American Journal of Civil Engineering
Volume 4, Issue 6, November 2016, Pages: 290-297

Prediction of Sediment Deposition in Reservoir Using Analytical Method

Rajendra Patil*, Rajeev Shetkar

Civil Engineering Department, Government College of Engineering, Aurangabad, India

Email address:

(R. Patil)

*Corresponding author

To cite this article:

Rajendra Patil, Rajeev Shetkar. Prediction of Sediment Deposition in Reservoir Using Analytical Method. American Journal of Civil Engineering. Vol. 4, No. 6, 2016, pp. 290-297. doi: 10.11648/j.ajce.20160406.14

Received: August 23, 2016; Accepted: August 31, 2016; Published: September 18, 2016


Abstract: Sediment particles, a product of erosion in the catchment are transported along the river with flowing water. The construction of Weir, barrage or a dam causes obstruction to the flow resulting in reduction of velocity. The reduced velocity causes sedimentation resulting in reduction of storage capacity which affects the overall life of the reservoir. The sediment deposition in the reservoir is a continuous and complex process which affects the useful life of a reservoir. The quantification of sediment deposition in a reservoir is necessary for effective reservoir and river basin management. The present study has been carried out to assess sediment deposition in Koyna Reservoir which is located in the Western Maharashtra, India. In India most of the rainfall is caused due to the southwest monsoon during the period from June to September, massive convective thunderstorms dominate the weather. In the present study analytical methods are used for estimation of sediment deposited in the Koyna reservoir. For the prediction annual inflow data is used. The storage capacity of Koyna reservoir is calculated considering the loss of storage due to sediment deposition for a period from 1961 to 2375. The results obtained indicated a loss of reservoir capacity by the year 2004, as 267.25 Mm3 (9.55%). The physical measurement indicated that the Koyna reservoir had lost 293.09 Mm3 (10.48%) of its capacity by the year 2004. The results obtained by analytical method have 8.82% error compared with the actual measurements.

Keywords: Reservoir, Inflow, Sedimentation, Capacity, Deposition


1. Introduction

India experiences very high unpredictability in the amount and the pattern of rainfall in various regions of the country. To cope up with such diverse situation, varieties of small and big projects are developed in India. Very few potential sites are to be considered as good sites for the major projects considering all constraints. The available storage capacity of existing reservoirs is to be utilized and evaluated very carefully as good storage sites being limited. The sediment deposition pattern basically affects the storage capacity of the catchment area. Conventional techniques, such as hydrographic surveys and the inflow-outflow methods being used for quantification of sediment deposition in a reservoir are expensive and time consuming. The effect of soil attrition from the catchment, sediment transport and catching efficiency of the reservoir affects the fertility of land. Considering the above issues, development of simple and cost effective method for quantification of sediment deposition in a reservoir is the need of time.

The reservoirs capacity is getting decaying due to filling up of sediments year after years. With yearly reduction in capacity by approximately 1%, the overall water storage capacity will become nearly half over a period of about 50 years. The reservoirs especially built for irrigation, water supply and power generation will hamper economics in a great extent and has environmental concerns. In this situation, reduction in the rate of sedimentation or cleaning the reservoirs becomes out most important. Many studies on reservoir sedimentation are going on since 1950s but the prediction phenomenon seems complex due to processes involved. The variables involved in sedimentation process need to be collected are not so reliable affecting the useful life [1]. The estimation of sedimentation depends on variable parameters such as sediments and inflow rates of water, which seems to be time dependent [2]. Prediction of forthcoming discharges of water and the sediments in river studies are found to be less reliable [3]. The empirical approaches can be used to generate future data if ample records of these parameters are available. Many times it is observed that the rate of sedimentation found in some of the Indian reservoirs is too high than the planned. The reservoirs are found to be losing its capacity annually by 0.2–1.0% [4] due to constant impingement of the live storage by sediments [5]. Studies on assessment of sedimentation in Bhakra Reservoir across Satluj River by a remote sensing approach indicated average sedimentation rate of 25.23 Mm3/year for a period of 32 years. Whereas by using hydrographic survey data showed 20.84 Mm3/year for the same period, which indicates that the remote sensing based approach provides results matching very closely with the hydrographic surveys [6]. The rating curves prepared from measurement data of suspended sediment and water discharge has shown 0.17% per year loss of storage capacity of reservoir in monthly and annual sediment inflow predictions of the reservoir [7] in India. The satellite studies on sedimentation rate by analyzing the images using the software noted 229 m3/km2 of catchment area per year [8].

