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2.0 SITE LOCATION AND CLOSURE <br /> The FSL is located at 9999 South Austin Road in Manteca, California and is a combination of <br /> two previously existing landfills, the Forward Landfill and the Austin Road Landfill. The <br /> facility is owned by Forward Landfill, Inc. and includes 567 acres,though only 388 acres have <br /> 1 been landfilled. <br /> The Stage 1 partial final closure area includes the northern slopes of the landfall; an <br /> environment that should represent the lowest ET microclimate on the site. The monolithic cover <br /> constructed over Stage 1 consists of a minimum 4-foot thick soil layer placed over the existing <br /> interim cover and/or waste, as necessary to meet final design grades. The soils used to construct <br /> ' the alternative final cover consisted of clayey silt derived from an on-site borrow source (Vector <br /> Engineering, Inc., 2006). <br /> ' 3.0 VEGETATION CHARACTERISTICS <br /> The finished surface of the alternative final cover system was hydroseeded after completion of <br /> closure construction and some areas were re-seeded in the fall of 2007, after minor grading <br /> repairs to the final cover were completed. Hydroseeding was completed using the seed mixture <br /> stipulated in the final closure documents (BAS, 2003). At the end of the first year of monitoring, <br /> vegetation at the site was in a post-emergent stage with a vegetative cover fraction estimated to <br /> be in excess of 20-30 percent overall. It is estimated that roots, in areas with established <br /> vegetation, extend to a depth in excess of 12-18 inches. Currently, the vegetative cover fraction <br /> for the North Slope area is estimated to be 30-40 percent. Roots continue to develop and it is <br /> estimated that vegetative rooting depths still average around 12-18 inches. Some plants and <br /> vegetation are still immature and the dry conditions typical at this site have stunted the <br /> development of vegetation. As a result,the ultimate performance of the alternative cover has not <br /> yet been realized. <br /> ' Mowing of the established vegetation also stunts the development of a robust vegetative <br /> community. Though mowing is conducted to limit the potential of a fire risk, mowing of plants <br /> that are trying to evolve into a mature vegetative community limits the alternative <br /> ' (evapotranspiration) cover system from full realization of its moisture control capabilities. <br /> Appendix A includes recent pictures taken in early 2009 at each of the monitoring station <br /> locations and illustrates the limited vegetation that has been allowed to develop within each of <br /> the monitored locations. <br /> 4.0 MONITORING SYSTEM <br /> The installation of final cover monitoring instrumentation was completed on July 28, 2006 in <br /> accordance with the manufacturer's recommendations as outlined in the equipment manuals. <br /> Heat dissipation sensors (HDU 229-L) from Campbell Scientific Inc., soil moisture probes (Echo <br /> ' Sensors from Decagon Devices, Inc.), and two Gee Passive Capillary Lysimeters manufactured <br /> by Decagon Devices, Inc., were installed at each of the two monitoring locations. Figure 2 <br /> illustrates the configuration of the instruments installed at each monitoring location. As part of <br /> 3 <br /> Geologic Associates <br />