Next Article in Journal
The Association of Drought with Different Precipitation Grades in the Inner Mongolia Region of Northern China
Previous Article in Journal
Functional Diversity of Macroinvertebrate Communities in River Nature Reserves of Spain
 
 
Font Type:
Arial Georgia Verdana
Font Size:
Aa Aa Aa
Line Spacing:
Column Width:
Background:
Article

A Hybrid Fuzzy Evaluation Method for Quantitative Risk Classification of Barrier Lakes Based on an AHP Method Extended by D Numbers

1
Changjiang Survey, Planning, Design and Research Co., Ltd., Wuhan 430000, China
2
Changjiang Institute Geoscience, Ministry of Water Resources, Wuhan 430011, China
3
Changjiang International Engineering Co., Ltd., Beijing 100032, China
*
Author to whom correspondence should be addressed.
Water 2024, 16(22), 3291; https://doi.org/10.3390/w16223291
Submission received: 20 August 2024 / Revised: 6 November 2024 / Accepted: 12 November 2024 / Published: 16 November 2024

Abstract

:
The risk classification of barrier lakes is the key to conducting emergency treatment in a scientific manner. However, risk classification faces difficulties such as a short time for risk evaluation, complex evaluation indicators, difficulty in obtaining information quickly, and quantifying index weights. Based on this, this paper constructs a quantitative risk classification model for barrier lakes based on D-AHP. On the basis of studies on nearly 100 cases of barrier lakes, an eight-factor evaluation index system and quantitative classification are proposed. The methods of rapid calculation of reservoir capacity curve of barrier lakes and intelligent identification of particles on the surface of barrier bodies were developed, which realized the rapid acquisition of eight-factor evaluation index information in an emergency environment. The D-AHP method dealt with inconsistent weight assignment to evaluation factors by experts, which helped achieve weight quantification of eight factors. The risk assessment on 15 barrier lakes such as Tangjiashan barrier lake shows that the conclusions drawn for the risk classification method proposed in this paper are basically consistent with those of the traditional table-lookup method. However, the table-lookup method ignores cumulative loss impacts on the risk level of barrier lakes and considers the extremely severe loss of barrier lakes as a sufficient condition for the evaluation level to be grade I, and thus a deviation in the evaluation. The risk classification method proposed in this paper is more reasonable and reliable.

1. Theoretical Background

A barrier lake is a natural damming of a river by collapse or slide of the bank slope of the river valley, which happens worldwide [1] (Figure 1). Such dammed lakes flood upstream areas and damage the critical infrastructures as well as lives and properties of residents downstream in cases of collapse. In 2000, a large landslide occurring along Yiong Tsangpo River created a barrier lake 54 m in length, 2500 m in width, 288 × 108 m3 in storage capacity, and 2.8 × 108~3.0 × 108 m3 in volume, endangering several million residents downstream [2,3]. The Wenchuan Earthquake in 2008 (Figure 2a) induced 257 barrier lakes, of which the largest was Tangjiashan barrier lake, threatening 1.3 million residents downstream. As a result, 275,000 residents were relocated [4,5]. Another case was the barrier lake dammed by a landslide on Bailong River caused by the sudden extraordinary rainstorm in the northern hilly area of Zhouqu County, Gansu Province, in 2010, killing 1799 people. The landslide (Figure 2b) in Baige village upstream of the Jinsha River in 2018 shaped a large barrier lake with a maximum reservoir volume of 760 million m3 and resulted in the relocation of 85,000 residents and direct economic loss of CNY 13.5 billion [6,7,8].
Studies on 73 barrier lakes by Costa and Schuser from the United States Geological Survey (USGS) demonstrated that 85% of the lakes lasted less than 1 year. A case study was done on 352 barrier lakes which have collapsed, with statistics showing 84.4% of the lakes existed less than 1 year, 68.2% of them with lifespans shorter than 1 month and 29.8% collapsing within one day. Peng and Zhang [9] and Shen et al. [10] also found similar statistical results based on 204 and 352 cases, respectively. Given such diversity in the duration of existence of barrier lakes and short time for emergency relief, scientific risk classification is critical for targeted and well-organized emergency response. Risk Management-Risk Assessment Techniques [11] defines risk as uncertainties confronted by an organization in accomplishing its targets. Identification of risks indicates evaluation of risk types, probability, and impact. Generally, the risk can be expressed as the risk probability (P) of an incident multiplied by the consequences (C) of such an incident, based on which the risks of barrier lakes can be expressed as R = PC, where R indicates risks of barrier lakes, P indicates the probability of dam failure, and C indicates the consequences of dam failure. P is mainly about the hazards of the barrier lakes; the larger the hazards, the higher the probability of dam failure. C mainly includes the damages caused by the barrier lake as well as floods due to dam failure.
The stability of a barrier dam is subject to several factors. Based on a database of 70 barrier dam cases collected in the northern Apennines, Casagli et al. [12] proposed the blockage index (BI) to evaluate barrier dam stability with barrier dam volume Vd and catchment area AL as input parameters. Based on the BI methodology, Ermini et al. [13] further introduced barrier dam height Hd into the BI method and proposed a new dimensionless blockage index (DBI). Based on 43 barrier dam cases in Japan, Dong et al. [14] proposed a quantitative risk assessment method for barrier dams with inflow water volume from upstream and barrier dam height, width, and length selected as input parameters. Subsequently, based on 300 cases in Italy, Stefanelli et al. [15] identified the hydromorphological dam stability index (HDSI), with barrier dam volume and catchment area as input parameters. Based on 79 barrier dam occurrences, Shi et al. [16,17] proposed a quantitative method to evaluate barrier dam stability in which five parameters were adopted as input parameters: barrier dam height, width, and length; dammed lake volume; and backwater length. All the parameters selected by the above-mentioned scholars fall into two categories, i.e., lake volume relevant and barrier dam relevant, as shown in Table 1.
Breaches of barrier lake dams bring a long disaster chain and induce disasters of a large scope. Studies show that the loss caused by failure of landslide barriers is similar to that of regular dams, including loss of lives, economy, and ecology. Assessments of life loss take into account such factors as the population at risk, population density, level of flooding, understanding of residents, timing of alarm, rate of young adults to the elderly and kids, time of dam failure, weather, distance to dam site, emergency response plan, dam height, reservoir volume, downstream river slope, topography, impact resistance of structures, temperature, rescue capability, etc. [3,18,19]. Major factors for economic loss include duration of floods, velocity of floods, sediment concentration, flood water temperature, depreciation of properties, timing of alarm, pollutant concentration, etc. [20,21,22,23]. Ecological loss is mainly assessed based on factors including geomorphology of the river channel; water environment; human ecology; natural reserves; damage to animal species; soil environment; vegetation coverage; reduction in agricultural, forestry, and fishery production; air quality; and dirty industries [24,25,26]. The factors for assessment of barrier dam failure are demonstrated in Table 2.
Proper allocation of weight to each factor is the key to risk assessments of barrier lakes [27,28,29]. AHP is a multi-criteria decision-making method combining qualitative and quantitative analyses while remaining simple and practical. However, there are still some deficiencies and limitations when applying this methodology. First, the comparative judgments are subjective because they rely heavily on expert opinion, which may sometimes cause inconsistency. Furthermore, AHP lacks the ability to adequately cope with any inherent uncertainty and imprecision in the data. Finally, in a real situation, an expert may have limited knowledge of and experience with alternatives; the preferred information may contain fuzziness and incompleteness, and AHP is unable to handle this incomplete information. In the actual risk classification of barrier lakes, the following situations often occur. Occasion 1: All 10 experts consider factor 1 more important than factor 2. Eight of them assigned a weight score of 0.8 to factor 1. However, the other two experts assign a weight score of 0.7 to factor 1. Occasion 2: Seven experts out of ten consider factor 1 more important than factor 2 and allocate a weight score of 0.6 to factor 1. However, the other three regard both factors as equally important. Occasion 3: Eight experts out of ten consider factor 1 more important than factor 2 and allocate a weight score of 0.7 to factor 1. However, the other two give no comment on either factor since they do not have a deep understanding of them. The D-AHP method can represent uncertain information more effectively because it overcomes the shortcomings and deficiencies of the traditional AHP and Dempster–Shafer theories. First, the D-AHP method uses a D numbers preference relation instead of a pairwise comparison; the D numbers preference relation is the classical fuzzy preference relation extended by D numbers. Although the preference relations of the alternatives or criteria given by the experts are imprecise, fuzzy, and incomplete, the D numbers preference relation can effectively express this uncertain information without causing inconsistency. Furthermore, the sum of all focal elements in a D numbers preference relation need not equal 1; i.e., if the assessment information given by experts is incomplete, this value may be less than 1. In view of these advantages of D-AHP, this paper uses the D-AHP method instead of the traditional AHP method to determine the weight distribution of the evaluation index [30,31,32].
Based on previous studies globally on the risk assessment of barrier lakes, in Section 2, a mathematical model is proposed for quantitative risk classification of barrier lakes based on D-AHP with a set of risk evaluation factors, a quick information acquisition method, and risk classification quantification functions. Section 3 presents the set of risk evaluation factors as well as standards for classification based on studies on about 100 barrier lake cases and domestic studies in China, solving the problem of complex evaluation indicators on the risk evaluation of barrier lakes. The proposed set of factors identifies proper ones amid a huge pool of factors and has been included in the Code for Risk Classification and Emergency Measures of Barrier Lake [33]. In Section 4, an elaboration is presented on the calculation method of the storage capacity curve and intelligent identification of particles on the surface of the dam. Such a method would allow for quick acquisition of information during an emergency rescue. A topographic database was constructed through data overlay and dynamic checking based on information obtained through topographic mapping, IEM modeling, multispectral data, RADAR data, and 3D topographic mapping, and the storage capacity curve of a barrier lake can be calculated based on this topographic database. A qualitative analysis was carried out on material components of barriers through the provenance methodology. Surface particles in a barrier dam were identified through the intelligent identification methodology. The diameters of particles in a barrier dam were calculated based on longitudinal profile data through a natural source surface wave. A grading curve for particles in a barrier dam was produced based on the above-mentioned data. Section 5 and Section 6 elaborate in details on the preference relation matrix and the calculation of a weight indicator based on D-AHP, solving the problem of quantifying weights for evaluation factors. In Section 7, the application of such a method on 15 barrier lake cases demonstrates that the proposed method is more scientific and reliable and shall be promoted for further application.

