 
          1166
        
        
          Proceedings of the 18
        
        
          th
        
        
          International Conference on Soil Mechanics and Geotechnical Engineering, Paris 2013
        
        
          half for Case 1. Figure 11 shows 3D MXCT images of pore
        
        
          structure isolated by mathematical morphology and cluster
        
        
          analysis for Case 1 and Case 2. Cluster analysis of continuous
        
        
          pore structure such as in soil materials allows defining pore
        
        
          elements, allowing for their statistical analysis. In Figure 11,
        
        
          the red cluster with greatest volume has a more complex shape
        
        
          than the blue cluster with small volume, which is shaped like
        
        
          balls. There were 99 LNAPL clusters isolated in Case 1 and 156
        
        
          in Case 2, implying that fingering flow with capillary force
        
        
          caused by LNAPL remained in wide area in the sample for Case
        
        
          1. On the other hand, Case 2 with the capillary number (
        
        
          
            Ca
          
        
        
          )
        
        
          twenty times greater than Case 1 reduced the capillary pressure
        
        
          more than Case 1 as Mayer & Miller, (1993) discussed; and
        
        
          hence, it can be concluded that the fingering flow with capillary
        
        
          force was restrained.
        
        
          3.5
        
        
          
            Factor of LNAPL trapping
          
        
        
          If LNAPL migrated in a single direction, water should be
        
        
          almost completely flushed out. However, pore structure was
        
        
          distributed in three dimensions, so pore structure connectivity
        
        
          and a three-dimensional bottleneck effect should be considered
        
        
          to evaluate residual LNAPL in the soil. In the case of sandy soil,
        
        
          small changes in capillary pressure in excess of the entry
        
        
          pressure significantly increased or decreased saturation. Factors
        
        
          for trapping LNAPL are thus related to the connectivity of pore
        
        
          structures and drastic changes in capillary pressure with
        
        
          bottleneck effect. Besides,
        
        
          
            Ca
          
        
        
          would be related to the trapping
        
        
          distribution in the sand as shown in Fig. 11 (a) and (b).
        
        
          4 CONCLUSIONS
        
        
          Sandy soil specimens were scanned by micro-focused X-ray CT
        
        
          scanners, and spatial distribution of pore structures with
        
        
          LNAPL were visualized and quantitatively evaluated by a
        
        
          newly developed image processing technique using marker-
        
        
          controlled watershed, a mathematical morphological method,
        
        
          and cluster analysis. Key conclusions are as follows:
        
        
          1) The developed thresholding technique worked well, and
        
        
          allowed objective definition of locations with changing
        
        
          greatest CT values without histogram analysis.
        
        
          2) Factors for trapping LNAPL are related to the connectivity
        
        
          of pore structures and drastic changes in capillary pressure
        
        
          with bottleneck effect.
        
        
          3) The capillary number (
        
        
          
            Ca
          
        
        
          ) more than 10
        
        
          -5
        
        
          reduced the
        
        
          capillary effect and residual LNAPL would be distributed
        
        
          in local position. Meanwhile, the less
        
        
          
            Ca
          
        
        
          had dominant
        
        
          flow with capillary effect so LNAPL was trapped in wide
        
        
          area of sample.
        
        
          5 ACKNOWLEDGEMENTS
        
        
          This research was financially supported by a Grant-in-Aid for
        
        
          Scientific Research (A) No. 23246156, for which Prof. Y.
        
        
          Obara of Kumamoto University is a corresponding researcher.
        
        
          The authors thank Mr. T. Sato of the Faculty of Engineering,
        
        
          Kumamoto University, for his valuable support.
        
        
          6 REFERENCES
        
        
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            (
          
        
        
          a) Pore with LNAPL in Case 1
        
        
          Property
        
        
          Case 1
        
        
          Case 2
        
        
          Initial LNAPL saturation (%)
        
        
          80.08
        
        
          83.14
        
        
          Residual LNAPL saturation (%)
        
        
          21.48
        
        
          9.47
        
        
          Cumulative pore volume at break
        
        
          through
        
        
          0.51
        
        
          0.56
        
        
          
            Fig
          
        
        
          ure 10. Histogram of pore size for Case 1 and Case 2
        
        
          (b) Pore with LNAPL in Case 2
        
        
          Figure 11. 3D MXCT images of isolated pore structures
        
        
          
            Table
          
        
        
          3. Test results