Remote analysis of an open-pit slope failure: Las Cruces case study, Spain

被引:0
作者
Juan López-Vinielles
Pablo Ezquerro
José A. Fernández-Merodo
Marta Béjar-Pizarro
Oriol Monserrat
Anna Barra
Pablo Blanco
Javier García-Robles
Antón Filatov
Juan C. García-Davalillo
Roberto Sarro
Joaquín Mulas
Rosa M. Mateos
José M. Azañón
Jorge P. Galve
Gerardo Herrera
机构
[1] Geohazards InSAR Laboratory and Modeling Group (InSARlab),School of Civil Engineering (ETSI CCP)
[2] Geoscience Research Department,School of Mines (ETSI ME)
[3] Geological Survey of Spain (IGME),Geomatics Division
[4] HEMAV SL,Department of Geodynamics
[5] Technical University of Madrid (UPM),undefined
[6] Technical University of Madrid (UPM),undefined
[7] Centre Tecnològic de Telecomunicacions de Catalunya (CTTC),undefined
[8] TRE ALTAMIRA SLU,undefined
[9] University of Granada,undefined
[10] Campus Universitario Fuentenueva,undefined
[11] EuroGeoSurveys: Earth Observation and Geohazards Expert Group (EOEG),undefined
来源
Landslides | 2020年 / 17卷
关键词
Open-pit mine; Structure from motion (SfM); Satellite radar interferometry (InSAR); Stability analysis; Finite element method (FEM); Shear strength reduction (SSR);
D O I
暂无
中图分类号
学科分类号
摘要
Slope failures occur in open-pit mining areas worldwide, producing considerable damage in addition to economic loss. Identifying the triggering factors and detecting unstable slopes and precursory displacements —which can be achieved by exploiting remote sensing data— are critical for reducing their impact. Here we present a methodology that combines digital photogrammetry, satellite radar interferometry, and geo-mechanical modeling, to perform remote analyses of slope instabilities in open-pit mining areas. We illustrate this approach through the back analysis of a massive landslide that occurred in an active open-pit mine in southwest Spain in January 2019. Based on pre- and post-event high-resolution digital elevation models derived from digital photogrammetry, we estimate an entire sliding mass volume of around 14 million m3. Radar interferometry reveals that during the year preceding the landslide, the line of sight accumulated displacement in the slope reached − 5.7 and 4.6 cm in ascending and descending geometry, respectively, showing two acceleration events clearly correlated with rainfall in descending geometry. By means of 3D and 2D stability analyses we located the slope instability, and remote sensing monitoring led us to identify the likely triggers of failure. Las Cruces event can be attributed to delayed and progressive failure mechanisms triggered by two factors: (i) the loss of historical suction due to a pore-water pressure increase driven by rainfall and (ii) the strain-softening behavior of the sliding material. Finally, we discuss the potential of this methodological approach either to remotely perform post-event analyses of mining-related landslides and evaluate potential triggering factors or to remotely identify critical slopes in mining areas and provide pre-alert warning.
引用
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页码:2173 / 2188
页数:15
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