The Indian rivers found to carry approximately 0.16 t/km2/year sediments along with flow of water, of which approximately 10% is found to be deposited in reservoirs and 29% is carried away into the sea [9]. Reservoir sedimentation affects water storage capacity and its availability during scarcity period. The analysis of 43 sedimentations surveys of major, medium and minor reservoirs in India indicates that, the sedimentation rate varies between 0.34 – 27.85 ha m/100 km2 / year for major reservoirs, 0.15 – 10.65 for medium reservoirs and 1.0 – 2.3 ha m/ 100 km2 / year for minor reservoirs [10].

The sediment coming from catchment results in to loss of capacity of reservoir, there is direct relation between runoff and sediment yield. For a sustainable development through water resources planning and management, timely and accurate estimation of runoff and sediment yield are essential. On arrival of sediment-laden water in to the reservoir, the coarser particles settle first in the upper reaches of the reservoir due to heavy weight, subsequently, the finer sediments also get deposited. Sediment deposition into reservoirs that are built for power generation are adversely affected due to loss of storage, damage to equipment, bank erosion, etc. All the major rivers of Central Asia are turbid watercourses affected by high sedimentation rates. It is of importance to quantify available water resources in reservoirs to ensure assured water supply to the stake holders. Geographic factors such as surface slope, soil texture, land use, climatic factors like rainfall, temperature, runoff etc., influence the soil erosion and sediment yield process. Rainfall, runoff and consequent soil erosion are temporally and spatially distributed processes. A better estimation of runoff and sediment yield is feasible by considering the watershed as small unit and applying the hydrologic model. Even though good results are obtained, it is a laborious and time consuming approach.

Assessment of reservoir sedimentation is part of the basic information needed for the operation and management of any reservoir. The knowledge of sedimentation process will help in ensuring remedial measures to be taken in advance so that the reservoir operation can be planned for optimum utilization. For this, capacity survey of a reservoir is conducted periodically using conventional equipment. The two most common conventional techniques for quantifying sedimentation in a reservoir are direct measurement of sediment deposition by hydrographic surveys, and indirect measurement using the inflow-outflow records of a reservoir. Both these methods are cumbersome, time consuming and expensive. Remote sensing techniques, offering data acquisition over a long time period and for a broad spectral range, are considered superior to the conventional methods for data acquisition. Spatial, spectral and temporal attributes of remote sensing data provide valuable and timely information regarding changes in the water-spread area after sedimentation and sediment distribution patterns in the reservoir [11].

2. Methods of Runoff and Sediment Yield

Hydrological models used for runoff and sediment yield estimation may be classified as empirical, conceptual and distributed models. Empirical models are developed by building a relationship between two or more hydrologic parameters with the long observed field data. The conceptual models are based on physics of the problem that consider some of the predominant processes on a watershed [12]. But the distributed models are based on incorporating the spatial and temporal variability of physiographic and climatic factors.

2.1. Modeling Methods

Estimates of runoff and sediment yield are essential for the solution of a number of problems of a watershed. The modeling of rainfall-runoff and soil erosion /sediment yield from watersheds has received considerable attention. The models are expected to assist in assessment of water yield, extent of soil and nutrient losses and sediment transport, Land use planning, soil conservation measures and understanding of runoff and erosion processes and their interactions. The hydrologic modeling efforts have moved from traditional empirical lumped models to distributed models. Attempts have been made to adopt computationally intensive and nonlinear but efficient techniques such as Neural Networks for rainfall- runoff and soil erosion modeling. Most of these models have adopted Neural Networks for temporal modeling of run off.

2.2. Conventional Hydrological Models

All models (conventional and modern) under real conditions are more or less incorrect [13,14], because of the abstractions and simplifications of the original complex and nonlinear hydrologic processes [15]. It is very difficult to measure all the model parameters precisely, they are always data based. About 28 hydrologic models, were evaluated by ASCE Task Committee, for adopting them in absence of data for un-gauged basins [16]. The hydrologic modeling took off from traditional empirical models to conceptual lumped models and to the present day distributed models. The availability of high speed and large memory computing systems have made the computationally intensive and nonlinear techniques such as neural networks most applicable to hydrologic modeling.

