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Marrb 2007 Hgden Guttb Ioadaut - 2006 AuuualHydrology Report ~ Page S <br />While sulfate and total dissolved solids (TDS) do not have agriculrure standazds promulgated in <br />Colorado, the Wyoming Depaztment of Environmental Quality has established livestock drinking <br />water standazds for these constituents that can be used as benchmark values to assess the <br />appropriateness of water for agriculture use. Sulfate and TDS concentrations commonly exceed the <br />WDEQ values. <br />• sulfate (guideline of 500 mg/I) <br />HGSDl - 5/8/06: 960 mg/1; 10/12/06: 1,420 mg/1 <br />HGSD3 - 5/8/06: 1,180 mg/1; 10/12/06: 1,810 mg/1 <br />• total dissolved solids (guideline of 2,500 mg/I): <br />HGSDl -10/12/06: 2,570 mg/1 <br />HGSD3 -10/12/06: 3,270 mg/1 <br />While [here values were greater than the benchmazk values used by WDEQ, historic values for these <br />constituents at both locations typically exceeded the respective benchmazk values. <br />Time-trend plots of manganese, sulfate and TDS concentrations aze presented in Appendix C. <br />3.3 GROUNDWATER DATA <br />Groundwater data for 2006, as well as historic data collected since 1993 aze presented in Appendix D, <br />Groundwater Quality Data. In 1993, HGTI installed HGDAL3 as a "new" downgradient alluvial <br />monitor well in response to CDMG concerns that the two existing alluvial wells, HGDALl and <br />HGDAL2, might have been paztially completed in the Lewis Shale, which could comprise the data. <br />Groundwater quality data was collected from monitoring wells HGDALl and HGDAL2 between <br />1987 and 1995. Groundwater monitoring of these two monitor wells ceased in 1995; these two wells <br />ue inactive. As part of the TR-06 adequacy review, CRMS raised concerns about the lack of an <br />upgradient alluvial monitor well at the Loadout. Consequendy, HGTI installed a "new" upgradient <br />well, HGDAL4 in November 2005. The locations of the groundwater monitoring wells aze shown on <br />Figure 1, Moxitoring Site Lacationr, <br />The spring runoff monitoring event occurred on May 8, 2006. The fall monitoring event was <br />conducted on October 12, 2006. <br />In general, the alluvial groundwater concentrations from HGDAL3 in the 2005 samples were similar <br />to previously observed values. All constituent concentrations were within historic ranges. While the <br />manganese concentrations exceeded the manganese numeric standard (0.2 mg/I) in both samples, the <br />values were within the historic range. <br />The observed concentrations in the HGDAL4 sample were generally similaz to what was observed in <br />the HGDAL3 samples. Most trace element concentrations were reported as less than the method <br />detection ]unit. There were reported concentrations Eor azsenic (October sample: 0.0013 mg/1), <br />boron, cadmium (October sample: 0.0002 mg/1) and manganese. Major ionic constituents (i.e., <br />calcium, magnesium, sodium, bicarbonate, chloride and sulfate) were generally less than their <br />respective values in the corresponding HGDAL3 sample. <br />Time trend plots for common constiruents aze presented in Appendix D <br />Hydro-Environmental Solutions, Inc. <br />P.O. Bax 772996 <br />57 70r^ Strzet, Suite B <br />Steamboat Spring; CO 80477 <br />(970) 871-6725 <br />