Experimental investigation of local half-cone scouring against dam

Similar documents
Local Scouring due to Flow Jet at Downstream of Rectangular Sharp-Crested Weirs

International Journal of Advance Research, IJOAR.org ISSN

Factors affecting confluence scour

Design of Stilling Basins using Artificial Roughness

Sediment Extraction and Flow Structure of Vortex Settling Basin

Flow Field Characteristics of In-ground Stilling Basin Downstream of Flood Mitigation Dams

Local scour proles downstream of adverse stilling basins

Study of the rate of sediment trapping and water loss in the vortex tube structure at different placement angles

Why do Golf Balls have Dimples on Their Surfaces?

Laboratory Investigation of Submerged Vane Shapes Effect on River Banks Protection

EXAMPLES (SEDIMENT TRANSPORT) AUTUMN 2018

5. TWO-DIMENSIONAL FLOW OF WATER THROUGH SOILS 5.1 INTRODUCTION

B-1. Attachment B-1. Evaluation of AdH Model Simplifications in Conowingo Reservoir Sediment Transport Modeling

Head Discharge Relationship of Thin Plated Rectangular Lab Fabricated Sharp Crested Weirs

Influence of geometry shape factor on trapping and flushing efficiencies

Experimental Investigation on Density Currents Propagating over Smooth and Rough Beds

FE Fluids Review March 23, 2012 Steve Burian (Civil & Environmental Engineering)

CVE 372 HYDROMECHANICS EXERCISE PROBLEMS

EFFECT OF BAFFLE BLOCKS ON THE PERFORMANCE OF RADIAL HYDRAULIC JUMP

VARIATION OF MANNING S ROUGHNESS COEFFICIENT WITH SEEPAGE IN SAND-BED CHANNEL *Satish Patel 1 and Bimlesh Kumar 2

State Water Survey Division SURFACE WATER SECTION

Zainab Mohamed Yusof*, Syura Fazreen Hamzah 1 & Shahabuddin Amerudin 2

Time dependent variation of river bed profile due to mining pit

A STUDY ON DEBRIS FLOW DEPOSITION BY THE ARRANGEMENT OF SABO DAM

EFFECT OF GRAIN DENSITY ON PLANE BED FRICTION. Václav Matoušek, Vojtěch Bareš, Jan Krupička, Tomáš Picek, Štěpán Zrostlík

Pressure Fluctuation around Chute Blocks of SAF Stilling Basins

Formation Of Hydraulic Jumps On Corrugated Beds

FORMATION OF HYDRAULIC JUMPS ON CORRUGATED BEDS

15. GRIT CHAMBER 15.1 Horizontal Velocity in Flow Though Grit Chamber

THE EFFECT OF THICKNESS OF PILLAR IN THE CHANNEL BEND TO CHANGES THE COEFFICIENT OF SUPERELEVATION

SCOPE OF PRESENTATION STREAM DYNAMICS, CHANNEL RESTORATION PLANS, & SEDIMENT TRANSPORT ANALYSES IN RELATION TO RESTORATION PLANS

PERFORMANCE OF A CENTRAL-TYPE JET PUMP II- EXPERIMENTAL STUDY ON WATER FLOW

MATHEMATICAL MODELING OF FLUVIAL SEDIMENT DELIVERY, NEKA RIVER, IRAN. S.E. Kermani H. Golmaee M.Z. Ahmadi

U.S. Army Corps of Engineers Detroit District. Sediment Trap Assessment Saginaw River, Michigan

Theoretical Design and Analysis of Gravity Assisted Heat Pipes

PET467E-Analysis of Well Pressure Tests 2008 Spring/İTÜ HW No. 5 Solutions

Erosion Rate is a Function of Erodibility and Excess Shear Stress = k ( o - c ) From Relation between Shear Stress and Erosion We Calculate c and

Sedimentation Scour Model Gengsheng Wei, James Brethour, Markus Grünzner and Jeff Burnham August 2014; Revised October 2014

