This paper proposes to optimise the operation of the A Vuong reservoir using the dynamic programming technique. The A Vuong is a large reservoir in Vietnam serving multiple purposes, including power generation, flood control, and downstream water supply. First, different flood control storage capacities (Vpl) are investigated, and the best one is chosen based on the criteria of power output and the reservoir's ability to fill up after each regulation cycle. That option is for Vpl to be 50, 30, and 10% of the active storage capacity in September, October, and November, respectively. The study also proposes new operating rule curves with various scenarios of different beginning water levels, ranging from 368 m to 380 m. The average lines of the operating rule curves are also suggested for easier and more efficient operation. Recommendations for using this operating rule curve, as well as its advantages compared to the current one, are also discussed. The results show that the proposed operating rule curves provide much better performance compared with the current in terms of increasing the power output, with a 3.1% increase, while also protecting other water uses.

  • The flood control storage capacity was proposed to ensure the objectives of flood control, power output, and water supply.

  • New operating rule curves with various beginning water levels.

  • The optimal operation rule curves can boost power output by 3.5% and 3.1% for the dry season and the whole year, respectively.

Graphical Abstract

Graphical Abstract

Water reservoirs are one of the most important components of the water resource system. Their main purpose is to control natural flow by storing excess water during the rainy season and releasing it during the dry season for different purposes (Jain 2019). Reservoirs serve as important sources of many water supply systems around the world and have become increasingly vital as water pollution problems worsen (Panagopoulos 2022a, 2022b; Panagopoulos & Giannika 2022). In addition, reservoirs are also used to generate electricity and prevent floods. Conflicts between flood control and other water uses are common when operating a multi-purpose reservoir. These operating goals of one reservoir will be achieved if it has a reasonable operating strategy. At the end of its regulation cycle, one reservoir's water level needs to reach the normal level for power generation, water supply, and irrigation. If flows are plentiful, there should be no problem in achieving reservoir operational goals. On the other hand, if river flow is limited, the reservoir's volume will be difficult to fill, leading to an insufficient water supply.

Flood limited water level (FLWL), or the empty space for flood control, is an important factor that greatly affects water allocation for flood prevention and other purposes. In order to maintain flood control during the flood season, reservoir water levels are generally not permitted to exceed the FLWL. In the past, many authors have studied this matter (Wu & Ping 2018; Xie et al. 2018; Li et al. 2022). The effects of reservoir operation on flood inundation in the Vu Gia Thu Bon basin were investigated by To et al. (2022). Vu et al. (2021) also studied and proposed a reasonable FLWL to replace the current one in the inter-reservoir procedure promulgated by the Prime Minister for the Tra Khuc basin. Moreover, if the flood control storage capacity is fixed during the flood season, a water shortage can happen due to the reservoir not being full at the end of the regulation cycle (Li et al. 2010). Liu et al. (2011) also confirmed the benefits of having these flood control storage capacity changes during the flood season while not affecting flood control objectives. The studies above show that determining the reservoir's flood control capacity is critical. However, these studies are mainly conducted on single-purpose reservoirs, very few of them include multi-purpose reservoirs. In this study, we will provide an option to determine the appropriate change in flood control storage capacity during flood season for a multi-purpose reservoir based on the assessment of the power output and the ability of the reservoir to be filled with water after each regulation cycle.

Today, the operation of most reservoirs is contingent on the operating rule curves due to their simplicity. These rules, presented in graphs or tables, guide the discharge based on the reservoir's water level status, hydrological conditions, and time of year. Generally, they are established at the reservoir construction planning stage (Wang et al. 2014). Though being simple, these operating rules must be constantly renewed to adapt with changes, especially when there is a shift in hydrological conditions or the reservoir's objectives (Oliveira & Daniel 1997). To reduce conflicts among operational goals, reservoir managers are trying to come up with reasonable operating rule curves. There are two main types of methods to develop the operating rule curves, i.e., conventional and optimization methods (Jiang et al. 2018). Between these two, optimization methods are widely used in water resource engineering. Labadie (2004) provided a summary of the optimization techniques used in water resource allocation in single-purpose and multi-purpose reservoir systems. When supporting data is available, optimization approaches provide direct optimal reservoir operation solutions (Thang et al. 2020).