2. Mathematical Model for Quantitative Risk Classification of Barrier Lakes Based on D-AHP

2.1. The Mathematical Model

The mathematical model for quantitative risks classification of barrier lakes based on D-AHP is shown in Figure 3. The model comprises three parts:
(1) Objective function;
(2) Datasets for modeling, including a set of evaluation factors, a set of evaluation grades, and a set of information collection methods ensuring proper selection of factors, risk classification, and quick acquisition of information.
(3) Risk classification quantification functions for modeling, including D-AHP preference relation calculation function, weight calculation function, and fuzzy functions, ensuring quantification of the weight vector and risk classification.
Explanation of symbols in the mathematical model in Figure 3:
  • U is the set of factors for risk classification of barrier lakes; D is the set of factors for hazards evaluation of the barrier with m elements, namely, d1, d2,……, dm; and L is the set of factors for the assessment of loss by dam failure with n elements, namely, l1, l2,……, ln.
  • V is the set of evaluation grades with P elements, namely, v1, v2,……, vp.
  • F is the set of information collection methods, with m+n elements, F1, F2,……, Fm + n, which is in compliance with the m elements in set D and information collection methods for number of n in set L.
  • R is the reference matrix of set U to set V. rik indicates the preference relation of the i-th parameter to the k-th evaluation grade; the range [αik, αik + 1] means the range corresponding to the k-th evaluation grade; xi is the i-th parameter. W is the weight vector of U for the set of factors for the risk classification of barrier lakes. f1() is the weight calculation function on the basis of D-AHP; G indicates the vector of evaluation grades, with p elements, g1, g2,……, gp; and max() is the function for maximum value.

2.2. Solution Using the Model

The solution using the model follows five procedures (see Figure 4) as follows:
(1) To establish set U, set D was the factors for risk classification, and set L was the factors for loss assessment. (2) Set V was built on evaluation grades to identify risk levels (grade I, II, III, etc.) of barrier lakes. (3) The fuzzy preference relation matrix R was established. Elements in the matrix indicate the preference relation of a certain parameter to its risk grade. (4) The weight vector W was calculated. The calculation of the weight vector on evaluation parameters was based on the following procedure: ① Establishment of the D numbers preference relation matrix (D Matrix); ② conversion of the D matrix into a crisp matrix; ③ establishment of a probability matrix based on the crisp matrix; ④ ranking of the parameters with the triangle method; and ⑤ calculation of the weight vectors of the parameters. (5) The risk grade evaluation function grade() was calculated based on R, the fuzzy preference relation matrix, and weight vector W, thus resulting in the risk grade of barrier lakes.

3. Selection and Grading of Risk Evaluation Factors

3.1. Selection and Grading of Risk Evaluation Factors for Barrier Dams

In accordance with the studies worldwide, the risk evaluation factors can be categorized into two groups: reservoir-volume-related factors and dam-body-related factors (see Table 1). The former group mainly includes the reservoir volume and inflow from upstream, both of which directly influence the damage to the barrier body by floods in case of breaching. The latter group mainly comprises the material component and geometry of the dam body. The larger the particles in the dam, the better it works against flushing; the lower the dam, the longer distance the water flows, the smaller potential energy the water flow takes, and the less risk. These four factors, reservoir capacity, inflow from upstream, material component, and geometry of the barrier, are reasonable and feasible since they cover most risk evaluation factors adopted in current studies.
D = [d1,d2,d3,d4] = [reservoir capacity, inflow from upstream, material component, and geometry of the barrier]
This paper analyzes the relation between such factors and the grading of barrier risks based on studies of about 100 barrier lake cases.

3.1.1. Relation Between Reservoir Volume (d1) and Risk Grades

The paper studies the relation between reservoir volume and peak flooding upon dam failure based on the statistics of 86 cases showing a linear relation in which the larger the reservoir volume, the higher the flood peak upon dam failure, the more destructive the flood to the barrier, and the higher the risks of the barrier (see Figure 5). When the reservoir volume is smaller than 1 million m3, the peak flow at the breach is normally less than 1000 m3/s. When the reservoir volume is 1 million–10 million m3, the peak flow at the breach is normally 1000–3000 m3/s. When the reservoir volume is 10 million–100 million m3, the peak flow at the breach is normally 3000–10,000m3/s. When the reservoir volume is large than 100 million m3, the peak flow at the breach is normally larger than 10,000 m3/s. Therefore, barrier lakes and their risk grades can be categorized into four groups regarding their reservoir volume: less than 1 million m3/s (low risk), 1 million–10 million m3/s (moderate risk), 10 million–100 million m3/s (high risk), and more than 100 million m3/s (extra high risk).

3.1.2. Relation Between Inflow from Upstream (d2) and Risk Grades

This paper studies the relation between reservoir volume and peak flood upon dam failure based on statistics of 86 cases (see Figure 6). Generally, the inflow from upstream can be categorized into four ranges, and the risks of the barrier are categorized into four corresponding grades: (1) 17 cases had an upstream inflow of less than 10 m3/s, 12 of which were evaluated as low risk with a risk probability of 70.5%; (2) 17 cases had an upstream inflow of 10–50 m3/s, 11 of which were evaluated as medium risk with a risk probability of 62.5%; (3) 15 cases had an upstream inflow of 50–150 m3/s, 10 of which were evaluated as high risk with a risk probability of 64.7%; and (4) 23 cases had an upstream inflow of more than 150 m3/s, 15 of which were evaluated as extra high risk with a risk probability of 65.2%.

3.1.3. Relation Between Material Components of Barrier (d3) and Risk Grades

Studies on the breach and dam failure process show the following: (1) When the discharge is less than 10 m3/s, the velocity is less than 1–2 m/s, and the flow is able to flush clay particles and sand. (2) When the discharge is 10–50 m3/s, the velocity is about 1–2 m/s, and the water flow is able to flush rubble. (3) When the discharge is 50–150 m3/s, the velocity is about 2–3 m/s, and the flow is able to flush gravel. (4) When the discharge is 150–1000 m3/s, the velocity is about 3–6 m/s, and the flow is able to flush stones of a small size. (5) When the discharge is larger than 1000 m3/s, the velocity is about 6–10 m/s, and the flow is able to flush stones of all sizes. A study by Wang et al. [34] from the Institute of Mountain Hazards and Environment, Chinese Academy of Science, reveals that the average grain size of the barrier is explicitly influential on the features of dam failure. The larger the average grain size, the more capable the barrier is against flood flushing, and the smaller the probability of risk. Based on the above-mentioned studies and classification according to the Code for investigation of Geotechnical Engineering [35], the mid-value (d50) of the grain distribution curve of the barrier was selected as the eigenvalue to judge the barrier’s capability to resist flushing. The risk probability was graded as extra high, high, medium, and low when the eigenvalue was less than 2 mm, 2–20 mm, 20–200 mm, and higher than 200 mm, respectively.

3.1.4. Relation Between Geometry of Barrier (d4) and Risk Grades

We collected data on the length/height ratio (L/H) of 54 landslide barriers and studied its relation to the duration of barrier lakes (see Figure 7), showing the following: (1) When L/H ≤ 5, the barrier collapses after several days of overtopping. (2) When 5 < L/H < 20, the barrier lasts until it has been flushed for tens of days to several months. (3) When L/H ≥ 20, the barrier lasts for more than 1 year. Furthermore, the height of the barrier decides the potential energy of the water flushing. With reference to Design Code for Rolled Earth-rock Fill Dams [36], barriers can be categorized into four groups in terms of their height: less than 15 m, 15–30 m, 30–70 m, and more than 70 m. In consideration of the two factors above, the relation between geometry and risk grading of barriers can be seen in Figure 8.