Tarbela Dam in Pakistan. Case study of reservoir sedimentation

THE HYDRAULIC PERFORMANCE OF ORIENTED SPUR DIKE IMPLEMENTATION IN OPEN CHANNEL

Experimental study of hydraulic-sediment properties on deltaic sedimentation in reservoirs

Flow Field Investigation in a Rectangular Shallow Reservoir using UVP, LSPIV and numerical model

The method by which this error has to be combined with other sources of error is I

Stage Discharge Tabulation for Only Orifice Flow

Trial dredging by a new ejector-pump system for the reservoir sedimentation

53:071 Principles of Hydraulics Laboratory Experiment #3 ANALYSIS OF OPEN-CHANNEL FLOW TRANSITIONS USING THE SPECIFIC ENERGY DIAGRAM

International Journal of Scientific & Engineering Research, Volume 5, Issue 7, July-2014 ISSN

The Effect of Bedform-induced Spatial Acceleration on Turbulence and Sediment Transport

A Model Answer for. Problem Set #7

PRESSURE AND SCOURING AROUND A SPUR DIKE DURING THE SURGE PASS

Erosion of sand under high flow velocities

DESIGN OF A WEIR. The purpose of this exercise is to acquaint with the basic scope of a small weir calculation. It must cover the following topics:

Investigation on Dynamics of Sediment and Water Flow in a Sand Trap

EARTH PRESSURES AGAINST RIGID RETAINING WALLS IN THE MODE OF ROTATION ABOUT BASE BY APPLYING ZERO-EXTENSION LINE THEORY

Free Flow Below Skew Sluice Gate

Flow and Bed Topography in a 180 Curved Channel

R09. d water surface. Prove that the depth of pressure is equal to p +.

This is a refereed journal and all articles are professionally screened and reviewed

Module 15 : Grit Chamber. Lecture 19 : Grit Chamber

Growing and decaying processes and resistance of sand waves in the vicinity of the Tone River mouth

Experiment (4): Flow measurement

A STUDY ON DEBRIS FLOW OUTFLOW DISCHARGE AT A SERIES OF SABO DAMS

How to predict the sedimentological impacts of reservoir operations?

Quasi-three dimensional computations for flows and bed variations in curved channel with gently sloped outer bank

GEOMETRY EFFECT ON FLOW AND SEDIMENT DEPOSITION PATTERNS IN SHALLOW BASINS

Exergy Analysis of Solar Air Collector Having W Shaped Artificial Roughness

1.060 Engineering Mechanics II Spring Problem Set 4

Calculating the suspended sediment load of the Dez River

Strategies for managing sediment in dams. Iwona Conlan Consultant to IKMP, MRCS

NPTEL Quiz Hydraulics

Concept of an Integrated Workflow for Geothermal Exploration in Hot Sedimentary Aquifers

Accurate and Estimation Methods for Frequency Response Calculations of Hydroelectric Power Plant

LOGO Self-Cleansing of Storm Drain through Incipient Motion Design Concept and Flushing Gate

Morphological Changes of Reach Two of the Nile River

CALCULATION OF STEAM AND WATER RELATIVE PERMEABILITIES USING FIELD PRODUCTION DATA, WITH LABORATORY VERIFICATION

UNIT I FLUID PROPERTIES AND STATICS

Possibility of Reducing Sedimentation at Lateral Diversion

INFLUENCE OF THE SPUR DIKE PERMEABILITY ON FLOW AND SCOURING DURING A SURGE PASS

CASE STUDY SOLIS, SWITZERLAND

The Process of Scour Surrounding Objects Freely Settling on the Seabed on the Effect of Typhoon Based on DRAMBUIE Model

Characteristic Variables and Entrainment in 3-D Density Currents

Hydromechanics: Course Summary

USING AN ALL-SPEED ALGORITHM TO SIMULATE UNSTEADY FLOWS THROUGH MIXED HYDRO-PNEUMATIC SYSTEMS

New computation method for flood flows and bed variations in a low-lying river with complex river systems

