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Pierre River Mine Project

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WATER AENV SIRS 15 – 43<br />

Section 12.1<br />

1-5 of the Muskeg <strong>River</strong> <strong>Mine</strong> Expansion EIA. Considering that most of the<br />

<strong>Pierre</strong> <strong>River</strong> <strong>Mine</strong> ETDA footprint will consist of areas of TT and of areas of<br />

tailings sand that are overlain by MFT, which will effectively limit the seepage<br />

rate to that of MFT, the overall hydraulic conductivity of 1 x 10 -8 m/s assigned to<br />

the ETDA deposits is considered conservative, leading to higher assumed<br />

seepage rates. Potential reduction of tailings sand hydraulic conductivity as a<br />

result of bitumen or sludge deposits and entrapment (Hunter, 2001) were not<br />

considered.<br />

ETDA Fluid Level Elevation for GHB<br />

The fluid level specified for the ETDA was constant and was based on the fluid<br />

elevation that will be present following complete filling of the ETDA. In reality,<br />

the fluid elevation will rise with time through the active lifetime of the ETDA.<br />

Therefore, the vertical hydraulic gradient between the ETDA and the underlying<br />

aquifer was also conservatively represented, as higher vertical gradients lead to<br />

higher seepage rates.<br />

Underlying Aquifer Hydraulic Conductivity<br />

Reference<br />

There is some uncertainty in the distribution and hydraulic conductivity of the<br />

sediments which underlie the ETDA, as described in EIA, Volume 4B, Appendix<br />

4-1, Section 1.2.4.5, page 98. Additional conservatism was built into the<br />

simulation of ETDA seepage, as the entire aquifer underlying the ETDA was<br />

represented by relatively high hydraulic conductivity sandy materials, with the<br />

assigned hydraulic conductivity (5 x 10 -5 m/s) being at the upper end of the range<br />

of hydraulic conductivity values measured in Quaternary deposits in Lease 9.<br />

Hunter, G. P. 2001. Investigation of groundwater flow within an oil sand tailings<br />

impoundment and environmental implications. M.Sc. Thesis, University<br />

of Waterloo,<br />

Request 17d Shell mentions that the expected time for groundwater extraction rates to<br />

stabilize or reach steady state will be defined when a detailed groundwater<br />

extraction system, with actual expected pumping well locations is designed and<br />

produced. Describe the timeframe and the standard procedures for designing<br />

and implementing a detailed groundwater extraction system.<br />

Response 17d The detailed design of a seepage management system requires that the conceptual<br />

models used to conservatively assess potential environmental impacts related to<br />

ETDA seepage be refined and updated. This typically requires additional<br />

geological and hydrogeological information specific to the proposed ETDA site<br />

and surrounding area, and tailoring of plans to align with detailed design<br />

purposes.<br />

12-8 Shell Canada Limited April 2010<br />

CR029

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