Many optimization algorithms have been used in reservoir operation, such as genetic algorithms (Feng et al. 2018; Olukanni et al. 2018; Tegegne & Kim 2020), particle swarm optimization (Oussama et al. 2019; Jahandideh et al. 2020), and progressive optimality algorithms. However, according to Jiang et al. (2018), these algorithms do have three disadvantages. Firstly, they often require a set of initial solutions and can only perform simulation optimization on those initial solutions. As a result, the quality of these initial solutions can greatly impact the final result. Secondly, it is very hard to attain a global optimal solution. Although many evolutionary algorithms have been shown to have global convergence, they are influenced by stochastic features, and hence they cannot guarantee a global optimal solution within a finite number of iteration calculations. Thirdly, some optimization methods, such as the progressive optimality algorithm, require constraints on the unsmooth and non-convex nature of the problems. Meanwhile, dynamic programming (DP) is a highly efficient optimization technique (Marano et al. 2012; Jiang et al. 2017). The most notable feature is that it can guarantee the global optimum without requiring an initial solution. Furthermore, there are no requirements for non-convex and unsmooth optimization problems in DP. DP is widely used in traditional optimization algorithms (Yakowitz 1982; Zhao & Jianshi 2014). Dynamic programming was used by Jiang et al. (2018) to create a new reservoir operation chart, which enhanced the power output by 2.68%. Pourahmadi & Boomsma (2022) proposed an approximate dynamic programming technique to assist reservoir operations that forecasts the future value of water using a linear approximation architecture. The results demonstrate that profit estimation improves by around 20% when the linear approximation includes inflow variables. Pant & Rani (2021) suggested an integrated approach that combines traditional dynamic programming and metaheuristic technique differential evolution. Kim et al. (2021) used stochastic dynamic programming to improve the robustness of reservoir operations. They introduced a new framework called robust stochastic dynamic programming, which combines robust optimization with objective function or constraint formulations used in stochastic dynamic programming.

An important consideration when creating an operating rule curve is the ease of use in assisting reservoir operators to make their decisions. Indeed, although optimal operating rule curves can significantly increase the efficiency of reservoir operation, researchers have also recognized that a gap still exists between theoretical models and practical activities (Yeh 1985; Pinthong et al. 2009). The problem with current operating rules for many reservoirs, including the A Vuong reservoir, is that there is a relatively large range between the limit lines. In practice, the presence of such a wide range can make it difficult for operators to make a quick decision on a course of action.

The purpose of this study is to use dynamic programming techniques to develop operating rules that are both convenient and optimized for operation. The A Vuong reservoir was selected as the case study. First, we suggest a reasonable time-varying flood control storage capacity. Then, we identify a number of operating rule curves for various initial water levels, along with the average line among limit lines. These simple, convenient, and optimal operating rules are essential for reservoir operators, who can easily accept and use them in practical operation. Finally, we compare power output performance with that of the current operating rules.

Study area

The A Vuong reservoir is located on the A Vuong river, which is a part of the Vu Gia Thu Bon basin. The region's climate is tropical monsoon with high temperatures. The annual rainfall in this area is about 2,200 mm, while the evaporation rate is 700 mm. The rainy season lasts four months, from September to December, and causes flooding. Little rain falls during the long dry season, which lasts from January to August and frequently causes water shortages. The A Vuong reservoir has a catchment area of 682 km2 (see Figure 1).
Figure 1

Location of the A Vuong reservoir.

Figure 1

Location of the A Vuong reservoir.

Close modal

The construction of the A Vuong reservoir began in 2003 and was completed in 2008. The primary purpose of the reservoir is power generation, but it was later on assigned additional tasks of flood control and water supply. As a result, many contradictions have arisen during the operational process. The operator wishes to maintain a high water level in order to increase power output, but in order to prevent flooding, they must have an empty capacity. Moreover, as reservoirs lower their water level, the risk of not being fully filled before the next cycle becomes higher, especially if the natural flow is low. These conflicts between flood control and downstream water supply are quite common for multi-purpose reservoirs (Nga et al. 2019; Nguyen 2019; Le et al. 2021; To et al. 2022). It is critical to find ways of improving operational efficiency to meet A Vuong reservoir's water consumption targets.

