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Pierre River Mine Project

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WATER ERCB SIRS 46 – 79<br />

Question No. 58<br />

Section 7.1<br />

quality constituents and that changes in water quality in the Athabasca <strong>River</strong><br />

would have negligible effects on aquatic, human and wildlife health.<br />

Request Volume 2, Section 21.1, Page 21-14, Supplemental Information Responses.<br />

Shell states, “The rates of inflow presented for the <strong>Pierre</strong> <strong>River</strong> <strong>Mine</strong> LSA<br />

include lateral groundwater inflows to the LSA from up gradient areas.”<br />

58a Describe the simulation of lateral recharge from upgradient areas in the model.<br />

Response 58a Lateral groundwater inflow rates to the local study are (LSA) were calculated<br />

based on the simulated groundwater flows across the LSA boundaries in the<br />

regional groundwater model (see EIA, Appendix 4-1, Section 1.2.4.4, page 94).<br />

In the model, groundwater levels from the regional model were represented as<br />

general head boundaries at the lateral boundaries of the <strong>Pierre</strong> <strong>River</strong> <strong>Mine</strong> local<br />

model in layers 4 (base of Quaternary), 9 (Basal Aquifer) and 12 (Methy<br />

Formation).<br />

Question No. 59<br />

Request Volume 2, Section 21.1, Page 21-59, Supplemental Information Responses.<br />

Shell states, “The Eymundson Sinkholes do not appear to have a marked<br />

influence on the groundwater flow pattern in the Quaternary deposits.”<br />

59a Provide the technical justification for this assumption including any geophysical<br />

surveys or detailed Karsts delineation studies.<br />

Response 59a The technical justification for this statement is the groundwater flow patterns<br />

illustrated in Figures 37 and 38 of the Hydrogeology Environmental Setting<br />

Report (WorleyParsons Komex 2007). Based on available groundwater-level<br />

information from piezometers in Quaternary deposits near the Eymundson<br />

Sinkholes, the groundwater flow patterns within and outside of the Eymundson<br />

Sinkholes Environmentally Sensitive Area (ESA) are similar. Overall, the<br />

groundwater flow patterns in the Quaternary deposits reflect topographical<br />

control and do not suggest any considerable alteration of the regional flow<br />

pattern within or near the Eymundson Sinkholes ESA.<br />

April 2010 Shell Canada Limited 7-13<br />

CR029

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