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n <br />U <br />C� <br />shows the TDS variation for well GC -3, while Figure 2.7-28t presents the changes for <br />the last year at the COY alluvial well. <br />The field pH values for the Pyeatt and Flume alluvial aquifers are close to <br />neutral and have not greatly varied with time. The same major constituents make up <br />the alluvial waters in the eastern portion of the Trapper permit that contribute to <br />the water quality of the Second and Third White Sandstone aquifers. <br />2-520uu REVISED FM I <br />