 
          1763
        
        
          Performance of the tunnel lining subjected to decompression effects on very soft
        
        
          clay deposits
        
        
          Performance du revêtement du tunnel soumis à des effets de décompression sur les dépôts
        
        
          d'argile très mous
        
        
          Rangel-Núñez J.L
        
        
          
            Universidad Autónoma Metropolitana, Azcapotzalco
          
        
        
          Aguilar-Tellez M.A.
        
        
          
            Ingenieros Civiles Asociados, Construcción especializada
          
        
        
          Ibarra-Razo E., Paniagua W.
        
        
          
            Ingeum
          
        
        
          ABSTRACT: Superficial channels on very soft clay deposits undergoing consolidation processes can generate tension zones that
        
        
          potentially can induce semi-vertical cracking. During construction of any underground works, such as tunnels, these cracks can be
        
        
          reactivated, especially if the construction process causes significant changes in the initial stress state of the ground, and then generates
        
        
          important deformation of the tunnel lining from confining loss around the tunnel, especially if dowels rings are used as lining. On the
        
        
          other hand, it is also possible to generate significant lining deformations if there are changes in the state of stress in the ground’s
        
        
          surface due to the dredging of channels. This paper presents a case history about the behavior and numerical modeling of the primary
        
        
          tunnel lining during and after tunneling with an EPB machine in Mexico City soft clay deposits subjected to decompression stresses
        
        
          caused by the dredging of channels. Total displacements induced during tunneling under superficial channels were high but less than
        
        
          1% of the tunnel diameter. After dredging, such channels’ additional deformations were induced in the lining because of a reactivation
        
        
          of pre-existent cracks in the clay deposit. Numerical modeling was carried out to study the optimal solution. Based on numerical
        
        
          results, two solutions were applied: lining reinforcement and soil improvement.
        
        
          RÉSUMÉ : Canaux superficiels sur les dépôts d'argile très douces en cours de processus de consolidation peut générer des zones de
        
        
          tension qui peut potentiellement induire des semi-verticale fissuration. Lors de la construction des ouvrages souterrains, tels que les
        
        
          tunnels, ces fissures peuvent être réactivés, surtout si le processus de construction entraîne des changements importants dans l'état
        
        
          initial des contraintes du sol, puis génère une déformation importante du revêtement du tunnel de la perte de confinement autour du
        
        
          tunnel, surtout si les chevilles des anneaux sont utilisés comme doublure. Cet article présente une étude de cas sur le comportement et
        
        
          la modélisation numérique du revêtement du tunnel principal pendant et après un tunnel avec une machine EPB dans les dépôts de
        
        
          Mexico argile molle soumis à une décompression contraintes provoquées par le dragage des chenaux. Déplacements totaux induits
        
        
          lors des tunnels sous canaux superficiels étaient élevés, mais moins de 1% du diamètre du tunnel. Après dragage ont été produites
        
        
          déplacement supplémentaire relance revêtement se craquelle. Les modèles numériques ont été utilisés pour étudier ces facteurs et
        
        
          déterminer la solution optimale. Avec ces résultats, nous proposons deux solutions: augmenter le revêtement et l'amélioration des sols.
        
        
          KEYWORDS: tunneling in soft soils, soil fracture, decompression stresses, Mexico city tunnels.
        
        
          1 INTRODUCTION
        
        
          The Túnel Emisor Oriente (TEO, Spanish acronym for Eastern
        
        
          Emitter Tunnel) will be the new drainage system for Mexico
        
        
          City. It is located to the north of the city and it is a circular
        
        
          tunnel 62 km long, of 7 m inner diameter, set at variable depths
        
        
          between 30 and 155 m. It crosses all types of soils along 97% of
        
        
          its length, from very soft to hard, with the rest of the length
        
        
          crossing volcanic rock. For its construction, Earth Pressure
        
        
          Balance (EPB) tunnel boring machines are used, with a  primary
        
        
          lining formed by dowels rings with sections 0.35 and 0.40m
        
        
          thick (COMISSA 2010). Almost the entire tunnel is under the
        
        
          groundwater level, with pore pressures of up to 0.8MPa.
        
        
          The project’s first trajectory, approximately 8 km long, is
        
        
          located at a zone of very compressible clays with low shear
        
        
          resistance, with water content in the order of 300%, running
        
        
          parallel to a surface channel. A particular aspect of this section
        
        
          is that on land near the channel surface cracks have been
        
        
          observed, and in the zone where the tunnel crosses under the
        
        
          channel (1+032 to 1+300) it has been observed that before the
        
        
          crossing (0+920 to 1+032) important primary lining
        
        
          deformations have occurred, with a tendency to their
        
        
          stabilization. This anomalous behavior of the tunnel has been
        
        
          caused by a diversity of factors, among which stand out the
        
        
          channel’s dredging and the presence of intense fracturing at the
        
        
          zone of that channel.
        
        
          The objective of this work is to evaluate the effects on the
        
        
          tunnels of the unloading induced by dredging surface channels
        
        
          located on cracked clayey deposits, and as a particular case the
        
        
          TEO project is presented.
        
        
          2 GEOTECHNICAL CONDITIONS
        
        
          Stratigraphy. Subsoil conditions at the zone where the atypical
        
        
          deformations occurred on the tunnel’s primary lining are (Fig
        
        
          1):
        
        
          i.
        
        
          
            Superficial Crust
          
        
        
          (0 to 3m). It is a stratum formed by
        
        
          interspersions of sandy silts and hard silty sands, and on
        
        
          occasions fills up to 2m thick.
        
        
          ii.
        
        
          
            Superior Clayey Series
          
        
        
          (3 to 26m). These are clays and silts
        
        
          of high plasticity with thin lenses of volcanic ash and sandy
        
        
          silts.
        
        
          iii.
        
        
          
            Hard Layer
          
        
        
          (26 to 28 m). These are interspersions of sandy
        
        
          silts and silty sands (tunnel is located at the inferior part of
        
        
          the Superior Clayey Series resting on the Hard Layer).
        
        
          iv.
        
        
          
            Inferior Clayey Series
          
        
        
          (28 and 42 m). It is a very
        
        
          compressible clayey deposit.
        
        
          Conditions of subterranean water. At this zone the groundwater
        
        
          level is located at 3m depth, and the pore pressure measured at
        
        
          the tunnel’s axis is in the order of
        
        
          
            u
          
        
        
          
            axis
          
        
        
          =145kN/m
        
        
          2
        
        
          , which is
        
        
          65kN/m
        
        
          2
        
        
          less than the hydrostatic pressure.