Upload
others
View
0
Download
0
Embed Size (px)
Citation preview
( 86 )
Application of Non-dominated Sorting Genetic Algorithm (NSGA) for Optimization of Flushing Operation
Considering Water Quantity and Quality
非支配型排序基因演算法於水量水質於排砂運作優化之應用
Hamid Khakzad*
Department of Engineering,
RusPers Group Company,
Project Manager
ABSTRACT
Water quantity and quality are considered to be the main driving forces for Flushing operation in dam reservoirs. In this study, we consider the knapsack problem based Non-dominated Sorting Genetic Algorithm (NSGA) optimization algorithm for the assessment of planning operations of a dam reservoir. The knapsack problem plays a significant role in the study of non-convex programming in discrete mathematics, and that calls for the optimal assignment of a set of items, each having a profit and a weight. The presented sediment-flushing model is developed to estimate the amount of the flushed sediment volume, water volume and the length of time of needed to complete flushing operation flushing, which can be taken into account in the reservoir simulation model. A study was conducted on Dez Hydropower reservoir in Iran, which is currently facing serious sedimentation problems. Total volume of water passed per flush (m3) and total volume of sediment passed per flush (m3) for scenario 1 (for protecting eggs & early life stage salmonids) and for scenario 2 (protecting adult non-salmonids) with acceptable sediment concentration downstream of the spillway= 8,000, 10,000, 15,000 (mg/l), are calculated. The results from this study help us identify a solution to satisfy water demand, and determine the appropriate hydraulic conditions to decrease negative environmental effects of Dez dam flushing operation on the downstream.
Keywords: Sediment management in reservoir, Non-dominated Sorting Genetic Algorithm (NSGA), Ecological flow, Dez Hydropower reservoir.
摘 要
水量及水質為水庫排砂之兩大重要驅力。本研究將非支配型排序基因演算法運用於背包問題,計算並評估水庫之最佳設計及運作模式。背包問題為離散數學中非凸性程式研究之重要一環,每一項目皆具其利益及重量,使得項目最佳分配成為必要。本研究建構並呈現一沈澱物-排砂模型,可用以預估排出之泥沙容積、水容積,以及完成排砂所需時間,
* Corresponding author: Project Manager/ RusPers Group Company, Department of Engineering, 109263, Moscow, Russia/ No. 25, Artyukhina St. Moscow, Russia/ [email protected]
臺灣水利 第 68 卷 第 1 期
民國 109 年 3 月出版
Taiwan Water ConservancyVol. 68, No. 1, March 2020DOI: 10.6937/TWC.202003/PP_68(1).0008
( 87 )
1. INTRODUCTION
Sediment deposition in reservoirs causes
loss of capacity, increases flood risks, degradation
of water quality, leads to difficulty in reservoir
operation and maintenance and consequently, raise
the overall associated cost. Besides this, sediment
storage can have a significant impact on ecosystem downstream of large river systems. Given the
scarcity of undeveloped new dam sites in watersheds
where extensive dam construction has already
been undertaken, it will be increasingly necessary
in the future to focus on storage preservation. The
effects of reservoir sedimentation can be mitigated
through implementation of reservoir sedimentation
management techniques (Nikolaos, 2017).
Flushing is one of the most economical
methods for recovering lost storage without
incurring the cost of dredging. Flushing involves the
remobilizing of deposited sediments by increasing
the flow velocity in the reservoir. The entrained
deposits are discharged into the downstream
of the reservoir through low-level outlets. The
flow velocity is increased by drawing down the
reservoir water level through a suitably designed
outlet structure. On the other hand, flushing also
releases large volumes of sediment downstream
creating potentially serious problems. Scouring of
polluted sediments from the reservoir threatens the
downstream water quality and ecology (Sloff, 1991).
Also, releasing high sediment concentration water
may have a great impact on the downstream biota
(Morris and Fan, 1997). This led to the development
of “environmentally friendly flushing” technique,
detailed in particular, by Fruchard (2008).
In this method the hypolimnic water from the
bottom outlet, which is high in suspended sediment,
mixes with the water from the mid depth outlet,
which is low in suspended sediment. Thus, the
flushing flow created during the event will have
much lower concentrations of suspended sediment
than would otherwise be the case. Actually this
technique also improves downstream oxygen
concentration and minimizes temperature changes
and pollution: water released from near the bottom
of a stratified reservoir is usually cold, oxygen-
depleted, and high in hydrogen sulfide and other
pollutants, whereas water released from a mid-depth
is more oxygenated, warmer and less concentrated
in heavy metals and pollutants (McCartney et al.,
2001).
