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C-PIT Hydrogeologic Investigations <br />Technical Revision No. 8 <br />3: Observations and Results Mining Permit M-1977-208 <br />and sulfate ions increased. The increase in these constituents could be associated with the addition of the fill, <br />the decrease in the pH and associated equilibrium reactions, or both. <br />The geochemical signature of water from monitoring well CEM-001 did not change significantly following <br />the placement of the fill in C-Pit. Furthermore, these samples notably lack Ca, Mg, and K, all of which aze <br />constituents of C-Pit water. <br />The groundwater flow system within the quarry area appears to be a poorly interconnected low flow system. <br />' Use of contents on This sheet is subject to the IimAabons specified at the end of this document. <br />\\BCDEN02\projects\DataWENlCemex\TR-S~Raporting\CEMEX Repotl 0031-O7.doc <br />