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Pierre River Mine Project

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WATER AENV SIRS 15 – 43<br />

Question No. 30<br />

Request Volume 2, SIR 298a – d, Page 21-53.<br />

Section 12.1<br />

It is likely that the polishing pond temperatures for Jackpine and <strong>Pierre</strong> <strong>River</strong><br />

will be within close range of each other. Similarly, the Muskeg and <strong>Pierre</strong> <strong>River</strong><br />

streams also exhibit comparable water temperature regimes. On this basis, the<br />

four questions (i.e., SIR 298 a – d) are applicable to <strong>Pierre</strong> <strong>River</strong>.<br />

30a Provide answers to the four questions posed, in terms of polishing pond<br />

temperatures of the <strong>Pierre</strong> <strong>River</strong> project and the streams of the <strong>Pierre</strong> <strong>River</strong><br />

project that flow to the Athabasca <strong>River</strong>.<br />

Response 30a The following are responses to the May 2009 <strong>Pierre</strong> <strong>River</strong> <strong>Mine</strong>, Supplemental<br />

Information, Volume 2, SIR 298 a to d, in terms of polishing pond temperatures<br />

of the <strong>Pierre</strong> <strong>River</strong> <strong>Mine</strong> <strong>Project</strong> and the streams of the <strong>Pierre</strong> <strong>River</strong> <strong>Mine</strong> <strong>Project</strong><br />

that flow to the Athabasca <strong>River</strong>:<br />

Original SIR 298a<br />

Clarify the first sentence of the pre-amble since most of the polishing pond<br />

temperatures presented in Figure 6.5-2 (Page 6-380) are above the seventy-fifth<br />

percentile of the Muskeg <strong>River</strong>, and not within the range of monthly background<br />

temperatures.<br />

Figure 6.5-2 shows that the range of polishing pond temperatures (0.0 to 20.6ºC)<br />

is within the range of background temperatures for the Muskeg <strong>River</strong> (-0.6 to<br />

23.3ºC). Episodic periods of warmer temperature for polishing ponds have been<br />

observed before ice-cover from August to December, and a few were outside of<br />

monthly background ranges (e.g., October 25, 2002). These periods corresponded<br />

to short-term periods of high solar radiation and air temperatures, when bottom<br />

heat flux from the shallow polishing ponds can appreciably affect water<br />

temperature.<br />

Original SIR 298b<br />

How will higher temperatures quantitatively influence downstream temperatures<br />

in the Muskeg <strong>River</strong>; that is, what will be the new downstream water<br />

temperatures at different times of the year under a range of river stages?<br />

A conservative temperature balance of a “worst-case” scenario for thermal<br />

impacts from polishing ponds releases was calculated as part of the EIA and is<br />

discussed in EIA, Volume 4A, Section 6.5.5.1, page 6-382. It was based on:<br />

• mean September and October streamflows and water temperature for the<br />

Muskeg <strong>River</strong><br />

• high flow from the polishing ponds<br />

12-42 Shell Canada Limited April 2010<br />

CR029

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