Skip to main content
Log in

Experimental investigation of erosion processes downstream of block ramps in mild curved channels

  • Original Article
  • Published:
Environmental Fluid Mechanics Aims and scope Submit manuscript

Abstract

Eco-friendly low-head river restoration structures such as block ramps are of paramount importance with regard to the control of sediment grade in rivers, particularly in the mountains. They also help in the stabilization of river bed and prevent damages due to excessive downstream erosion by dissipating flow energy. Although the hydraulic characteristics of block ramps in straight channels have been thoroughly studied, there are very less studies dealing with the analysis of scour mechanism downstream of block ramps in curved channels. In fact, to the authors’ best knowledge, there are no studies till date investigating the scour process downstream of block ramps in river bends, involving the effect of tailwater and ramp bed slope. Therefore, this study aims to analyze the hydraulic behaviour of block ramps placed at various positions on a curved channel incorporating the effects of the mentioned parameters. Furthermore, the equilibrium morphology of the resulting downstream scour has been analyzed and classified. A dedicated hydraulic model was constructed, and a large range of in situ hydraulic conditions were simulated. Tests were carried out varying ramp slope and locating the structure at different positions along the channel bend. Data analysis revealed that the scour morphology is essentially three-dimensional and depends on flow characteristics, tailwater level and slightly on its location. Finally, a useful design relationship was also developed to evaluate the maximum scour depth taking into consideration the effect of channel curvature and the tailwater level.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10

Similar content being viewed by others

Abbreviations

B :

Channel width

d xx :

Size of bed material for which xx% is finer

f :

Function of

Fd :

Densimetric Froude number

\({\dot{\text{F}}}\) d90 :

Equivalent densimetric Froude number for curved channels

g :

Gravitational acceleration

g′:

Reduced gravitational acceleration

h 1 :

Approach flow depth at ramp toe

h 0 :

Downstream tailwater depth

l 0 :

Scour length

Q :

Discharge

S 0 :

Block ramp slope

V 1 :

Average approach flow velocity at the ramp toe

x :

Longitudinal coordinate

z :

Vertical coordinate

z max :

Maximum scour depth

z max(t=2 h) :

Maximum scour depth after 2 h from the beginning of the test

z max(t=6 h) :

Maximum scour depth after 6 h from the beginning of the test

z M :

Maximum ridge height

Z m :

Non-dimensional scour depth in straight channels

Z msc :

Non-dimensional scour depth in curved channels

R :

Radius of curvature of the channel

α :

Location of the block ramp in the curved channel

Π i :

ith non-dimensional group

ρ :

Water density

ρ s :

Sediment density

σ :

Sediment non-uniformity parameter

Ψ i :

ith re-arranged non-dimensional group

References

  1. Adduce C, Rocca M (2006) Local scouring due to turbulent water jets downstream of a trapezoidal drop: laboratory experiments and stability analysis. Water Resour Res 42:W02405. https://doi.org/10.1029/2005WR004139

    Article  Google Scholar 

  2. Bombardelli FA, Palermo M, Pagliara S (2018) Temporal evolution of jet induced scour depth in cohesionless granular beds and the phenomenological theory of turbulence. Phys Fluids 30:1–19. https://doi.org/10.1063/1.5041800

    Article  Google Scholar 

  3. Bormann E, Julien PY (1991) Scour downstream of grade control structures. J Hydraul Eng 117(5):579–594. https://doi.org/10.1061/(ASCE)0733-9429(1991)117:5(579)

    Article  Google Scholar 

  4. Breusers HNC, Raudkivi AJ (1991) Scouring. IAHR hydraulic structures design manual. Balkema, Rotterdam

    Google Scholar 

  5. D’Agostino V, Ferro V (2004) Scour on alluvial bed downstream of grade-control structures. J Hydraul Eng 130(1):1–14. https://doi.org/10.1061/(ASCE)0733-9429(2004)130:1(24)

    Article  Google Scholar 

  6. Dey S, Raikar RV (2005) Scour in long contractions. J Hydraul Eng 131(12):1036–1049. https://doi.org/10.1061/(ASCE)0733-9429(2005)131:12(1036)