UNCERTAINTY SCOPE OF THE FORCE CALIBRATION MACHINES. A. Sawla Physikalisch-Technische Bundesanstalt Bundesallee 100, D Braunschweig, Germany

Presented by: S. Ali Akbar Salehi Neyshabouri

SEDIMENT MANAGEMENT IN HYDROPOWER PLANTS AN OVERVIEW

Long-Term Effects Of River Bed Variations Downstream Of The Shihmen Reservoir Due To Climate Change

10.52 Mechanics of Fluids Spring 2006 Problem Set 3

A New Method for Calculating Oil-Water Relative Permeabilities with Consideration of Capillary Pressure

Conclusion Evaluating Methods for 3D CFD Models in Sediment Transport Computations

Hydraulics and hydrology

NUMERICAL SIMULATION OF EROSION PROCESSES ON CROSSBAR BLOCK RAMPS

EROSION RATE OF RESERVOIR DEPOSIT AS REVEALED BY LABORATORY EXPERIMENT

EFFECT OF VERTICAL CURVATURE OF FLOW AT WEIR CREST ON DISCHARGE COEFFICIENT

COMPARISON OF LABORATORY AND FIELD MEASUREMENTS OF BRIDGE PIER SCOUR

Fluid Dynamics Exercises and questions for the course

CIE4491 Lecture. Hydraulic design

FE Exam Fluids Review October 23, Important Concepts

Scour Analysis in High Vertical Drop Shallow Using Numerical and Physical Models M. Habibi 1, M.J khanjani 2 1 M.S, 2 PHD, Bahonar university - kerman

Transcription:

River Flo 2010 - Dittrich, Koll, Aberle & Geisenhainer (eds) - 2010 Bundesanstalt für Wasserbau ISBN 978--9920-00-7 Experimental investigation of local half-cone scouring against dam M. E. Meshkati Shahmirzadi & A. A. Dehghani Dept. of Water Engineering, Gorgan University of Agricultural Sciences and Natural Resources, Iran T. Sumi Water Resources Research Center, Disaster Prevention Research Institute, Kyoto University, Japan Gh. Naser School of Engineering, Faculty of Applied Sciences, University of British Columbia Okanagan, Canada A. Ahadpour M.Sc Student of Water construction Engineering, Shiraz University, Iran ABSTRACT: Several methods have been proposed to control sedimentation process. These may include catchment s management, flushing, sluicing, density current venting and dredging. Flushing is used to erode previously deposited sediments. In pressurized flushing, the sediment in the vicinity of the outlet openings is scoured and a funnel shaped crater is created. In this study, the effect of bottom outlets cross section on the dimensions of flushing cone as investigated experimentally. For this purpose, experiments as carried out ith three bottom outlet diameters, five discharges release for each desired depth of ater and three ater depths above the center of bottom outlets. The results indicate that the volume and dimensions of flushing cone are strongly affected by the bottom outlet diameter. Finally, by using regression analysis, a dimensionless equation as presented for calculating the volume of sediment released from dam and also its dimensions of half-cone scouring. Keyords: Pressure Fushing, Local Scouring, Bottom Outlet, Sediment, Reservoir 1 INTRODUCTION Sustaining the storage capacity of existing reservoirs has become an important issue rather than building ne reservoirs hich is difficult due to strict environmental regulations, high costs of construction, and lack of suitable dam site (Shen, 1996). Several methods have been proposed to control sedimentation process. These may include catchment s management, flushing, sluicing, density current venting and dredging. Flushing is used to erode previously deposited sediments (Brandt, 2000). One of the most effective techniques is flushing through hich the deposited sediment is hydraulically removed by the flo. The oldest knon method of flushing, practiced in Spain in the 16th century, as referred to by D Rohan (Bron, 194). The excess in shear force of accelerated flos created by sudden opening of the bottom outlets of dams loosens and re-suspends the sediment. The flo ill then ash them up from the system. If flushing takes place under a pressurized this flushing is called pressure flushing and has only local effects around the outlet. In pressurized flushing, the sediment in the vicinity of the outlet openings is scoured and a funnel shaped crater is created. Figure 1 illustrates the longitudinal vie of flushing cone in the vicinity of bottom. This is only an option in reservoirs ith small reservoir capacity to ater inflo, and large capacity of sluices (Qian, 1982). Pressurized flushing has been studied extensively in the literature (White, 1984- Shen and Lai, 199- Fang and Cao, 1996- Scheuerlein, 2004- Emamgholizadeh, 2005 and 2006). In spite of advances in the investigation of pressure flushing technique at reservoir storage, studies about the effect of bottom outlet diameter on flushing cone development are limited and more information about this phenomenon is needed. Water Level Sediments Reservoir Storage Flushing Cone Dam Wall Bottom Outlet Figure 1. Longitudinal and plan vie of flushing half-cone in the vicinity of bottom 1267