3.2. Selection and Grading of Loss Evaluation Factors for Barrier Dams

Previous studies show that there are three main factors for loss evaluation due to dam failure: life loss, economic loss, and ecological loss (see Table 2). Life loss mainly indicates the population under barrier risks [37]. For example, Tangjiashan barrier lake threatens a population of 1.3 million downstream [5]. Economic loss mainly includes the loss of cities and towns downstream and loss of public facilities and infrastructures. For example, due to the collapse of the Baige barrier lake, 16 downstream villages and towns in four counties of Diqing and Lijiang were lost, 8051 houses collapsed, and there was damage to 18189 rooms. Loss in public facilities and infrastructures included damage to 632.12 km of road, 13 bridges flushed and destroyed, and 13 bridges damaged [6]. Ecological loss mainly included loss of ecological diversity, human ecology, the river channel, and the water environment [24]. Based on previous studies and a case study of about 100 barriers, evaluation factors for loss due to dam failure and grading methods (Table 3) were decided.
L = [l1,l2,l3,l4] = [population at risk, impacted cities and towns, impacted public facilities and infrastructures, impacted ecological environment]
The final eight selected factors are all based on Cole’s analysis of more than 100 barrier lakes globally (SL/T 450-2021) [33], which is the only official code for risk assessment of barrier lakes in China. Therefore, the reliability and validity are ensured. In Section 3.1, the hazards of barriers are graded using four levels: extra high, high, moderate, and low. In Section 3.2, the loss induced by dam failure is graded as extremely severe, severe, relatively severe, and moderate. Based on these two grading methods, the risk evaluation grades can be classified as grade I (extremely high), II (high), III (medium), and IV (low), as shown in Equation (3).
V = [v1,v2,v3,v4] = grade I, II, III, and IV

4. Information Acquisition for Risk Evaluation Factors

Quick acquisition of information is key for risk grading of barrier lakes under emergency circumstances within a short time frame. The information acquisition method for risk grading with eight factors is demonstrated in Table 4. (1) Capacity of barrier lake (d1) data can be acquired dynamically through predication of possible highest water level based on the capacity curve of the barrier lake (see Section 4.1). (2) Inflow from upstream (d2) data can be calculated based on runoff-yielding rules [38,39,40]. (3) Material components (d3) data can be calculated dynamically from multiple dimensions, including intelligent identification of surface particles, geophysical investigation of space-equivalent particles, tracing provenance analysis, etc. (see Section 4.2). (4) Geometry of the barrier (d4) data can be obtained through Boolean calculation based on oblique photography with UVA, LiDAR, satellite images, and multi-dimensional 3D modeling with DEM [41,42]. (5) Data on the population at risk (l1) can be acquired through quick identification technology based on LBS (Location-Based Services). (6) Data on impacted towns and cities (l2), impacted public facilities and infrastructures (l3), and impacted ecological environment (l4) can be acquired from corresponding government authorities based on a risk map of flooding induced by dam failure.

4.1. Acquisition of Information on the Capacity of a Barrier Lake (d1)

This paper builds up a topographic database for the Tangjiashan barrier lake and produces its capacity curve through overlaying; dynamic checking; elevation unification based on 1:50,000, 1:2000, and 1:5000 topographic maps acquired; 1:50,000 DEM data through remote sensing technology; multispectral data (8 m resolution, Beichuan county) and RADAR data (3 m resolution, barrier lake area); and a 3D topographic map acquired through an airborne LIDAR system. The highest water level for the Tangjiashan barrier lake is an elevation of 752 m, and its capacity (d1) is 316 million m3, as shown in the capacity curve. Figure 9 shows the process of the acquisition of d1.

4.2. Acquisition of Data on the Material Components of a Barrier Dam (d3)

A qualitative analysis was carried out on the material components of a barrier dam using the provenance methodology. Surface particles in a barrier dam were identified through an intelligent identification methodology. The diameter of particles in a barrier dam was calculated based on the longitudinal profile data through a natural source surface wave. A grading curve for particles in a barrier dam was produced based on the above-mentioned data. In accordance with such a calculation, the mid-value of the particle diameters for Tangjiashan’s material components was 83 mm, and the mid-value of the particle diameterfor Baige’s material components was 4.3 mm. Figure 10 shows the process of the acquisition of d3.

5. Solution to Preference Matrix (R)

5.1. The Range for Evaluation and Values of Parameters

As has been listed in Section 3, there are eight parameters for risk evaluation for barrier lakes, and each parameter evaluated has four ranges: [αi1 = 0, αi2 = 25], [αi2 = 25, αi3 = 50], [αi3 = 50, αi4 = 75], and [αi4 = 75, αi5 = 100]. Parameter d1 (capacity), d2 (inflow from upstream), d3 (geometry), d4 (material components of barrier dam), and l1 (population at risk) can be calculated through linear interpolation. This paper will demonstrate the calculation process of d1 (capacity) as an example. Parameter l2 (impacted cities and towns), l3 (impacted public facilities and major infrastructures), and l4 (impacted ecological environment) can be valued through quantifying the number of impacted cities/towns, facilities, and the environment. This paper will demonstrate the calculation process of l2.
(1)
Calculation of d1 (capacity)
1)
When 0 < d1 ≤ 100, x1 = 25 × d1/100;
2)
When 100 < d1 ≤ 1000, x1 = 25 + (50 − 25) × (d1 − 100)/(1000 − 100);
3)
When 1000 < d1 ≤ 10,000, x1 = 50 + (75 − 50) × (d1 − 1000)/(10,000 − 1000);
4)
When 10,000 < d1 ≤ 100,000, x1 = 75 + (100 − 75) × (d1 – 10,000)/(100,000 − 10,000);
5)
When 100,000 > d1, x1 = 100.
(2)
Calculation of l2 (impacted cities and towns)
1)
When the impacted area is residential areas within a village, x6 = 3 × l21 and x6 ≤ 25, l21 indicates the number of impacted villages and towns;
2)
When the impacted area is villages and towns, x6 = 25 + 3 × l21 and x6 ≤ 50;
3)
When the impacted area is county-level cities, x6 = 50 + 6 × l22 and x6 ≤ 75, l21 indicates the number of county-level cities and prefecture-level cities;
4)
When the impacted area is prefecture-level cities, x6 = 75 + 6 × l22 and x6 ≤ 100.

5.2. Function for Calculation of the Preference Relation

Calculation of the preference relation (rik) of i-th parameter to the k-th evaluation grade in the preference relation matrix R (8 × 4) is shown in Figure 11.

6. Calculating the Weights of the Indicators Based on the D-AHP Method

6.1. Definition of D Number

D numbers, first developed by Deng [43], are a good representation of uncertain information. They are widely used in many fields, such as supplier selection problems [44] and fault analysis [45].
Definition 1. 
Let Ω be a finite nonempty set. A D number is a mapping formulated by
D : Ω 0 , 1
B Ω D B 1   and   D Θ = 0
where  Θ  is an empty set and B is a subset of Ω.
From this definition, we notice that the completeness constraint is released if D numbers are used. If  B Ω D B = 1 , then the information is complete; and if  B Ω D B < 1 , the information is incomplete.
Suppose that the set Ω = {b1,b2,…,bibn}, where bi ∈ R and bibj if i ≠ j. Then, a special form of D numbers can be expressed as: D = b 1 , v 1 , b 2 , v 2 , , b i , v i , , b n , v n , where vi > 0 and i = 1 n v 1 1 .
Definition 2. 
Let  D = b 1 , v 1 , b 2 , v 2 , , b i , v i , , b n , v n  be a D numbers. The integration representation of D is defined as:
I D = i = 1 n b i v i
where, vi > 0, and  i = 1 n v 1 1 .

6.2. D Numbers Extended Fuzzy Preference Relation

The fuzzy preference relation is provided to construct pairwise comparison matrices based on expert judgment and is described by a fuzzy pairwise comparison with an additive reciprocal (rij + rji = 1) that is different from the multiplicative preference relation. rij denotes the preference degree of an alternative Ai over another alternative Aj and can be expressed as follows:
r i j = 0 A j   is   absolutely   preferred   to   A i 0 , 0.5 A j   is   preferred   to   A i   to   some   degree 0.5 indifference between   A i   and   A j 0.5 , 1 A i   is   preferred   to   A j   to   some   degree 1 A i   is   absolutely   preferred   to   A j
There are some shortcomings when using the fuzzy preference relation to represent certain situations. For example, if the expert assessments are uncertain or incomplete, it is difficult to construct the fuzzy preference relation. To overcome these shortcomings, Deng et al. [43] extended the classical fuzzy preference relation by using D numbers. The derived relation is called a D numbers preference relation, and the corresponding matrix is called a D numbers preference matrix, which can be abbreviated as a D matrix. The D matrix is defined as follows.
Definition 3. 
A D numbers preference relation RD on a set of alternatives A is represented by a D matrix on the product set A × A, whose elements are formulated by
R D : A × A D
The D numbers preference relation in matrix form is
  R D =   A 1 A 2 A n A 1 A 2 A n D 11 D 21 D n 1 D 12 D 22 D n 2 D 1 n D 2 n D n n
where  D i j = b 1 i j , v 1 i j , b 2 i j , v 2 i j , , b m i j , v m i j , {1,2,…,n},
D j i = 1 b 1 i j , v 1 i j , 1 b 2 i j , v 2 i j , , 1 b m i j , v m i j , i , j and bkij ∈ [0,1], ∈ {1, 2, …, m}.
Consequently, with the help of the D numbers preference relation, the preference relations of the three situations presented in Section 1 as an example are shown in Equations (10)–(12), respectively.
  R D 1 =   A 1               A 2 A 1 A 2 0.5 , 1.0 0.2 , 0.8 , 0.3 , 0.2 0.8 , 0.8 , 0.7 , 0.2 0.5 , 1.0
  R D 2 =   A 1                 A 2 A 1 A 2 0.5 , 1.0 0.4 , 0.7 , 0.5 , 0.3 0.6 , 0.7 , 0.5 , 0.3 0.5 , 1.0
  R D 3 =   A 1       A 2 A 1 A 2 0.5 , 1.0 0.2 , 0.8 0.7 , 0.8 0.5 , 1.0

6.3. Calculating Procedure of the Weights of Alternatives Using the D-AHP Method

The calculation process includes five steps: ① establish the D numbers preference matrix (D matrix); ② convert the D matrix to a crisp matrix; ③ construct a probability matrix based on the crisp matrix; ④ rank the alternatives using the triangularization method; and ⑤ calculate the relative weights of alternatives.

