD

=

Tz is mean period

Page 13: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012 13

Recession according to Tørum (2)

3 2 20 0 0 0 0 0

506

6

( ) ( ) ( ) ( 9.9 23.9 10.5)

2.7 109 100.11

g g hn

Rec A H T B H T C H T f f fd

ABC

= + + − − + − −

=

==

85 15/ 1.3 1.8g n n gf d d f= < <

50

0.1 3.2hn

hfd

⎛ ⎞=− +⎜ ⎟

⎝ ⎠

gradation factor

depth factor

Page 14: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012 14

Recession according to Tørum (3)

50 50 50

0.2 0.5 12.5 25f

n

h h hford d d

= + < <

Place of the intersection of profiles:

Page 15: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012 15

Longshore transport of stone

• apply same type of formula as longshore sand transport

• to prevent excessive transport, apply

• for heads use a value of 3

• Curve fitted transport formula:

504.5s

n

HD

≤Δ

2

50 50( ) 0.00005 105s

pn n

H gS x TD D

⎛ ⎞= −⎜ ⎟⎜ ⎟Δ⎝ ⎠

Page 16: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012 16

cross section of the Sirevåg breakwater

20-3010-204-101-4

IIIIIIIV

Wmin-Wmax (tonnes)Stone class

€ 20.000/m (2000/2001)

Page 17: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012 17

Design conditions• 100 years return period Hs = 7.0 m, Tp=14.2 s

(based on hindcast + refraction study)• Storm of December 1998:

Hs=7.0 m, Tp=14 s• Storm of February 1999:

Hs=6.7 m, Tp=15 s• Storm of January 2002:

Hs=9.3 m at deep water (450 m offshore)

Hs=7.9, Tp=10 s

•Damage to breakwater: 8 stones removed, 6 stones moved

Page 18: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012 18

Prototype and model

Page 19: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012 19

Stone classes and Quarry yieldSirevåg

1.59

1.36

1.26

1.114

dmx/dmin

19.3%4.02.01-4IV

13.7%2.56.04-10III

9.9%2.013.310-20II

5.6%1.523.320-30I

Expected quarry yield

Wmax/WminWmeanWmin-WmaxStone Class

Page 20: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012 20

Sirevåg yield cure

Page 21: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012 21

Sirevåg breakwater

Page 22: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012 22

Sirevåg breakwater

Page 23: Chapter 8: Dynamic Stability - TU Delft OCW · 2016. 3. 3. · Chapter 8: Dynamic Stability ct5308 Breakwaters and Closure Dams H.J. Verhagen Faculty of Civil Engineering and Geosciences

March 29, 2012 23

Sirevåg breakwater