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Investigating the Connection of Turquoise Lake and Mine Tunnel Flow in the Sugarloaf Mining District Using Dissolved Gas Tracers

William E. Sanford
Department of Geosciences
Colorado State University

Abstract:  The purpose of the study is to determine if there is a hydrologic connection between the waters of Turquoise Lake and Dinero Tunnel drainage water (Sugar Loaf Mining District).  Preliminary site investigations suggest that mine tunnels, especially the Dinero tunnel, may intersect North-South trending faults, mineral veins, and mine audits inundated by the lake, creating zones of preferential flow during periods of elevated lake levels resulting from spring snowmelt.  Several intact and collapsed mine audits exist along the south shore of Turquoise Lake and are submerged during normal spring and summer lake levels.  The study will involve injecting tracers directly into mine audits submerged by the elevated lake levels and sampling of waters in the Dinero Tunnel.  A detection of the tracers in waters discharged at the tunnel will confirm a connection.  Two dissolved gasses will be used as tracers, helium and sulfur hexafluoride.  Helium gas provides a low cost, simple method of making corrections of diffusive gas losses during transport. Sulfur hexafluoride has a very low detection limit compared to its solubility which allows an analysis over several orders of magnitude.

Funding Agency:
Bureau of Reclamation
#03FC601821
$15,832

 

 

                        

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