Over the last 20 years, many researchers,
including those in the environmental resources
management, have embarked on the implementation
of a wide range of various evolutionary algorithms:
Genetic algorithms, Ant colony optimization,
Par t ic le swarm opt imizat ion (PSO), mul t i
objective evolutionary algorithm (EA) based
on decomposition (MOEA/D), Non-dominated
Sorting Genetic Algorithm (NSGA), Ant Colony
optimization (ACO), simulated annealing, shuffled complex evolution and harmony search among
many others (Katsifarakis, 2012). Chen et al,
(1998) use a GA with an aggregating approach
(a multiplication of the aspiration levels of each
objective) for a water quality control problem. Three
objectives are considered: maximize the assimilative
capacity of the river, minimize the treatment cost for
water pollution control and maximize the economic
value of the river flow corresponding to recreational
其皆可納入水庫模擬模型之計算。本研究於伊朗的德茲水力發電水庫進行實驗,該地當前正經歷嚴重的泥砂沈積問題。情境一(為保護鮭科魚類的卵及幼魚)以每次排砂排出的水及沈積物總容積(立方公尺)計算,情境二(保護非鮭科成魚)則以溢道下游可接受的沉積物濃度8000、10,000、15,000 (毫克/公升)計算之。本研究成果有助計畫因應供水需求之方案,並擬定適合的水利設計,降低德茲水庫排洪對於下游環境造成之負面影響。
關鍵詞: 水庫泥沙管理,非主導分類遺傳算法,生態流量,德茲水電站。
( 88 )
aspects (Coello, 2007). Srigiriraju (2000) uses
the Noninferior Surface Tracing Evolutionary
Algorithm (NSTEA) to solve an estuary water
quality management problem. Two objectives are
considered: minimize cost of BOD control, and
maximize equity with respect to levels of treatment
among the different dischargers. About 2005 more
scientific impetus was added to water management models by the use of environmental variables to
indicate global climatic changes and environmental
pollution levels (Uslaender, 2010). Additionally,
the inclusion of socio-economic relationships and
the evaluation of ecosystem services has gradually
become the focal point in environmental informatics
and management (Rauschenbach, 2016).
This study presents the principles of Non-
dominated Sorting Genetic Algorithm (NSGA),
which is one of the evolutionary algorithms that
has shown great potential for the solution of
various optimization problems. By developing the
necessary elements, we then provide an adaptation
of this algorithm for multi-objective Optimization
for Eco-Friendly flushing in reservoirs. Finally,
we demonstrated the results of application of the
proposed methodology to selected case-study.
2. MATERIAL AND METHOD
2.1 Study area and data collection
This s tudy was carr ied out a t the Dez
Reservoir, which is located in southern Iran. The
Dez Dam is a large hydroelectric dam in Iran, which
was built in 1963 by an Italian consortium. At the
time of construction, the Dez Dam was Iran’s largest
development project. The Dez Dam is a 203 m-high
double curvature arch dam, and the level of its crest
is 352 m above sea level. The original reservoir
volume was 3,315 × 106 m3, and the estimated
volume of arrival sediment was 840 × 106 m3 for
a 50-year period. The minimum and maximum
operating water levels of the reservoir are 300 m and
352 m from the sea level, respectively. Although the
project has been well-preserved, the project is now
more than 40 years old, reaching its midlife period.
The useful life of the Dez Reservoir is threatened
by a sediment delta, which is approaching the
dam’s intake tunnels. A hydrographic study in 2002
showed that sedimentation reduced useful storage
of the Dez Reservoir from 3,315.6 × 106 m3 to 2,700
× 106 m3 (19% reduction). The difference between
levels of the inlet of turbine and bed surface of
deposited sediment is 14 m, and the sedimentation
rate near the inlet of turbine is 2 m/year. Therefore,
sediment management in the Dez Reservoir is of
considerable importance (Khakzad, 2014).
A f ie ld measurement program for the
measurement of the turbidity currents in the
Dez Reservoir commenced in December 2002
and finished in June 2003 (Dezab Consulting
Engineers, 2004). The measuring was performed on
a daily basis. The program consisted of a series of
measurements at various depths and locations across
seven cross-sections. The measurement station
locations are shown in Fig. 1. RCM9 and Valeport
108 MK II were used to measure the current velocity
and direction, electrical conductivity, temperature,
and pressure, and their specifications can be found in Dezab Consulting Engineers in Association with
ACTRES International (2004).
