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• previous years for this well. The pH values for well GE-3 were also similar and above <br />neutral, <br />Twenty Mile Sandstone weft GF-1 generally contains water with a pH near neutral, <br />while the latest pH from U aquifer well (GF-2) was 8.0. The KLM aquifer well (GF-3) at this <br />site contained water with a pH greater than 8. A similar pH was observed for the HI <br />aquifer at well GF-4 in 2000. Backfill well GF-5 had field pH values above 7.5 in 2000, <br />while the field pH for backfill well GF-7 was just below neutral at 6.9. The field pH values <br />in backfill well GF-11 for 2000 were near neutral. The field pH in well GF-6 (QR) was also <br />near neutral in 2000. <br />Well GP-1 (QR) has water with pH values above 8.0, while well GP-2 (KLM) water <br />was above neutral in 2000. The field pH values for wells GP-3 and GP-4 have shown little <br />• ~ change fur water rntlected from the HI and Ia_M aquifers, respectively. Well GP-3 has <br />generally had pH values near neutral, while values for well GP-4 have been around 9. <br />Wells GP-5 and GP-6 are completed in the QR aquifer. The field pH values from <br />well GP-5 are generally above 8, while the pH from well GP-6 is generally above 7. <br />The 2000 field pH values for HI aquifer welt GP-7 were 6.9 and 7.1, while welt GP-8 <br />(fCLM) water had field pH values of 8.0 and 8.1 in 2000. The 3rd White Sandstone aquifer <br />well GP-9 field pH values are typically near neutral. <br />The alluvia! (P-1), Lewis Shale (P-3), 2nd White (P-5), and 3rd White Sandstone (P- <br />8) wells in Pyeatt Gulch all contain water with field pH that is generally near neutral. The <br />field pH values for well 81-03a are generally above 8 units. The field pH values for the <br />GLUX-1 well were 7.8 and 7.4 in 2000. The field pH for well GMP-1 was near 8 in 2000. <br /> <br />3-9 <br />