 
          1574
        
        
          Proceedings of the 18
        
        
          th
        
        
          International Conference on Soil Mechanics and Geotechnical Engineering, Paris 2013
        
        
          
            Proceedings of the 18
          
        
        
          
            th
          
        
        
          
            International Conference on Soil Mechanics and Geotechnical Engineering, Paris 2013
          
        
        
          instability mechanism in more detail, subsoil numerical models
        
        
          were carried out with the finite elements method, FEM,
        
        
          considering the geometrical and mechanical conditions
        
        
          measured. The section of analysis corresponds to the one known
        
        
          as Axis Section 10, where important cracking has been observed
        
        
          on the slope’s crown.
        
        
          Modeling. Fig. 7 shows the mesh of finite elements used in the
        
        
          analysis that represents in an app
        
        
          roximate way the slope’s
        
        
          condition as obtained with a topographical survey. It is a bi-
        
        
          dimensional mesh with triangular elements of 12 integration
        
        
          points. Inter-phase elements were placed between the platform
        
        
          ’s
        
        
          natural material and the fill.
        
        
          To determine
        
        
          the slope’s stability, a numerical process was
        
        
          carried out in which the strata’s mechanical properties are
        
        
          reduced step by step, from the measured resistance, until
        
        
          producing a cinematically admissible failure mechanism.
        
        
          Parametric non linear analyses were made varying the resistance
        
        
          properties of the inter-phase elements to verify their influence
        
        
          on the stability. The results obtained are shown below.
        
        
          Figure 7 Finite elements mesh
        
        
          Derived from the analyses described above, a probable
        
        
          failure mechanism was obtained, as shown in Fig. 8. The
        
        
          slope’s failure is observed not to be rotational, but rather that
        
        
          there is a sliding or creep of the fill over the natural material of
        
        
          the Gran Basamento. Such sliding occurs at the point of contact
        
        
          between both materials, and it generates tension zones at the
        
        
          slope’s crown, which in turn can produce cracking, such as is
        
        
          physically observed on the site, as well as a plastification zone
        
        
          at the point of contact between fill and platform.
        
        
          Figure 8 Mechanism of probable failure
        
        
          For current conditions, the safety factor associated to this
        
        
          failure mechanism is only 1.2. This shows that although the
        
        
          slope is stable, the condition could easily deteriorate if current
        
        
          conditions change; for example, when doing a cut, applying a
        
        
          surface overload and/or when water infiltrates.
        
        
          6 CONCLUSIONS
        
        
          The Gran Basamento of Cacaxtla is an earth structure that in the
        
        
          last few years has presented cracking on the crown of the slopes
        
        
          and on the top platform, which has affected the main
        
        
          archeological structures, for example the walls of the Red
        
        
          Temple and the Venus Temple. If this cracking continues to
        
        
          develop, slope failures could occur. Therefore, it is necessary to
        
        
          learn the origin of this cracking. In first instance, the
        
        
          characteristics of the materials that form the pyramid must be
        
        
          known, but since it is an archeological monument, it is not
        
        
          possible to use conventional geotechnical exploration
        
        
          equipment because important damage would be induced, so
        
        
          indirect exploration methods have been used, such as the radar
        
        
          technique, and direct ones, as with the ultra-light penetrometer,
        
        
          where induced damage is small. Also, a geo-boroscope has been
        
        
          used, introduced into the drilling made by the penetrometer, in
        
        
          order to observe directly the characteristics of the materials
        
        
          penetrated.
        
        
          The model of the materials that form the pyramid, obtained
        
        
          through these methods, consists of three basic units: organic
        
        
          soils, fills and volcanic tuff. Out of these materials surface fills
        
        
          stand out, consisting of sandy silt and/or silty sand that in some
        
        
          zones are loose, poorly compacted or of low consistency. Based
        
        
          on the results of the numerical analyses carried out, it was
        
        
          concluded that the frontier be
        
        
          tween these fills and the pyramid’s
        
        
          natural material (volcanic tuff) is a marked sliding surface that
        
        
          is activated by the humidification that occurs in some of the
        
        
          pyramid’s zones or when excavating on the slopes.
        
        
          Also, with the results from the penetrometer and the geo-
        
        
          boroscope it was possible to determine different construction
        
        
          stages of the pyramid, when identifying the various types of fill
        
        
          and the compacting qualities of those fills. This characteristic
        
        
          serves as support to carry out archeological studies about the
        
        
          construction processes applied to the pyramid.
        
        
          7 REFERENCES
        
        
          Barba L. 2006.
        
        
          
            Estudios de radar en el área del Gran Basamento de
          
        
        
          
            Cacaxtla
          
        
        
          , Technical report, UNAM, México.
        
        
          Diseño e Ingeniería Aplicada 1985.
        
        
          
            Estudio de mecánica de suelos de la
          
        
        
          
            zona arqueológica de Cacaxtla
          
        
        
          , Technical report, INAH, México.
        
        
          inGeum 2005.
        
        
          
            Estudio del fenómeno de evapotranspiración en la zona
          
        
        
          
            de Coacalco, Edo. De México
          
        
        
          . Techncial report, INAH, México.
        
        
          Instituto Nacional de Antropología e Historia INAH 2001.
        
        
          
            Levantamiento fotogramétrico Xichitecatl
          
        
        
          , Technical report.
        
        
          Mexico.
        
        
          Martínez Romero E. 1985.
        
        
          
            Proyecto estructural de la techumbre
          
        
        
          
            metálica
          
        
        
          , INAH, México.
        
        
          Mooser F. 2005. Inspección geológica en Cacaxtla, personal
        
        
          comunition, México.
        
        
          National geographic 1992. Map digitized from page 123 (William H.
        
        
          Bond), September.
        
        
          Rangel J. L., E. Ovando, L. Barba, D. Molatore, B. Palavicini y J. C.
        
        
          Araiza, 2006. Análisis geotécnico del Gran Basamento de Cacaxtla,
        
        
          
            Coloquio Internacional Cacaxtla a sus treinta años de
          
        
        
          
            investigación
          
        
        
          , Tlaxcala, México.
        
        
          Archeological
        
        
          fills
        
        
          Volcanic tuff
        
        
          Interface