# Application of a hybrid model of neural networks and genetic algorithms to evaluate landslide susceptibility

- H. B. Wang
^{1, 2}Email author, - J. M. Li
^{1}, - B. Zhou
^{1}, - Y. Zhou
^{1}, - Z. Q. Yuan
^{1}and - Y. P. Chen
^{3}

**4**:15

**DOI: **10.1186/s40677-017-0076-y

© The Author(s). 2017

**Received: **19 September 2016

**Accepted: **23 March 2017

**Published: **14 April 2017

## Abstract

### Background

In the last few decades, the development of Geographical Information Systems (GIS) technology has provided a method for the evaluation of landslide susceptibility and hazard. Slope units were found to be appropriate for the fundamental morphological elements in landslide susceptibility evaluation.

### Results

Following the DEM construction in a loess area susceptible to landslides, the direct-reverse DEM technology was employed to generate 216 slope units in the studied area. Of the 216 slope units, 123 involved landslides. To analyze the mechanism of these landslides, six environmental factors were selected to evaluate landslide occurrence: slope angle, aspect, the height and shape of the slope, distance to river and human activities. The spatial analysis demonstrates that most of the landslides are located on convex slopes at an elevation of 100-150 m with slope angles from 135°-225° and 40°-60°. Landslide occurrence was then checked according to these environmental factors using an artificial neural network with back propagation, optimized by genetic algorithms. A dataset of 120 slope units was chosen for training the neural network model, and the parameters of genetic algorithms and neural networks were set.

### Conclusion

After training on the datasets, the susceptibility of landslides was mapped for the land-use plan and hazard mitigation. Comparing the susceptibility map with landslide inventory, the verification shows satisfactory agreement with an accuracy of 86.46% between the susceptibility map and the landslide locations. In the landslide susceptibility assessment, ten new slopes were predicted to show potential for failure, which can be confirmed by the engineering geological conditions of these slopes.

### Keywords

Landslide Geographical Information Systems Genetic algorithms Back propagation neural networks Susceptibility evaluation## Background

Landslides are local phenomena occurring in different geomorphic contexts; they can be triggered by a variety of mechanisms, such as earthquakes or rainfall, and some of the causes are not yet well known. Landslides cannot be predicted accurately; however, the susceptibility of a given area to landslides can be determined and depicted using hazard zonation. Various methods have been proposed to partition landscape for the purpose of landslide hazard assessment and zonation mapping, including grid cells, terrain units, unique-condition units, slope units and topographic units (Carrara et al. 1991; van Westen, 1994; Guzzetti et al. 1999; Chung and Fabbri, 2003). With respect to the landscape partitioning methods mentioned above, slope units can be resized according to the prevailing failure type and dimension, thereby partitioning a river basin into nested subdivisions: coarser for larger landslides and finer for smaller failures. Because a clear physical relationship exists between landslides and the fundamental morphological elements of a hilly or mountain region, namely, drainage and divided lines, the slope-unit technique seems appropriate for landslide susceptibility assessment.

A careful review of the concepts, principles, techniques and methodologies for landslide susceptibility evaluation reveals that the most commonly used methods are geomorphological hazard mapping, analysis of landslide inventories, heuristic or index-based methods, functional, statistically based models and geotechnical or physically based models (Guzzetti et al. 1999; Wang et al. 2005; Fell et al., 2008). Recently, probabilistic models such as frequency ratio and logistic regression methods have been applied to evaluate landslide susceptibility and have been integrated with Geographical Information Systems (GIS) (Ayalew and Yamagishi, 2005; Chung, 2006; Dahal et al., 2008; Nefeslioglu, et al., 2008; Yilmaz, 2009; Bai et al. 2011; García-Rodríguez and Malpica, 2010; Hasekiogullar and Ercanoglu 2012; Martinovic et al., 2016). Due to geological complexity of slopes and self-organized system, however, many variables are involved in slope stability evaluation, and these variables display a highly nonlinear relationship with the evaluation results. Under the consideration of the nonlinear characteristics of the sliding process, artificial neural networks (ANNs) have thus been introduced to produce landslide susceptibility and hazard maps (Ercanoglu and Gokceoglu, 2002; Neaupane and Achet, 2004; Catani et al., 2005; Gómez and Kavzoglu, 2005; Kanungoa et al. 2006; Nefeslioglu, et al., 2008; Nefeslioglua et al., 2011).

