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sample. The parameter list used for ell wells sampled in 1993 is given on Table 4. <br />Analyses have been performed by AC2 Laboratory in Steamboat Springs, Colorado since May <br />31, 1983. AC2 Laboratory performs all anaLys es by EPA or equivalent methods. Samples ere <br />delivered the day of collection to the lab in an iced cooler. The following discussion of <br />the analytical data collected during the reporting period is arranged by strata being <br />monitored and coincides with the format (by aquifer type) in which the analytical data are <br />presented in Appendix D. Sampling techniques for each well are given in the remarks page <br />in the same appendix. Abbreviations used in the remarks are: CV = casing volume, BHV = <br />bore hole volume, EC = electrical conductivity, and FP = field parameters (pH, <br />temperature, and electrical conductivity). <br />Tables 5 through 10 tabulate the percentage of milliequivalents per liter of major ions <br />and total dissolved solids (TDS) for each well sampled in 1993. Historical data is <br />provided for comparison purposes. The following discussion of water quality will be <br />limited to a description of major ions and total dissolved solids (TDS) Concentrations. A <br />separate section, Comparison of Ground Water Quality to Water Use Standards, will discuss <br />any samples that exceed water use standards. <br />Alluvium. Well 32-A, located furthest upstream on Little Grassy Creek, displays a <br />CaMgNa-504HC03 type water (Table 5). The average annual TDS value of 1520 mg/t for this <br />year is within the range of those values previously observed. Progressing down valley, <br />the alluvium picks up spoils water discharge typified by en increase in sulfate and TDS <br />and a corresponding decrease in sodium and potassium at Well b-A. The annual average TDS <br />value of 3307 mg/l for Well 6-A also is within the range previously observed. Well 31-A2 <br />is downstream of the discharge of the Wadge Impoundment. It is a CaMg-S04 type water with <br />the average annual TDS value of 2733 mg/l; again within the historic range. <br />The one well sampled in the Grassy Creek alluvium, 33-A, has a CaMg-SO4HC03 type water. <br />The annual average TDS value of 7447 mg/l is within the historic range. <br />In the Cow Camp Creek (tributary of Fish Creek) alluvium, water quality is measured at two <br />wells. Nell 46-A has a MgCaNa-SO type water. The annual average TDS values for this <br />4 <br />well peaked in 1987 (3,426 mg/l ), then steadily decreased until 7992 (2,339 mg/l ), but has <br />• increased slightly this year (2,603 mg/l). This is in spite of the fact that 705 values <br />upstream at the 004 pond have increased steadily since 1982 (3,494 mg/l 7993 annual <br />5 <br />