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Management of Commercially Generated Radioactive Waste - U.S. ...

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5.3<br />

3. Tectonic stability <strong>of</strong> the repository area and region. Proper consideration <strong>of</strong><br />

this important factor will reduce the likelihood <strong>of</strong> deformation or disruption <strong>of</strong><br />

the host rock and thus increase the probability <strong>of</strong> repository integrity.<br />

4. Hydrologic regime (i.e., surface-water and ground-water considerations). This is<br />

important because the existence <strong>of</strong> connected water channels could provide potential<br />

pathways for waste transport away from the repository.<br />

5. Resource potential <strong>of</strong> the repository site and area. A low resource potential is<br />

desirable to avoid loss <strong>of</strong> any economic resource by the repository existence and<br />

to reduce the likelihood <strong>of</strong> future exploration activities for resource recovery.<br />

6. The multibarrier safety feature. This combines the redundant isolation features<br />

provided by the rock properties, the geologic setting, and engineered barriers to<br />

give overall added confidence that the waste will remain isolated.<br />

These six factors are discussed in the following sections.<br />

5.1.1.1 Disposal Media Properties<br />

Four geologic media are examined in this Statement to illustrate a range <strong>of</strong> rock prop-<br />

erties for a radioactive waste repository: salt deposits (bedded and dome), granite, shale<br />

and basalt. All four rock types possess properties that are favorable for waste isolation.<br />

These, as well as.some unfavorable characteristics, are discussed in the following pages.<br />

For the purpose <strong>of</strong> this Statement, the physical properties <strong>of</strong> a disposal medium<br />

describe the characteristics <strong>of</strong> both the host rock and surrounding rock mass. The disposal<br />

rock material is characterized in terms <strong>of</strong> its texture, i.e., the size, shape, and arrange-<br />

ment <strong>of</strong> the component crystal grains. Texture is a consideration in the assessment <strong>of</strong> a<br />

medium's behavior under stress and heat, and its hydrologic flow potential.<br />

Rock mass structures include the discontinuities <strong>of</strong> bedding and joints. Bedding<br />

refers to variations in texture because <strong>of</strong> changes in the sedimentation process by which<br />

the rock was formed. It may be present in both sedimentary and metamorph.c rocks. Joints<br />

are fractures along which little or no displacement <strong>of</strong> the rocks has occurred. They are<br />

generally formed by extensional release <strong>of</strong> confining earth pressures. Descriptive features<br />

<strong>of</strong> these discontinuities include orientation, width, spacing, filling material, waviness,<br />

and extent (length). The potential for the transport <strong>of</strong> waste material correlates with the<br />

number and extent <strong>of</strong> host rock discontinuities.<br />

The rock properties <strong>of</strong> principal interest for waste disposal are those related to<br />

strength, stress-strain, thermal, and hydrologic characteristics. These properties and<br />

characteristics are discussed and presented in tabular form in Appendix B. For comparative<br />

purposes index properties defined as unit weight and natural moisture content are included<br />

in the tabulation.<br />

Substantial strength is desirable for engineering design <strong>of</strong> subsurface repository<br />

facilities, especially in maintaining tunnel integrity. Strength properties provide the<br />

durability or resistance <strong>of</strong> a material to processes such as erosion and weathering and

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