The first four months of data gathering were
done by Valeport 108 MK II. Data gathering is a
direct reading. After the fourth month, a RCM9
instrument was used to collect data. In addition to
previously mentioned parameters, it can measure
water turbidity as well. Also, it is a self-recording
equipment. Figs. 2 to 5 show a sample of field
measurement records on turbidity currents at
A2, B3, C3, E, and F stations, collected on April
24, 2003, where the water level is 351 m, the
maximum depth is 94 m; the reservoir inflow is
1,210.6 m3/s, and the reservoir outflow is 590.8
m3/s (KWEO 2003). With help from these field
measurement records, we estimated a flow regime
( 89 )
and an annual inflow of turbidity currents in Dez
dam reservoir, then we studied and reviewed the
various environmental issues that may influence
the recommended hydraulic conditions enacted to
decrease the negative environmental impacts of Dez
Dam flushing operation (Khakzad, 2014, 2015).
According to the field studies over the period
of December 2002 to April 2003, there were only
two significant turbidity currents. The measurements of velocity and suspended sediment concentration
at section A indicated that the first turbidity current occurred on January 28 and 29, 2003. The thickness
Fig. 1. Sketch of measurement stations.
( 90 )
of the turbid layer was about 15 m. The flow
direction of the water near the surface was upstream,
but the velocity was low. It goes without saying that
large slow-moving eddies were present above the
turbidity current. The magnitude of velocity and
its direction changed with time. The fine sediment
moved into the reservoir on January 29, 2003,
reaching a volume of 44,000 m3.
The second turbidity current occurred on
April 23 and 24, 2003. It is difficult to quantify the turbidity load based on the available measurements.
However, on the basis of the average reservoir
inflow values, the turbidity load value for rainstorm events rose to 1,188,475 m3 over the two days. Table
1 shows the range and values of different parameters
used in this study. The median particle size of all
samples was less than 0.01 mm, with the median
particle size of sediments taken upstream in the
reservoir slightly larger than those closer to the dam.
2.2 Non-dominated Sorting Genetic Algorithms
(NSGA) for Knapsack Problems
The knapsack problem (KP) can be formally
defined as follows: we are given an instance of the knapsack problem with item set N, consisting of n
items j with profit Pj and weight Wj, and the capacity
value c. (Usually, all these values are taken from
the positive integer numbers.) Then the objective
is to select a subset of N such that the total profit
of the selected items is maximized and the total
weight does not exceed c. Alternatively, a knapsack
problem can be formulated as a solution of the
following linear integer programming formulation
(Kellerer, 2004):
Fig. 2. Temperature-dimensionless water depth profiles at different stations.
Fig. 3. Current speed-dimensionless water depth profiles at different stations.
Fig. 4. Current direction-dimensionless water depth profiles at different stations.
Fig. 5. Turbidity-dimensionless water depth profiles at different station.
( 91 )
maximize ∑ j = 1 pj xj (1)
subject to ∑ j = 1 wj xj ≤ c (2)
xj ∈{0, 1}, j = 1, …, n. (3)
We will denote the optimal solution vector by
x* = (x1*, ..., xn*) and the optimal solution value
by z*. The set X* denotes the optimal solution set,
i.e. the set of items corresponding to the optimal
solution vector.
The knapsack problem has been studied
for centuries as it is the simplest prototype of a
maximization problem. The set of all the Pareto-
optimal solutions forms the tradeoff surface in the
objective space. This tradeoff surface is called the
Pareto front. EMO algorithms are usually designed
to search for a set of well-distributed non-dominated
solutions that approximates the entire Pareto
front very well. In recent years knapsack problem
turned out to be one of the favorite playgrounds
for experiments with metaheuristics, in particular
Particle Swarm Optimization, Non-dominated
Sorting Genetic Algorithm (NSGA), Ant Colony
Optimization and Tabu search (Coello Coello,
2007).
NSGA algorithm is based on several layers of
classifications of the individuals. Before selection
is performed, the population is ranked on the basis
of nondomination: all nondominated individuals are
classified into one category (Fig. 6) (with a dummy
Table 1. Parameters of turbidity currents in Dez Reservoir from December 2002 to June 2003
Date StationWater depth
(m)
Observed deposit depth
(m)
Width of turbidity
current (m)
Mean velocity (m/s)
Direction of turbidity current (°)
Sediment transport rate
(m3/d)
Jan. 29, 2003 A2 58 15 300 0.17 163 to 231 44,000
Apr. 23, 2003 A2 94 20 300 0.8 180 1,014,120
Apr. 23, 2003 F 77 23.5 200 0.75 180 622,080
Apr. 24, 2003 A2 94 10 300 0.3 180 524,880
Apr. 24, 2003 B3 92 12 700 0.1 90 145,150
Apr. 24, 2003 C3 94 18.5 1,000 0.08 180 525,312
Fig. 6. NSGA algorithm
( 92 )
fitness value, which is proportional to the population size, to provide an equal reproductive potential for
these individuals). To maintain the diversity of the
population, these classified individuals are shared
with their dummy fitness values. Then this group of classified individuals is ignored and another layer of nondominated individuals is considered. The process
continues until all individuals in the population
are classified. Stochastic remainder proportionate
selection is adopted for this technique. Since
individuals in the first front have the maximum
fitness value, they always get more copies than the rest of the population. This allows for a better search
of the PFknown regions and results in convergence
of the population toward such regions. Sharing, by
its part, helps to distribute the population over this
region (i.e., the Pareto front of the problem). The
NSGA was relatively successful over the course
of many years (Weile, 1996, Blumel, 2000, Reed,
2001), and the NSGA was also a highly inefficient algorithm because of the way in which it classified individuals.