Estimation of sediment volume removed or volume of flushing cone is important for designing of bottom outlet gates, in hich the optimum and the best bottom outlet can be designed ith respect to the cross section. Researches for evaluation of geometric characteristics of scouring cone against various cross section of the bottom outlet are necessary, in order to proper design of the bottom outlet. Moreover, dimensions of flushing cone are also effective on rescue of poer plant intakes. This paper deals experimentally ith pressure flushing phenomena and investigation about the effect of bottom outlet cross section on volume and dimensions of flushing cone. The results are tabulated in terms of statistical measures and also illustrated in the scatter plots. 2 MATERIALS AND METHODS 2.1 Experimental arrangements The experiments ere conducted at hydraulic laboratory of Gorgan University of Agricultural Sciences and Natural Resources in Iran (Meshkati, 2010). Experiments tests carried out on hexahedral shallo basin hose overall dimensions consist of meter length, 2 meter ide and 1.5 meter height. Using to reticulate sheets at the reservoir s entrance, a smooth flo is created. The front all of model ill be easy to change to modify different cross sections of reservoir bottom outlets. The outlets of main reservoir include four different gate valves ith diameter of 2.54,.81, 5.08 and. The sediment deposits at the main reservoir as consists of silica particles ith uniform size distribution, ith a median diameter of d 50 =1 mm and geometric standard deviation of σ=1.25. Settling basin area.60 Flo dissipater area 1 m Adjacent to the reservoir, an underground tank as ell as a pump as used to prepare and recirculate the desired inflo ater discharge hich named ater supply system. Water supply system of model as also supported by an adjusting valve, a digital flo-meter, and an 11- meter flume upstream of model. Along the basin side alls, a movable frame as mounted to carry the measuring instruments. After each experiment, the scour cone configuration as measured by a digital point gage device. For the donstream section it as use another stilling basin hich the mixing flo of ater and sediment as collect in it and through a plastic pipe in a closed circuit ith the underground tank. The settling basin as a rectangular flume of.6 meter long, 1 meter ide, and 0.76 meter height. At the end of settling reservoir there as a V-notch eir (ith angle of 90 o ) to measure of outflo discharge. In Figure 2 a schematic plan vie of the experimental setup and the hydraulic circuits is given. T e notation of flushing halfcone under a discharge of 2 lit/s, ater depth of 6 cm and diameter of the outlet are illustrated in Figure. Figure. Local Half-cone scouring at the vicinity of bottom outlet Maine reservoir W max Scouring Flo direction Returning flo from the model toard ater supply L max Scouring Local Half-Cone Scouring Weir 1m Sediment 2 m Inlet Flo P Supply System Returning flo from 1m 1 m the model toard ater Deposited Flo supply sediment area dissipater area Figure 2. Schematic plan vie of the experimental setup and its hydraulic circuits 1268