The main characteristics of ANNs dealing with quantitative and qualitative indices include large-scale parallel distributed processing, continuously nonlinear dynamics, collective computation, high fault-tolerance, self-organization, self-learning and real-time treatment (Rumelhart and McClelland 1986). It is worth noting that a neural network system is a processing device, implemented as an algorithm or in hardware, whose design is inspired by the design and the function of mammalian brains; they react to training data input in such a way to alter their initial state, and they learn using unconventional algorithms. Neural networks integrated with GIS may be an effective approach when dealing with landslide hazard assessments where meaningful outcomes are difficult to achieve by means of standard mathematical models. Because artificial neural network models are adaptive and capable of generalization, they can handle imperfect or incomplete data and can capture nonlinear and complex interactions among the several variables of a system (Ermini et al. 2005; Melchiorre et al. 2008; Lee and Pradhan 2010; Conforti et al., 2014; Pham et al., 2017).

However, it was found that the slow training speed and difficulty in achieving a local minimum cannot be resolved in practical applications for the most commonly used back propagation neural networks (BPNN). To solve this problem, several methods were proposed to improve the training speed of networks, such as improving error functions and adjusting the studying rates. For this kind of solutions, the BPNN is likely to converge to a local solution, which may not be the global solution, with the random selection of initial weights. Thus, a global search algorithm was then introduced, e.g., evolutionary programming, simulated annealing or genetic algorithms (GAs) (Kavzoglu et al., 2015). Among them, GA has mainly been used to search for the optimal solution in BPNNs due to its excellent global search ability (Holland 1975; Sexton and Gupta, 2000; Kesign, 2004; Madaeni, et al., 2010; Nourani, et al., 2014). There are two main aspects of applying GA to BPNNs for finding global optima in complex problems: one is to optimize the weights of the network, and the other is to optimize the topological structure of the network.

After an overview on landslide susceptibility using ANNs, it was noted that the weights were randomly selected and that the optimization cannot be carried out for global searching. This paper thus proposes a hybrid model of a GA and BPNN to evaluate landslide susceptibility for the optimization of weights. In this study, landslide inventory was mapped after detailed field investigation and interpretation from high-resolution imagery. The outline of the watershed polygons was mapped as the ridge line using DEM, and reverse DEM data were used to detect the valley line. The combined DEM and reverse DEM, slope units were then mapped within ArcGIS. After the definition of slope units, environmental factors were analyzed for the presence of landslide occurrence, and a hybrid of GA and BPNN was developed to evaluate landslide susceptibility. In this method, the GA was used to search for the optimal or approximately optimal connection weights and thresholds for the networks, and then, using back-propagation learning rules and training algorithms, the final weights could be adjusted.

## Study area

Historical records show that three earthquakes with Ms ≥ 8 occurred on Loess Plateau, which triggered numerous landslides in loess areas (Zhang et al. 1995; Derbyshire et al. 1999). However, only three earthquakes with around Ms 3.5 have been recorded in the study area.

The climate of the study area is notable for Asiatic monsoons and marked seasonal shifts in dominant winds. The mean annual temperature is 12.9 °C, and the maximum is up to 41.6 °C. The mean annual precipitation reaches 679.1 mm, and almost 50% of the precipitation falls in the period from July to September.

## Data preparation

### Landslide inventory

It was also observed that the landslides are concentrated at the confluence of two streams. As described in the previous section, these landslides are attributed to the undercutting of the slopes associated with gullying. Major factors affecting the initiation of slope failure and subsequent modes of movement appear to be dependent upon the morphology, the nature and degree of weathering of the underlying bedrock, and the moisture status of the loess deposits. Numerous ancillary factors include bedrock-loess interface, slope steepness, vegetation cover, and land utilization. As already noted, the upper surface of the Neogene bedrock is often weathered and contains variable amounts of smectites. In this zone, wetting-drying results in a progressive decrease in strength that may ultimately lead to slope failure. Undercutting of the slopes along the gullies is frequent, which increases the risk of slope failure. As a result of the high relative relief, the steep slopes and the relatively uniform geological and geomorphological conditions, the landslides tend to be very large and to occur in groups.