2.3. Runoff Modeling

In any hydrologic analysis, rainfall-runoff relationship plays the key role. To determine the amount of runoff, besides observations made in the field, computer models and simulations can also be used. These are useful for extrapolating the observed runoff records. Depending on the purpose, data availability, type of runoff result desired, the estimation is done by any of the methods, such as, linear and multiple linear regression models, unit hydrograph method, rational method and hydrological models. Linear and multiple linear regression models relate rainfall and runoff, using a statistical relation fitting a linear regression. Runoff estimation in India has also been carried out traditionally by using Barlow's tables, Strange's tables and Inglis formula. Empirical Models are developed using observed rainfall and runoff data and correlating with other basin parameters which influence the runoff transformation process. Some of them are rational formula, Cook's table, SCS model, Dicken's formula, Ryves formula, Inglis formula, Craig's formula, Time of concentration, etc. Rational Method is based on the catchment area, rainfall intensity and a runoff coefficient that depends on the land use [17,18]. Cook's Method is a relationship between rainfall factor of a basin, return period of peak runoff and rainfall [17].

2.4. Sediment Yield Modeling

Some of the efforts made to develop methods to estimate soil erosion that total soil loss is related to the degree and length of slope [19]. A soil loss equation was developed based on factors such as soil erodibility, land cover, degree and length of slope and 30-minute maximum rainfall with a frequency of 2 years [20]. Sediment Yield Prediction Equation was developed for soil erosion assessment including terrain factors such as topography, soils, rainfall, and the climatic factors [21]. This equation was modified into a multiple linear regression form. Another regression based sediment yield model was developed using data from 50 catchments in India that includes the physiographic factors such as slope, drainage density, soils, land use and climatic factor i.e. rainfall [6]. Assessment of sediment yield is carried out using the model developed by Garde and Kothyari for varying land [22].

3. Present Study

In the present study, analytical method proposed by Garde et al [23] is used to calculate the volume of sediment deposited (Vac) in the Koyna reservoir for the available annual inflow data, available for a period from 1961 to 2013 and also for future. The available annual inflows are used to generate the flows for the subsequent years using Brittan’s method by means of Markov-Chain model as given by VenTe Chow [18].

3.1. Objective of the Study

In view of the above, the specific objectives of the present study are,

a)  To predict the volume of sediment deposition in Koyna reservoir using analytical method.

b)  To compute the capacity of reservoir by analytical method.

3.2. Study Area

The area selected for the present study model application is the Koyna watershed, situated on the west coast of Maharashtra, India, lies between the latitude of 17000’-17059’ N and longitude of 73002’–73035’ E. The location of the study area along with nine rain-gauge stations in the Koyna watershed is shown in figure 1 [24]. The Koyna project is a multi- purpose project, initially designed as a hydro- electric project with an installed capacity of 1920 MW. The Koyna watershed has an elongated leaf shape. The total catchment area of the Koyna reservoir is 891.8 sq. km. The catchment is approximately 64 km. in length and 12 to 14 km. in width. The catchment is bounded by hills. The water spread area is 115.36 sq.km. The catchment is broadly classified as 41% forest area, 49% cultivated area, 6% waste land, 4% others. The total capacity of the reservoir is 2797.5 Mm3, out of which live storage is 2677.7 Mm3 and dead storage is 119.8 Mm3.

Figure 1. Study area, Koyna watershed.

4. Methodology

The Empirical or analytical methods are used for calculating the sediment deposition in the reservoir. One of the methods which is proposed by Garde et al [23] is used in this study to estimate the sediment deposition in the Koyna reservoir. This method is more practical and it is extremely useful technique since it represents a procedure relying on the integration of complex erosion, sediment transport and deposition process in reservoirs [22]. This method makes use of the data which is generally available for any reservoir. The data used is the annual inflows to the reservoir, initial capacity of reservoir, average initial bed slope, width of reservoir at full reservoir level. Using these details the inflow in to the Koyna reservoir and sediment deposition due to this inflow is calculated.

4.1. Inflow Generation

The available annual inflow (1961-2013) is used to generate the flows for subsequent years using Brittan’s method by means of Markov-chain Model [18].