7. Case Application

Based on the D-AHP method, this paper calculates the risk level of 15 barrier lakes (see Figure 12): Jiguanling in Chongqing, Yigong in Tibet, Qingyandong in Chongqing, Houziyan in Dadu River, Hongshiyan in Niulan River, Tangjiashan in Sichuan, Jiala in Tibet, Baige in Jinsha River, Yankou in Guizhou, Shaziba in Hubei, Xiaojiaqiao in Sichuan, Tanggudong in Yalong River, Zhouqu in Gansu, Xiaogangjian in Sichuan, and Xujiaba in Sichuan.

7.1. Calculation of Matrix R

Based on the calculation formula in Section 5, eight evaluation indicators (see Table 5) were assigned, and the preference relation matrixes (see Table 6) were obtained for the 15 cases.

7.2. Calculation of Weight Vectors

The D numbers preference matrix (i.e., D matrix) must be constructed before calculating the weights of the indicators using the D-AHP method. The weight ratings of eight indicators by 10 experts are shown in Table 7 and Table 8. All 10 experts worked with Changjiang Water Resources Commission (CWRC), Hohai University, Power Construction Corporation of China, etc., and all of them were senior engineers with master’s degrees. They had been working in the area of emergency treatment for barrier lakes and other water disasters, hydropower, and water resources. They all contributed to emergency treatment for the Tangjiashan and Baige barrier lakes. The following four indicators of the risks of barrier lakes were taken as an example to construct the D matrix based on the D numbers preference relation as follows:
(1)
Ten experts were asked to score the importance of the four indicators and then construct the D matrix based on the D numbers preference relation, as shown in Equation (13):
  R D =       d 1         d 2         d 3     d 4   d 1       d 2       d 3     d 4       {   ( 0.50 , 1.0 )     }   { ( 0.45 , 0.2 ) , ( 0.55 , 0.3 ) ,       ( 0.60 , 0.3 ) , ( 0.65 , 0.1 ) ,       ( 0.90 , 0.1 ) } { ( 0.40 , 0.2 ) , ( 0.55 , 0.1 ) ,       ( 0.60 , 0.4 ) , ( 0.65 , 0.1 ) ,       ( 0.70 , 0.2 ) } { ( 0.35 , 0.1 ) , ( 0.60 , 0.2 ) ,       ( 0.65 , 0.3 ) , ( 0.80 , 0.4 ) } { ( 0.55 , 0.2 ) , ( 0.45 , 0.3 ) ,       ( 0.40 , 0.3 ) , ( 0.35 , 0.1 ) ,       ( 0.10 , 0.1 ) }   {   ( 0.50 , 1.0 ) }   { ( 0.35 , 0.2 ) , ( 0.40 , 0.1 ) ,       ( 0.45 , 0.1 ) , ( 0.50 , 0.1 ) ,       ( 0.55 , 0.2 ) , ( 0.60 , 0.2 ) ,       ( 0.65 , 0.1 ) } { ( 0.40 , 0.2 ) , ( 0.45 , 0.1 ) ,       ( 0.50 , 0.1 ) , ( 0.60 , 0.2 ) ,       ( 0.65 , 0.2 ) , ( 0.70 , 0.2 ) } { ( 0.60 , 0.2 ) , ( 0.45 , 0.1 ) ,       ( 0.40 , 0.4 ) , ( 0.35 , 0.1 ) ,       ( 0.30 , 0.2 ) } { ( 0.65 , 0.2 ) , ( 0.60 , 0.1 ) ,       ( 0.55 , 0.1 ) , ( 0.50 , 0.1 ) ,       ( 0.45 , 0.2 ) , ( 0.40 , 0.2 ) ,       ( 0.35 , 0.1 ) }   {   ( 0.50 , 1.0 )   }   { ( 0.45 , 0.1 ) , ( 0.50 , 0.1 ) ,       ( 0.55 , 0.4 ) , ( 0.60 , 0.2 ) ,       ( 0.65 , 0.1 ) , ( 0.70 , 0.1 ) } { ( 0.65 , 0.1 ) , ( 0.40 , 0.2 ) ,       ( 0.35 , 0.3 ) , ( 0.20 , 0.4 ) } { ( 0.60 , 0.2 ) , ( 0.55 , 0.1 ) ,       ( 0.50 , 0.1 ) , ( 0.40 , 0.2 ) ,       ( 0.35 , 0.2 ) , ( 0.30 , 0.2 ) } { ( 0.55 , 0.1 ) , ( 0.50 , 0.1 ) ,       ( 0.45 , 0.4 ) , ( 0.40 , 0.2 ) ,       ( 0.35 , 0.1 ) , ( 0.30 , 0.1 ) }   { ( 0.50 , 1.0 ) }
(2)
The D matrix was converted to a crisp matrix Rc using the integration representation of D numbers as follows:
  R C =         d 1           d 2             d 3           d 4       d 1 d 2 d 3 d 4 0.500 0.590 0.580 0.670 0.410 0.500 0.495 0.565 0.420 0.505 0.500 0.570 0.330 0.435 0.430 0.500
(3)
According to the rules proposed to generate the probability matrix by Deng et al. [43], the probability matrix was constructed as below:
  R P =     d 1 d 2 d 3 d 4 d 1 d 2 d 3 d 4 0 1 1 1 0 0 0 1 0 1 0 1 0 0 0 0
(4)
Using the triangularization method, the ranking of the indicators was calculated as d1 >> d3 >> d2 >> d4, where the symbol “>>” indicates preference.
(5)
Then, we calculated the relative weights of the indicators. First, based on the ranking of the indicators, the matrix Rc was converted to a triangulated crisp matrix RcT:
  R C T =       d 1             d 3             d 2           d 4       d 1 d 3 d 2 d 4 0 . 500 0 . 580 0 . 590 0 . 670 0 . 420 0 . 500 0 . 505 0 . 570 0 . 410 0 . 495 0 . 500 0 . 565 0 . 330 0 . 430 0 . 435 0 . 500
(6)
Using the weight relation of the indicators represented in the matrix, the weight equations were constructed by incorporating necessary constraints:
  λ w 1 w 3 = 0.580 0.500 λ w 3 w 2 = 0.505 0.500 λ w 2 w 4 = 0.570 0.500 w 1 + w 2 + w 3 + w 4 = 1 λ > 0 w i 0 , i 1 , 2 , 3
where wi refers to the weight of the i-th indicator, and λ indicates the granular information about the pairwise comparison and is associated with the cognitive ability of the experts.
(7)
According to Deng et al. [43], a feasible scheme of λ is:
  λ = λ ¯ = 1 , n , n 2 / 2 , The   information   is   with   high   credibility The   information   is   with   mudium   credibility The   information   is   with   low   credibility
The 10 experienced experts had strong cognition towards various indicators. The information reliability was high, thus λ = 1. After calculation, the weights of the four indicators d1, d2, d3, and d4 were 0.33, 0.245, 0.25, and 0.175, respectively. Similarly, the weights of the four indicators of loss evaluation factors for barrier dams l1, l2, l3, and l4 were calculated to be 0.393, 0.268, 0.228, and 0.113, respectively. The weight indicators for the danger of barrier dam D and the dam break loss L were 0.525 and 0.475. After integrating the weights of various levels, eight indicator weight value vectors W = [0.173, 0.129, 0.131, 0.092, 0.186, 0.127, 0.108, 0.053] were obtained.

