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~i <br />revision and description of the environmental <br />setting as it relates to pertinent closure <br />components aze presented in detail in the <br />following sections. <br />2.0 GENERAL CLOSURE ACTIVITIES <br />2.1 Introduction <br />Under this alternative, the leach pad closure <br />would require the following activities: <br />• Continue leaching ore while evaporating <br />process solution until it is no longer <br />economical; <br />• Dtaindown the leach pad and dschazge <br />solution to tailings facility if available for <br />evaporation, recirculate it to another heap <br />leach pad as make up solution, land apply <br />it, or evaporate the residual solution on the <br />heap leach pad; <br />• Recontour and compact the surface, spread <br />topsoil and revegetate the leach pad; <br />• Construct a Biopass System with dischazge <br />to a leach field; and, <br />• Monitor short-term to verify that physical <br />stabilization and closure objectives are <br />being met. <br />A[ the comple[ion of metals extraction all <br />process solutions in the leach circuit aze <br />allowed to drairrdown. Draindown solution is <br />collected in the ponds at the facility and <br />subsequently pumped either to other leach pads <br />for make up solution, pumped to a tailings <br />impoundment for evaporation or [o a land <br />applica[ion operation. Once draindown rates <br />stabilize, all remaining seepage is routed into <br />the Biopass System, which is designed to <br />accommodate expected long-term seepage. <br />The reclaimed heaps will contain a residual <br />moisture content after draindown, which is <br />generally immobile. Precipitation and extreme <br />s[orm events can contribu[e moisture to a heap <br /> <br />tha[ is discharged in a combination of the <br />following processes: <br />• Evaporation or evapotranspiration; <br />• Uptake by spent ore raising the residual <br />moisture content; <br />• Redistribute via unsaturated flow within the <br />heap if the field capacity moisture content is <br />reached; and, <br />• Discharge from the heap, should the field <br />capacity be exceeded or, if saturated <br />conditions occur at the base of the heap. <br />These processes can be modeled for each heap <br />leach pad using an unsaturated flow code which <br />accounts for pad thickness, laboratory <br />determined moisnrre release characteristics, and <br />site-specific climatic data. <br />Extensive research has been done on the <br />theoretical and field measuremenrs of <br />infiltration and evaporation from covers on <br />mine waste facilities (Wilson, et al, 1993; <br />Swanson, et al, 1994). The unsarurated flow <br />modeling can be designed to act as a <br />quantitative closure evaluation regarding the <br />effectiveness of the selected closure <br />alternatives. Climatic inputs to the system can <br />be modeled using site-specific precipitation and <br />temperature data in conjunction with the <br />synthetic weather generator (WGEN) included <br />as pan of the Hydrologic Evaluation of Landfill <br />Performance (HELP) (USEPA, 1984) model. <br />The WGEN model is used to simulate daily <br />precipitation, solar radiation and [emperarure <br />for a one year period. These values are used as <br />input to the unsarurated flow model VS2DT <br />(Lapalla, 1987) to approximate climatic <br />conditions duough out the simulation period. <br />The unsaturated flow characteristics of both the <br />topsoil and spent ore materials must be <br />determined empirically in the laboratory or <br />estimated using information gathered during <br />similar investigations at other heap leach <br />facilities. The laboratory characterization <br />includes es[imating saturated hydraulic conduc- <br />-3- <br />