Figure 2 shows the original design rule curves of the A Vuong reservoir. Three operating zones have been established for different water levels. When the water level is below the dead water level, hydropower generation is stopped. When the water level falls into Zone III, hydropower generation is controlled with a discharge through turbines to meet the minimum water demand downstream. When the reservoir water level is in Zone II, the turbines are operated at a flow rate between the minimum and maximum capacity. If the water level is above the upper limit (Zone I), hydropower generation is controlled with maximum discharge through turbines. Although the operating rule curves seem simple, the history of operations shows the following problems: (i) contradictions between water goals occur frequently; (ii) the reservoir sometimes can't be refilled to the normal level at the end of the regulation cycle; and (iii) the operator's activity is challenged by the wide range between the limit lines, and the operation results are subject to the operator's subjective judgment.
Figure 2

The original design rule curve of the A Vuong reservoir.

Figure 2

The original design rule curve of the A Vuong reservoir.

Close modal

Data used

The 10-day inflow data collected during 2002–2021 were selected as inputs to the operation model for the A Vuong reservoirs. Figure 3 shows average 10-day inflow data for each year. It can easily be seen that there is more inflow between September and December (rainy season), and much less water between January and August (dry season).
Figure 3

Average 10-day inflow of the A Vuong reservoir (2002–2021).

Figure 3

Average 10-day inflow of the A Vuong reservoir (2002–2021).

Close modal

The capacity, efficiency, power output, and operational documents of the hydroelectric power plant are taken from the reservoir design documents that have been approved by the appropriate authorities. Additional documents are collected, including those related to evaporation loss, water level relationships, and the reservoir characteristic curve. Table 1 shows the main characteristics of the A Vuong reservoir.

Table 1

Characteristic parameters of the A Vuong reservoir

No.DataUnitA Vuong reservoir
I Parameter of reservoir   
Basin area Flv km2 682 
Annual flow m3/s 39.8 
Normal water level 380 
Dead water level 340 
Total storage capacity (Vtotal106 m3 343.55 
Active storage capacity (Vhi106 m3 266.48 
II Hydroelectric power plant   
Maximum flow (Qmaxm3/s 78.4 
Installed capacity (NlmMW 210 
Annual power output (E) 106 Kwh 815 
Number of turbines set 
No.DataUnitA Vuong reservoir
I Parameter of reservoir   
Basin area Flv km2 682 
Annual flow m3/s 39.8 
Normal water level 380 
Dead water level 340 
Total storage capacity (Vtotal106 m3 343.55 
Active storage capacity (Vhi106 m3 266.48 
II Hydroelectric power plant   
Maximum flow (Qmaxm3/s 78.4 
Installed capacity (NlmMW 210 
Annual power output (E) 106 Kwh 815 
Number of turbines set 

Optimization model

Since the A Vuong is a multi-purpose reservoir, we first need to establish a multi-objective optimal operation. The optimization model's objective functions and constraints are as follows:

Objective function:
  • - Maximize hydropower generation (HG):
    (1)
  • - Maximize flood control capacity: Vpl

where
  • HG: total hydropower generation of the A Vuong reservoir

  • : Average water head for power generation at time period i, unit: m

(2)
  • ZTL−i: upstream water elevation at time period i, unit: m
    (3)
    where Vi and Vi+1 are the reservoir storages at time periods i and i +1; f2 is a function of the relationship of storage and elevation
  • ZHL−i: the downstream water elevation at time period i, unit: m

  • ΔHi: the head loss at time period i due to friction in the tunnel and the penstock

  • Qi: average flow through turbine at time period i, unit: m3/s

  • t: the time step.

Constraints:

  • - Water volume balance:
    (4)
    (5)
    where Vi and Vi+1 represent the reservoir storages at the beginning of time periods i and i+1, respectively, in volume units; Ii, ELi are inflow and evaporation, respectively; Vpower and Vspillway are water discharges through the turbine and spillway, respectively.
  • - Reservoir storage volumes limits:
    (6)
    where Vdead and Vnormal represent the reservoir storage corresponding to the dead water level and the normal water level, repectively, unit: m3.
  • - Power generation limits:
    (7)
    where Nmin and Nmax represent the minimum and maximum power capabilities, unit: KW
  • - Flood control storage capacity limits:
    (8)