    Article  Google Scholar 

  7. Dey S, Sarkar A (2006) Scour downstream of an apron due to submerged horizontal jets. J Hydraul Eng 132(3):246–257. https://doi.org/10.1061/(ASCE)0733-9429(2006)132:3(246)

    Article  Google Scholar 

  8. Hoffmans GJCM (1998) Jet scour in equilibrium phase. J Hydraul Eng 124(4):430–437. https://doi.org/10.1061/(ASCE)0733-9429(1998)124:4(430)

    Article  Google Scholar 

  9. Hoffmans GJCM, Verheij HJ (1997) Scour manual. Balkema, Rotterdam

    Google Scholar 

  10. Hughes WC, Flack JE (1984) Hydraulic jump properties over a rough bed. J Hydraul Eng 110(12):1755–1772. https://doi.org/10.1061/(ASCE)0733-9429(1984)110:12(1755)

    Article  Google Scholar 

  11. Mason PJ, Arumugam K (1985) Free jet scour below dams and flip buckets. J Hydraul Eng 111(2):220–235. https://doi.org/10.1061/(ASCE)0733-9429(1985)111:2(220)

    Article  Google Scholar 

  12. Pagliara S, Mahmoudi Kurdistani S (2015) Clear water scour at J-Hook Vanes in channel bends for stream restorations. Ecol Eng 83:386–393. https://doi.org/10.1016/j.ecoleng.2015.07.003

    Article  Google Scholar 

  13. Pagliara S, Mahmoudi Kurdistani S, Palermo M, Simoni D (2016) Scour due to rock sills in straight and curved horizontal channels. J Hydro-Environ Res 10:12–20. https://doi.org/10.1016/j.jher.2015.07.002

    Article  Google Scholar 

  14. Pagliara S, Palermo M (2008) Scour control downstream of block ramps. J Hydraul Eng 134(9):1376–1382. https://doi.org/10.1061/(ASCE)0733-9429(2008)134:9(1376)

    Article  Google Scholar 

  15. Pagliara S, Palermo M (2008) Scour control and surface sediment distribution downstream of block ramps. J Hydraul Res 46(3):334–343. https://doi.org/10.3826/jhr.2008.3208

    Article  Google Scholar 

  16. Pagliara S, Palermo M (2010) Influence of tailwater depth and pile position on scour downstream of block ramps. J Irrig Drain Eng 136(2):120–130. https://doi.org/10.1061/(ASCE)IR.1943-4774.0000132

    Article  Google Scholar 

  17. Pagliara S, Palermo M (2015) Hydraulic jumps on rough and smooth beds: aggregate approach for horizontal and adverse-sloped beds. J Hydraul Res 53(2):243–252. https://doi.org/10.1080/00221686.2015.1017778

    Article  Google Scholar 

  18. Pagliara S, Palermo M, Carnacina I (2009) Scour and hydraulic jump downstream of block ramps in expanding stilling basins. J Hydraul Res 47(4):503–511. https://doi.org/10.1080/00221686.2009.9522026

    Article  Google Scholar 

  19. Pagliara S, Palermo M, Das R (2016) Eco-friendly countermeasures for enlarged basins erosion. River Res Appl 32(3):441–451. https://doi.org/10.1002/rra.2869

    Article  Google Scholar 

  20. Pagliara S, Radecki-Pawlik A, Palermo M, Plesiński K (2017) Block ramps in curved rivers: morphology analysis and prototype data supported design criteria for mild bed slopes. River Res Appl 33(3):427–437. https://doi.org/10.1002/rra.3083

    Article  Google Scholar 

  21. Palermo M, Pagliara S (2017) D-jump in rough sloping channels at low Froude numbers. J Hydro-Environ Res 14:150–156. https://doi.org/10.1016/j.jher.2016.10.002

    Article  Google Scholar 

  22. Veronese A (1937) Erosioni di fondo a valle di uno scarico. Ann Lav Pubblici 75(9):717–726 (in Italian)

    Google Scholar 

Download references

Acknowledgements

All authors equally set up the research, analyzed the results, and contributed to writing the paper. This research was funded by University of Pisa Research Project PRA_2018_35 “Approcci eco-sostenibili per i sistemi idrici e la riqualificazione del territorio in ambito urbano”.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Michele Palermo.

