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With the widespread application of machine learning methods, the continuous improvement of forecast accuracy has become an important task, which is especially crucial for landslide displacement predictions. This study aimed to propose a novel prediction model to improve accuracy in landslide prediction, based on the combination of multiple new algorithms. The proposed new method includes three parts: data preparation, multi-swarm intelligence (MSI) optimization, and displacement prediction. In the data preparation, the complete ensemble empirical mode decomposition (CEEMD) is adopted to separate the trend and periodic displacements from the observed cumulative landslide displacement. The frequency component and residual component of reconstructed inducing factors that related to landslide movements are also extracted by the CEEMD and -test, and then picked out with edit distance on real sequence (EDR) as input variables for the support vector regression (SVR) model. MSI optimization algorithms are used to optimize the SVR model in the MSI optimization; thus, six predictions models can be obtained that can be used in the displacement prediction part. Finally, the trend and periodic displacements are predicted by six optimized SVR models, respectively. The trend displacement and periodic displacement with the highest prediction accuracy are added and regarded as the final prediction result. The case study of the Shiliushubao landslide shows that the prediction results match the observed data well with an improvement in the aspect of average relative error, which indicates that the proposed model can predict landslide displacements with high precision, even when the displacements are characterized by stepped curves that under the influence of multiple time-varying factors.
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http://dx.doi.org/10.3390/s21248352 | DOI Listing |
PLoS One
September 2025
School of Geological Engineering, Institute of Disaster Prevention, Langfang 065201, China.
Bedrock fault dislocations significantly influence the rupture instability of rock and soil slopes adjacent to fault zones. Understanding the dynamic processes, kinematic characteristics, and genesis mechanisms of landslides induced by strong seismic fault dislocations is crucial for advancing the theoretical framework of landslide studies. This paper presents a representative experiment simulating the emergence of seismic faults (internal rupture belts within the soil mass) at the shoulders and toes of slopes due to bedrock fault dislocations.
View Article and Find Full Text PDFPLoS One
August 2025
Hydrogeological and Engineering Geological Brigade, Hubei Provincial Bureau of Geology, Jingzhou, Hubei, China.
In the context of intensifying global environmental pressures, heavy rainfall in extreme climate regions significantly increases landslide risks, threatening societal stability and sustainable development. While research on rainfall-induced landslides is well-established, the deformation and instability mechanisms of landslides under complex rainfall patterns warrant further investigation. This study focuses on the Wangjiapo landslide in the Three Gorges Reservoir area.
View Article and Find Full Text PDFData Brief
October 2025
College of Civil Engineering and Mechanics, Lanzhou University, Lanzhou 730000, China.
Landslides pose significant threats to human life and infrastructure globally. In China, the intensification of urbanization and human activities has exacerbated loess landslide risks, making monitoring and mitigation efforts increasingly critical. Rainfall, surface displacement, pore pressure, and seismic waves as key parameters for landslide monitoring.
View Article and Find Full Text PDFSci Rep
August 2025
School of Intelligence and Civil Engineering, Harbin University, Harbin, China.
Both the 2023 M 7.8 Pazarcık earthquake (strike-slip fault) in Turkey, and the 2008 M 7.9 Wenchuan earthquake (reverse-slip fault) in China occurred on the Eurasian seismic belt, with comparable moment magnitudes.
View Article and Find Full Text PDFSensors (Basel)
August 2025
School of Mines, China University of Mining and Technology, Xuzhou 221008, China.
Landslide displacement prediction is crucial for disaster mitigation, yet traditional methods often fail to capture the complex, non-stationary spatiotemporal dynamics of slope evolution. This study introduces an enhanced prediction framework that integrates multi-scale signal processing with dynamic, geology-aware graph modeling. The proposed methodology first employs the Maximum Overlap Discrete Wavelet Transform (MODWT) to denoise raw Global Navigation Satellite System (GNSS)-monitored displacement time series data, enhancing the underlying deformation features.
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