Skip to main content

Numerical modeling of the Sakuma Dam reservoir sedimentation

Abstract

The present study attempts to predict the reservoir sedimentation in 32 km region of the Tenryu River between the Hiraoka and Sakuma Dams in Japan. For numerical simulations of the reservoir sedimentation, the one-dimensional model of the Hydrologic Engineering Centre-River Analysis System (HEC-RAS) is used together with the inclusion of channel geometry, bed gradation curve, Exner-5 bed sorting mechanisms, fall velocity of the particle, and flow and sediment boundary conditions pertaining to modeling region. The modeling region of the Tenryu River is divided into 48 river stations with 47 reaches in the numerical simulations. The numerical model is calibrated using the available data for 48 years from 1957 to 2004. The formulae of sediment transport function, Manning’s roughness coefficient, computational increment and fall velocity have been identified for getting the best estimation of the Sakuma Dam reservoir sedimentation. Combination of obtained sensitive parameters and erodible limits of 2 m gave the best comparison with the measured bed profile. The computed results follow the trend of measured data with a small underestimation. Although Manning’s roughness coefficient has an effect on the sedimentation, no direct relation is found between the Manning’s roughness coefficient and reservoir sedimentation. It is found that the temperature of water has no effect on the reservoir sedimentation.

This is a preview of subscription content, access via your institution.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11
Fig. 12
Fig. 13
Fig. 14
Fig. 15

Abbreviations

A :

Cross-sectional area

h :

Depth of flow

Q :

Flow rate

Q s :

Sediment transport rate of size class i

V :

Average channel velocity

S f :

Energy slope

d :

Representative particle diameter

s f :

Particle shape factor

d i :

Geometric mean diameter of particles in size class i

T :

Temperature of water

λ :

Bed porosity

\( \partial \eta \) :

Change in bed level

x :

Streamwise coordinate

t :

Time step

Δx :

Spatial step

η :

Bed elevation

f :

Dependent variable

α :

Weighting factor

a :

Length of particle along the longest axis perpendicular to the other two axes

b :

Length of particle along the intermediate axis perpendicular to the other two axes

c :

Length of particle along the short axis perpendicular to other two axes

j, k :

Grid coordinates

n :

Manning’s roughness coefficient

q l :

Volumetric rate of lateral inflow or outflow per unit length of the channel

References

  • Ackers P, White WR (1973) Sediment transport: new approach and analysis. J Hydraul Div 99(hy11):2041

    Google Scholar 

  • Ahm J, Yang C (2015) Determination of recovery factor for simulation of non-equilibrium sedimentation in reservoir. Int J Sedim Res 30(1):68–73

    Article  Google Scholar 

  • Beebo Q, Bilal AR (2012) Simulating bathymetric changes in reservoirs due to sedimentation (tvvr-12/5018)

  • Brunner GW (2002a) HEC-RAS river analysis system hydraulic reference manual, version 3.1, Hydrologic Engineering Center

  • Brunner GW (2002b) HEC-RAS river analysis system: User’s manual. US Army Corps of Engineers, Hydrologic Engineering Center, Davis

    Google Scholar 

  • Brunner GW (2010) HEC-RAS Hydraulic Reference Manual. US Army Corps of Engineer, Hydrological Engineering Center, Davis

    Google Scholar 

  • Caputo M, Carcione JM (2013) A memory model of sedimentation in water reservoirs. J Hydrol 476:426–432

    Article  Google Scholar 

  • Chaishi T, Kikuchi T, Maeda S (2002) Accumulation of sediments in a reservoir and its countermeasures” a case study of Sakuma Dam”. J Jpn Soc Eng Geol 43(5):316–319

    Article  Google Scholar 

  • Chen Ridong, Shao Songdong, Liu Xingnian (2015) Water–sediment flow modeling for field case studies in Southwest China. Nat Hazards 78(2):1197–1224

    Article  Google Scholar 

  • Ching-Hseinm W, Ching-Nuo C, Chih-Heng T, Chang-Tai T (2012) Estimating sediment deposition volume in a reservoir using the physiographic soil erosion-deposition model. Int J Sedim Res 27(3):362–377

    Article  Google Scholar 

  • Corey AT (1949) Influence of shape on the fall velocity of sand grains. Colorado State University, Fort Collins

    Google Scholar 

  • Dietrich WE (1982) Settling velocity of natural particles. Water Resour Res 18(6):1615–1626

    Article  Google Scholar 

  • Engelund F, Hansen E (1967) A monograph on sediment transport in alluvial streams. Tech. rep., TEKNISKFORLAG Skelbrekgade 4 Copenhagen V, Denmark

  • Haq IU, Abbas ST (2007) Sedimentation of Tarbela and Mangla reservoirs. In: Proceedings of the 70th annual session of the pakistan engineering congress

  • Harb G (2013) Numerical modeling of sediment transport in alpine reservoirs. Dissertation of Doctor of Engineering Science, Graz University of Technology, Austria