Figures 4 and 5 depict the entire flowchart for calculating the reservoir operation chart based on the DP technique, where k represents the index of a discretized water level combination at the end of a stage; k = 1, 2, …. m; m is the number of discrete points of the feasible water level; j represents the index of a discretized water level combination at the beginning of a stage; j= 1, 2, …. m; i is the index of a stage and i = 1, 2, …., n; n is the total number of stages over the entire planning horizon; E and Ecum are power output and cumulative power output, respectively. Qpower is the flow discharge through the turbine; η-ass and η-cal are the assumed and calculated efficiency coefficients, respectively.
Figure 4

Flow chart of calculating the reservoir operation.

Figure 4

Flow chart of calculating the reservoir operation.

Close modal
Figure 5

Schematic diagram of the calculating the reservoir operation based on DP.

Figure 5

Schematic diagram of the calculating the reservoir operation based on DP.

Close modal

The specific steps involved in calculating reservoir operation based on DP are summarized below.

Step 1: Divide the entire operation period into n stages, and then get the discrete water level combinations in the range of Zdead to Znormal for each stage. There will be m discrete water level points in each stage.

Step 2: Start the backward recursion from stage n. In this step, the calculation of the reservoir's storage capacity in the current stage must be repeated for each discretized water level combination in order to obtain the optimal cumulative benefit (power generation) of the current stage. Set i=i1 and proceed to the next stage of the calculation.

Step 3: Once the first stage's calculation is completed, the reverse recursion procedure is finished. Then, using the saved optimal candidate paths, retrace the optimal path from the first to the nth stage to obtain the best combination of power output and reservoir operation water level.

Proposed flood control storage capacity

In this section, we use the above optimization model to calculate reservoir regulation and find a reasonable flood control storage capacity. Suggested scenarios are listed in Table 2, along with water levels, flood control storage capacities, and their duration. There is no flood control storage in the base scenario (Scenario 1a). The proposed Vpl varies from 10% to 50% of the active storage capacity (Vhi), with a duration of 30, 60, or 90 days starting from September 1st (Scenarios 2a–16a). We determine the ability to refill the reservoir to its normal water level, the reduction in power output for each scenario, and compared them to one another. From there, we can select the best option for flood control storage capacity. In the next part, the selected storage capacity will be used to develop the optimal operating rule curves.

Table 2

Scenarios for flood control storage capacity

ScenarioThe duration of the flood control capacityFlood control storage capacity (%Vhi)Water level (m)Flood control storage capacity (106 m3)
1a 0%Vhi 380 
2a 1/9–30/9 (30 days) 10%Vhi 377 26.65 
3a 1/9–30/9 (30 days) 20%Vhi 373.9 53.30 
4a 1/9–30/9 (30 days) 30%Vhi 370.6 79.94 
5a 1/9–30/9 (30 days) 40%Vhi 367.1 106.592 
6a 1/9–30/9 (30 days) 50%Vhi 363.5 133.24 
7a 1/9–30/10 (60 days) 10%Vhi 377 26.65 
8a 1/9–30/10 (60 days) 20%Vhi 373.9 53.30 
9a 1/9–30/10 (60 days) 30%Vhi 370.6 79.94 
10a 1/9–30/10 (60 days) 40%Vhi 367.1 106.592 
11a 1/9–30/10 (60 days) 50%Vhi 363.5 133.24 
12a 1/9–30/11 (90 days) 10%Vhi 377 26.65 
13a 1/9–30/11 (90 days) 20%Vhi 373.9 53.30 
14a 1/9–30/11 (90 days) 30%Vhi 370.6 79.94 
15a 1/9–30/11 (90 days) 40%Vhi 367.1 106.592 
16a 1/9–30/11 (90 days) 50%Vhi 363.5 133.24 
ScenarioThe duration of the flood control capacityFlood control storage capacity (%Vhi)Water level (m)Flood control storage capacity (106 m3)
1a 0%Vhi 380 
2a 1/9–30/9 (30 days) 10%Vhi 377 26.65 
3a 1/9–30/9 (30 days) 20%Vhi 373.9 53.30 
4a 1/9–30/9 (30 days) 30%Vhi 370.6 79.94 
5a 1/9–30/9 (30 days) 40%Vhi 367.1 106.592 
6a 1/9–30/9 (30 days) 50%Vhi 363.5 133.24 
7a 1/9–30/10 (60 days) 10%Vhi 377 26.65 
8a 1/9–30/10 (60 days) 20%Vhi 373.9 53.30 
9a 1/9–30/10 (60 days) 30%Vhi 370.6 79.94 
10a 1/9–30/10 (60 days) 40%Vhi 367.1 106.592 
11a 1/9–30/10 (60 days) 50%Vhi 363.5 133.24 
12a 1/9–30/11 (90 days) 10%Vhi 377 26.65 
13a 1/9–30/11 (90 days) 20%Vhi 373.9 53.30 
14a 1/9–30/11 (90 days) 30%Vhi 370.6 79.94 
15a 1/9–30/11 (90 days) 40%Vhi 367.1 106.592 
16a 1/9–30/11 (90 days) 50%Vhi 363.5 133.24 