7.3. Calculation of Risk Level of Barrier Lakes

For comparison, this paper refers to the hybrid fuzzy evaluation method for quantitative risk classification based on D-AHP as Method A. The risk levels of 15 barrier lakes after calculation are shown in Table 9. The table-lookup method is referred to as Method B, and the corresponding risk level calculation method is shown in Table 10. The comparison of the two methods for calculating the level of barrier lakes risk is shown in Figure 13.
The following conclusions can be drawn from Figure 13:
(1)
After calculation, the risk level calculation results of the two methods for 13 barrier lakes were the same, accounting for 86.7%. Overall, the evaluation conclusions of the two methods showed good consistency.
(2)
Analysis of reasons for inconsistent calculation results of risk evaluation levels for two barrier lakes:
1)
Tanggudong Barrier Lake: From the preference relation matrix R of Tanggudong barrier lake, the preference relation degrees r11, r21, and r41 corresponding to d1, d2, and d4 were all 1, indicating that the barrier dam is extremely risky. From the perspective of dam break losses, the downstream population at risk of Tanggudong barrier lake exceeds 1000. The regions and facilities at risk include Bayirong Village, Yayihe Village, Bosihe Town, three hydrological stations, eight bridges, 51 km of highway, and large amounts of farmland and township water sources, indicating severe losses. Method B indicates that the extremely severe loss of the barrier lake is a sufficient condition for the risk evaluation level to be level I; however, based on the scores given by 10 experts, the weight of the risk indicator of the barrier dam is greater than the weight of the dam break loss, indicating that it is unreasonable to consider the extremely severe losses due to the barrier lake as a sufficient condition for the evaluation level to be level I. Therefore, it is recommended to supplement Method B with the sufficient condition that “the risk level of the barrier lake is extremely high, and the losses due to the barrier lake are more than relatively severe” for the barrier lake risk level to be classified as Level I.
2)
Zhouqu Barrier Lake: The loss indicators l1, l2, and l4 of the Zhouqu Barrier Lake have all reached severe level, but Method B uses the level with the highest loss severity among the l1, l2, l3, and l4 single grading indicators as the level of loss severity for the barrier lake, failing to reflect cumulative losses. Meanwhile, due to the different weights of l1, l2, l3, and l4, there are differences in the social impacts brought by the same level of loss. Only using the highest-level loss of a certain indicator as the severity level of the barrier lake is one-sided. Method A considers both cumulative losses and weight differences, resulting in a more objective evaluation conclusion.
3)
Based on the above analysis, both Method A and Method B are relatively reliable in evaluating the risk level of barrier lakes. However, Method B has certain deviations in evaluating the risk level of individual cases. It is recommended that Method B supplement “the risk level of the barrier lake is extremely high, and the losses due to the barrier lake are more than relatively severe” as a sufficient condition for classifying the risk level of the barrier lake into Level I, while considering the impact of cumulative losses on the risk level of barrier lakes.

8. Conclusions

This paper addresses the problems faced by the risk classification of barrier lakes, including a short evaluation window period, complex evaluation indicators, difficulty in obtaining information quickly, and difficulty in quantifying index weights. For the first time, a hybrid fuzzy evaluation model for quantitative risk classification of barrier lakes based on D-AHP is constructed, and an eight-factor evaluation index system and quantitative weight indicators are proposed to achieve the rapid acquisition of eight-factor evaluation index information for emergency rescue conditions. The specific conclusions are as follows:
(1)
This paper proposed a risk classification method for barrier lakes based on D-AHP, which solved the problem of difficult quantification of evaluation index weights. The D-AHP method proposed in this article has three advantages over the AHP method: Firstly, AHP’s comparative judgments are subjective because they heavily rely on expert experience and professionalism, which may sometimes lead to inconsistencies. Secondly, AHP lacks the ability to adequately cope with any inherent uncertainty and imprecision in the data. Finally, the preferred information may contain fuzziness and incompleteness, and AHP is unable to handle this incomplete information. The risk evaluation results of 15 barrier lakes, including Tangjiashan Barrier Lake, show that the proposed barrier lake risk classification method in this paper has good consistency with the results using the traditional table-lookup method. The risk classification conclusions of 13 barrier lakes are consistent, but the table-lookup method considers that the extremely severe loss of barrier lakes is a sufficient condition for the evaluation level to be level I and does not consider the impact of cumulative loss on the risk level of barrier lakes, resulting in deviations in the risk level classification of some individual barrier lakes. Further correction is needed to the table-lookup method.
(2)
This paper, on the basis of international and domestic research of risk assessments of barrier lakes and studies on about 100 barrier lake cases, proposed a set of risk classification factors and grading criteria, which is U = [D,L] = [d1,d2,d3,d4,l1,l2,l3,l4] = [reservoir capacity, inflow from upstream, material component and geometry of the barrier, population at risk, impacted cities and towns, impacted public facilities and infrastructures, and impacted ecological environment], solving the problem of complex evaluation indicators on the risk assessment of barrier lake. The proposed set of factors is included in the Code for Risk Classification and Emergency Measures of Barrier Lake (SL/T 450-2021).
(3)
Rapid acquisition of information in a short time period and extremely dangerous conditions are the conditions for risk evaluations of barrier lakes. This paper developed the methods of rapid calculation of the reservoir capacity curve of barrier lakes and intelligent identification of particles on the surface of barrier dams, which realized the rapid acquisition of an eight-factor evaluation index of information, thus solved the problem of acquiring information within a short time period.
(4)
The hybrid fuzzy evaluation method for quantitative risk classification of barrier lakes based on D-AHP proposed in this paper is reasonable in evaluation index’s systems and classification, feasible for information acquisition methods, and scientific regarding weight evaluation indicators, thus generating reliable risk level evaluation results.
The limitation of the method is as follows. For the application of such a method, experts/scholars with rich experience on emergency treatment or risk analysis of barrier lakes are preferred. Therefore, the professionalism and experience of the expert team will impact the outcomes of the study.

Author Contributions

Conceptualization, Q.Y., F.Y., Y.C. and W.D.; methodology, Q.Y., F.Y., Y.C., Y.L., D.Y., H.L. and Z.Z.; software, Q.Y., Y.C., Y.L., D.Y. and H.L.; validation, F.Y., Y.L., D.Y., H.L. and Z.Z.; formal analysis, F.Y., D.Y., H.L., W.D. and Z.Z.; investigation, Q.Y., W.D. and Z.Z.; resources, Q.Y., Y.L., D.Y. and Z.Z.; data curation, Y.C., Y.L., D.Y., H.L. and Z.Z.; writing—original draft preparation, Q.Y., F.Y., Y.C., Y.L., D.Y., H.L., W.D. and Z.Z.; writing—review and editing, Q.Y., F.Y., Y.C., Y.L., D.Y., H.L., W.D. and Z.Z.; visualization, Y.C., Y.L., D.Y. and H.L.; supervision, Q.Y., Y.L., H.L., W.D. and Z.Z.; project administration, Q.Y. and F.Y.; funding acquisition, F.Y., Y.C. and W.D. All authors have read and agreed to the published version of the manuscript.

Funding

This study was financially supported by the Joint Research Fund of Changjiang River Water Science Research (Grant No. U2340232).

Data Availability Statement

The data presented in this study are available on request from the corresponding author. The data are not publicly available since the research is still on-going.

Conflicts of Interest

Authors Qigui Yang, Fugen Yan, Yaojun Cai were employed by the company Changjiang Survey, Planning, Design and Research Co., Ltd. Author Zhongtian Zou was employed by the company Changjiang International Engineering Co., Ltd. The remaining authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.

