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Well GPI has water with pH values of 7.9 to B.S, while well <br />• GP2 water is generally slightly above neutral. The pH values for <br />wells GP3 and GP4 have shown little change for water collected <br />from the HI and KLM aquifers, respectively. Well GP3 teas had pH <br />values near neutral, while values for well GP4 have been slightly <br />less than 9 with the March 1988 value at 7.8. <br />Wells GPS and GPb are completed in the QR aquifer. The pH <br />values for both wells have been similar at an average value of <br />8.6. The 1988 pH values for well GPb have decreased to near 7. <br />The alluvial, Lewis Shale, Second White and Third White <br />Sandstone aquifers in Pyeatt Gulch all contain water with a pH <br />that generally is slightly above 7. Values for 1988 are near <br />neutral. <br />HI aquifer well GP7 has typically had water with pH values <br />slightly above 7. Well GP8 is completed in the KLM aquifer and <br />has water with a pH of near 8 with the September 1987 value at 7. <br />Third White Sandstone aquifer well GP9 pH values are typically <br />slightly above 7. <br />The pH values for well 81-03a have been near 8.5. The 1986 <br />values for well JI during March and June were slightly lower than <br />the remainder of the 1988 values. The 1988 pH values for the COY <br />well were stable. The pH values for the Glux-1 well are near <br />neutral. Cottonwood Spring had near neutral pH values during <br />most of 1988. The West Buzzard seep had a pH of near 8 during <br />1988, while No Name Seep had a pH of 7.3. <br />3.4 SAR <br />The sodium-adsorption ratio (SAR) is tabulated on the second <br />3-19 <br />