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HYDRO27875
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HYDRO27875
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Entry Properties
Last modified
8/24/2016 8:47:14 PM
Creation date
11/20/2007 8:34:38 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1978091UG
IBM Index Class Name
Hydrology
Doc Date
9/4/2007
Doc Name
SWMP control response
From
Gault Group Inc
To
Water Quality Control Division
Media Type
D
Archive
No
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x: <br />z: <br />Currently, the mine is owned by LKA Int., and operated by Au Mining. The methods by which <br />water is managed at the site has evolved over time in response to site conditions and regulatory <br />guidance. The underground features manage encountered water by use of an underground <br />infiltration sump (as per direction provided by H. Posey/DRMS; 2000). The site also has a <br />current stormwater plan that addresses stonnwater related to surface disturbance azeas on the <br />mine. As part of the existing stormwater management practices, an evaporation sump is <br />maintained on the Leve16 pad that captures any pad sheet flow from flowing offsite. <br />Up unfil recently, there has been no concern raised in regazds to seeps located at the toe of the <br />waste rock pile associated with the Leve16 pad, lazgely because these seeps have been non- <br />existent. As previously described, the waste rock pile occurs on top of the historic Deadman <br />Gulch channel. The Gulch is intermittent and flows only in response to substantial snow- <br />precipitation yeazs. Therefore it stands to reason that the seep flow is closely associated to the <br />Deadman Gulch flows, and not related to any water management strategy at the mine site. <br />In order to delineate the water source that is related to the waste rock toe seeps, this Chemical <br />Trace study was completed. A Chemical Trace study is designed based upon the premise that <br />water can be `typed' by analyzing the water for common anion and cation content. The results <br />from the various samples can be wmpazed to determine if samples aze of the same type, thereby <br />delineating possible flow pathways. In this study, three possible sources of water were <br />tentatively linked to the waste rock toe seep water. These include the underground managed <br />water associated with the mine workings, stormwater infiltrated through the stormwater sump on <br />the Leve16 pad surface, and Deadman Gulch base flows. <br />Methods <br />A single sampling event during spring melt conditions was completed in order to gather the <br />various samples necessary for this study. On June 20, 2007 the Chemical Trace suite of samples <br />were collected and included eight water samples and four solids samples. Figure 1 depicts a <br />conceptual diagram depicting each sample location. A nan•ative description of each location is as <br />follows; <br />Surface Water Locations <br />• SEEP (BKG): a seep adjacent to the Leve16 pad that occurs within the background <br />setting for Deadman Gulch, <br />• DM-BKG: a location within Deadman Gulch above the Leve16 pad area that would <br />represent background, <br />• WRT-A: a seep located at the toe of the Leve16 waste rock dump, <br />• WRT-B: a seep located at the toe of the Leve16 waste rock dump, <br />• DM-MZ: a location downgradient of the WRT locations that captures the mixing zone of <br />the combined flows from the WRT seeps, <br />• DM@HWY149: Deadman Gulch at the Highway 149 crossing, and <br />• SUMP: the underground sump within the Leve16 mine workings <br />• SUMP-DUP: a field created duplicate for the SUMP location. Results were used for <br />Quality Assurance/Quality Control purposes. <br />Page 8 of 16 <br />
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