(1) Dimensional Analysis The volume of flushing cone (V Scouring ) may be ritten as a function of the folloing variables: VScouring = φ( UOutlet, DOutlet, H, Hs, B, d50, ρs ρ, ρ, g, ν ) (1) here, U Outlet= velocity of flo at the entrance of bottom outlet, D outlet = the cross section of bottom outlet, H = the height of ater above the center of bottom outlet, H s = the height of sediment deposited above the center of outlet, B= the idth of reservoir, d 50 = the median size of sediment particles, ρ s = the density of sediment, ρ = ater density, g= the acceleration due to gravity and ν = the kinematics viscosity. By using Buckingham theorem, and choosing the ρ, H, and U Outlet as repeating variables, folloing functional relationship describes dimensionless flushing volume: V U H D (,, ) H Scouring Outlet s = ϕ H g( Gs 1) d H 50 Where G s = ρ s /ρ, also using the same procedure, the idth of flushing cone (W Scouring ) can be expressed as: WScouring UOutlet Hs D = ϕ(,, ) H g G H H ( 1) d 50 s 2.2 Experiment Designing As mentioned above, for considering the effect of bottom outlet cross section on dimensions of flushing cone, the experiments ere conducted ith three different outlet diameters (1, 2 and Inch), three ater depth above the center of bottom outlet i.e. 6, 66, 96 cm and at least four different discharges for each ater depth. Table 1 and 2 respectively shos the range of variables conducted for measured experimental data and dimensionless parameters uses in dimensional analysis. Table 1. Range of variables in this research Parameters Variations Discharge release (Q Outlet ) -15 Lit sec - 1 Depth of ater (H ) 6, 66, 96 cm Outlet diameter (D Outlet ) 2.54,.81, 5.08 and d50 1mm (2) () Table 2. Range of dimensionless parameters Parameters Variations V Scouring /H 0.00046-0.72 Fr* 0.16-2.2 H s /H 0.166-44 D Outlet /H 0.026-1 2. Experimental investigation For running the experiments, the deposited sediment ere flattened and leveled firstly to a specific level above the center of bottom outlet (16 cm), and the model as sloly filled ith ater until the ater surface elevation reached to a desired level. Then, the bottom outlet as manually opened until the outflo discharge, become equal to the inflo discharge. Consequently, the sediment as released from main reservoir. At the beginning of the experiment hen the donstream outlet opened, sediment as discharged ith high concentration, but the concentration of sediment flushing decrease ith time. Experiments ere continued until the flushing cone reached to an equilibrium (no further particle motion ill be observe) condition in hich the sediment concentration as negligible at the end of the experiment. The time required for the formation of the flushing cone depends on hydraulic conditions. The development of flushing cone as very fast, and the process finished in less than one minute to ten minutes in the experimental model. In this study, the time for running the experiment as set to 45 minute. At the end of each experiment, the flushing outlet as closed in hich the incoming discharge as set to zero then ater as carefully and sloly drained from the main reservoir. After the run of each experiment, the bed level of scouring as measured using digital point gages, and the volume of flushing cone as calculated by Surfer8.0) softare. RESULTS AND DISCUSION As mentioned before, a half-funnel shape of scouring is created at the vicinity of outlet gates in the pressure flushing operation. The maximum scour depth of this cone is found very close to the dam all. Surface development of scouring cone is same in both idth and length, but the plan shape of the flushing cone over the deposited sediment is close to half a circumference. The cone slopes of both longitudinal and side are approximately equal, 1269