3. RESULTS AND DISCUSSION
Optimization models for Eco-Friendly flushing operation generally consist of an objective function,
constraints and an optimization technique. In
this paper, the ecological flow constraint and its
improvement as compared to the previous studies
are highlighted. According to the core function
of a reservoir, a) Minimization of irrigation
deficits, b) Maximization of sediment evacuated,
c) Minimization of out flowing water volume d)
Maximization of power generated, could be used as
the objective function in the model. Assignment of
priority weight to individual objective depends on
policy of the reservoir operation. A multi-objective
optimal operation model of water-sedimentation
in Dez Hydropower reservoir is established to
coordinate Maximization of sediment evacuated
and Minimization of out flowing water volume and
improve the comprehensive benefits of reservoirs.
opt E = {Max∑t = 1 V(so)t , Min∑t = 1 V(o)t} (4)
where E is the comprehensive benefits; V(so)t is
outflowing sediment volume during flushing in time interval t ; V(o)t is outflowing water volume in time interval t ; T is the total number of time intervals.
The optimization is carried out under the following
two constraints which are incorporated in NSGA
by the penalty factor method. General descriptions
on constraints can be found in Atkinson (1996) and
Kawashima, (2003) for Existing flushing criteria
and Khakzad (2015) for Ecological flow constraints.Criteria for determining whether flushing at a
particular reservoir will be successful are required.
There are two key requirements for effective
flushing. First, the sediment quantities transported
through the low level outlets during flushing are
sufficient to enable a long term balance between
the sediment inflow and the sediment flushed, and
second, the volume of deposits remaining in the
reservoir after a sediment balance has been achieved
is sufficiently small to enable a specified storage
requirement to be met. These criteria depend on
the hydraulic efficiency of flushing. By applying
these criteria, reservoirs at which flushing might be viable can be identified. The hydraulic efficiency
of flushing can be defined in several ways. Some
definitions are shown in Table 2 ( Khakzad, 2014).In this paper, we concerned the sediment
balance and the ratio between useful storage
capacity that can be maintained in reservoir and a
substantial proportion of the original capacity, as
criteria to predict the feasibility of flushing sediment from reservoirs. For this purpose, the main criteria
such as the sediment balance ratio (SBR), the long
term capacity Ratio (LTCR), the draw down ratio
(DDR), flushing width ratio (FWR), reservoir top
width ratio (TWR), capacity inflow ratio (C/I) and sediment potential (SP) are used. These criteria
are defined as the following (Atkinson 1996,
Kawashima. S., 2003):
( 93 )
SBR = ediment mass flushed annually
sediment mass depositing annually > 1
(5)
LTCR = sustainable capacity
original capacity > 0.35 (6)
DDR = 1 ‒ flow depth for the flushing water level
flow depth for the normal impounding level > 0.7 (7)
FWR = predicted flushing width
representative bottom width of reservoir > 1 (8)
TWR = top width of scoured valley
actual top width ~ 1 (9)
SP = Mean annual sediment inflow
Original storage capacity > 1 (10)
Following our previous research (Khakzad,
2015), which evaluated effect of sediment on
aquatic ecosystems using Decision tree forest (DTF)
and Group method of data handling (GMDH) for
198 data about aquatic ecosystem, we propose,
in this study, scale of the severity (SEV) of ill
effect for fishes for Ecological flow constraints.
This is more complicated than the conventional
reservoir operation that does not consider ecological
flow requirement or only considers a constant
minimum flow. Equation 11-15 show SEV base on concentration of suspended sediment, species, life
stage and duration of exposure.
