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<br />The Operator should describe the ACP and ANP methods used jot the static rests given in <br />Appendix A. /f the carbonate minerals include an appreciable percent ojeirher siderite or <br />attkerite, the ANP should be adjusted accordingly. /jtoral carbon tests tivere run, and if the rock <br />contains carbon species other than carbonates, those should be reported. If the test methods <br />employed titrations or other neutralization reactions that x gold include silicate buffering, the <br />ANP values should be re-examit7ed..46sent this, the Operator should address the question itt a <br />narrative ar in further calculations showing that, high estimated NNP values aside, the n~srem <br />still brill be able to minimize impacts to the h}~drologic balance. <br />5. The geological and mineralogical presentations show that average NNP of the Cresson pit is <br />somewhat strongly positive (acid neutralizing) while the average NNP for the proposed North <br />Cresson, East Cresson, and the Main Cresson lateral extension are somewhat negative (acid <br />generating). While the overall NNP of the diatreme as a whole appear to be strongly positive, <br />for the system to contain a substantial increase in metal concentrations waste rock from the <br />negative NNP areas would need to be amended with alkali or blended or interstratified with <br />waste rock from the positive NNP areas to neutralize acid generation at its source, or the waste <br />would need to be capped to minimize infiltration of surface water. Provided acid produced <br />from the upper mining zone is neutralized at or very near its source this could minimize <br />dissolution of metal-bearing minerals. <br />The mine-diatreme-groundwater system may have a limited capacity to precipitate and adsorb <br />zinc (and other potentially problem metals) during non-upset conditions. Although modeling <br />predictions show that the Carlton dischazge is saturated with respect to hemimorphite - <br />Zn(SizO~)(OH)t~H~O) - none has yet been observed in the system. Absent confirming <br />mineralogy it is presumed that zinc adsorption by carbonates precipitated in the diatreme and <br />outside the Carlton is the dominant control over dissolved zinc. It appears important to <br />maintain zinc contributions to the groundwater at steady state levels and this may mean not <br />increasing the Zinc load to the subsurface without increasing the volume of carbonate <br />precipitates. <br />The operator should demonstrate that the x~aste hartdlirrg plan will assure either acid <br />neutralization in the Arequa Gulch and Squaw Gulch overburden storage areas, or minimize <br />surface water infiltration to ACOSA and SGOSA, or submit an alternative plan. <br />XIII. 6.4.8 EXHIBIT H -Wildlife Information -Adequate <br />IX. 6.4.9 EXHIBIT I -Soil Information <br />A. All available growth material no matter how small, has to be salvaged. The Division will allow <br />temporary placement of these stockpiles in close proximity prior to placement in a permanent area. <br />7i. 6.4.10 EXHIBIT J -1'egetation Information -Adequate <br />XI. 6.4.1] EXHIBIT K -Climate -Adequate <br />XII. 6.4.12 EXHIBIT L -Reclamation Costs <br />