and also these are similar to the angle of sediment submerged repose. Figure 4 to 8 shos the variation of flushing cone dimensions (idth and volume) versus the outflo discharge of bottom outlet for four bottom outlets hich it as used in this research. These figures sho, for constant ater depth in the model, ith increasing outflo discharge the dimensions of flushing cone increase, and as could be found, approximately there is same trend beteen all of outlets. Also, for constant outflo discharge, loer ater depth in reservoir causes bigger scouring dimensions, as it could be seen in Fig 4 to 8. Therefore, for more sediment removal and for having greater dimensions of flushing cone, pressure flushing operation must perform under both possible loest level of ater and must be use in full open outlets condition. This is clear that by decreasing ater surface elevation under constant discharge, vertical gradient of velocity and bed shear stress increase hich lead to an increase in sediment carrying capacity in the reservoir. Also for constant ater depth, ith increasing the outflo discharge, ater velocity and bed shear stress increases and consequently greater amount of sediment releases from dam. These results are in agreement ith previous research completely. As can be understood from figures 9 to14, there is direct relation beteen cross section of bottom outlet and dimensions of flushing cone. In other ord, for constant outflo discharge and constant ater depth, ith increasing the diameter (cross section) of bottom outlet, dimensions of flushing cone increases. 0. 0 0.8 1.2 1.6 Outflo Discharge(L/s) H =6 cm H =66 cm H =96 cm Figure 4. The variation of flushing cone idth versus outflo discharge, for different ater depth and the bottom outlet ith diameter. Volume of Flushing Cone(ccm) 6500 5500 4500 500 0. 0 0.8 1.2 1.6 Outflo Discharge(L/s) H =6 cm H =66 cm H =96 cm Figure 5. The variation of flushing cone volume versus outflo discharge, for different ater depth and the bottom outlet ith diameter. 0.5 Width of Flushing Cone(m) Volume of Flushing Cone(ccm) 9500 8500 7500 6500 5500 4500 500 0 0.6 1.2 1.8 2.4.6 Outflo Discharge(L/s) H =6 cm H =66 cm H =96 cm Figure 6. The variation of flushing cone idth versus outflo discharge, for different ater depth and the bottom outlet ith.81 cm diameter. 0 0.6 1.2 1.8 2.4.6 Outflo Discharge(L/s) H =6 cm H =66 cm H =96 cm Figure 8. The variation of flushing cone volume versus outflo discharge, for different ater depth and the bottom outlet ith.81 cm diameter. 1270

0.6 8 4.81 cm Outflo Discharge(L/s) Figure 9. The variation of flushing cone idth versus outflo discharge, for different outlets cross sections and 6 cm ater depth. Volume of Flushing Cone (m) 19000 15000 11000 7000 000 Outflo Discharge(L/s).81 cm Figure 10. The variation of flushing cone volume versus outflo discharge, for different outlets cross sections and 6 cm ater depth. 0.5 0. Outflo Discharge(L/s).81 cm Figure 11. The variation of flushing cone idth versus outflo discharge, for different outlets cross sections and 66 cm ater depth. Volume of Flushing Cone (m) 19000 15000 11000 7000 000 Outflo Discharge(L/s).81 cm Figure 12. The variation of flushing cone volume versus outflo discharge, for different outlets cross sections and 66 cm ater depth 19000 0.5 0..81 cm Outflo Discharge(L/s) Volume of Flushing Cone (m) 15000 11000 7000 000.81 cm Outflo Discharge(L/s) Figure 1. The variation of flushing cone idth versus outflo discharge, for different outlets cross sections and 96 cm ater depth. Figure 14. The variation of flushing cone volume versus outflo discharge, for different outlets cross sections and 96 cm ater depth. The comparison of the prediction accuracy using multiple linear regression analysis on training data set and testing data set, by using the 1271