SEV (For Adult salmonids and rainbow smelt) = Log concentration (mg/L) × ‒0.8697 + Log concentration (mg/L) × Log Exposure duration (h) × 0.4377 + Log Exposure duration
(h) × 3.886 (11)
MAE = 0.3781 RMSE = 0.4465 R2 = 0.9883
SEV (For Juvenile salmonids) = 15.28 + Log concentration (mg/L) × ‒2.415 + Log
concentration (mg/L) × Log Exposure duration
(h) × 0.0543 + Log concentration2 (mg/L) ×
0.2024 + Log Exposure duration (h) × ‒0.6366 + Log Exposure duration2 (h) × 0.0442 (12)
MAE = 0.7787 RMSE = 0.9875 R2 = 0.8214
SEV (For Salmonid eggs and larvae) = 4.665
+ Log concentration (mg/L) × 0.7655 + Log
Exposure duration (h) × 0.7376 (13)
Table 2. Different definitions of flushing efficiency
Efficiency expression Author
E = Vo / Vd Qian (1982)
E = Lo / Li Ackers et al. (1987)
E = (V2 ‒ V1) / Vo Mahmood (1987)
E = (V2 ‒ V1) / Vori Mahmood (1987)
E = Tr / (1 ‒ Tf ) Mahmood (1987)
E = Lo / Ld Atkinson (1996)
E = (Vso - Vsi) / Vo Lai et al. (1996)
E = (VoCo ‒ ViCi) / (ρVo) Morris et al. (1997)
Ci is total sediment concentration of inflow [kg m‒3] Vd is volume of deposit flushed out [m3] Co is total sediment concentration of outflow [kg m‒3] Vi is inflowing water volume [m3]E is flushing efficiency Vo is outflowing water volume [m3]Ld is annual quantity of sediment deposited [kg] Vori is original live capacity of the reservoir [m3]Li is annual quantity of sediment inflow [kg] Vso is outflowing sediment volume during flushing [m3]Lo is annual quantity of sediment flushed out [kg] Ssi is inflowing sediment volume during flushing [m3]Tf is fraction of year used for flushing V1 is storage capacity of reservoir before flushing [m3]Tr is fraction of year that the river’s sediment load will V2 is storage capacity of reservoir after flushing [m3]take to refill V2
‒ V1 ρ is bulk density of deposit [kg m‒3]
( 94 )
MAE = 0.4412 RMSE = 0.5634 R2 = 0.9246
SEV (For Juvenile salmonids) = ‒12.81 + Log concentration (mg/L) × 9.677 + Log
concentration (mg/L) × Log Exposure duration
(h) × 0.4975 + Log concentration2 (mg/L) ×
‒1.006 + Log Exposure duration (h) × ‒2.402 (14)
MAE = 0.6866 RMSE = 0.7934 R2 = 0.9620
SEV (For Adult nonsalinonids) = 15.94 + Log concentration‒1 (mg/L) × ‒108.1 + Log
concentration (mg/L) × Log Exposure duration
(h) × ‒0.0694 + Log concentration‒1 (mg/
L) × Log Exposure duration (h) × 8.871 + Log concentration‒1 (mg/L) × Log Exposure duration‒1 (h) × 195.7 (15)
MAE = 0.9787 RMSE = 1.273 R2 = 0.6398
The Dez river provides fish habitat and supports commercial (market), subsistence and recreational
fisheries. A list of economically important fish
species found along the Dez river downstream of Dez
dam are listed in Table 3. Local fishermen indicate that high suspended sediment during flood seasons reduces a catch substantially because fish abandon their usual locations and cannot be found and also
that the likelihood of damaging nets is higher during
high turbidity events. This is consistent with the
responses from fishermen the day following flushing is that the fish was not biting or that only small fish was being caught in the nets.
Turbidity current sediments accumulate at the
dam could be flushed downstream during operations of the existing powerhouse, spillway facilities and
low-level outlets (Figure 7). The historical outflows experienced from powerhouse, spillway facilities
and low-level outlets are 200 (m3/s), 80 (m3/s) and
150 (m3/s) respectively. In Dez Hydropower, it is
provided with three low-level outlets within the dam
body. The original purpose of the low-level outlets
was to provide irrigation releases downstream
during periods of low flow through the turbines. In addition, these outlets were to provide a means of
Table 3. Fish species in the downstream of Dez dam
Scientific Name English Name Farsi Name
Aspius vorax Mesopotamian asp Shelej
Barbus esonicus Tigris Salmon Ghonreh, Bej, Song
Barbus grypus Large-scaled Barb Shirbot, Shebbot, Sorkheh
Barbus luteus Golden Barb Hamri, Zardak, Orange Zangool
Barbus pectoralis Levantine barbel Barzam, Nabash
Barbus sharpeyi Binni Benni
Barbus subquincunciatus Black Spot Barb Soleimani, Barzam-e-Khaldar
Capoeta damansara n/a Toini, Gel Khorak
Capoeta trutta Long-spine scraper Toini
Carassius auratus Goldfish Kapourche, Mahie Dehghan
Chalacaburuns mossulensis n/a Shah Kolie Jonoubi
Chondrostoma regium Mesopotamian nase Nazok
Cyprinion kais Kais kingfish, smallmouth lotak Botak-e-Dahan Koochak
Cyprinion Macrostomum Large-mouthed Barb Botak-e-Dahan Bazorg
Silurus triostegus Mesopotamian Catfish Esbele, Yari
Heteropneustes fossilis Stinging catfish Shlambo, Doodeh
Liza abu Abu Mullet Biah, Zoory, Shouchi
Tenualosa ilisha Ilisha, Hilsa Shad Shobour, Zabour
( 95 )
emergency release from the reservoir as required.
