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Moun(ain Coal Compam 1997 Annual Hydrology Report Wes EIk Mine <br />Fork drainage basin; (3) springs and other water resources above the B-Seam in the Jumbo <br />• Mountain area in the North Fork drainage basin; and (4) springs above the E-Seam in the Dry <br />Fork drainage. Field water quality samples were taken three times during the water year at all <br />stations that were flowing. On an annual basis, all stations were sampled and the samples were <br />analyzed for a full suite of pazameters (Table 2). <br />Baseline monitoring continued on eight springs initiated in WY96 (15-1, 15-2, E15-3, E10-2, <br />E10-3, E10-4, 26-1 and 27-1) as well as spring J-4, which was re-initiated in WY96. Baseline <br />monitoring was to be conducted on springs G-7 and G-8 to re-establish baseline, however these <br />springs were sampled under the regular monitoring program. The springs will be sampled under <br />the baseline schedule in WY98. No new springs were added to the monitoring program in <br />WY97. <br />MCC, in cooperation with the U.S. Forest Service District Office in Paonia, Colorado, has agreed to <br />informally monitor the U.S. Forest Service surface water resources, as depicted on Map 3, that are <br />located directly over panels to be mined, and within the angle-of--draw per the agreement letter in <br />Exhibit 19C of the permit. These resources are listed in Table 3. <br />Sampling Methods <br />Monitoring included spring flow, field parameters, and laboratory parameters. In sampling springs. <br />a location was selected which approximated a channel as closely as possible. A step may have been <br />cut into the channel base to facilitate positioning of a container. Flow measurements were made by <br />• the timed volumetric method: where a field technician times the filling of a container of known <br />volume to determine the flow rate. Several measurements were taken and averaged prior to <br />reporting. Field parameters of temperature, pH, and conductivity were made at the springs by <br />collecting a sample from the flowing springs and measuring the sample for the parameters using <br />standard instruments that were calibrated in the field. Samples for analysis of laboratory parameters <br />per Table Z, Footnote 2 were collected by filling a clean, pre-fixed sample bottle from non-aerated <br />spring flow. Care was taken to minimize any increases in turbidity. Sample bottles were sealed, <br />labeled, placed on ice, and transported to the laboratory for analysis. <br />Groundwater Monitoring <br />There were thirty-two wells in the WY97 groundwater monitoring program and are summarized in <br />Table 4 along with the formation each of the wells monitor. Table 5 provides more detail on the <br />completion of each of the wells in the monitoring program. Field water quality samples were taken <br />three times during the water year at all stations if sufficient volume was present to fill the <br />appropriate sample containers and if the well allowed access to the formation of completion. On an <br />annual basis, all stations were similarly sampled and the samples were analyzed for a full suite of <br />parameters (Table 4), when conditions allowed. <br />• <br />8 -03 .4 0 Page {Vrig t Water ngineers <br />