Developed operation rule curves

The authors develop a new operating rule curve based on the previously mentioned flood control capacities. Using the DP technique, we perform optimal calculations for different water levels on January 1st, changing from 368 m to 380 m. The scenarios of different water levels at the beginning of the cycle are depicted in Table 3. During operation, the reservoir water level will be controlled to: (1) reach the water level corresponding to the flood control capacities of 50%Vhi, 30%Vhi, and 10%Vhi in September, October, and November, respectively; and (2) reach 380 m at the end of the cycle. Our results show that for each scenario of the water level on January 1st, there are 20 optimal operating curves that correspond to the 20 years of hydrological data (2002–2021). The upper limit lines are derived from the maximum water level values of the 20 optimal operating lines. Similarly, the lower limit lines are derived using the lowest water level values. In addition, the average line between the two limit lines is also derived from the average values of the water levels.

Table 3

Scenarios of different water levels at the beginning of the regulation cycle

ScenarioWater levels on January 1st (m)
1b 380 
2b 378 
3b 376 
4b 374 
5b 372 
6b 370 
7b 368 
ScenarioWater levels on January 1st (m)
1b 380 
2b 378 
3b 376 
4b 374 
5b 372 
6b 370 
7b 368 

Proposed flood control storage capacity

Figure 6 shows the power output for various flood control capacity scenarios as well as their durations (scenarios 2a–16a). In the scenarios of Vpl = 10%–50%Vhi with 30-day duration (scenarios 2a–6a), power outputs are quite similar, with the exception of 2009 (see Figure 6(a)).
Figure 6

Power output for different flood control capacity options (a): scenarios 2a–6a; (b) scenarios 7a–11a; and (c) scenarios 12a–16a.

Figure 6

Power output for different flood control capacity options (a): scenarios 2a–6a; (b) scenarios 7a–11a; and (c) scenarios 12a–16a.

Close modal

In cases where the duration is extended to 90 days (scenarios 12a–16a), the effect of different flood control capacities on power output becomes clear (Figure 6(c)). However, there is a small difference in the power output when the flood control capacity changes for a few years, including 2012, 2018, and 2019. This can be explained by the fact that the inflow is small in these years, the reservoir water level is low, and there is almost no discharge of water over the spillway. The amount of water in the reservoir for power generation is nearly the same among these flood control capacity options, so the power output varies slightly. In contrast, the power outputs in 2007, 2009, 2013, 2020, and 2021 have a more visible change. In these years, there may have been major floods and large inflows. The amount of water discharged through the spillway is high, and the size of the flood control capacity will have a significant impact on the power output. For example, with the option of Vpl = 50%Vhi, the large flood control capacity leads to more water being discharged through the spillway, resulting in a decrease in power output.