  • Haun S, Kjaerås H, Løvfall S, Olsen NRB (2013) Three-dimensional measurement and numerical modeling of suspended sediments in a hydropower reservoir. J Hydrol 479:180–188

    Article  Google Scholar 

  • Hosseinjanzadeh H, Hosseini K, Kaveh K, Mousavi SF (2015) New proposed method for prediction of reservoir sedimentation distribution. Int J Sedim Res 30(3):235–240

    Article  Google Scholar 

  • Huang G (2011) Dual behavior of suspended sediment concentration in a regulated river. World J Mech 1:115–121

    Article  Google Scholar 

  • Issa IE, Al-Ansari N, Sherwany G, Knutsson S (2016) Evaluation and modification of some empirical and semi-empirical approaches for prediction of area-storage capacity curves in reservoirs of dams. Int J Sediment Res 32:127

    Article  Google Scholar 

  • Ji U, Jang EK, Kim G (2016) Numerical modeling of sedimentation control scenarios in the approach channel of the Nakdong river estuary barrage. South Korea. Int J Sediment Res 31:257

    Article  Google Scholar 

  • Jiménez JA, Madsen OS (2003) A simple formula to estimate settling velocity of natural sediments. J Waterw Port Coast Ocean Eng 129(2):70–78

    Article  Google Scholar 

  • Lauer JW, Viparelli E, Piegay H (2016) Morphodynamics and sediment tracers in 1-d (mast-1d): 1-d sediment transport that includes exchange with an off-channel sediment reservoir. Adv Water Resour 93:135

    Article  Google Scholar 

  • Laursen EM (1958) The total sediment load of streams. J Hydraulics Div 84(1):1–36

    Google Scholar 

  • Meyer-Peter E, Muller R (1948) Formulas for bed-load transport. IAHR

  • Miyahara S, Uda T, Furuike K, Serizawa M, San-nami T, Ishikawa T (2010) Effect of sand bypassing at Sakuma dam in the Tenryu River as a measure against erosion of the Tenryu River delta coast. In: Coastal engineering proceedings vol 1, no 32, pp 12

  • Molinas A, Yang CT (1986) Computer program user’s manual for GSTARS. US Bureau of Reclamation Engineering and Research Center, Denver, p 80225

    Google Scholar 

  • Morris Gregory L, Fan Jiahua (1998) Reservoir sedimentation handbook. McGraw-Hill Book Co., New York

    Google Scholar 

  • Okano M, Kikui M, Ishida H, Sumi T (2005) Study on reservoir sediment excavation management and sediment replenishment to downstream rivers. J Jpn Soc Dam Eng 15(3):200–215

    Google Scholar 

  • Palmieri A, Shah F, Annandale GW, Dinar A (2003) Reservoir conservation volume in the rescon approach economic and engineering evaluation of alternative strategies for managing sedimentation in storage reservoirs

  • Report-12 (1957) Some fundamentals of particle size analysis: A study of methods used in measurement and analysis of sediment loads in streams. Tech. rep., Inter-Agency Committee of Water Resources and St. Anthony Falls Hydraulic Laboratory, Minneapolis, Minnesota, USA

  • Rubey WW (1933) Settling velocity of gravel, sand, and silt particles. Am J Sci 148:325–338

    Article  Google Scholar 

  • Sato S, Liu H (2008) A comprehensive study on sediment movement in Tenryu River watershed and Enshu coast

  • Toffaleti FB (1968) A procedure for computation of the total river sand discharge and detailed distribution, bed to surface. Tech. rep., DTIC Document

  • Tsai CW, Hsu Y, Lai KC, Wu NK (2014) Application of gamblers ruin model to sediment transport problems. J Hydrol 510:197–207

    Article  Google Scholar 

  • Van Rijn LC (1993) Principles of sediment transport in rivers, estuaries and coastal seas, vol 1006. Aqua Publications, Amsterdam

    Google Scholar 

  • Wilcock PR, Crowe JC (2003) Surface-based transport model for mixed size sediment. J Hydraul Eng 129(2):120–128

    Article  Google Scholar 

  • Wong M, Parker G (2006) Reanalysis and correction of bed-load relation of Meyer-Peter and Muller using their own database. J Hydraul Eng 132(11):1159–1168

    Article  Google Scholar 

  • Yang CT (1973) Incipient motion and sediment transport. J Hydraul Div 99(10):1679–1704

    Google Scholar 

  • Yang CT (2006) Erosion and sedimentation manual. US Department of the Interior, Bureau of Reclamation, Denver

    Google Scholar 

  • Yin K, Xu S, Huang W (2016) Modeling sediment concentration and transport induced by storm surge in Hengmen Eastern Access Channel (HEAC). Nat Hazards 82:617–642

    Article  Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Prashanth Reddy Hanmaiahgari.

Rights and permissions

Reprints and Permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Hanmaiahgari, P.R., Gompa, N.R., Pal, D. et al. Numerical modeling of the Sakuma Dam reservoir sedimentation. Nat Hazards 91, 1075–1096 (2018). https://doi.org/10.1007/s11069-018-3168-4

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s11069-018-3168-4

Keywords