statistical parameters such as root mean square error (RMSE) and R-squared value ere calculated(table ). Table. Statistical verification for presented equations Perfor mance index V Scouring W Scouring Training Testing Training Testing R 2 0.997 0.997 0.997 0.999 MAE 0.002 0.007 7.9E-05 6.2E-05 RMSE 1.6E-05 5.E-05 9.E-09 8.E-09 A close fit as obtained during the training, testing and especially in validation, and the results sho that the errors in predicting the flushing cone volume and flushing cone idth are much lo. 4 CONCOLUSION This study shos that A Outlet is the main parameters in correlating the flushing cone dimensions. The results indicate that ith increase of diameter of bottom outlet, the ne hydraulically condition established on flushing mechanism. And this mechanism is common beteen all of scouring dimensions. The results indicate that ith increasing the diameter (cross section) of bottom outlet, dimensions of flushing cone increases, and the ne hydraulically condition established on flushing mechanism. And this mechanism is common beteen all of scouring dimensions. So that, for bigger bottom outlet, there is greater diameter influence and they can make stronger orifice flo, consequently they can erode the sediment particle form farther distance from outlet. Based upon experimental data, under clear ater flo, dimensionless equations for prediction of flushing cone characteristics are presented. The present equations have high correlation coefficient and in spite of their correlation there applicability should be tested using other experimental and field data. Further experiments are necessary by using different size, shape and graduation of bed material, under different hydraulic conditions to conform the results obtained from this study. The bigger bottom outlets have greater diameter influence, so they can make stronger orifice flo, consequently they can erode the sediment particle form farther distance from outlet. In addition to, in the bigger outlets there is more space on dam all for releasing, also outflo streamlines or on the other means sediments have feer compress to each other and as result, less friction force make against erosion force during flushing operation. The multiple linear regression ere developed using the non-dimensional of experimental data, according to the dimensional analysis and functional relationship given by equations 2 and, folloing equations are obtained for volume and idth of flushing cone, respectively: VScouring UOutlet 1 Hs 2.2 D 0.89 = 4.6( ) ( ) ( ) (4) H g( Gs 1) d H 50 H WScouring UOutlet 0.1 Hs 0.75 D = 0.02( ) ( ) ( ) (5) H g( Gs 1) d H 50 H The experimental data related to this research consisting of 65 data series are divided into to parts randomly: a training set consisting 50 series and a testing set consisting of 15 data series, for assess the performance of proposed regression model. Figure 15 depict the results ith the performance indices beteen estimated and observed experimental data for the testing data sets. Calculated V Scouring /H 0.5 0. 0.1 Figure 15. Plot of observed and estimate of dimensionless flushing cone volume for testing data set using regressive model. REFRENCES R 2 = 0.997 MAE=0.007 RMSE= 5.027E-05 0 0 0.1 0. 0.5 Experimental data of V Scouring /H Brandt, S. A., A revie of reservoir desolation, International Journal of Sediment Research. Vol. 15, No. 2. pp. 21-42, 2000. Bron, C.B., The Control of Reservoir Silting, United States Department of Agriculture, Miscellaneous Publication No. 521, Washington, D.C. p. 166, 194. Emamgholizadeh, S., Bina, M., Fathimoghadam, M. and Ghomeyshi, M., Investigation and Evaluation of the Pressure Flushing through Storage Reservoir, ARPN Journal of Engineering and Applied Sciences. Vol. 1, No. 4, 2006. 1272

Fang, D. and Cao, S., An experimental study on scour funnel in front of a sediment flushing outlet of a reservoir, Proceedings of the 6th Federal Interagency Sedimentation Conference, Las Vegas, March 10-14 1996, pp. I.78-I.84, 1996. Meshkati Shahmirzadi, M. E, Experimental investigation of pressure flushing operation in reservoir storage, M Sc thesis, Gorgan University of Agriculture Sciences and Natural Resources, Iran, 2010. Qian, N., Reservoir sedimentation and slope stability; technical and environmental effects, Fourteenth International Congress on Large Dams, Transactions, Rio de Janeiro, Brazil, -7 May, Vol. III. pp. 69-690, 1982. Scheuerlein, H., Tritthart, M. and Nunez Gonzalez, F., Numerical and physical modeling concerning the removal of sediment deposits from reservoirs, Conference proceeding of Hydraulic of Dams and River Structures, Tehran, Iran, 2004. Shen, H.W., Lai, J.S. and Zhao, D., Hydraulic desiltation for noncohesive sediment, Proceeding of the 199 Annual ASCE Hydraulic Engineering Conference, San Francisco, H.W Shen, S.T. Su, and F. Wen, eds, pp. 119-124, 199. Shen, H.W. and Lai, J. S., Sustain reservoir useful life by flushing sediment, International Journal of Sediment Research. Vol. 11(): 10-17, 1996. White, W.R. and Bettess, R., The feasibility of flushing sediments through reservoirs, Challenges in African Hydrology and Water Resources, Proceeding of Harare Symposium, July, D.E. Walling, S.S.D. Foster, P. Wurzel, eds, IAHS Publication No, 1984. 127