(1)

 Generated water inflow in (t+1)th year

 = Annual water inflow in tth year

 = Mean annual inflow of historic data

R = First order serial correlation coefficient. of historic inflow data

 = Standard deviation of historic inflow data.

Z = Random normal deviate having zero mean and unit standard deviation.

First order serial correlation co-efficient (R), standard deviation () and random normal deviate are calculated for inflow generation.

a) First order serial co-efficient R is given by

b) Standard deviation of historic inflow data (σ)

where,

Xi = Historic annual inflow in ith year

Xi+1 = Historic annual inflow in (i + 1)thyear

N = Number of years

c) Random normal deviate (Z)

It is found out by the Box Muller method using rectangular distributed random numbers using the equations.

where, U1 and U2 are the uniformly distributed random numbers in the range (0, 1).

4.2. Volume of Sediment Deposited

The cumulative volume of sediment deposited is calculated from the cumulative volume of water inflow into the reservoir which is used for the generation of future rate of sedimentation [22].

(2)

Where,

Vs = Volume of sediment in Mm3

Vac = Cumulative volume of sediment in M3/m width of reservoir in t years

Vw = Cumulative volume of water inflow in M3/m width in t years

S0 = Average initial longitudinal bed slope along the deepest course of reservoir

Qc = Cumulative annual volume of water inflow in Mm3

B = Average width of reservoir at full reservoir level in m

5. Results and Discussion

The inflow prediction is generated based on the historical flow data and Generated inflows are used to estimate the future sediment deposition in Koyna reservoir.

5.1. Inflow Generation

The available annual inflows are used to generate the flows for subsequent years using Brittan’s method based on the Markov-Chain Model [18], given by equation (1).

 = Mean annual inflow of historic data= 3983.02Mm3

N = Number of historical data available= 53

R = First order serial correlation co-efficient of historic inflow data = 0.1520

 = Standard deviation of historic inflow data = 982.8414

The above values are taken as input to generate the inflow for Koyna reservoir and inflow was generated from 2014 to 2375 (362 years) and the generated inflow is as given table 1 and represented in Figure 2.

5.2. Sediment Deposition

The volume of sediment deposit in the reservoir was calculated by using the equation (2).

B = Average width of reservoir at F.R.L = 2097 m.

S0 =Average initial longitudinal bed slope along the deepest course of reservoir = 1 in 705.94.

The future sediment deposition in reservoir is shown in table 2 and represented in Figure 3.

5.3. Discussion

Using Equation (1), the predicted inflow into the reservoir is generated. Flow is generated for the period from 2014 to 2375; i.e. for 362 years, which is as shown in Table 2. The predicted volume of sediment deposit in the Koyna reservoir is also calculated using the equation (2) and capacity of the reservoir is also calculated, is given in the Figure 3. Volume of sediment deposition was calculated up to the year 2375, as this is the year, when reservoir will lose 75% of its capacity. It is to be noted that any reservoir that loses its intended capacity to 75% of original capacity it becomes non-feasible [25]. The percentage loss in reservoir capacity is shown in Figure 4.

6. Conclusions

The capacity of Koyna reservoir is calculated based on the sediment deposition in the reservoir from 1961 to 2375 by analytical method. According to this method, in the year 2004, the loss in capacity of reservoir was 267.25 Mcum (9.55%). But Koyna reservoir has lost 293.09 Mcum (10.48%) of its capacity in the year 2004 [26]. From this result, one can say that analytical method suggested [23] gives better results.

Table 1. Generated inflow.