Table 4 and Figure 7 show the power reduction when flood control capacity changes compared to the base scenario, where flood control capacity is not available. Power output is the annual average for the year series from 2002 to 2021. The findings show that the power reduction is strongly influenced by the size and duration of the flood control capacity. The larger the flood control capacity and the longer the duration, the greater the reduction in power. For example, if Vpl = 30%Vhi and lasts for 30 days, the power output will decrease by 0.019% (scenario 4a). If the Vpl = 50%Vhi, the power output will decrease by 0.169% (scenario 6a). If the durations of these two flood control capacity options are 90 days, the power output will decrease by 2.56% and 5.301% for scenarios 14a and 16a, respectively.
Table 4

Power outputs for scenarios 1a–16a in comparison to the base scenario

ScenarioAnnual power output (106 Kwh)Power output reduction (106 Kwh)Power output reduction (%)
1a 680.43 0.00  
2a 680.43 0.00 0.000 
3a 680.43 −0.07 −0.010 
4a 680.36 −0.13 −0.019 
5a 680.30 −0.31 −0.045 
6a 680.12 −1.15 −0.169 
7a 679.27 −1.11 −0.163 
8a 679.32 −2.96 −0.435 
9a 677.47 −5.23 −0.769 
10a 675.20 −7.67 −1.128 
11a 672.75 −10.81 −1.588 
12a 669.62 −3.26 −0.478 
13a 677.17 −10.06 −1.479 
14a 670.36 −17.42 −2.560 
15a 663.00 −24.95 −3.667 
16a 655.47 −36.07 −5.301 
ScenarioAnnual power output (106 Kwh)Power output reduction (106 Kwh)Power output reduction (%)
1a 680.43 0.00  
2a 680.43 0.00 0.000 
3a 680.43 −0.07 −0.010 
4a 680.36 −0.13 −0.019 
5a 680.30 −0.31 −0.045 
6a 680.12 −1.15 −0.169 
7a 679.27 −1.11 −0.163 
8a 679.32 −2.96 −0.435 
9a 677.47 −5.23 −0.769 
10a 675.20 −7.67 −1.128 
11a 672.75 −10.81 −1.588 
12a 669.62 −3.26 −0.478 
13a 677.17 −10.06 −1.479 
14a 670.36 −17.42 −2.560 
15a 663.00 −24.95 −3.667 
16a 655.47 −36.07 −5.301 
Figure 7

Trade-off between power output reduction and the flood control storage capacity.

Figure 7

Trade-off between power output reduction and the flood control storage capacity.

Close modal

Table 5 shows the possibilities of the reservoir being refilled at the end of each regulation cycle for different scenarios. The number of times when the reservoir was refilled fully (hereinafter referred to as Tf) for the simulation 21-year time series is also displayed. If the duration is 30 days, Tf can reach a maximum of 17 regardless of the flood control capability (scenarios 2a–6a). The smallest Tf is 2 when the Vpl is 40%–50% of the Vhi and lasts for three months (scenarios 15a, 16a). It should also be noted that in some years, such as 2012 and 2019, the reservoir cannot be fully refilled for all scenarios, even when the flood control capacity and duration are short. According to historical data, these have been years of very low inflows. In contrast, in years with large inflows, such as 2016 and 2020, the reservoir can be fully refilled for all scenarios.

Table 5

Statistics that the reservoir is fully refilled under different scenarios for each year

YearScenario
2a3a4a5a6a7a8a9a10a11a12a13a14a15a16a
2002 − − − 
2003 − − − − − 
2004 − − − 
2005 − − − − 
2006 − − − − − − 
2007 − − − − 
2008 − − − − 
2009 − − − − 
2010 − − − − 
2011 − − − 
2012 − − − − − − − − − − − − − − − 
2013 − − − 
2014 − − 
2015 − − − − − − 
2016 
2017 − − − − 
2018 − − − − − − − − − − − − − − − 
2019 − − − − − − − − − − − − − − − 
2020 
2021 − − − − 
Tf 17 17 17 17 17 17 17 17 16 14 16 7 3 2 2 
YearScenario
2a3a4a5a6a7a8a9a10a11a12a13a14a15a16a
2002 − − − 
2003 − − − − − 
2004 − − − 
2005 − − − − 
2006 − − − − − − 
2007 − − − − 
2008 − − − − 
2009 − − − − 
2010 − − − − 
2011 − − − 
2012 − − − − − − − − − − − − − − − 
2013 − − − 
2014 − − 
2015 − − − − − − 
2016 
2017 − − − − 
2018 − − − − − − − − − − − − − − − 
2019 − − − − − − − − − − − − − − − 
2020 
2021 − − − − 
Tf 17 17 17 17 17 17 17 17 16 14 16 7 3 2 2 

The symbol ‘ + ’ indicates that the reservoir's capacity has been reached, while the symbol ‘ − ’ indicates that it has not been reached.