References

  1. Shan, Y.B.; Chen, S.H.; Zhong, Q.M. Rapid prediction of landslide dam stability using the logistic regression method. Landslides 2020, 17, 2931–2956. [Google Scholar] [CrossRef]
  2. Xing, A.G.; Xu, N.N.; Song, X.Y. Numerical simulation of lake water down-stream flooding due to sudden breakage of Yigong landslide dam in Tibet. J. Eng. Geol. 2010, 18, 78–83. [Google Scholar]
  3. Du, Z.H.; Zhong, Q.M.; Dong, H.Z.; Shan, Y.B. A review of risk assessment studies on dammed lake. J. Hohai Univ. (Nat. Sci.) 2022, 50, 13–25. [Google Scholar]
  4. Liu, J.J.; Duan, Y.Z. Summary of emergency construction of Tangjiashan barrier lake. J. Water Resour. Hydropower Eng. 2008, 39, 10–14. [Google Scholar]
  5. Wu, G.R.; Yue, X. Emergency rescue construction technology of Tangjiashan barrier lake. J. Water Resour. Hydropower Eng. 2008, 39, 5–9, 18. [Google Scholar]
  6. Zhou, X.B.; Zhou, J.P.; Du, X.H.; Chen, Z.Y. Lessons and experiences from emergency management of Baige Barrier Lake on the Jinsha River, China. J. Shuili Xuebao 2021, 52, 1229–1239. [Google Scholar]
  7. Zhong, Q.M.; Chen, S.S.; Shan, Y.B. Numerical modeling of breaching process of Baige dammed lake on Jinsha River. J. Adv. Eng. Sci. 2020, 52, 29–37. [Google Scholar]
  8. Costa, J.E.; Schuster, R.L. The formation and failure of natural dam. J. Geol. Soc. Am. Bull. 1988, 100, 1054–1068. [Google Scholar] [CrossRef]
  9. Peng, M.; Zhang, L.M. Breaching parameters of landslide dams. Landslides 2012, 9, 13–31. [Google Scholar] [CrossRef]
  10. Shen, D.Y.; Shi, Z.M.; Peng, M.; Zhang, L.M.; Jiang, M.Z. Longevity analysis of landslide dams. Landslides 2020, 17, 1797–1821. [Google Scholar] [CrossRef]
  11. ISO31010:2019; Risk management-Risk Assessment Techniques. IEC: Geneva, Switzerland, 2019.
  12. Casagli, N.; Ermini, L. Geomorphic analysis of landslide dams in the Northern Apennine. J. Trans. Jpn. Geomorphol. Union 1999, 20, 219–249. [Google Scholar]
  13. Ermini, L.; Casagli, N. Prediction of the behaviour of landslide dams using a geomorphological dimensionless index. J. Earth Surf. Process. Landf. 2003, 28, 31–47. [Google Scholar] [CrossRef]
  14. Dong, J.Y.; Tung, Y.H.; Chen, C.C.; Liao, J.J.; Pan, Y.W. Logistic regression model for predicting the failure probability of a landslide dam. J. Eng. Geol. 2011, 117, 52–61. [Google Scholar] [CrossRef]
  15. Stefanelli, C.T.; Segoni, S.; Casagli, N.; Asagli, N.; Catani, F. Geomorphic indexing of landslide dams evolution. J. Eng. Geol. 2016, 208, 1–10. [Google Scholar] [CrossRef]
  16. Shi, Z.M.; Ma, X.L.; Peng, M.; Zhang, L.M. Statistical analysis and efficient dam burst modelling of landslide dams based on a large-scale database. J. Chin. J. Rock Mech. Eng. 2014, 33, 1780–1790. [Google Scholar]
  17. Shi, Z.M.; Cheng, S.Y.; Zhang, Q.Z.; Xue, D.X. A fast model for landslide dams stability assessmen: A case study of Xiaogangjian (Upper) landslide dam. J. Water Resour. Archit. Eng. 2020, 18, 95–100, 146. [Google Scholar]
  18. Zhou, K.F.; Li, L. Dynamic forecasting evaluation model of flood loss due to dam breach based on socioeconomic development. J. Resour. Environ. Yangtze Basin 2008, 17, 145–148. [Google Scholar]
  19. Wu, H.Q.; Fu, Q.H.; Dong, J.L. Discussion on the methods of estimating loss of life in dam failure in China. J. China Water Resour. 2010, 8, 24–26. [Google Scholar] [CrossRef]
  20. Xiao, Q.; Chen, J.R.; Zhou, W.K. Research on the evaluation method of flood economic loss. J. Collect. Sci. Educ. Cult. 2009, 5, 180. [Google Scholar] [CrossRef]
  21. Yang, J.M.; Feng, M.Q.; Lu, Q.L.; Han, Q.Q. Prediction of Dam- break Flood Damage in Wenyuhe Reservoir. J. Wut (Inf. Manag. Eng.) 2010, 32, 598–601. [Google Scholar]
  22. Wang, Z.J.; Song, W.T. Study of estimation model of loss of life caused by dam break. J. Hohai Univ. (Nat. Sci.) 2014, 3, 205–210. [Google Scholar]
  23. Liu, X.X.; Gu, S.P.; Zhao, Y.M.; Lv, W.W.; He, L.; He, J. Study on economic loss assessment method of dam-break flood with modified loss rate. J. Econ. Water Resour. 2016, 34, 36–40. [Google Scholar]
  24. Wang, R.K.; Li, L.; Sheng, J.B. On criterion of social and environmental risk of reservoir dams. J. Saf. Environ. 2006, 6, 8–11. [Google Scholar]
  25. Li, Z.K.; Li, W.; Ge, W.; Xu, H.Y. Dam breach environmental impact evaluation based on set pair analysis-variable fuzzy set coupling model. J. Tianjin Univ. (Sci. Technol.) 2019, 52, 269–276. [Google Scholar]
  26. Wu, M.M.; Ge, W.; Li, Z.K.; Wu, Z.N.; Zhang, H.X.; Li, J.J.; Pan, Y.P. Improved set pair analysis and its application to environmental impact evaluation of dam break. Water 2019, 11, 821. [Google Scholar] [CrossRef]
  27. Xue, D.X.; Jiang, T.; Meng, W.W. Comprehensive rapid risk assessment of barrier dam based on fuzzy analytic hierarchy process System research. Ewrhi 2019, 40, 37–41. [Google Scholar]
  28. Wang, R.B.; Wang, Y.; Yang, L.; Zhao, Y. Risk analysis of barrier dam diseases based on fuzzy analytic hierarchy process and generalized entropy method. J. China Three Gorges Univ. (Nat. Sci.) 2020, 42, 16–21. [Google Scholar]
  29. Luan, Y.S.; Zhu, M.; Zhang, L. Risk assessment of Gala barrier lake in Yarlung Zangbo River. J. Resour. Environ. Eng. 2022, 36, 646–650. [Google Scholar]
  30. Dehe, B.; Bamford, D. Development, test and comparison of two multiple criteria decision analysis (mcda) models: A case of healthcare infrastructure location. J. Expert Syst. Appl. 2015, 42, 6717–6727. [Google Scholar] [CrossRef]
  31. Lu, Y.L.; Lian, I.B.; Lien, C.J. The application of the analytic hierarchy process for evaluating creative products in science class and its modification for educational evaluation. J. Int. J. Sci. Math. Educ. 2015, 13, 413–435. [Google Scholar] [CrossRef]
  32. Dong, M.; Li, S.; Zhang, H. Approaches to group decision making with incomplete information based on power geometric operators and triangular fuzzy AHP. J. Expert Syst. Appl. 2015, 42, 7846–7857. [Google Scholar] [CrossRef]
  33. SL/T 450-2021; Code for Risk Classification and Emergency Measures of Barrier Lake. Ministry of Water Resources of the People’s Republic of China: Beijing, China, 2021.
  34. Wang, D.Z.; Chen, X.Q.; Luo, Z.G. Experimental Research on Breaking of Barrier Lake Dam under Different Grading Conditions. J. Disaster Prev. Mitig. Eng. 2016, 36, 827–833. [Google Scholar]
  35. GB 50021-2001; Code for investigation of geotechnical engineering. CHINA ARCHITECTURE&BUILDING PRESS: Beijing, China, 2009.
  36. SL274-2020; Design Code for Rolled Earth-rock Fill Dams. Ministry of Water Resources of the People’s Republic of China: Beijing, China, 2021.
  37. Wang, L.; Yuan, P.F.; Zhong, Q.M.; Hu, L.; Shan, Y.B.; Xue, Y.F. Research on rapid quantitative risk assessment for barrier lake based on dam breach mechanism. J. Nat. Disasters 2024, 33, 51–62. [Google Scholar]
  38. Luo, Q.Y.; Wang, W.W.; Zhao, Y.Z.; Liu, L.N.; Guo, H.L. Research and application on calculation method of yield and confluence in mountain torrent disaster analysis and evaluation within small watershed. J. Water Resour. Power 2018, 36, 59–62. [Google Scholar]
  39. Zhan, L.D.; Chen, X.H.; Wang, Y.M. A simple yield and confluence calculation method for surface runoff modeling based on DEM data. J. China Hydrol. 2023, 43, 51–57, 73. [Google Scholar]
  40. Zhao, J.F.; Liang, Z.M.; Liu, J.T.; Li, B.Q.; Duan, Y.N. Variable runoff generation layer distributed hydrological model for hilly regions. J. Adv. Water Sci. 2022, 33, 429–441. [Google Scholar]
  41. Sun, L.M.; Wei, Y.Q.; Wu, S.F.; Xiao, J.Z.; Yan, J. Building of 3d dynamic virtual simulation software platform for barrier lake based on multiple source heterogeneous spatial data. J. Yellow River 2023, 45, 133–137. [Google Scholar]
  42. Sun, L.M. Study on quick information perception and simulative calculation method of landslide dammed-body in alpine and gorge region:taking Baige Landslide-Dammed Lake as study case. J. Water Resour. Hydropower Eng. 2021, 52, 44–52. [Google Scholar]
  43. Deng, Y.D. Numbers: Theory and applications. J. Inf. Comput. Sci. 2012, 9, 2421–2428. [Google Scholar]
  44. Deng, X.; Hu, Y.; Deng, Y.; Mahadevan, S. Supplier selection using AHP methodology extended by D numbers. J. Expert Syst. Appl. 2014, 41, 156–167. [Google Scholar] [CrossRef]
  45. Liu, H.; You, J.; Fan, X.; Lin, Q. Failure mode and effects analysis using D numbers and grey relational projection method. J. Expert Syst. Appl. 2014, 41, 4670–4679. [Google Scholar] [CrossRef]
Figure 1. Worldwide distribution of barrier lakes (incomplete statistics).
Figure 1. Worldwide distribution of barrier lakes (incomplete statistics).
Water 16 03291 g001
Figure 2. (a) Tangjiashan barrier lake; (b) Baige barrier lake.
Figure 2. (a) Tangjiashan barrier lake; (b) Baige barrier lake.
Water 16 03291 g002
Figure 3. Mathematical model for quantitative risks classification of barrier lake based on D-AHP.
Figure 3. Mathematical model for quantitative risks classification of barrier lake based on D-AHP.
Water 16 03291 g003
Figure 4. Procedure for barrier lake risk grading through mathematical model.
Figure 4. Procedure for barrier lake risk grading through mathematical model.
Water 16 03291 g004
Figure 5. Relation between lake capacity and peak flood upon collapse.
Figure 5. Relation between lake capacity and peak flood upon collapse.
Water 16 03291 g005
Figure 6. Relation between inflow from upstream and duration of barrier lake.
Figure 6. Relation between inflow from upstream and duration of barrier lake.
Water 16 03291 g006
Figure 7. Relation between L/H and the duration of barrier lakes.
Figure 7. Relation between L/H and the duration of barrier lakes.
Water 16 03291 g007
Figure 8. Geometry of barriers and their risk grading.
Figure 8. Geometry of barriers and their risk grading.
Water 16 03291 g008
Figure 9. The process of the acquisition of d1 (case study of Tangjiashan).
Figure 9. The process of the acquisition of d1 (case study of Tangjiashan).
Water 16 03291 g009
Figure 10. The process of the acquisition of d3.
Figure 10. The process of the acquisition of d3.
Water 16 03291 g010
Figure 11. Calculation function of preference relation rik.
Figure 11. Calculation function of preference relation rik.
Water 16 03291 g011
Figure 12. Location of the 15 barrier lakes.
Figure 12. Location of the 15 barrier lakes.
Water 16 03291 g012
Figure 13. Comparison between Method A and Method B calculation results on risk level of barrier lakes.
Figure 13. Comparison between Method A and Method B calculation results on risk level of barrier lakes.
Water 16 03291 g013
Table 1. Hazard assessment parameters for barrier dams worldwide.
Table 1. Hazard assessment parameters for barrier dams worldwide.
List of ScholarsNo. of SamplesLake Volume Relevant ParametersBarrier Dam Relevant Parameters
ALVLLLQVdHdWdLdSdI
Casagli et al. [12].70Yes Yes
Ermini et al. [13].84Yes YesYes
Dong et al. [14].43 YesYesYesYesYes
Stefanelli et al. [15].300Yes Yes
Shan et al. [1].115Yes Yes YesYes
Shi et al. [16,17].79 YesYes YesYesYes
Table 2. The factors for assessment of barrier dam failure.
Table 2. The factors for assessment of barrier dam failure.
AuthorsType of LossFactors
Zhou et al. [18]; Wu et al. [19]Life lossPopulation at risk, population density, level of flooding, understanding of residents, timing of alarm, rate of young adults to the elderly and kids, time of dam failure, weather, distance to dam site, emergency response plan, dam height, reservoir volume, downstream river slope, topography, impact resistance of structures, temperature, rescue capability
