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Pierre River Mine Project

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WATER ERCB SIRS 46 – 79<br />

Question No. 67<br />

Request Volume 4A, Section 6.1.2, Page 6-222.<br />

Section 7.1<br />

Shell states, “Simulation results suggest that in the absence of mitigation, TDS<br />

will have migrated through the overburden deposits to Big Creek and the<br />

Athabasca <strong>River</strong> valley by 2031 (Figure 6.3-90), 13 years after the initiation of<br />

ETDA operation.”<br />

67a Define the techniques (e.g. pumping tests, geophysical surveys, infiltration tests)<br />

and assumptions that were used in assigning the hydraulic parameters to the<br />

various formations in the conceptual model.<br />

Response 67a Within the local study areas (LSAs) for each of the <strong>Pierre</strong> <strong>River</strong> <strong>Mine</strong> and<br />

Jackpine <strong>Mine</strong> Expansion, hydraulic parameters were assigned based on<br />

geometric mean values calculated from single well response tests. The response<br />

tests were conducted on monitoring wells installed in Quaternary deposits and<br />

the McMurray Formation (including the basal aquifer) during the baseline<br />

hydrogeological investigation (WorleyParsons Komex 2007).<br />

Reference<br />

Question No. 68<br />

In areas outside of the <strong>Pierre</strong> <strong>River</strong> <strong>Mine</strong> and Jackpine <strong>Mine</strong> Expansion LSAs<br />

and for the Devonian formations, model hydraulic parameters were assigned<br />

based on the parameterization described in previous hydrogeology baseline and<br />

EIA investigations in the region. For some formations, other data sources (i.e.,<br />

laboratory permeability testing and drill-stem testing data) were also reviewed if<br />

available well response testing (i.e., pumping test and single well response test)<br />

data were insufficient.<br />

WorleyParsons Komex. 2007. Hydrogeology Environmental Setting Report for<br />

the Jackpine <strong>Mine</strong> Expansion and <strong>Pierre</strong> <strong>River</strong> <strong>Mine</strong> <strong>Project</strong>. Prepared<br />

for Shell Canada Limited, Calgary, AB. Submitted December 2007.<br />

Request Volume 4A, Section 6.3.6, Page 6-229.<br />

In Figure 6.3-95, the ETDA is overlying the basal aquifer outcropping recharge<br />

area; and in Figure 6.3-102, the intercepting wells are only capturing horizontal<br />

flow from the overburden sediments.<br />

68a Was the direct contact of the external tailings dump area (ETDA) with the basal<br />

aquifer considered in the model? If yes, then discuss the assumptions considered<br />

to simulate this zone.<br />

7-22 Shell Canada Limited April 2010<br />

CR029

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