Additional information

Publisher's Note

Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Appendix: dimensional analysis

Appendix: dimensional analysis

According to Hoffmans [8] and Bombardelli et al. [2], the theoretical diffusion length (zmax + h0), i.e., the sum of the maximum scour depth, zmax, and the water depth over the original sediment bed level, h0, depends on the following variables:

$$z_{max} + h_{0} = f\left( {Q, h_{1} ,B, g,\Delta \rho ,\rho ,d_{90} ,\alpha ,R,S_{0} } \right)$$
(10)

By assuming Q, h1 and ρ as repeating variables, we obtain the following non-dimensional groups:

$$\varPi_{1} = \frac{{z_{max} + h_{0} }}{{h_{1} }}$$
(11)
$$\varPi_{2} = \frac{B}{{h_{1} }}$$
(12)
$$\varPi_{3} = \frac{{h_{1}^{5} g}}{{Q^{2} }}$$
(13)
$$\varPi_{4} = \frac{\Delta \rho }{\rho }$$
(14)
$$\varPi_{5} = \frac{{d_{90} }}{{h_{1} }}$$
(15)
$$\varPi_{6} = \alpha$$
(16)
$$\varPi_{7} = \frac{R}{{h_{1} }}$$
(17)
$$\varPi_{8} = S_{0}$$
(18)

Let’s now re-arrange some of the non-dimensional groups Πi as follows:

$$\varPsi_{3} = \sqrt {\frac{1}{{\varPi_{3} }}\frac{1}{{\varPi_{2}^{ 2} }}\frac{1}{{\varPi_{5} }}\frac{1}{{\varPi_{4} }}} = \sqrt {\frac{{Q^{2} }}{{h_{1}^{2} B^{2} gd_{90} \frac{\Delta \rho }{\rho }}}} = \frac{V}{{\sqrt {gd_{90} \frac{\Delta \rho }{\rho }} }} = F_{d90}$$
(19)
$$\varPsi_{5} = \frac{{\varPi_{5} }}{{\varPi_{2} }} = \frac{{d_{90} }}{B}$$
(20)
$$\varPsi_{7} = \frac{{\varPi_{2} }}{{\varPi_{7} }} = \frac{B}{R}$$
(21)

Therefore, the non-dimensional functional relationship can be expressed as follows:

$$\varPi_{1} = f\left( {\varPi_{2} , \varPsi_{3} ,\varPi_{4} ,\varPsi_{5} ,\varPi_{6} ,\varPsi_{7} ,\varPi_{8} } \right)$$
(22)

Considering that B, d90, Δρ and ρ are constant, and that the effect of the non-dimensional group Π2 (= B/h1) is negligible, Eq. (22) can be re-written as:

$$\varPi_{1} = f\left( {\varPsi_{3} ,\varPi_{6} ,\varPsi_{7} ,\varPi_{8} } \right)$$
(23)

Or, equivalently:

$$\frac{{z_{max} + h_{0} }}{{h_{1} }} = f\left( {F_{d90} ,\alpha ,\frac{B}{R},S_{0} } \right)$$
(24)

As α has negligible effect on the variable (zmax + h0)/h1, the governing functional relationship becomes:

$$\frac{{z_{max} + h_{0} }}{{h_{1} }} = f\left( {F_{d90} ,\frac{B}{R},S_{0} } \right)$$
(25)

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Pagliara, S., Palermo, M. & Roy, D. Experimental investigation of erosion processes downstream of block ramps in mild curved channels. Environ Fluid Mech 20, 339–356 (2020). https://doi.org/10.1007/s10652-019-09681-1

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s10652-019-09681-1

Keywords

Navigation