The impacts of Vpl options on Tf and power reduction are summarized in Figure 8. It can be seen that the changing of Vpl from 50%Vhi to 30%Vhi and 10%Vhi in September, October, and November, respectively, is the most effective. This is the option with the highest Tf and the least amount of power reduction. This option will be chosen for developing the optimal operating rule curve.
Figure 8

The impact of Vpl options on Tf and power reduction.

Figure 8

The impact of Vpl options on Tf and power reduction.

Close modal

Developed operation rule curves

Figures 9 and 10 show the optimal operating rule curves for the different scenarios. Figure 9(a) depicts the optimal operating curves for the 2002–2021 flow series for scenario 1b. These curves may differ depending on the inflows of each year, but they must still satisfy the above-mentioned objective functions. According to the flood control capacity option selected above, the A Vuong reservoir was operated so that its water level had to satisfy the Vpl of 50, 30, and 10% of the Vhi in September, October, and November, respectively. The water level drops at the end of the dry season (August 30th), but it should not fall below the dead water level and return to normal water level at the end of the flood season.
Figure 9

The optimal operating rule curves for scenario 1b: (a) with respect to the 2002–2021 flow series; (b) the average, upper and lower limit lines.

Figure 9

The optimal operating rule curves for scenario 1b: (a) with respect to the 2002–2021 flow series; (b) the average, upper and lower limit lines.

Close modal
Figure 10

The optimal operating rule curves for scenarios 2b–7b.

Figure 10

The optimal operating rule curves for scenarios 2b–7b.

Close modal

The average, upper and lower limit lines for scenario 1b are shown in Figure 9(b). Based on these curves’ operating ranges, particularly the position of the average line, operators can select the right action plan. From January 1st to September 1st, the water level gradually decreases but is guaranteed not to be lower than 340 m (the dead water level). The water level begins to rise after September 1st. From September to October, flood control capacity ranges from 50% to 30% of the Vhi. During this time, the probability of a flood occurring is relatively high. With this change in flood control capacity, the reservoir ensures flood control, optimal power output, and the ability to be completely refilled at the end of the cycle to serve other water needs. Flooding becomes less likely after October 30th, and flood control capacity has fallen to 10%Vhi. The water level gradually rises until it reaches its normal level of 380 m by December 31st.

The average, upper and lower limit lines for scenarios 2b–7b with water levels ranging from 378 m to 368 m at the beginning of the regulation cycle are depicted in Figure 10. Depending on the water level at the beginning of the regulation cycle, there will be corresponding operating curves. These operating curves all comply with the values of flood storage capacities defined above, ensuring the safety of flood control and water supply. In addition, they also help to improve power output in cases where the water levels at the beginning of the cycle are different. Unlike the current operating chart, providing each specific case of the beginning water level simplifies operations for managers. Operators can select the appropriate operating chart based on the water level at the beginning of the cycle. Furthermore, the presence of an average line specifically assists operators in making decisions. Details will be discussed further in the following section.

Discussions

The decision to operate a reservoir at one point in time will have an impact on not only power output and water supply at that time, but also on all subsequent stages in the reservoir's regulatory cycle. The hydrological regime in Vietnam is complex, and long-term forecasting is still challenging. Furthermore, power generation planning is typically developed for 10-day periods at the request of the power authority. Under the current operating rules, the range between the limit lines is quite large, causing operational difficulties. Operational decisions are easily influenced by the subjectivity of the users in the absence of proper instructions.

Most of the previous studies mainly focused on optimization algorithms and were performed on a general graph (Jiang et al. 2018; Thang et al. 2020; Pant & Rani 2021; Pourahmadi & Boomsma 2022). Few studies have been conducted on a large number of cases corresponding to different early-cycle water levels. Meanwhile, this water level does not always reach the normal water level. Offering a variety of operating charts depending on the beginning water level will allow operators to act more accurately, reducing the operator's subjective factors. In addition, the introduction of the average line makes the operation process run more conveniently. Indeed, the average line will serve as a guide for operators to follow. Operation managers can increase or decrease the number of turbine sets and adjust the water level to follow the average line.

