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2009-07-01_REPORT - C1980007 (6)
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2009-07-01_REPORT - C1980007 (6)
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Last modified
8/24/2016 3:48:23 PM
Creation date
7/1/2009 1:52:42 PM
Metadata
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Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
REPORT
Doc Date
7/1/2009
Doc Name
2008 Annual Hydrology Report
From
HydroGeo, Inc
To
DRMS
Annual Report Year
2008
Permit Index Doc Type
Hydrology Report
Email Name
TAK
Media Type
D
Archive
No
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West Elk Mine 2008 Annual Hydrology Report 16 <br />monitoring data than the Lower Dry Fork flume since it isn't influenced by variations related to <br />reservoir activities. Baseline monthly monitoring of the Minnesota Reservoir Flume began in the <br />spring of 2006 and included measuring instantaneous flow, collecting field water quality data, and <br />collecting samples for laboratory water quality analyses from April 2006 through October 2006 <br />(CDMG, 2006). Routine monitoring (three times per year) at this location began in WY 2007. <br />3.1.4.3 South Prong Creek <br />South Prong Creek is an ephemeral stream that is tributary to upper Minnesota Creek. The north <br />fork of South Prong Creek drains the southern portion of the SOD mine plan area. The monitoring <br />station on South Prong Creek is located at the mouth of the drainage and does not have a flume or <br />data logger (Map 2). Preliminary flow and water quality data were collected during a one time <br />sampling round of this site in 2005 (HydroGeo, 2006). Baseline monitoring is scheduled to resume <br />in 2017, or at least one year prior to when mining begins in the area to monitor potential mining <br />induced impacts. <br />3.1.5 Temperature Monitoring Sites <br />The surface lands of the West Elk Mine are drained to the north by the North Fork of the Gunnison <br />. River. Water from the mine water pumping facility (MWPF) discharge point enters the North Fork <br />of the Gunnison River from Sylvester Gulch. In September, 2007, MCC contracted GEI <br />Consultants (GEI) to install temperature loggers (a.k.a. thermistors) in Sylvester Gulch and in the <br />North Fork of the Gunnison River in order to monitor the effect of discharge from Sylvester Gulch <br />on the water temperature of the North Fork of the Gunnison River. Five temperature loggers <br />(ONSET Corp. HOBO Water Temp Pro v2) were deployed within Sylvester Gulch, and three <br />within the North Fork of the Gunnison River (Table 4). The loggers were installed by GEI on <br />September 21, 2007 and were programmed to record temperature data at 15 minute intervals. Data <br />from the temperature loggers are downloaded on-site monthly by HydroGeo (whenever snow/ice or <br />dangerously high water levels do not prevent access to the loggers) using a laptop computer and an <br />ONSET adapter cable. <br />Each temperature logger was attached to a steel rebar rod using galvanized cable and stainless steel <br />hose clamps. The rebar was driven into the streambed. In October, 2007 HydroGeo re-anchored <br />each of the loggers to secure points on the shore using 1/16 inch aircraft grade galvanized steel <br />cable. In the summer of 2008, each logger was reprogrammed to record temperature data at one- <br />hour intervals, in order to increase the data logger battery life, and to increase the length of time it <br />takes for the logger memory to become full and stop recording. The temperature logger sites were <br />June 2009 HydroGeo, Inc.
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