^{7}m

^{3}. Steeper slopes are generally over 40°around the crest, with forested landslide terraces. Remote-sensing interpretations and field investigations indicate a maximum vertical displacement of 150 m along the slip surface of the landslides. The shape and slope angle of the landslide scars suggest a single, major semi-circular failure plane. For these studied landslides, the failure planes occurred either along the contacts between the fluvial deposits and the Neogene argillites or partially within the bedrock. With regard to the Neogene argillite in the loess plateau, the clay minerals are dominated by illite, chlorite, smectite, and kaolinite, similar to the overlying Quaternary loess (Peng and Guo 2007). This type of argillite is thus subjected to long-term softening due to saturation in the contact zone. After a point is reached, at which they are no longer able to support the overlying loess, a progressive failure occurs. The occurrence of planar slides in the study area depends on the shear-strength conditions of the failure surface and the cohesion of the materials involved, usually presented in the Malan loess and in reworked loess slope deposits.

### Defining slope units

### Selection of environmental factors

- (1)
Slope angle

Using the function of Mean in the ArcGIS Spatial Analyst model, an average slope angle was defined for each slope unit. In the study area, slope angles were categorized into six classes: 0–20°, 21°–30°, 31°–40°,41°–50°, 51°–60° and larger than 60° (Fig. 5). - (2)
Slope height

Slope height plays an important role in landslide occurrence, especially in loess areas. Considering only the slope height for slope failures, higher slopes can increase stress values in different areas of slope, making the slopes unstable. The slope height was classified into five classes: 0–50 m, 51–100 m, 101–150 m, 151–200 m and 201–300 m (Fig. 6). Using Min and Max functions in the model of ArcGIS Spatial Analyst, the slope height was obtained from the difference of the minimum and maximum elevation. - (3)
Slope aspect

The slope aspect information can be obtained from the Majority function within the ArcGIS. Aspect was categorized as 0–15°,16°–90°, 91°–135°, 136°–180°, 181°–225°, 226°–270°, 271°–315 ° and 316°–360° (Fig. 7). - (4)
Slope morphology

It is known that water concentrates in concave topographic positions and makes the slope susceptible to (sub) surface flow as the main hydrological triggering mechanism. According to the analysis of the relationships between the landslide occurrence and slope morphology, however, most of landslides are located in the convex topographic positions (Fig. 8). - (5)
Human activities

Human activities influence the susceptibility due to the land use. In the Changshou valley, the land-use is very homogenous. Forests are present closed to the boundary of the loess plateau, upper the slope of the valley. Areas covered by shrubby and herbaceous vegetation are scattered into the study area, while parts of space are open with more vegetation for local farmers. In the analysis of human activity, the influence was simply determined by whether the slope area had been used for vegetation or not.

- (6)
Distance to river

The distance to the river is presented by the proximity of the Changshougou valley and various drainages. These data were obtained from the buffer of rivers and drainages using maps at the scale of 1:25000 in ArcGIS.

## Methods

### Normalization of data

where *X* represents the original data, *X*
_{max} and *X*
_{min} are the maximum and minimum of original data, respectively. T is the target data after normalization.

### GA-based BPNN

where *mse* represents mean square errors for BPNN, and *k* is training time.

Using BPNN modeling optimized by genetic algorithms, the parameters of GAs and neural networks are set in the present study. The population size is 100; crossover probability is 0.65; mutation probability is 0.01; momentum factor is 0.60; learning rate is 0.7; max learning number is 10000; and target error is 0.000001. From a database of 216 landslides in units of slope, 120 landslides were randomly used for training the neural network models, and 96 landslides were used for the validation of landslide susceptibility.

## Results and discussion

Following the process of mapping the slope units, the environmental factors can be categorized into slope, aspect, slope height, and the shape of the slope, human activity and distance to river. These factors were statistically analyzed by slope units within the scope of GIS, after the construction of the geo-database. As mentioned above, the geological condition is almost the same in the study area, in which the strata in these units are mainly Neogene argillites, and the fluvial deposits consist of clayey silts and gravels and Quaternary loess. Due to human activity to effect the landslide susceptibility, it was simply determined by whether the slope area had been used for vegetation or not. The land use for vegetation needs more space and artificial excavation, even irrigation, then affecting the stability of landslides. With respect to the distance to river, the buffer of the Changshougou valley and drainages was selected for the analysis of susceptibility. A small number of landslides, which are closed to the river and drainage, can be in partial deformation, especially at the toe of slope due to erosion. The environmental factors are analyzed by focusing on the slope parameters, such as slope angle, aspect, height and the shape of the slope.

