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Mr. J.C. York <br />July 13, 2015 Page 2 <br />Table 1 — Wells within area of Influence of Proposed Slurry Wall <br />Well Data from Wells Within Area of Influence <br />Model Results <br />Name <br />Pemit <br />Well <br />Depth <br />Rate (gpm) <br />Reported <br />Depth to <br />Water (ft) <br />Saturated <br />Thickness <br />(ft) <br />Max. Change <br />in Water <br />Levels (ft) <br />Future Depth <br />to Water (ft) <br />Future <br />Saturated <br />Thickness (ft) <br />%Change <br />in Sat. <br />Thick (ft) <br />DOWNGRADIENT WELLS <br />VARRA <br />75865 F NO <br />ND <br />ND <br />NO <br />ND <br />ND <br />ND <br />NO <br />DAVIS FARMS <br />14960 R 101 <br />1150 <br />31 <br />70 <br />-1 <br />32 <br />69 <br />-1% <br />BAAB A C <br />620 Al45 <br />800 <br />9 <br />36 <br />-1 <br />10 <br />35 <br />-3% <br />TAYLOR JAMES <br />223885 <br />44 <br />10 <br />11 <br />33 <br />-1 <br />ND <br />ND <br />ND <br />UPGRADIENT WELLS <br />TRUJILLO <br />23312 <br />25 <br />10 <br />5 <br />20 <br />1 <br />4 <br />21 <br />5% <br />ORONA <br />28174 <br />19 <br />20 <br />8 <br />11 <br />1 <br />7 <br />12 <br />9% <br />PALMA <br />297435 <br />ND <br />ND <br />NO <br />ND <br />1 <br />Uncertain <br />Uncertain <br />Uncertain <br />HARRELL ELDON <br />226878 <br />50 <br />15 <br />16 <br />34 <br />2 <br />14 <br />36 <br />6% <br />ROTHE <br />259513 <br />27 <br />20 <br />2 <br />25 <br />1 <br />1 <br />26 <br />4% <br />TRUYELLO <br />2947 F 21 <br />400 <br />6 <br />15 <br />1 <br />5 <br />16 <br />7% <br />HARRELL BRIAN <br />287278 <br />30 <br />50 <br />ND <br />ND <br />2 <br />Uncertain <br />Uncertain <br />Uncertain <br />DILKA <br />44539 <br />34 <br />25 <br />3 <br />31 <br />1 <br />2 <br />32 <br />3% <br />VANBEBER <br />25941 <br />25 <br />50 <br />2 <br />23 <br />1 <br />1 <br />24 <br />4% <br />WADSWORTH <br />19472 F ND <br />105 <br />ND <br />NO <br />1 <br />Uncertain <br />Uncertain <br />Uncertain <br />VANBEBER <br />16038 <br />25 <br />24 <br />4 <br />21 <br />1 <br />3 <br />22 <br />5% <br />Three down gradient wells can be expected to experience a decline in water levels of <br />approximately 1 foot. Since well yield is proportional to the saturated thickness, we would <br />expect less than a 5% decrease in the maximum theoretical pumping rate of those wells. We do <br />not believe this is a significant impact. <br />Based on our modeling, eleven up gradient wells can be expected to have 0.5 to 2 foot increases <br />in water levels. Only one of those wells (Harrell Eldon) has a reported pre -mining water level <br />depth exceeding 10 feet. The rest of the wells either have reported depths to water of less than <br />10 feet or no recorded level so the depth remains "uncertain." If the recorded well locations and <br />depth to water are correct relative to the pit and if the wells are located near vulnerable structures <br />(homes with basements or excavations), those structures could be vulnerable to rising <br />groundwater resulting from the slurry wall. <br />Uncertainty <br />Whether future flooding or water logging will occur depend on numerous factors including: 1) <br />well location relative to the pit and slurry wall; 2) the location and depth of vulnerable structures <br />such as homes with basements; 3) the location, magnitude and timing of well pumping and <br />recharge from precipitation, agriculture, and canal seepage that could also affect water levels; <br />and 4) the location of existing drainage or canals that may intercept rising groundwater. <br />Therefore, there is considerable uncertainty whether there is a real and quantifiable risk of <br />significant impact. <br />Mitigation <br />Potential mitigation includes: 1) installing a drain around the slurry wall to minimize any <br />mounding or shadow effect to keep the aquifer at equilibrium 2) or moving or abandoning <br />