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• <br />water collected from the HI and KLM aquifers, respectively. Well GP3 <br />has had pH values near neutral, while values for well GP4 have been <br />slightly less than 9. <br />Wells GP5 and GP6 are completed in the QR aquifer. The pH values <br />for both wells are similar at an average value of 8.6. <br />The pH value for well 81-03A was 8.7 for September of 1987. The <br />pH values from alluvial wells J1 and Coy have been slightly above 7 <br />and seem to be stable. pH values for the Lux well and the West Spring <br />on the Lux property are near 6, while the North Spring has a pH near <br />neutral. Colt Seep and Cottonwood Spring had near neutral pH values <br />• in 1987. <br />3.3 SAR <br />The sodium-absorption ratio (SAR) is tabulated on the second <br />series of pages in Table B-1, starting on page 8-53. The SAR values <br />measured for water from well GA1 and GA2 are low with an average value <br />of approximately 0.3. SAR values for water from well GB2 are <br />typically slightly less than one. The SAR from well GBS has typically <br />been slightly less than 10, while the last three complete analyses in <br />August 1985, September 1986 and September 1987 have shown SAR values <br />significantly higher. A definite trend in SAR is not observable. <br />The SAR of water from wells GC1, GC2, and GC3 have been typically <br /> <br />3-10 <br />