Longitudinal dams as an alternative to wing dikes in river …€¦ · insight into the range of...
Transcript of Longitudinal dams as an alternative to wing dikes in river …€¦ · insight into the range of...
Longitudinal dams as an alternative to wing dikes in river engineering
Fredrik Huthoff
Contents • Introduction
– Why consider longitudinal dams? – “Room for the river” in the Netherlands
• The pilot study – The Dutch Rhine – Wing dike lowering – Pilot study for longitudinal dams
• Numerical model • Results
– Impacts on flow
– Morphodynamic effects • Discussion & Conclusions
Introduction • Are longitudinal dams a suitable
alternative for wing dikes? • Functions of wing dikes
– Protection of banks – Maintain required flow depths for navigation during
low-discharge situations – Wing dikes force the flow field towards the main
channel in the river during low flows • Larger flow depths • Less sedimentation in the main channel
• Disadvantages of wing dikes – during high-discharge conditions wing dikes obstruct
the flow and may lead to higher flood levels – Design is not flexible – Wing dikes cause local disturbances to flow and river
beds
Longitudinal dams: a pilot study
• A study for longitudinal dams in the Rhine • Use dams instead of (lowered) wing dikes • Computational study to investigate
hydrodynamic and morphodynamic effects – Consider different types of dams in order to get
insight into the range of possible effects
The Rhine
Wing dike lowering
Wing dike lowering in the Rhine
Room for the river – Main objective: increase safety by reducing water levels
on the Rhine – The target is approximately 10 cm water level lowering
at the design discharge of 16000 m3/s – This can be (partly) achieved by lowering the wing dikes
by approx. 1,5 m over a length of 76 km (DHV 2011) – Is a longitudinal dam a suitable alternative for wing
dikes?
Lowering of groynes has already started!
Pilot longitudinal dams
• Remove 37 (lowered) wing dikes on inner bends and add longitudinal dams in a river section of 11 km length
• Wing dikes on outer bends are not lowered
• Height of dam is comparable to height of the (unlowered) wing dikes
• Consider variations in dams: – vertical wall and dam with side
slope – with and without openings
Effect on flood levels: translate bed elevation to WAQUA 2D
• 2D hydrodynamic model • Curvilinear grid (cell size ~ 80 by 20 m) • Calculate water levels at design discharge
(16000 m3/s) • Several cases considered:
1a: dam as vertical wall (without openings) 1b: dam as vertical wall (with openings) 2a: dam with side slope 1:3 (without openings) 2b: dam with side slope 1:3 (with openings) 3: dam with side slope 1:2.5 (with openings) and
removal of obstacles in the river bank section
Effect on flood levels (WAQUA 2D)
• 2D hydrodynamic mode • Curvilinear grid (cell size ~ 80 by 20 m) • Calculate water levels at design discharge (16000 m3/s) • Several cases considered:
1a: dam as vertical wall (without openings) 1b: dam as vertical wall (with openings) 2a: dam with side slope 1:3 (without openings) 2b: dam with side slope 1:3 (with openings) 3: dam with side slope 1:2.5 (with openings) and removal of
obstacles in the river bank section
-0.2
-0.18
-0.16
-0.14
-0.12
-0.1
-0.08
-0.06
-0.04
-0.02
0
865870875880885890895900905910915920925930935940945950955960
kribvlg tov refdamopbr tov refdamopsl tov refoptimale variant 1 tov refopeningen in dam
(2b) (1b)
(3)
(groynes)
Water level difference
River kilometer
Long. dams Lowered groynes Lowered groynes
Morphodynamic effects: translate bed elevation to Delft3D
• Deltares’ open source package • 2D hydro- & morphodynamic mode • Curvilinear grid (cell size ~ 80 by 20 m)
– Refined grid in pilot study area (factor 3)
• Sediment transport – Uniform sediment – Van Rijn
• Morphological calibration – Adopt grain size to get agreement with measured
sediment transport loads • Study the RELATIVE EFFECT of longitudinal dam
– Compare to projected development of current situation
Computational grid
Case 2a: dam with side slope 1:2.5 (without openings)
Dam with side slope without openings
Case 2b: dam with side slope 1:2.5 (with openings)
Dam with side slope with openings
Input discharge hydrograph (8 discharge levels)
Results (velocity field)
Q = 1409 m3/s
Bed level changes After 1 year
Bed level changes After 2 years
Bed level changes After 5 years
Bed level changes After 8 years
Bed level changes After 10 years
Quick morphodynamic response (1-2 years)
Bed level changes
Groyne lowering
With openings in dam
Bed level change (m
)
Bed level changes
Groyne lowering
Without openings in dam
Potential steering parameter?
Bed level change (m
)
Conclusions • LDs may be a suitable alternative for wing
dikes – Maintain flow depths & sediment transport rates during
low flows – Quick morphodynamic response (1-2 years)
• Advantages over wing dikes are: – LDs give less resistance to flow during high discharge
events (lower flood levels) – Additional flow area can be created behind the dams to
lower flood levels – LDs allow easy readjustment of inlets/outlets to correct
for unwanted morphodynamic effects (minimize dredging efforts)
• Future studies of LDs should also focus on – Combination of LD-designs and monitoring strategies to
optimize LD-design (openings in dam) – morphodynamics behind the LD in order to get insight into
stability (or required maintenance) of LD-designs
Questions?
Fredrik Huthoff
Changes in discharge capacity (with respect to current situation)
Correlates well with bed level changes
Q = 3813 m3/s