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• Although the commonly exceeded domestic drinking water standards are considered secondary <br />by the CDOH (CDOH, 1994), the comparisons show that all geologic units monitored in the <br />Yoast mining area ere unsuitable for domestic use. Ground water from Yoest monitoring <br />wells would require substantial treatment and intensive monitoring according to <br />regulations prescribed for public water supplies before the water could be used for <br />domestic drinking water purposes. <br />Agricultural Meter Suitability. Table 7-21 presents apritulturel (irrigation) standards <br />developed by the CDON and other agencies for ground water. The agricultural standardc <br />were compared against sample constituent concentrations meecured in each Coast monitoring <br />well. Table 7-22 presentc the results of the comparisons in a format identical to Table <br />7-20. <br />The comparison results presented in Table 7-22 show that the manganese agricultural ground <br />water standard is commonly exceeded in the Annand Drew and Grassy Creek alluvium, end et <br />Sege Creek alluvial Yell YSALB. Yith the exception of the Yolf Creek coal seem, manganese <br />in all other units monitored at the Yoest mining area has been measured in excess of the <br />• egriculturel standard. Both the sulfate end TDS standards were commonly exceeded in all <br />units. The iron standard has been commonly exceeded in three of the four Grassy Creek <br />alluvial wells, end occasionally in Yadge overburden well YOV1. The pH standard was <br />exceeded et least once Cgreater then 8.5 S.U.) in all alluvium monitored, Yadge coal seam, <br />Madge overburden, end wedge underburden. The cadmium agricultural standard was only <br />exceeded once in the Yadge overburden (YOV28) end the Madge underburden (YYU28). The only <br />exceedence of the arsenic standard was observed et Yadge coal YeLI YY2 (250 ug/l); <br />however, this first measurement for arsenic is considered suspect es subsequent analyses <br />have not yielded detectable tontentrations. <br />Based on the comparisons, ground water in the alluvium monitored along Annand Drew, <br />Grassy, end Sege Creeks is unsuitable for egriculturel use. Yith the exception of the <br />Wolf Creek coal seem, occasional exceedences of manganese and pN et select bedrock wells <br />suggest that ground water quality in these bedrock units may also be unsuitable for <br />egriculturel purposes. <br /> Another method of assessing the suitability of ground water for irrigation is to use <br />• sodium-salinity hazard diagrams, where specific conducta nce is plotted against <br /> sodium-adsorption ratio (U.S. Salinity Laboratory, 1954). Figure 7-1 presents a <br /> sodium-salinity hazard diagram constructed with mean values for specific conductance (EC) <br /> 63 Revised 03/01/95 <br />