Xiao et al. [20]; Yang [21]; Wang et al. [22]; Liu et al. [23]Economic lossDuration of floods, velocity of floods, sediment concentration, flood water temperature, depreciation of properties, timing of alarm, pollutant concentration
Wang et al. [24]; Li et al. [25]; Wu et al. [26]Ecological lossGeomorphology of river channel; water environment; human ecology; natural reserves; damage to animal species; soil environment; vegetation coverage; reduction in agricultural, forestry, and fishery production; air quality; dirty industries
Table 3. Evaluation factors for loss due to dam failure and grading methods.
Table 3. Evaluation factors for loss due to dam failure and grading methods.
Grades of Loss Due to Flooding and Dam FailureEvaluation Factors
l1l2l3l4
Extremely severe≥105Prefecture-level cityImportant state-level infrastructures: transportation, power transmission, oil and gas transmission, large water resources and hydropower projects, cascade development, large-scale chemical industries, pesticide plants, highly toxic chemical industries, heavy metals, etc.Cultural relics and rare animals/plants of the world. Water sources for urban areas involved. Major geological disasters can lead to river blocking, impacting a population of more than 1000.
Severe104–105County-level cityImportant provincial-level infrastructures: transportation, power transmission, oil and gas transmission, medium-sized water resources and hydropower projects, relatively large chemical industries, pesticide plants, highly toxic chemical industries, heavy metals, etc.Cultural relics and rare animals/plants at the state level. Water sources for counties involved. Geological disasters can lead to river narrowing, impacting a population of 300–1000.
Relatively severe103–104Villages and townsImportant municipal infrastructures: transportation, power transmission, oil and gas transmission, mining industries, ordinary chemical industries, heavy metals.Cultural relics and rare animals/plants at the township level. Water sources for counties involved. Geological disasters can lead to river narrowing or impact a population of 100–300.
Moderate<103Residential areas within villagesInfrastructure of a smaller size than those in the relatively severe level.Cultural relics and rare animals/plants at the county level. Water sources for villages involved. Geological disasters can lead to river narrowing or impact a population of less than 100.
Table 4. Information acquisition method for risk grading with eight factors.
Table 4. Information acquisition method for risk grading with eight factors.
FactorsMethods of Data AcquisitionFactorsMethods of Data Acquisition
d1Capacity curve of the barrier lakel1Acquisition through quick identification technology based on LBS (Location-Based Services)
d2Calculated based on runoff yielding in barrier lake areal2
d3Intelligent identification of surface particles, geophysical investigation of space-equivalent particles, tracing provenance analysis, etc.l3Acquisition from corresponding government authorities based on risk map of flooding induced by dam failure
d4Oblique photography with UVA, LiDAR, satellite images, and multi-dimensional 3D modeling with DEMl4
Table 5. Assignment results of eight evaluation indicators for the 15 cases.
Table 5. Assignment results of eight evaluation indicators for the 15 cases.
Barrier Laked1d2d3d4d1l2l3l4
JiguanlingData12,000101090H = 10 m
L/H = 11
65,000Baitao TownG319Water source for villages
Results75.0586.6240.2816.6765.28287929
YigongData260,00088.530H = 100 m
L/H = 25
6000Yigong Village8 bridgesSame as Jiguanling
Results81.3159.6348.6159.3838.89342429
Qingyanlo-ngData15034.480H = 30 m
L/H = 7
60009 villages and townsS201Same as Jiguanling
Results26.3940.2541.675038.8944929
HouziyanData6000257085H = 40 m
L/H = 7.5
20,0003 counties and citiesS306Water source for cities
Results63.8910040.9756.2552.78685454
HongshiyanData26,0003609.44H = 89 m
L/H = 10.22
30,00010 villages and towns33,000 mu of farmlandSame as Jiguanling
Results75.477.8464.6780.9455.56493329
Tangjiasha-nData24,7008583H = 89 m
L/H = 9.67
1,303,500Beichuan County S302, S105Same as Houziyan
Results75.3758.7541.2579.0680.94745454
JialaData55,000160035H = 60 m
L/H = 36.7
16,0007 villages and towns2 bridgesSame as Jiguanling
Results87.510043.0654.6951.6746429
BaigeData57,8007004.3H = 64 m
L/H = 20.31
76,00011 villages and townsG214Same as Jiguanling
Results76.2182.4371.8046.2568.33497929
YankouData64001370H = 54 m
L/H = 4.67
50,000Yinjiang County, 1 village, 1 town7050 housesSame as Houziyan
Results6526.8843.069061.11563354
ShazibaData6921513H = 43 m
L/H = 16.28
8397Tunpu VillageMultiple housesSame as Jiguanling
Results41.447573.6158.1345.5528429
XiaojiaqiaoData200011201H = 65 m, L/H = 5.54114,0006 townsNational factoriesSame as Houziyan
Results52.7825.6324.9271.8875.04437954
Tanggulon-gData68,000150010H = 170 m
L/H = 11.53
1102Bayirong Village3 hydrological stationsSame as Jiguanling
Results76.4693.2463.8910025.28343329
ZhouquData150128.338.65H = 9 m
L/H = 166
69,400Zhouqu County2/3 of Zhouqu CountySame as Houziyan
Results26.3969.5865.761566.5743754
Xiaogangji-anData120015378H = 70 m
L/H = 4.26
47,188HanwangHanqing HighwaySame as Jiguanling
Results50.5628.1310.177560.33462929
XujiabaData9808201H = 150 m
L/H = 4.67
44,000Qingping Village, Hanwang TownFactories and minesSame as Jiguanling
Results49.4420.0224.9210059.4431829
Table 6. Calculation results for preference relation for the 15 cases.
Table 6. Calculation results for preference relation for the 15 cases.
JiguanlingYigongQingyandongHouziyanHongshiyan
1.000 0.000 0.000 0.000 1.000 0.000 0.000 0.000 0.000 0.611 0.389 0.000 0.000 0.000 0.667 0.333 0.611 0.389 0.000 0.000 0.000 0.120 0.880 0.000 1.000 0.000 0.000 0.000 0.000 0.160 0.840 0.000 1.000 0.000 0.000 0.000 0.385 0.615 0.000 0.000 0.000 0.944 0.056 0.000 0.375 0.625 0.667 0.333 0.000 0.556 0.444 0.000 0.000 0.360 0.640 0.000 0.000 0.000 0.960 0.040 0.000 0.160 0.840 0.000 0.000 0.056 0.944 0.000 0.000 0.610 0.390 0.000 0.000 0.667 0.333 0.000 0.000 1.000 0.000 0.000 0.000 0.056 0.944 0.000 0.000 0.000 0.160 0.840 0.000 0.960 0.040 0.000 0.000 0.160 0.840 0.000 0.556 0.444 0.000 0.000 1.000 0.000 0.000 0.000 0.000 0.639 0.361 0.000 0.250 0.750 0.000 0.000 0.111 0.889 0.000 0.000 0.720 0.280 0.000 0.000 0.160 0.840 0.000 0.000 0.160 0.840 0.000 0.000 1.000 0.000 0.000 0.000 1.000 0.000 0.000 0.000 0.587 0.413 0.000 0.000 1.000 0.000 0.000 0.000 0.222 0.778 0.000 0.000 0.000 0.940 0.040 0.000 0.000 0.320 0.680 0.000 0.000 0.160 0.840 0.000
TangjiashanJialaBaigeYankouShaziba
1.000 0.000 0.000 0.000 0.350 0.650 0.000 0.000 0.000 0.650 0.350 0.000 1.000 0.000 0.000 0.000 1.000 0.000 0.000 0.000 0.960 0.040 0.000 0.000 0.160 0.840 0.000 0.000 0.160 0.840 0.000 0.000 1.000 0.000 0.000 0.000 1.000 0.000 0.000 0.000 0.000 0.722 0.278 0.000 0.188 0.812 0.000 0.000 0.067 0.933 0.000 0.000 0.000 0.840 0.160 0.000 0.000 0.000 0.160 0.840 0.000 0.160 0.840 0.000 1.000 0.000 0.000 0.000 1.000 0.000 0.000 0.000 0.872 0.128 0.000 0.000 0.000 0.850 0.150 0.000 0.733 0.267 0.000 0.000 0.000 0.960 0.040 0.000 1.000 0.000 0.000 0.000 0.000 0.160 0.840 0.000 0.600 0.400 0.000 0.000 0.000 0.075 0.925 0.000 0.000 0.722 0.278 0.000 1.000 0.000 0.000 0.000 0.444 0.556 0.000 0.000 0.240 0.760 0.000 0.000 0.000 0.320 0.680 0.000 0.160 0.840 0.000 0.000 0.000 0.658 0.342 0.000 1.000 0.000 0.000 0.000 0.944 0.056 0.000 0.000 0.325 0.675 0.000 0.000 0.000 0.822 0.178 0.000 0.000 0.120 0.880 0.000 0.000 0.000 0.160 0.000 0.000 0.160 0.840 0.000
XiaojiaqiaoTanggudongZhouquXiaogangjianXujiaba
0.011 0.889 0.000 0.000 0.000 0.025 0.975 0.000 0.000 0.000 0.997 0.003 0.875 0.125 0.000 0.000 1.000 0.000 0.000 0.000 0.000 0.720 0.280 0.000 1.000 0.000 0.000 0.000 0.160 0.840 0.000 0.000 1.000 0.000 0.000 0.000 1.000 0.000 0.000 0.000 0.556 0.444 0.000 0.000 1.000 0.000 0.000 0.000 0.000 0.011 0.989 0.000 0.000 0.360 0.640 0.000 0.000 0.320 0.680 0.000 0.000 0.160 0.840 0.000 0.000 0.056 0.944 0.000 0.783 0.217 0.000 0.000 0.630 0.370 0.000 0.000 0.000 0.000 0.600 0.400 0.660 0.340 0.000 0.000 0.960 0.040 0.000 0.000 0.000 0.480 0.520 0.000 0.160 0.840 0.000 0.000 0.022 0.978 0.000 0.000 0.000 0.125 0.875 0.000 0.000 0.000 0.407 0.000 1.000 0.000 0.000 0.000 0.413 0.587 0.000 0.000 0.000 0.840 0.160 0.000 0.000 0.160 0.840 0.000 0.000 0.160 0.840 0.000 0.000 0.978 0.022 0.000 0.000 0.000 0.801 0.199 0.000 0.000 0.997 0.003 1.000 0.000 0.000 0.000 0.378 0.622 0.000 0.000 0.000 0.240 0.760 0.000 0.000 0.000 0.320 0.680 0.000 0.160 0.840 0.000
Table 7. The weight ratings of four indicators of barrier lake risks by 10 experts.
Table 7. The weight ratings of four indicators of barrier lake risks by 10 experts.
Expertd1/d2d1/d3d1/d4d2/d3d2/d4d3/d4
10.550.650.650.60.60.5
20.550.60.80.550.650.55
30.550.60.650.550.60.55
40.450.40.350.450.40.45
50.450.60.650.650.70.55
60.90.70.80.350.40.6
70.60.70.80.550.650.55
80.60.60.80.50.70.7
90.650.550.60.40.450.6
100.60.40.60.350.50.65
Table 8. The weight ratings of four indicators of barrier lake loss by 10 experts.
Table 8. The weight ratings of four indicators of barrier lake loss by 10 experts.
Expertl1/l2l1/l3l1/l4l2/l3l2/l4l3/l4
10.550.650.650.60.60.5
20.550.60.80.550.650.55
30.550.60.650.550.60.55
40.450.40.350.450.40.45
50.450.60.650.650.70.55
60.90.70.80.350.40.6
70.60.70.80.550.650.55
80.60.60.80.50.70.7
90.650.550.60.40.450.6
100.60.40.60.350.50.65
Table 9. Evaluation result for the risk levels of 15 barrier lakes (Method A).
Table 9. Evaluation result for the risk levels of 15 barrier lakes (Method A).
Barrier Lakeg1g2g3g4Grade()Risk Level
Jiguanling0.5240.1770.2690.0310.524I
Yigong0.2570.4180.3200.0040.418II
Qingyandong0.0000.4830.4100.1070.483II
Houziyan0.3860.5670.0470.0000.567II
Hongshiyan0.5120.3640.1230.0000.512I
Tangjiashan0.6440.3100.0460.0000.644I
Jiala0.3320.4590.1190.0910.459II
Baige0.6610.2750.0640.0000.605I
Yankou0.3180.4530.2290.0000.453II
Shaziba0.2820.3600.2660.0910.360II
Xiaojiaqiao0.4030.3050.2920.0000.403I
Tanggudong0.4670.1490.3840.0000.467I
Zhouqu0.4370.2510.2750.0370.437I
Xiaogangjian0.1730.4270.3220.0780.427II
Xujiaba0.1620.3240.4140.1000.414III
Table 10. Calculation table for the risk levels of barrier lakes (Method B).
Table 10. Calculation table for the risk levels of barrier lakes (Method B).
Risk Level of Barrier DamSeverity of Losses Due to Barrier LakeRisk Level of Barrier Lake
Extra high risk, high riskExtremely severeI
Extra high riskSevere, relatively severeII
High riskSevere
Moderate riskExtremely severe, severe
Low riskExtremely severe
Extra high riskModerateIII
High riskRelatively severe, moderate
Moderate riskRelatively severe
Low riskSevere, relatively severe
Moderate risk, low riskModerateIV
Notes: 1. Risk Level of Barrier Dam: When S ≥ 3.0, it is considered an extremely high risk. When 2.25 ≤ S < 3.0, it is considered a high risk. When 1.5 ≤ S < 2.25, it is considered a moderate risk. When S < 1.5, it is considered a low risk. S = 0.25 (S1 + S2 + S3 + S4). S1, S2, S3, and S4 are the assigned values for the four grading indicators d1, d2, d3, and d4, with extra high risk, high risk, moderate risk, and low risk assigned values of 4, 3, 2, and 1, respectively. 2. Severity of Losses: The level of severity of losses due to the formation of a barrier lake is based on the highest level of loss severity among the single grading indicators l1, l2, l3, and l4.
Disclaimer/Publisher’s Note: The statements, opinions and data contained in all publications are solely those of the individual author(s) and contributor(s) and not of MDPI and/or the editor(s). MDPI and/or the editor(s) disclaim responsibility for any injury to people or property resulting from any ideas, methods, instructions or products referred to in the content.