Figure 11 shows the observed water level and the calculated water level with the proposed average line for 2018. The upper and lower limits are also shown in the figure. The calculated water level is close to the average line during the dry season (1/1–1/9), but the actual observed water level is significantly lower. After September 1st, both observed and calculated water levels are lower than the average line. Because 2018 was a year with very low inflows, the water level did not reach normal levels at the end of the regulation cycle.
Figure 11

Comparison of observed water level and calculated water level using proposed operating curves (2018).

Figure 11

Comparison of observed water level and calculated water level using proposed operating curves (2018).

Close modal
Figure 12 shows the increase in the power output when operating under the proposed curves in 2018. For the dry season, the power output calculated using the dynamic programming method and the observed output are 504.12 kWh and 486.74 kWh, respectively. For the whole year, power outputs are 598.18 kWh and 579.75 kWh, respectively. The results show that this method can boost power output by 3.5% and 3.1% for the dry season and the whole year, respectively. Thus, applying dynamic programming helps increase the output of hydropower reservoirs. Jiang et al. (2018) used dynamic programming to boost the Ya Yangshan reservoir's power output by 2.68%. Particularly for the A Vuong reservoir, the application of dynamic programming has really brought high efficiency compared to other methods. Le (2012) conducted a study using genetic algorithms to optimize the operation of the A Vuong reservoir and increase the power output by about 3%.
Figure 12

Comparison of observed power output and calculated power output using proposed operating curves (2018).

Figure 12

Comparison of observed power output and calculated power output using proposed operating curves (2018).

Close modal

Recommendations

Figure 13 shows the incoming flow values corresponding to the different frequency levels (P%). During operation, the water level should be kept between the upper and lower limit curves. If the inflow is relatively large (P > 50%), the operating range should be between the average and upper limit curves. If the inflow is low (P < 50%), the operating range is from the average curve to the lower limit curve. The authors recommend that the operating water level should be kept in line with the average curve. Depending on the variation of inflow over a 10-day period, the operating water level is adjusted to follow the average curve by increasing or decreasing the number of turbine units or the amount of discharge.
Figure 13

The incoming flow values corresponding to the frequency levels.

Figure 13

The incoming flow values corresponding to the frequency levels.

Close modal

In addition to the amount of the inflow, the power output of the A Vuong reservoir in each period is determined by the power system's requirements. The output power is generally registered 10 days in advance. Based on the prior period's inflow, the number of turbine units used to generate electricity will be estimated. If the inflow is small, register one turbine unit; otherwise, register two turbine units. It should be noted that the goal of the reservoir operation is to maximize total power output while also satisfying the reservoir's other functions. As a result, it is critical to follow these guidelines to ensure that the goals are met. Due to the small amount of inflow, the operators must accept little power generation for a few months during the operation, not generating electricity in any way that causes the water level to exceed the established limits.

The current operation of the A Vuong reservoir has several conflicts among its flood prevention, power generation, and water supply goals. In addition, the current operation curves with a wide range also cause difficulties for the operator. This study contributes to resolving the above conflicts and improving the operational efficiency of the reservoir. The study's main findings are as follows:

  • - The Vpl options were proposed to ensure the objectives of flood control, power output, and water supply. The best solution is that Vpl has values of 50, 30, and 10% of Vhi in September, October, and November, respectively.

  • - The study developed a new optimal operation curve, including the limit and average curves. These new curves help to meet operational goals and are also more convenient for operators. In addition, to meet actual operational needs, various scenarios for the beginning water levels from 360 m to 380 m were considered. The optimal operation curves can boost power output by 3.5% and 3.1% for the dry season and the whole year, respectively, in check for 2018.

  • - We also recommend some adjustments for reservoir operation practice: the operator should always stay close to the average curve. The number of turbine units can be adjusted based on the value and frequency of incoming flow, as well as the current water level position relative to the average line.

  • - Although this paper proposes a new method for constructing operation rule curves, there are some limitations and simplifications, such as a calculation time step of 10 days and implementation for single reservoirs. All of the above are aspects worth researching further in the future.

The authors wish to express their appreciation to the Ministry of Education and Training for supporting this research project # B2021-DNA-13.

Data cannot be made publicly available; readers should contact the corresponding author for details.

The authors declare there is no conflict.

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