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Ontario Power Generation's Response to the Joint Review

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Attachment 1 <strong>to</strong> OPG letter, Albert Sweetnam <strong>to</strong> Dr. Stella Swanson, “Deep Geologic Reposi<strong>to</strong>ry Project for Low and Intermediate Level Waste – Submission of<br />

<strong>Response</strong>s <strong>to</strong> <strong>the</strong> Final Sub-set of Package #4 Information Requests”, CD#: 00216-CORR-00531-00143.<br />

IR# EIS Guidelines<br />

Section<br />

Information Request and <strong>Response</strong><br />

For <strong>the</strong> NE-GG1 (increased gas generation in <strong>the</strong> reposi<strong>to</strong>ry) and NE-GT5 (as NE-GG1 but also with increased<br />

permeability and reduced gas entry pressures for shaft seal materials) cases, enhanced gas generation causes<br />

reposi<strong>to</strong>ry pressures <strong>to</strong> increase rapidly, which in turn initiates gas flow up <strong>the</strong> shaft. This prevents complete<br />

resaturation of <strong>the</strong> shaft sealing materials below <strong>the</strong> Guelph Formation. However, as shown in Figure 2, <strong>the</strong> shaft<br />

materials above <strong>the</strong> Guelph Formation still resaturate quickly because of <strong>the</strong>ir proximity <strong>to</strong> more permeable rock and<br />

would isolate <strong>the</strong> biosphere from reposi<strong>to</strong>ry sourced gas.<br />

Figure 2: 2D Shaft Model Results for Ben<strong>to</strong>nite-Sand Shaft Material Saturation at Selected<br />

Formations<br />

The gas flows in <strong>the</strong> shafts calculated by T2GGM are imported directly in<strong>to</strong> <strong>the</strong> AMBER safety assessment model (see<br />

Appendix J.4.3 of QUINTESSA 2011). A range of calculation cases with differing assumptions as <strong>to</strong> <strong>the</strong> performance<br />

and resaturation rates of <strong>the</strong> shaft have been evaluated in AMBER for <strong>the</strong> Normal Evolution Scenario. These are<br />

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