Based on recent studies, the acceptable sediment
concentrations downstream of the spillway can be
maximum 15,000 (mg/L) (Khakzad, 2015).
The parameters of NSGA for optimization of
flushing operation were set as follows: Maximum
Number of Iterations = 100, Population Size = 50,
Crossover Percentage = 0.7, Mutation Percentage
= 0.4 and Mutation Rate = 0.02. These parameter
settings are regarded as optimal to the standard
NSGA algorithms. Figure 8 and 9, present the
Pareto-optimal front of NSGA for Scenario 1 (for
Fig. 7. General layout of powerhouse, spillway facilities and low-level outlets.
Fig. 8. Pareto-optimal front for Scenario 1.
( 96 )
protecting Eggs & early life stages salmonids) and
Scenario 2 (for protecting Adult non-salmonids).
With help of Figure 8 and 9, assuming of a given
defined total volume of water passed per flush (m3),
total volume of sediment passed per flush (m3)
could be determined in Dez Hydropower reservoir.
Table 4, 5 present the results of optimization of
Eco-friendly flushing operation in Dez Hydropower reservoir for acceptable sediment concentrations
downstream of the spillway 8,000 (mg/L), 1,000
(mg/L), 15,000 (mg/L). Total volume of water
passed per flush (m3) were considered maximum
30000000 (m3) for Scenario 1 (for protecting Eggs
& early life stages salmonids) and 45000000 (m3)
for Scenario 2 (for protecting Adult non-salmonids).
As most fish in the Dez River spawn in March or April, the most conservative of the eggs and
larvae or the adult graphs should be employed from
March through June (Scenario 1) and the adult
graphs throughout the rest of the year (Scenario 2).
Results of the proposed framework to optimize of
flushing operation showed that this method provides a powerful tool for the selection of optimum
response scenario against the identified risks and
can be an important instrument for change in quality
of sediment management.
4. SUMMARY AND CONCLUSIONS
There is an increasing attention turning towards
river ecosystem conservation in Iran due to the
massive dam constructions and reservoir regulations.
Releasing ecological flow to the downstream
has gradually reached a consensus in reservoir
operations. In this study, Non-dominated Sorting
Genetic Algorithm (NSGA) was used successfully
to optimize flushing operation in Dez Hydropower reservoir and to evaluate the derived prediction
model. This study is based on Maximization of
sediment evacuated and Minimization of out flowing water as objectives and Existing flushing criteria and Ecological flow as constraints. All of the scenarios proposed in this study improve sediment evacuation
and thus the enhanced sustainability of the reservoir.
Computational results show that NSGA algorithm is
capable of quickly obtaining high-quality solutions
for multiple objectives knapsack problems and
that allowed establishing an objective quantitative
Fig. 9. Pareto-optimal front for Scenario 2.
