Christian Ledezma
Pontifical Catholic University of Chile
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Publication
Featured researches published by Christian Ledezma.
Earthquake Spectra | 2002
Pedro Hidalgo; Christian Ledezma; Rodrigo M. Jordan
The behavior of reinforced concrete walls that exhibit the shear mode of failure is studied, through the results of an experimental program that included the test of 26 full-scale specimens subjected to cyclic horizontal displacements of increasing amplitude. Test parameters were the aspect ratio of the walls, the amount of vertical and horizontal distributed reinforcement, and the compressive strength of concrete. The results include the cracking shear strength, the maximum shear strength, the drifts associated to these loads and the drift associated to a collapse limit state for each of the specimens tested. Conclusions are drawn concerning the deformation capacity, the energy absorption, the dissipation characteristics and the strength deterioration after maximum strength shown by the walls and the influence of vertical distributed reinforcement on the seismic behavior of walls.
Journal of Geotechnical and Geoenvironmental Engineering | 2010
Christian Ledezma; Jonathan D. Bray
Liquefaction-induced ground deformation has caused major damage to bridge and wharf structures in past earthquakes. Large lateral ground displacements may induce significant forces in the foundation and superstructure, which may lead to severe damage or even collapse. A performance-based earthquake engineering (PBEE) approach can provide an objective assessment of the likely seismic performance, so that agencies can evaluate bridge or wharf structures, compare retrofit strategies, and rank them within their overall system. In this paper, a probabilistic PBEE design procedure that incorporates findings from recent research on this problem is presented. The proposed approach can provide answers in terms that are meaningful to owners, such as expected repair costs and downtimes. The methodology is validated through its application to a well-documented case history. Results show that the proposed approach provides a good estimate of the seismic performance of pile-supported structures at sites with liquefaction-induced lateral displacement.
Earthquake Spectra | 2012
Jonathan D. Bray; Kyle M. Rollins; Tara C. Hutchinson; Ramón Verdugo; Christian Ledezma; George Mylonakis; Dominic Assimaki; Gonzalo A. Montalva; Pedro Arduino; Scott M. Olson; Robert E. Kayen; Youssef M. A. Hashash; Gabriel Candia
Soil liquefaction occurred at many sites during the 2010 Maule, Chile, earthquake, often leading to ground failure and lateral spreading. Of particular interest are the effects of liquefaction on built infrastructure. Several buildings were damaged significantly due to foundation movements resulting from liquefaction. Liquefaction-induced ground failure also displaced and distorted waterfront structures, which adversely impacted the operation of some of Chiles key port facilities. Important case histories that document the effects of ground failure on buildings, ports, and industrial facilities are presented in this paper.
Earthquake Spectra | 2012
Dominic Assimaki; Christian Ledezma; Gonzalo A. Montalva; Andres Tassara; George Mylonakis; Rubén Boroschek
A set of observations on site effects and damage patterns from the Mw 8.8 Maule, Chile, earthquake is presented, focusing on identification of structural damage variability associated with nonuniform soil conditions and subsurface geology. Observations are reported from: (1) the City of Santiago de Chile (Américo Vespucio Norte Ring Highway, Ciudad Empresarial business park), (2) the Municipality of Viña del Mar, and (3) the City of Concepción, extending over 600 km along the Chilean coast. Reconnaissance information and ground motion recordings from the megathrust event are combined with site investigation data in the regions of interest. Comparisons against macroseismic observations related to uneven damage distribution from the Mw 8.0 1985 Valparaíso earthquake are discussed. Complexities associated with identifying the mechanics and underlying physical processes responsible for the manifestation of these effects are elucidated.
Earthquake Spectra | 2012
Christian Ledezma; Tara C. Hutchinson; Scott A. Ashford; Robb E.S. Moss; Pedro Arduino; Jonathan D. Bray; Scott M. Olson; Youssef M. A. Hashash; Ramón Verdugo; David Frost; Robert E. Kayen; Kyle M. Rollins
The long duration and strong velocity content of the motions produced by the 27 February 2010 Maule earthquake resulted in widespread liquefaction and lateral spreading in several urban and other regions of Chile. In particular, critical lifeline structures such as bridges, roadway embankments, and railroads were damaged by ground shaking and ground failure. This paper describes the effects that ground failure had on a number of bridges, roadway embankments, and railroads during this major earthquake.