Ten slopes (in yellow in Fig. 19) were predicted to be prone to landslides. In view of the environmental factors, all of these slopes were toward the southeast and southeast, were higher than 100 m and had slope angles greater than 43°. Furthermore, seven of the slopes were in convex topographic conditions, whereas the other slopes were located in concave topographic conditions.

As a useful tool, which addresses a nonlinear system and is capable of response to inputs and adaptation to the environment, the most widely used BPNNs are capable of evaluating landslide susceptibility at both the regional and site-specific scales (Lee et al. 2003; Neaupane and Achet 2004). BPNNs can be applied better over a wide area using non-parametric variables with large extensions. However, BPNNs are prone to falling into local extremes, and their convergence is slow. To overcome these drawbacks, a GA-based BPNN was proposed to optimize the neural network weights for landslide susceptibility assessment, and the topology was subjectively kept in three layers. In the optimization of the GA-based BPNN, the number of neurons can be decided in the hidden layer by the Kolmogorov theorem. For the training of the BPNN, the weights and thresholds were represented as genes of a chromosome, and the global optimum was then searched for using the selection, crossover and mutation operators of the genetic algorithm. To sum up, the advantages of using genetic algorithms were based on the performance of neural networks on the testing datasets, instead of only on the minimal square error in the modeling datasets. In addition, the minimal improvement of the genetic algorithms in this study occurred in the ratios between the numbers of chromosomes of a generation.

## Conclusions

In this study, through the use of direct-reverse DEM technology, the Changshougou valley was divided into 216 slope units, of which 123 units included landslides. According to the mechanism analyses of the landslides in the loess area, six environmental factors were selected to evaluate landslide occurrence, such as slope height, slope angle, aspect, shape of slope, distance to rivers, and human activities. The spatial analysis shows that most of landslides in the Changshougou valley are located at an elevation of 100–150 m, have a slope angle of 135°–225° and 40°–60° in the slope, and have convex slope conditions. After the spatial analysis of the environmental factors, a case study was presented for landslide susceptibility prediction using BPNN modeling optimized by genetic algorithms. From a database of 216 slopes, 120 units, including 80 with landslide presence and 40 without, were used for training the neural network models, and 96 slopes, i.e., 43 with landslide presence and 53 without landslide presence, were used for the validation of landslide susceptibility. Comparing landslide presence with a susceptibility map, it was noted that the prediction accuracy for landslide occurrence is 93.02%, whereas units without landslide occurrence could be predicted with an accuracy of 81.13%. It was also noted that 10 slopes were predicted to be prone to landslides. In view of the environmental factors, all of these slopes are toward southeast and southeast, are at an elevation greater than 100 m, and have slope angles greater than 43°. It was also noted that seven of the slopes are in convex topographic conditions, whereas the other slopes are located in concave topographic conditions. Furthermore, the prediction of 10 slopes can be used as a general planning tool but is not intended for individual site-specific evaluations.

## Declarations

### Acknowledgements

This research was supported by funding from the National Natural Science Foundation of China (No.41372296 and 41672267). A special note of appreciation is extended to the Ministry of National Science and Technology for their funding support (2012BAK10B00). Two anonymous reviewers were greatly appreciated for their comments and suggestions.

### Authors’ contributions

HB carried out the improvement of GA-BPNN for landslide susceptibility, and drafted the manuscript as the corresponding author. JM carried out the data analysis for landslide susceptibility, and drafted parts of the manuscript. BZ carried out the GIS dataset preparation, and helped to draft the manuscript. YZ participated in the preparation of all figures. ZQ participated in the design of the methodology and performed the statistical analysis for landslide susceptibility. YP conceived of the study, and participated in its design and coordination and helped to draft the manuscript. All authors read and approved the final manuscript.

### Competing interests

The authors declare that they have no competing interests.

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## Authors’ Affiliations

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