( 97 )
Table 4. Results of Acceptable single flushing time (hrs) for Scenario 1
SenariosAcceptable Single Flushing Time (hrs)
for different outflow (m3/s)Total volume of water passed
per flush (m3)Total volume of sediment
passed per flush (m3)
Scenario 1 (for protecting Eggs & early life stages
salmonids)
Acceptable sediment concentration downstream of the spillway =
8,000 (mg/L)Day 1 (T = 2.90 (h), Q = 350 (m3/s))Day 2 (T = 2.90 (h), Q = 280 (m3/s))Day 3 (T = 3.15 (h), Q = 350 (m3/s))Day 4 (T = 3.15 (h), Q = 350 (m3/s))Day 5 (T = 3.15 (h), Q = 280 (m3/s))Day 6 (T = 3.15 (h), Q = 200 (m3/s))
19967239 474894
Acceptable sediment concentration downstream of the spillway =
10,000 (mg/L)Day 1 (T = 2.90 (h), Q = 430 (m3/s))Day 2 (T = 2.90 (h), Q = 350 (m3/s))Day 3 (T = 2.90 (h), Q = 200 (m3/s))Day 4 (T = 3.15 (h), Q = 350 (m3/s))Day 5 (T = 3.15 (h), Q = 280 (m3/s))Day 6 (T = 3.15 (h), Q = 200 (m3/s))Day 7 (T = 3.15 (h), Q = 200 (m3/s))Day 8 (T = 3.54 (h), Q = 200 (m3/s))
24469490 579309
Acceptable sediment concentration downstream of the spillway =
15,000 (mg/L)Day 1 (T = 2.90 (h), Q = 280 (m3/s))Day 2 (T = 2.90 (h), Q = 200 (m3/s))Day 3 (T = 3.15 (h), Q = 430 (m3/s))Day 4 (T = 3.15 (h), Q = 350 (m3/s))Day 5 (T = 3.15 (h), Q = 280 (m3/s))Day 6 (T = 3.15 (h), Q = 280 (m3/s))Day 7 (T = 3.15 (h), Q = 280 (m3/s))Day 8 (T = 3.54 (h), Q = 280 (m3/s))
29223193 636579
Table 5. Results of Acceptable single flushing time (hrs) for Scenario 2
SenariosAcceptable Single Flushing Time (hrs)
for different outflow (m3/s)Total volume of water passed
per flush (m3)Total volume of sediment
passed per flush (m3)
Scenario 2 (for protecting Eggs & early life stages
salmonids)
Acceptable sediment concentration downstream of the spillway =
8,000 (mg/L)Day 1 (T = 5.99 (h), Q = 430 (m3/s))Day 2 (T = 5.99 (h), Q = 280 (m3/s))Day 3 (T = 5.99 (h), Q = 200 (m3/s))Day 4 (T = 6.67 (h), Q = 430 (m3/s))Day 5 (T = 6.67 (h), Q = 350 (m3/s))Day 6 (T = 7.76 (h), Q = 280 (m3/s))
33603560 820255
Acceptable sediment concentration downstream of the spillway =
10,000 (mg/L)Day 1 (T = 5.99 (h), Q = 350 (m3/s))Day 2 (T = 5.99 (h), Q = 200 (m3/s))Day 3 (T = 6.67 (h), Q = 350 (m3/s))Day 4 (T = 6.67 (h), Q = 280 (m3/s))Day 5 (T = 6.67 (h), Q = 280 (m3/s))Day 6 (T = 7.76 (h), Q = 280 (m3/s))
39287341 886628
Acceptable sediment concentration downstream of the spillway =
15,000 (mg/L)Day 1 (T = 5.99 (h), Q = 430 (m3/s))Day 2 (T = 5.99 (h), Q = 350 (m3/s))Day 3 (T = 5.99 (h), Q = 280 (m3/s))Day 4 (T = 5.99 (h), Q = 200 (m3/s))Day 5 (T = 6.67 (h), Q = 430 (m3/s))Day 6 (T = 6.67 (h), Q = 280 (m3/s))
44200594 1141134
( 98 )
re la t ion be tween Technica l and execut ive
requirements and Environmental impacts. Although
in this study, the model has only been applied in Dez
dam Hydropower reservoir, its generic formulation
allows the application of which to a broad range of
reservoirs to extend their useful life.
REFERENCES
Ackers P. and Thompson G., 1987. Reservoir sedimentation and influence of flushing. Sediment Transport in Gravel-bed Rivers, C. R. Thorne, J. C. Bathurst, and R. D. Hey, eds, John Wiley & Sons, Chichester, pp. 845-868.
Atkinson, E. 1996. The feasibility of flushing sediment from reservoirs. HR Wallingford, UK. Report no. OD 137. pp21.
Blumel A. L., Hughes E. J., and White B. A., 2000. Fuzzy Autopilot Design using a Multiobjective Evolutionary Algorithm. In 2000 Congress on Evolutionary Computation, volume 1, pages 54-61, Piscataway, New Jersey, IEEE Service Center.
Chen, H. W. and Chang, N.-B., 1998. Water pollution control in the river basin by fuzzy genetic algorithm-based multi-objective programming modeling. Water Science and Technology, 37(8): 55-63.
Coello Coello Carlos A., Lamont Gary B. and Van Veldhuizen David A., 2007. Evolutionary Algorithms for Solving Multi-Objective Problems. Springer Science.
Dezab Consulting Engineers in association with ACTRES international, 2004. Dez Dam Rehabilitation Project Contract No. 81-5M334.
