 
        
          
            Geotechnical News • June 2016
          
        
        
          
            
              47
            
          
        
        
          
            GROUNDWATER
          
        
        
          to 55 cm for liner No.1, and from 23
        
        
          to 59 cm for liner No. 2. The samples
        
        
          had a few subvertical cracks crossing
        
        
          the full thickness. In addition, 30% of
        
        
          clay samples contained thin, less than
        
        
          1-mm thick, layers of sand within the
        
        
          clay liner, probably resulting from
        
        
          poor handling of materials during con-
        
        
          struction. Therefore, the first suspected
        
        
          reason for poor performance, some
        
        
          clay damage or poor quality work
        
        
          in the upper parts of the slopes, was
        
        
          verified.
        
        
          The second suspected reason, a poor
        
        
          seal along the pipes, was also inves-
        
        
          tigated. During a site visit, when the
        
        
          water levels had been lowered, the
        
        
          author could see open spaces just
        
        
          below the pipes with widths between
        
        
          5 and 8 cm. The spaces were sounded
        
        
          using a rod: they were opened along
        
        
          the full liner thickness. Smaller (1-2
        
        
          cm) open spaces were also found
        
        
          above and around the pipes, after the
        
        
          crushed stone had been removed to
        
        
          expose the contact between clay and
        
        
          pipe. A representative pipe is shown
        
        
          in Fig. 4. Thus, the second suspected
        
        
          reason was also verified.
        
        
          
            Reason for the poor seal along
          
        
        
          
            the pipes
          
        
        
          Initially, the clay had been tightly
        
        
          compacted against the pipes, which
        
        
          had been installed during dike con-
        
        
          struction and before liner construction.
        
        
          Subsequently, a gravel protection was
        
        
          laid everywhere over the liner, with
        
        
          a special shape and increased thick-
        
        
          ness around the ends of the pipes, as a
        
        
          protection against erosion. The open
        
        
          spaces that were found along the pipes
        
        
          may have been caused first by thermal
        
        
          dilation and contraction, and then
        
        
          enlarged by water erosion.
        
        
          The pipes were laid in June. The field
        
        
          inspector reported that the contact
        
        
          between clay and pipe was good.
        
        
          During its installation, a pipe was at a
        
        
          temperature close to that of the newly
        
        
          placed clay (≈ 10°C). However, in
        
        
          the next few weeks, its temperature
        
        
          increased significantly (from about 10
        
        
          up to 35
        
        
          °C),
        
        
          because the empty pipe
        
        
          was in contact with the hot air inside
        
        
          it. All pipes were made of plastic.
        
        
          Their thermal dilation coefficient is
        
        
          about 12 times higher than that of
        
        
          cement concrete or steel (Chapuis
        
        
          1990a). Therefore, the plastic pipes
        
        
          dilated, their wall pushed away the
        
        
          clay, thus tightening the seal at the
        
        
          
            Figure 3. Full-scale leakage test, lagoon 2: (a) water level versus time; (b)
          
        
        
          
            non-dimensional graph of relative flow rate Q/Qmax versus relative water
          
        
        
          
            thickness h/hmax for the same lagoon geometry.