Laserfiche WebLink
S~csr - 2.04.7 <br />included, az a min~rm~m analysis of surface water samples for pH, electrical conductivity (EC), total <br />• suspended solids ('I'SS), total dissolved solids ('IDS), total iron (Fe), and total manganese (NII~. <br />Table 2.04.7-T1, Surface and Ground Water Parameters, lists the analysis parameters for ongoing <br />operational hydrologic monitoring. Generally, bazeline and operational surface water monitoring have <br />focused on specific mine disturbance areas, so there have been some changes over time in the <br />designated surface water monitoring sites. <br />Table 2.04.7-T5, Iltstoric Surface Water Monitoring Suntnrary, identifies all of the sites for which <br />surface water monitoring recondc are available and notes the monitoring interval(s) for each. The <br />following sections summarize water quahry characteristics, based on available monitoring and analysis <br />infomtation, for each of the identified surface drainages or drainage categories. <br />North Fork of the Gunnison River -Information on the quality and characteristic of surface water <br />flows in the North Fork of the Gunnison River is based on sampling and analysis of wacer samples <br />from monitoring Stations R-1, R-2, G1, G2, NF-1, and NF-2. Bazed on available surface water <br />quality analysis resulu for the North Fork and az shown on Figure 2.04.7-F12, North Fork of the <br />Gunnison River Trilinear Diagram, the Nonh Fork surface water is a calciurrrcarbonate chemical <br />type. Analysa values indicate a neutral to moderately alkaline pH and low to moderate EC, TSS, and <br />TDS values, az summarized by Table 2.04.7-T6, North Fork of the Gunnison River Surface Water <br />Quality Surmnary. <br />In general, surface flows in the North Fork increase significantly following spring runoff, with a lag <br />corresponding to filling of Paonia Reservoir upstream and initiation of releazes from the reservoir. <br />Elevated flows continue throughout the summer, during irrigation season, declining in late surruner to <br />early fall. The increase in spring stream flows is typically accompanied by significant increases in TSS, <br />minor increases in TDS, and minor to moderate increases in Fe and Mg. Decreases in stream flows in <br />]ate summer and through the Fall and winter are commonly accompanied by minor to moderate <br />mcreazes in TDS az dilution effects decline with reduced flows. While the noted changes reflex <br />general trends, it u important to recognize that the pattern and range of water quality fluctuations are <br />not consistent over tune. Generally, the quality of the North Fork surface water is good in the <br />vicinity of the mine permit area. Some degradation of North Fork water quality occurs well <br />downstream from the mine az a result of imgation return flows. <br />Hubbard Geek -Information on the quality and characteristics of surface water flows in Hubbard <br />Geek is based on sampling and analysis of water samples from monitoring Stations H 1 and I-I2. <br />Bazed on available surface water quality analysis results for the Hubbard Geek and az shown on <br />Figure 2.04.7-F13, Hubbard Geek Trilinear Diagram, Hubbard Geek surface water it a calcium- <br />carbonate chemical type. Analysis values indicate a neutral to moderately alkaline pH and low to <br />moderate EC, TSS, and TDS values, az sunurrari7xd by Table 2.04.7-T7, Hubbard Creek Surface <br />Water Quality Sunurrary. The general pattern of seasonal water quality variation previously discussed <br />for the North Fork u ako observed for Hubbard Geek, with fluctuations being slightly more <br />pronounced and occumng earlier in the year due to a shover flow path for runoff and reduced <br />dilution effects. Generally, the quality of the Hubbard Geek surface water is good in the mine permit <br />and adjacent areas. <br />Intermittent and Ephemeral Drainages -Information on the quality and characteristics of surface <br />water flows in the numerous small intermittent and ephemeral drainages within the tnine permit and <br />adjacent areas is based on sampling and analysis of water samples from those monitoring stations <br />identified on Table 2.04.7-T5, Surface Water Monitoring Surmnary. Based on available surface water <br />quality analysis resulu for the intermittent and ephemeral drainages and az shown on Figures 2.04.7- <br />F14 Intermittent Drainages Ttilinear Diagram, and 2.04.7-F15, Ephemeral Drainages Trilinear <br />• Diagram, surface water in these drainages is typically a calciurrrcarbonate chemical type, with some of <br />the intemuttent drainages tending toward asodium-carbonate type. <br />PR04 2.04-69 Revised August 2000 <br />