Fruchart F., 2008. Why and how to flush a reservoir without environmental impacts. Regional Workshop on Discharge and Sediment Monitor ing and Geomorphological Tools for the Lower-Mekong Basin Vientiane, Lao PDR, 21-22 October 2008. 33 pp.
Katsifarakis K. L., 2012. Hydrology, hydraulics and water resources management; a heuristic optimization approach.. WIT Press.
Kawashima, S., T. Johndrow, G. Annandale, and F. 2003. Shah Reservoir Conservation Volume II: The RESCON Model & User Manual, Washington, D.C.: World Bank.
Kellerer, Hans, Pferschy, Ulrich, Pisinger, David, 2004. Knapsack Problems. ISBN 978-3-540-40286-2. Springer.
Khakzad Hamid and Elfimov V.I 2014. Evaluation of flow regime of turbidity currents entering Dez Reservoir using extended shallow water model, Water Science &
Technology 7(03): 267-276.Khakzad H., Elfimov V. I., 2014. An Alternative Approach
to Assessing Feasibility of Flushing Sediment from Reservoirs. Proceedings of Moscow State University of Civil Engineering. No 6. С. pp 126-136.
Khakzad H., Elfimov V. I., 2015. Evaluation of effect of sediment on aquatic ecosystems using decision tree forest and group method of data handling. Water Quality. Vol 50 No 2 pp 123-139.
Khakzad Hamid and Elfimov V. I., 2015. A Review of Environmental Characteristics and Effects of Dez Dam Flushing Operation on Downstream, Environmental Practice 17(03): 211-232.
Khuzestan Water and Electricity Organisation (KWEO), 2003. Turbidity Current Measurement in Dez Dam Reservoir.
Lai J. S. and Shen H. W., 1996. Flushing sediment through reservoirs. Journal of Hydraulic Research, Vol. 34(2), pp. 237-255.
Mahmood K., 1987. Reservoir Sedimentation: Impact, Extent, and Mitigation. World Bank Technical Paper Number 71, Washington, D.C.
McCartney M. P., Sullivan C., Acreman M. C., 2001. Ecosystem impacts of large dams. Background Paper Nr. 2 Prepared for IUCN (International Union for Conservation of Nature and Natural Resources), Gland, Switzer land; UNEP (Uni ted Nat ions Environmental Programme), Nairobi, Kenya; and WCD (World Commission on Dam). 82 pp.
Morris, G., and J. Fan., 1997. Reservoir Sedimentation Handbook; design and management of dams, reservoirs and watersheds for sustainable use. McGraw Hill New York.
Nikolaos P. E. Sebastian Palt, George W. Annandale, Pravin Karki, 2017. Reservoir Conservation Model Rescon 2 Beta. International Bank for Reconstruction and Development / The World Bank.
Qian N., 1982. Reservoir sedimentation and slope stability; technical and environmental effects. Fourteenth International Congress on Large Dams, Transactions, Rio de Janeiro, Brazil, 3-7, Vol III, pp. 639-690.
Rauschenbach T. , 2016. Modeling, Control and Optimization of Water Systems Engineering. Methods for Control and Decision Making Tasks. Springer-Verlag, Berlin, Heidelberg.
Reed P. M., Minsker B. S., and Goldberg D. E., 2001. Designing a New Elitist Nondominated Sorted Genetic Algorithm for a Multiobjective Long Term Groundwater Monitoring Application. In Proceedings of the 2001 Genetic and Evolutionary Computation Conference. Late-Breaking Papers, pages 352-358, San Francisco, California.
Sloff C. J., 1991. Sedimentation in Reservoirs. Ph.D.
( 99 )
Thesis, Report no. 97-1, Communications on Hydraulic and Geotechnical Engineering, Delft Univers i ty of Technology, Facul ty of Civ i l Engineering.
Srigiriraju, K. C., 2000. Noninferior Surface Tracing Evolutionary Algorithm (NSTEA) for Multi Objective Optimization. Master's thesis, North Carolina State University, Raleigh, North Carolina.
Uslaender, T., 2010. Service-oriented Design of Environmental Information Systems. Ph.D. Thesis,
Karlsruhe Institute of Technology (KIT), Karlsruhe.Weile D. S., Michielssen E., and Goldberg D. E., 1996.
Multiobjective synthesis of electromagnetic devices using nondominated sorting genetic algorithms. In 1996 IEEE Antennas and Propagation Society International Symposium Digest, volume 1, pages 592-595, Baltimore, Maryland, July.
Received: 108/04/30
Revised: 108/05/14
Accepted: 108/06/17