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TAgIE 7-33 • <br />Summery of Tril{near Diegrem end <br />Schoeller Plot Analyses <br />Steam Site Summary Discussion <br />TSSF2 Three water types, principal water type is MgCa504 XC03; appreciable cation <br />end anion scatter with no overall trend; a majority of the cation scatter is <br />due to increase in Mg end we concentrations while the anion scatter is <br />largely the result of increasing S0~ and decreasing XC03. Depending on the <br />length of the snowmelt influence, TDS appears to initially increase in early <br />Spring then decrease into Mey end increase into the Summer. <br />YSA F4 Four water types, two principal water types are MgCe504HC03 and CaxgSO4HL03, <br />these two types account for 82X of the water quality analyses et this site; <br />there is some cation scatter and considerable anion scatter on the trilineer <br />and Schoeller plots. A majority of the cation scatter is attributable to Ca <br />and Mg variability and the anion scatter is principally the result of S04 <br />variability. <br />YSGFS Two water types, principal type is CaM gSO4xC03, there is very minimal cation <br />scatter and measurable anion scatter with no overall trend. A majority of • <br />the anion scatter is due to variability in the XC03 and SO` concentrations. <br />TDS tends to increase in early Spring, then decrease into April and Mey and <br />then increase in the Summer. fell levels appear comparable to the Summer <br />levels. <br />J <br />102 <br />