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REP14825
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REP14825
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Last modified
8/24/2016 11:44:34 PM
Creation date
11/27/2007 1:31:08 AM
Metadata
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Template:
DRMS Permit Index
Permit No
C1981013
IBM Index Class Name
Report
Doc Date
6/14/1984
Doc Name
1st Quarter 1984 Water Sampling
Permit Index Doc Type
Hydrology Report
Media Type
D
Archive
No
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constructed and Stevens Type F continuous recorders were installed. During each visit to <br />these two stations, the records were visually inspected and maintained. This included: <br />1. Checking to see that the clock mechanism was functioning properly and marking the <br />recorder charts with data points; <br />2. Comparing the staff gage reading and recorder stage height to verify proper <br />functioning of the stage recorder; <br />3. Removing the chart from the recorder indicating the station, date, time, stage <br />height, and initials of the person servicing the recorder; and <br />4. Back-flushing the inlet pipe to prevent sediment build-up and clogging. <br />2.2 Results <br />Results of all surface water chemistry analyses and flow measurements are <br />presented in Tables 2-1 through 2-11. <br />Surface water sampling during the quarter related to a late winter-early spring <br />period of the year. Snow melt and runoff occurred in the immediate area, however, spring <br />snow melt from the higher mountains had not yet begun. On the Purgatoire River, diurnal <br />flow fluctuations were apparent during the samplings caused by the freeze/thaw cycle of <br />the day. Water quality parameters collected on the Purgatoire over the three stations <br />found pH ranging from 7.3 to 7.9 (S.U.), conductivity ranging from 286 to 415 (umhos), <br />temperature ranging from 1.0 to 15.6 (oC), and dissolved oxygen ranging from 1.4 to 4.0 <br />(ppm) (Tables 2-1 through 2-3). These measurements are within normal stream conditions <br />and indicate a stable base stream flow. <br />Samples collected at the two mine discharge points indicate an elevated Level of pH <br />and conductivity (Tables 2-4 and 2-5). Discharge of mine water from the Golden Eagle <br />Mine is into Ciruela Canyon. With the coarse nature of Ciruela and Purgatoire alluvial <br />materials, this discharge is absorbed into the alluvium before the confluence with the <br />Purgatoire River. As a result, the discharge does not have a direct effect on surface <br />water quality but may have potential effects on alluvial ground water (to be disccussed in <br />Section 3.0). The New EIk Mine water discharge is directly into the Purgatoire River, <br />however, dilution with the Purgatoire indicates negligible effects at the two downstream <br />stations. <br />
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