Earthquake Spectra | 2012
Keith Kelson; Robert C. Witter; Andrés Tassara; Isabelle Ryder; Christian Ledezma; Gonzalo A. Montalva; David Frost; Nicholas Sitar; Robb E.S. Moss; Laurie Johnson
Tectonic deformation from the 2010 Maule (Chile) Mw 8.8 earthquake included both uplift and subsidence along about 470 km of the central Chilean coast. In the south, deformation included as much as 3 m of uplift of the Arauco Peninsula, which produced emergent marine platforms and affected harbor infrastructure. In the central part of the deformation zone, north of Constitución, coastal subsidence drowned supratidal floodplains and caused extensive shoreline modification. In the north, coastal areas experienced either slight uplift or no detected change in land level. Also, river-channel deposition and decreased gradients suggest tectonic subsidence may have occurred in inland areas. The overall north-south pattern of 2010 coastal uplift and subsidence is similar to the average crestal elevation of the Coast Range between latitudes 33°S and 40°S. This similarity implies that the topography of the Coast Range may reflect long-term permanent strain accrued incrementally over many earthquake cycles.
Journal of Geotechnical and Geoenvironmental Engineering | 2017
Kevin W. Franke; Kyle M. Rollins; Christian Ledezma; John D. Hedengren; Derek Wolfe; Samantha Ruggles; Christopher Bender; Brandon Reimschiissel
AbstractSmall unmanned aerial vehicles (sUAVs) were used to reconnoiter, image, and model the effects of soil liquefaction at two separate sites following the M8.2 and M7.6 earthquakes near Iquique...
Earthquake Spectra | 2017
Gabriel Candia; Gregory P. de Pascale; Gonzalo A. Montalva; Christian Ledezma
The 2015 Illapel earthquake sequence in Central Chile, occurred along the subduction zone interface in a known seismic gap, with moment magnitudes of M w 8.3, M w 7.1, and M w 7.6. The main event triggered tsunami waves that damaged structures along the coast, while the surface ground motion induced localized liquefaction, settlement of bridge abutments, rockfall, debris flow, and collapse in several adobe structures. Because of the strict seismic codes in Chile, damage to modern engineered infrastructure was limited, although there was widespread tsunami-induced damage to one-story and two-stories residential homes adjacent to the shoreline. Soon after the earthquake, shear wave measurements were performed at selected potentially liquefiable sites to test recent V S -based liquefaction susceptibility approaches. This paper describes the effects that this earthquake sequence and tsunami had on a number of retaining structures, bridge abutments, and cuts along Chiles main highway (Route 5). Since tsunami waves redistribute coastal and near shore sand along the coast, liquefaction evidence in coastal zones with tsunami waves is sometimes obscured within minutes because the tsunami waves entrain and deposit sand that covers or erodes evidence of liquefaction (e.g., lateral spread or sand blows). This suggests that liquefaction occurrence and hazard may be under estimated in coastal zones. Importantly, the areas that experienced the greatest coseismic slip, appeared to have the largest volumes of rockfall that impacted roads, which suggests that coseismic slip maps, generated immediately after the shaking stops, can provide a first order indication about where to expect damage during future major events.
Earthquake Engineering and Engineering Vibration | 2018
Gabriel Ferrer; Esteban Sáez; Christian Ledezma
Copper production is an essential component of the Chilean economy. During the extraction process of copper, large quantities of waste materials (tailings) are produced, which are typically stored in large tailing ponds. Thickened Tailings Disposal (TTD) is an alternative to conventional tailings ponds. In TTD, a considerable amount of water is extracted from the tailings before their deposition. Once a thickened tailings layer is deposited, it loses water and it shrinks, forming a relatively regular structure of tailings blocks with vertical cracks in between, which are then filled up with “fresh” tailings once the new upper layer is deposited. The dynamic response of a representative column of this complex structure made out of tailings blocks with softer material in between was analyzed using a periodic half-space finite element model. The tailings’ behavior was modeled using an elasto-plastic multi-yielding constitutive model, and Chilean earthquake records were used for the seismic analyses. Special attention was given to the liquefaction potential evaluation of TTD.
Obras y proyectos: revista de ingeniería civil | 2015
Gabriel de la Maza; Nicole Williams; Esteban Sáez; Kyle M. Rollins; Christian Ledezma
El presente articulo describe un estudio de terreno detallado que se efectuo en caleta Lo Rojas, comuna de Coronel, donde se observo una importante extension lateral gatillada por licuacion durante el pasado terremoto del Maule, 2010. El estudio de terreno incluyo sondajes SPT y CPT, asi como la aplicacion de algunas tecnicas geofisicas basadas en ondas de superficie. Sobre la base de esta informacion, se evaluaron expresiones empiricas de prediccion de extension lateral y se elaboro un modelo detallado de elementos finitos hidro-mecanico. Los resultados de ambos metodos se ajustan razonablemente bien a las observaciones post-sismicas en el lugar.