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

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3-37<br />

3-38<br />

Comment<br />

Number<br />

Comment<br />

Number<br />

.1i.9 p. 3.1.2<br />

Considering the multitude <strong>of</strong> variables and unknowns, it would seem extremely<br />

difficult to predict the lower depth <strong>of</strong> glacial erosion at any particular<br />

site with any degree <strong>of</strong> certainty. A more acceptable approach would seem<br />

to be that, if the decision has been made to seriously consider a repository<br />

.i.12 .12 p. 3.1.125<br />

Individual and population doses, as well as health effects, are calculated<br />

and presented in the GEIS for certain postulated accidents. The potential<br />

decontamination cost and property damage associated with the same postulated<br />

accidents should also be evaluated.<br />

within a previously glaciated area that the repository designer would .3 . 3<br />

3.1.13 p. 3.1.125<br />

simply assume surficial erosion (deposition and various deformation/faulting Uncertainties in doses<br />

Uncertainties<br />

predicted<br />

in doses predicted<br />

by<br />

by models<br />

models is<br />

is<br />

misleading.<br />

misleading.<br />

The<br />

The<br />

discussion<br />

discussion<br />

features) to occur within, say the upper 65 to 100 m <strong>of</strong> the surface.<br />

should indicate the uncertainty to be expected when a critical parameter<br />

Other than probably uniform S, crustal depression, a repository located at"<br />

has a range <strong>of</strong> values such as the magnitude <strong>of</strong> earthquakes, floods, etc.<br />

the 500-600 m depth should be relatively unaffected by direct glacial<br />

processes. It would seem to be overly-conservative to assume that a 3.1.14 p.<br />

3.1.14<br />

3.1.125<br />

p. 3.1.125<br />

postulated future glacial postulated front would future advance glacial beyond the areas formerly The discussion in the section entitled "Land Use and Transportation Consideroccupied<br />

by continental occupied glaciers. glaciersations" by continental<br />

focused on some possible land use conflicts and refers the reader<br />

3.1.10 p.<br />

3.<br />

3.1.65<br />

3.1.5 . p.<br />

It is stated that "containment times <strong>of</strong> 500 years are the most important."it<br />

to a body <strong>of</strong> literature, some <strong>of</strong> which is described as speculative. It<br />

would be useful for the GEIS to summarize this information and to present<br />

for review.<br />

However, on page 3.1.59 it was stated that a significant release" could<br />

occur at 1000 years and on page 3.1.64 it stated that after "700 years,<br />

the radioactivity in the repository poses a greatly reduced threat." Some<br />

consistency should exist in the document for the period <strong>of</strong> concern and .<br />

basis for arriving at this time should be clearly delineated.<br />

i.5<br />

3.1.15<br />

p. 3.1.<br />

pp. 3.1.136-172<br />

.<br />

In this section several scenarios resulting in the release to the biosphere<br />

<strong>of</strong> large amounts <strong>of</strong> radioactivity are postulated. Because <strong>of</strong> the generic<br />

nature <strong>of</strong> the repositories and the lack <strong>of</strong> specific data needed in the<br />

Ln<br />

.. 11<br />

3. p. 3<br />

p. 3.1.67<br />

Table 3.1.3 - It is stated that the Poisson process is used to model the<br />

occurrence <strong>of</strong> geologic events, based on past observation. It is not<br />

clear, however, whether this table presents the probability that one event<br />

occurs for the "interval" <strong>of</strong> concern or, more properly, e ( ) that one or more<br />

event occurs during the probability this period. From P(x)<br />

event occurs during this period. From P(x).= e 2)' the probability<br />

x!<br />

calculation, many <strong>of</strong> the parameters controlling the physical transport <strong>of</strong><br />

the radionuclides are not even known to order <strong>of</strong> magnitude certainty. The<br />

resulting dilutions that are used in the dose models have even larger<br />

error bands. Therefore, breaking down the resulting doses by reprocessing<br />

procedure and rock type makes little sense, when the differences between<br />

them are much less than the error band due to transport-dose modeling.<br />

<strong>of</strong> one or more events occurring is (1 - the probability <strong>of</strong> zero occurrences) = i.16 p. 3.1.136<br />

(1 - P(0)) = 1 - e Q . This formulation, however, produces somewhat Section 3.1.5.2 is entitled, "Potential Impacts Associated with Respository<br />

higher probabilities than those listed in Table 3.1.3, e.g., for the <strong>Waste</strong>s in the Long-Term." Although this section gives population doses<br />

"number <strong>of</strong> occurrence years" equal to 10 6 years, and an "interval" equal due to different accident scenerios, it does not discuss the problem <strong>of</strong><br />

to 104 year, the probability that one or more geologic event occurs is land contamination due to these accidents.<br />

-3 -<br />

9.95x10 3 as compared to 6.9x10 "3 . Thus, more explanation <strong>of</strong> the probabilities<br />

in Table 3.1.3 is needed.

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