Share and Cite

MDPI and ACS Style

Yang, Q.; Yan, F.; Cai, Y.; Luan, Y.; Yi, D.; Liu, H.; Dai, W.; Zou, Z. A Hybrid Fuzzy Evaluation Method for Quantitative Risk Classification of Barrier Lakes Based on an AHP Method Extended by D Numbers. Water 2024, 16, 3291. https://doi.org/10.3390/w16223291

AMA Style

Yang Q, Yan F, Cai Y, Luan Y, Yi D, Liu H, Dai W, Zou Z. A Hybrid Fuzzy Evaluation Method for Quantitative Risk Classification of Barrier Lakes Based on an AHP Method Extended by D Numbers. Water. 2024; 16(22):3291. https://doi.org/10.3390/w16223291

Chicago/Turabian Style

Yang, Qigui, Fugen Yan, Yaojun Cai, Yuesheng Luan, Duliangzi Yi, Haitao Liu, Wanli Dai, and Zhongtian Zou. 2024. "A Hybrid Fuzzy Evaluation Method for Quantitative Risk Classification of Barrier Lakes Based on an AHP Method Extended by D Numbers" Water 16, no. 22: 3291. https://doi.org/10.3390/w16223291

APA Style

Yang, Q., Yan, F., Cai, Y., Luan, Y., Yi, D., Liu, H., Dai, W., & Zou, Z. (2024). A Hybrid Fuzzy Evaluation Method for Quantitative Risk Classification of Barrier Lakes Based on an AHP Method Extended by D Numbers. Water, 16(22), 3291. https://doi.org/10.3390/w16223291

Note that from the first issue of 2016, this journal uses article numbers instead of page numbers. See further details here.

Article Metrics

Back to TopTop