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                       The Sanitary Landfill                                                       301
                       10.4.9 SURVIVABILITY TESTS
                       Several tests are available to determine the survivability of unexposed polymeric liners. For exam-
                       ple, puncture tests are useful to estimate the survivability of geomembranes in the field. During a
                       puncture test, a 5/16 in. steel rod with rounded edges is pushed down through an anchored mem-
                       brane (Figure 10.5). A very flexible membrane that is shown to have high strain capacity under ten-
                       sion may have great survivability in the field. High-density polyethylenes provide a high penetration
                       force but experience high brittle failure.  Thus, puncture data may not adequately predict field
                       survivability (U.S. EPA, 1989).
                       10.4.10 PERMEABILITY

                       Even if a liner is installed correctly, i.e., without punctures and defects, liquid will inevitably
                       diffuse through. However, such rates are extremely low. U.S. EPA data (1988) for water vapor
                       transmission across various geomembranes is given in Table 10.5. Permeability of a geomem-
                       brane is evaluated using ASTM E96, the Water Vapor Transmission test (ASTM, 2000). A sam-
                       ple of the membrane is attached to the top of a small aluminum cup containing a known volume
                       of water. The cup is then placed in a chamber of controlled humidity and temperature. The
                       chamber is typically set to 20% relative humidity while the humidity in the cup is 100%; thus,
                       a concentration gradient is set up across the membrane. Moisture diffuses through the membrane
                       and with time the liquid level in the cup will fall. From these measurements, the rate at which
                       moisture is moving though the membrane is measured and the permeability of the membrane is
                       calculated with a simple diffusion equation (Fick’s first law)
                                                  J    D(dC/dx)                                  (10.2)
                                               2
                                                                               2
                       where  J is the flux (mol/cm sec), D the diffusion coefficient (cm /sec), C the concentration
                             3
                       (mol/cm ), and x the length in the direction of movement (cm).
































                                                                  FIGURE 10.5 Puncture apparatus for geomem-
                                                                  brane testing.
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