Page 360 - Materials Chemistry, Second Edition
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CAT3525_C10.qxd  1/31/2005  12:00 PM  Page 331
                       The Sanitary Landfill                                                       331
                       the soil and from plant uptake and transpiration are typically combined into a single term, evapo-
                       transpiration. Design requirements under RCRA make the quantities of surface water run-on and
                       water entering through the sides and bottom of the fill negligible.
                          The hypothetical water balance is represented by the equation

                                            L   P   R   U   E   R  off                          (10.10)
                                                     on
                       where
                               L   leachate
                               P   precipitation
                              R   run-on surface water
                               on
                               U   underflow of groundwater into the cell
                               E   evapotranspiration
                              R off    run-off surface water
                       If the landfill is designed and operated properly, surface water will be diverted from the waste and
                       therefore  R    0. Additionally, a landfill constructed above the water table and possessing an
                                on
                       impermeable liner will give U   0 (i.e., there is no underflow).
                          The equation can thus be simplified to:

                                                 L   P   E   R off

                          The integration of these concepts is shown in Figure 10.22.
                          The amount of runoff depends upon the soil permeability, the slope of the surface, the type of
                       vegetation, duration and frequency of precipitation, and whether the precipitation is in the form of
                       rain or snow. The fraction of precipitation that becomes runoff is expressed by a runoff coefficient.
                       The fraction of precipitation that is converted into runoff is in the range 0.05 to 0.35 (Table 10.16).
                       In utilizing the water-balance approach for predicting leachate at landfills, a number of references
                       are available (Thornwaite and Mather, 1957; Fenn et al., 1975; Bagchi, 1994); for estimating evap-
                       otranspiration rates.

                       EXAMPLE 10.6

                       Calculate the annual volume of leachate generated per hectare for a sanitary landfill located in
                       the northcentral United States. The climate is temperate, average annual rainfall is 1.07 m/year
                       (42 in./year), and evapotranspiration is estimated at 55%. The wastes are covered with soil and


                                                Precipitation (P)
                                                                    Evapotranspiration (E)
                               Runoff (R )
                                      off
                                                                Infiltration






                                                          Leachate (L)
                       FIGURE 10.22 Mass balance of moisture in a sanitary landfill.
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