Year Generated inflow Mm3 Year Generated inflow Mm3 Year Generated inflow Mm3
2015 3918.09 2140 5436.63 2265 6894.04
2020 3816.53 2145 3094.97 2270 3115.86
2025 3148.29 2150 3119.54 2275 4049.08
2030 4724.06 2155 3600.80 2280 2289.14
2035 4101.79 2160 5040.12 2285 3284.95
2040 2035.25 2165 3345.07 2290 3716.92
2045 5726.20 2170 2729.44 2295 3372.66
2050 2688.24 2175 5409.03 2300 4807.98
2055 5880.27 2180 3435.43 2305 3435.55
2060 2900.40 2185 3889.20 2310 3294.99
2065 4660.56 2190 3667.64 2315 4123.17
2070 3278.42 2195 3339.98 2320 1273.14
2075 3878.84 2200 4435.69 2325 4250.99
2080 3751.97 2205 1991.52 2330 2314.41
2085 3088.23 2210 1631.91 2335 5502.83
2090 4122.68 2215 4135.86 2340 3674.20
2095 3327.52 2220 3222.34 2345 3433.19
2100 2163.67 2225 3356.96 2350 3606.26
2105 5069.02 2230 3538.77 2355 3059.00
2110 4759.12 2235 4106.59 2360 4863.67
2115 3419.55 2240 3288.95 2365 3380.79
2120 4193.18 2245 3033.59 2370 1681.17
2125 2716.15 2250 4862.34 2375 4040.18
2130 4271.71 2255 4376.23
2135 3361.24 2260 3534.77

Figure 2. Yearly generated inflow.

Figure 3. Sediment deposition and reservoir capacity.

Figure 4. Percentage capacity loss.

Table 2. Volume of sediment deposition.

Year Volume of sediment accum. Mm3 Capacity of Reservoir Mm3 % Loss in Reservoir Capacity Year Volume of sediment accum. Mm3 Capacity of Reservoir Mm3 % Loss in Reservoir Capacity
1961 10.36 2787.14 0.37 2001 252.62 2544.88 9.03
1962 16.96 2780.54 0.61 2002 257.04 2540.46 9.19
1963 24.30 2773.20 0.87 2003 261.25 2536.25 9.34
1964 32.06 2765.44 1.15 2004 267.25 2530.25 9.55
1965 39.09 2758.41 1.40 2005 276.75 2520.75 9.89
1966 44.54 2752.96 1.59 2006 286.50 2511.00 10.24
1967 53.32 2744.18 1.91 2007 293.91 2503.59 10.51
1968 57.67 2739.83 2.06 2008 299.58 2497.92 10.71
1969 64.81 2732.69 2.32 2009 303.98 2493.52 10.87
1970 71.77 2725.73 2.57 2010 308.73 2488.77 11.04
1971 78.11 2719.39 2.79 2011 315.81 2481.69 11.29
1972 82.17 2715.33 2.94 2012 321.10 2476.40 11.48
1973 89.00 2708.50 3.18 2013 327.96 2469.54 11.72
1974 94.08 2703.42 3.36 2014 331.38 2466.12 11.85
1975 101.06 2696.44 3.61 2015 337.09 2460.41 12.05
1976 108.28 2689.22 3.87 2035 429.99 2367.51 15.37
1977 114.84 2682.66 4.11 2055 548.35 2249.15 19.60
1978 122.36 2675.14 4.37 2075 640.64 2156.86 22.90
1979 128.09 2669.41 4.58 2095 727.26 2070.24 26.00
1980 135.20 2662.30 4.83 2115 817.27 1980.23 29.21
1981 141.24 2656.26 5.05 2135 920.95 1876.55 32.92
1982 146.72 2650.78 5.24 2155 1026.31 1771.19 36.69
1983 152.89 2644.61 5.47 2175 1132.13 1665.37 40.47
1984 158.53 2638.97 5.67 2195 1243.31 1554.19 44.44
1985 163.48 2634.02 5.84 2215 1343.00 1454.50 48.01
1986 168.31 2629.19 6.02 2235 1444.72 1352.78 51.64
1987 172.24 2625.26 6.16 2255 1539.51 1257.99 55.03
1988 178.07 2619.43 6.37 2275 1641.97 1155.53 58.69
1989 182.33 2615.17 6.52 2295 1734.56 1062.94 62.00
1990 190.22 2607.28 6.80 2315 1833.29 964.21 65.53
1991 196.78 2600.72 7.03 2335 1923.00 874.50 68.74
1992 201.95 2595.55 7.22 2355 2014.71 782.79 72.02
1993 208.44 2589.06 7.45 2375 2100.72 696.78 75.09
1994 217.99 2579.51 7.79        
1995 222.05 2575.45 7.94        
1996 226.83 2570.67 8.11        
1997 234.01 2563.49 8.36        
1998 238.99 2558.51 8.54        
1999 244.90 2552.60 8.75        
2000 248.79 2548.71 8.89        

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