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GENERAL55767
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Last modified
8/24/2016 8:40:44 PM
Creation date
11/23/2007 10:45:39 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1977378
IBM Index Class Name
General Documents
Doc Date
8/6/2003
Doc Name
Consent Decree
From
Gold King Mines Corporation
To
DMG
Media Type
D
Archive
No
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Koehler Tunnel bulkhead design Page 2 July 31, 2003 <br />shaft collar elevation. The maximum static hydraulic head is <br />497-ft above the bulkhead, a hydraulic pressure of 215 psi. The <br />design maximum 0.136 g horizontal earthquake acceleration was <br />calculated from the maximum credible 6.5 magnitude earthquake <br />along the Ridgeway Fault, 20 miles to the north. Previous <br />earthquake studies for the Sunnyside Gold Corp. tailings at <br />Gladstone (Sullivan, et al, 1980; Weisser, 1982; Knight Piesold <br />Co., 1988) predicted a maximum credible horizontal acceleration of <br />0.087 g at Gladstone, 25 miles south-southeast from the Ridgeway <br />Fault. It was conservatively assumed that the earthquake <br />acceleration would act along the axis of the Koehler Tunnel. The <br />tunnel axis is actually at a large angle from the line-of-sight <br />toward the Ridgeway Fault which should reduce the maximum <br />earthquake acceleration component along the tunnel axis. <br />The Koehler Tunnel was inspected on July 18, 2003 to a <br />distance of approximately 600-ft from the portal, Figure 1. The <br />Koehler Tunnel was driven S74°E. The initial 600-ft of the tunnel <br />was dry except for the water flowing along the invert, despite two <br />steeply dipping joint sets. The water in the tunnel is flowing <br />from further back in the tunnel. One of the steeply dipping joint <br />sets is nearly vertical and is sub-parallel to the tunnel axis. <br />Individual joints of this joint set locally form the entire right <br />tunnel rib for lengths of up to 20-ft. The other joint set dips <br />roughly 65° to the west and strikes nearly perpendicular to the <br />tunnel axis. This joint set forms the roughly 100-ft high dip <br />slope cliff behind the portal. The tunnel walls were coated with <br />a generally thin layer of red mud to the level of water that had <br />been impounded behind a debris dam in the portal area before the <br />debris dam was removed for access. An up to 1-ft thick layer of <br />red mud was resting on the tunnel floor, except where disturbed by <br />walking in the tunnel. The location selected for the Koehler <br />Tunnel bulkhead, between Station 3+02 and Station 3+14, is in a <br />dry and apparently impermeable rock section of the tunnel. The <br />ribsides and back at the bulkhead section selected are irregular <br />and contain only short segments of the sub-parallel joint set. <br />The joint spacing in the back and ribs at the bulkhead site <br />appears to average approximately 1-f t, or more, in all directions <br />and to be minimally altered. The irregularities in the back and <br />ribs are more than sufficient to resist the thrust from the <br />maximum static water head and maximum credible earthquake <br />acceleration. The slight narrowing of the tunnel toward the <br />portal within the selected bulkhead location will increase the <br />bulkhead's thrust resistance. The porphyritic rock appears to be <br />extremely competent and hard. Block samples were barred from the <br />back and ribs at the bulkhead site for strength testing and have <br />been sent for compressive strength testing. <br />
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