 
          3071
        
        
          Technical Committee 215 /
        
        
          
            Comité technique 215
          
        
        
          
            Proceedings of the 18
          
        
        
          
            th
          
        
        
          
            International Conference on Soil Mechanics and Geotechnical Engineering, Paris 2013
          
        
        
          Figure 2. Relationship between suction and vane shear strength at five
        
        
          natural and artificial intertidal flats
        
        
          was a strong correlation and unique interrelationship between
        
        
          suction and hardness of the surficial intertidal flat soils (Fig. 2).
        
        
          Indeed, the vane shear strength varied by a factor of 20
        
        
          –
        
        
          50 due
        
        
          to suction, that stemmed from the combined effects of suction
        
        
          development and suction-dynamics-induced cyclic elastoplastic
        
        
          soil compaction in the essentially saturated states (Sassa and
        
        
          Watabe, 2007). Such suction is found to be closely linked with
        
        
          the distributions of the various species as described below.
        
        
          For the purpose of later discussion, the relationship between
        
        
          the shell lengths and wet weights of the two different bivalves,
        
        
          
            R. philippinarum
          
        
        
          (Manila clam) and
        
        
          
            M. veneriformis
          
        
        
          at the
        
        
          Shirakawa intertidal flat are shown in Fig. 3. We categorized
        
        
          adult and juvenile bivalves according to the shell length
        
        
          distributions in Fig. 4a. The individual densities of the juvenile
        
        
          and adult bivalves (mean
        
        
          ±
        
        
          SE) are plotted in Fig. 4b and c. The
        
        
          figure shows that for both Manila clam and
        
        
          
            M. veneriformis,
          
        
        
          the
        
        
          juveniles inhabited the area even where suction developed, but,
        
        
          the adults, particularly the adult Manila clams inhabited only the
        
        
          waterfront area where suction did not develop. Also, the peak
        
        
          density of the adult
        
        
          
            M. veneriformis
          
        
        
          manifested where the
        
        
          developed suctions were higher than those for the adult Manila
        
        
          clam. These field results are well consistent with the ecohabitat
        
        
          chart indicating the following. Namely, the burrowing
        
        
          capability of the Manila clam decreased considerably toward
        
        
          adult stages when the shell lengths exceeded 20mm
        
        
          corresponding to the wet weigths 1.5 to 2g in Fig. 3. This means
        
        
          that the adult Manila clam could not effectively burrow in
        
        
          denser soils as a consequence of the suction dynamics.
        
        
          Furthermore, the suitable geoenvironment for the adult
        
        
          
            M.
          
        
        
          
            veneriformis
          
        
        
          was above that for the adult Manila clam in the
        
        
          chart. This fact also conforms to the observed results.
        
        
          Figure 5 shows the relationship between suction and
        
        
          burrow densities of the sand bubbler crab
        
        
          
            S. globosa
          
        
        
          and the
        
        
          decapod crustacean
        
        
          
            C. japonica
          
        
        
          at the Naha and Isumigawa
        
        
          intertidal flats. Both species inhabited the geoenvironment
        
        
          particular to each species, irrespective of the survey locations
        
        
          and periods. In fact, the individual densities increased markedly
        
        
          at suction equal to 1kPa for the
        
        
          
            S. globosa
          
        
        
          , and about 0.2kPa for
        
        
          the
        
        
          
            C. japonica
          
        
        
          . This observation conforms quantitatively to the
        
        
          ecohabitat chart showing that the suitable geoenvironment for
        
        
          
            S.
          
        
        
          
            globosa
          
        
        
          was well above that for
        
        
          
            C. japonica
          
        
        
          .
        
        
          Figure 6 shows the relationship between suction and
        
        
          individual densities of Arthropoda, Mollusca, and Annelida at
        
        
          the Tokuyama artificial intertidal flat. The survey was conducted
        
        
          soon, one and half year, after the reclamation. It is seen that in
        
        
          the unsaturated region where suction exceeded the air-entry
        
        
          suction of the soils, the densities of all species declined,
        
        
          indicating the importance of water retention in soils for the
        
        
          survival of species. In the saturated region, the density of
        
        
          
            C.
          
        
        
          
            erythraeensis
          
        
        
          outnumbered the other species. This fact is also
        
        
          Figure 3. Relationships between shell length and wet weight of
        
        
          
            R. philippinarum
          
        
        
          and
        
        
          
            M. veneriformis
          
        
        
          Figure 4. Relationships between suction and individual densities of the
        
        
          two different bivalves at the Shirakawa intertidal flat
        
        
          (a)
        
        
          (b)
        
        
          (c)