 
          3336
        
        
          Proceedings of the 18
        
        
          th
        
        
          International Conference on Soil Mechanics and Geotechnical Engineering, Paris 2013
        
        
          thermal and thermodynamics aspects. It is only recently that the
        
        
          importance of the thermo-mechanical behavior of soil has come
        
        
          to the fore, particularly in the context of geothermal energy
        
        
          piles, which are now commonly used in some European
        
        
          countries to perform the dual role of supporting buildings and
        
        
          extracting shallow geothermal energy (Brandl 2006, de Moel et
        
        
          al. 2010). The thermo-mechanical stresses induced in the energy
        
        
          pile and the surrounding soil affect the pile-soil interaction and
        
        
          alter the pile capacity. Therefore, several research studies
        
        
          investigating the thermo-mechanical behavior of energy piles
        
        
          have been initiated in the recent past.  It goes without saying
        
        
          that the practice of extraction of geothermal energy through heat
        
        
          pumps, pile foundations and other geo-structures can
        
        
          significantly reduce the use of fossil fuel and carbon dioxide
        
        
          emission, and is therefore an important part of sustainable
        
        
          geotechnical practices.
        
        
          As mentioned previously, there are several applications of
        
        
          thermal geomechanics other than geothermal energy extraction,
        
        
          an important one being deep injection of nuclear wastes. For all
        
        
          these applications, it is important to understand the relevant
        
        
          thermo-hydro-chemo-mechanical behavior of soil and rock, and
        
        
          relate the fundamental behavior to the corresponding
        
        
          applications. Thus, studies related to thermal geomechanics can
        
        
          be classified into (i) study of elemental soil and rock behavior
        
        
          through laboratory tests and constitutive model development,
        
        
          and (ii) study of the applications using centrifuge and field
        
        
          experiments, and through theoretical modeling of the
        
        
          corresponding boundary value problems.
        
        
          This general report provides a review of 18 papers related to
        
        
          thermal geomechanics that are accepted for publication in the
        
        
          proceedings of 18
        
        
          th
        
        
          ICSMGE. The topics covered by these
        
        
          papers can be grouped into the following broad areas: (i)
        
        
          thermal geomechanics, and (ii) geothermal energy. As the
        
        
          general theme in all these papers is closely linked with
        
        
          sustainable development and a few papers deal with geothermal
        
        
          piles, these papers were assigned to the Sustainability (TC 307)
        
        
          and Deep Foundations (TC 212) committees of ISSMGE with
        
        
          the responsibility of organizing a discussion session and
        
        
          producing a general report based on these papers. In the
        
        
          following section, a summary of the papers is provided and the
        
        
          salient information put forward by each paper are outlined.
        
        
          2 REVIEW OF PAPERS
        
        
          
            2.1 Thermal geomechanics
          
        
        
          This sub-section includes the papers that describe the
        
        
          fundamental thermo-hydro-chemo-mechanical behavior of soil
        
        
          and rock through experimentation and modeling studies. Eight
        
        
          papers focus on this fundamental aspect of thermal
        
        
          geomechanics.
        
        
          Tsutsumi and Tanaka studied the consolidation behavior of
        
        
          clayey soil under the combined effects of strain rate and
        
        
          temperature using a constant rate of strain (CRS) loading
        
        
          apparatus (Figure 1). The CRS apparatus was built based on the
        
        
          Japanese Industrial Standard (JIS) A 1227 (2009) and holds soil
        
        
          specimens with a diameter of 60 mm and an initial height of 20
        
        
          mm. The water pressure was measured by connecting the
        
        
          bottom of the specimen to a transducer. The soil specimens
        
        
          were subjected to a back pressure of 100 kPa for ensuring full
        
        
          saturation. The displacement was obtained by counting the
        
        
          number of revolutions of the step motor and correcting for the
        
        
          deformation of the apparatus system. The displacement values
        
        
          were used to calculate the nominal strain, void ratio and
        
        
          nominal strain rate. The tests were conducted on reconstituted
        
        
          Louiseville clay samples (collected from Louiseville, Quebec,
        
        
          Canada) at temperatures varying between 10°C and 50°C with
        
        
          strain rates varying over 3×10
        
        
          -6
        
        
          s
        
        
          -1
        
        
          to 3×10
        
        
          -8
        
        
          s
        
        
          -1
        
        
          . Tsutsumi and
        
        
          Tanaka observed that the clay hydraulic conductivity was
        
        
          strongly dependent on temperature, that the preconsolidation
        
        
          stress decreased with increase in temperature, and that the
        
        
          viscous behavior disappeared with decrease in the void ratio
        
        
          (Figure 2). The authors also examined the ageing effects of the
        
        
          clay samples and inferred that it was caused by the acceleration
        
        
          of secondary consolidation wherein the clay particles are
        
        
          rearranged closely because an increase in temperature reduce
        
        
          the viscosity of the adsorbed water layer on the surface of the
        
        
          soil particles. Thus, the specimen developed a new structure
        
        
          exhibiting higher stiffness against subsequent loading.
        
        
          Figure 1. A schematic view of CRS testing apparatus for controlling
        
        
          temperature (Figure 2 of Tsutsumi and Tanaka).
        
        
          10
        
        
          1
        
        
          10
        
        
          2
        
        
          10
        
        
          3
        
        
          0.8
        
        
          1
        
        
          1.2
        
        
          10
        
        
          -11
        
        
          10
        
        
          -10
        
        
          10
        
        
          -9
        
        
          10
        
        
          -8
        
        
          
            p'
          
        
        
          
            e
          
        
        
          log (kPa)
        
        
          
            k
          
        
        
          log (m/s)
        
        
          
            e
          
        
        
          -log
        
        
          
            p’
          
        
        
          (10
        
        
          ℃
        
        
          )
        
        
          
            e
          
        
        
          -log
        
        
          
            k
          
        
        
          (10
        
        
          ℃
        
        
          )
        
        
          
            e
          
        
        
          -log
        
        
          
            p’
          
        
        
          (50
        
        
          ℃
        
        
          )
        
        
          
            e
          
        
        
          -log
        
        
          
            k
          
        
        
          (50
        
        
          ℃
        
        
          )
        
        
          
            k
          
        
        
          50
        
        
          /
        
        
          
            k
          
        
        
          10
        
        
          =2.44
        
        
          Figure 2. Variation of hydraulic conductivity
        
        
          
            k
          
        
        
          with void ratio
        
        
          
            e
          
        
        
          and
        
        
          effective stress
        
        
          
            p'
          
        
        
          (Figure 4 of Tsutsumi and Tanaka).
        
        
          Zihms et al. described the effect of high temperature on soil
        
        
          properties. Soils are subjected to high temperatures due to
        
        
          several natural and man-made processes including wild fires,
        
        
          forest fires, and thermal remediation technologies. High
        
        
          temperature affects the particle size distribution, mass loss,
        
        
          mineralogy and permeability of soil. In sandy soils, the particle
        
        
          size decreases with increase in temperature because of
        
        
          mobilization of fines. In clayey soils, the overall particle size
        
        
          increases with increasing temperature owing to aggregation and
        
        
          cementation of the clay fraction. The authors studied the effects
        
        
          of moderate and high temperatures and of smoldering on soil
        
        
          properties and used the results to determine the changes in the
        
        
          soil composition due to temperature change and to predict
        
        
          possible complications that may arise during or after the
        
        
          remediation treatments. Both kaolin clay and its mixture with
        
        
          silica sand were tested, and it was observed that high