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

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4-9 4-10<br />

Comment<br />

Comment<br />

Number Number<br />

final for such a large region and cannot be justified without detailed ~.e.8 Section 3.6.2.3<br />

discussion.<br />

This section starts <strong>of</strong>f with the identification <strong>of</strong> the barriers to the<br />

movement <strong>of</strong> radionuclides, then fails to discuss two <strong>of</strong> them: "any<br />

A much more reasonable and specific statement is that made for fracture controlled modification <strong>of</strong> the medium," and "the benthic boundary layer."<br />

zones in the mid-ocean ridge: "On the basis <strong>of</strong> present knowledge, A discussion <strong>of</strong> these barriers should be provided.<br />

therefore, the fracture zones are not probable candidates as study sites."<br />

4.e.9 p. 3.6.7<br />

Similarly.the statement, "The abyssal plains...are therefore unacceptable Previous reports on the U.S. seabed disposal program have not included the<br />

for further consideration." should be modified, water column as a design barrier. Is it.the program's intention to now<br />

identify the water column as a primary design barrier to radionuclide<br />

4.e.5 p. 3.6.4 migration, or rather to investigate its properties as a barrier only for<br />

It is stated that: "Bottom currents in the MPG areas <strong>of</strong> the North Pacific unexpected releases? In other words, do the conceptual plans allow for<br />

are generally weak and variable." A reference should be provided. How radionuclides to enter the water column during the period when they may<br />

weak and variable bottom currents affect emplacement, radionuclide present a hazard to man or the ecosysteip? What is meant by inadvertant<br />

migration, heat transfer, etc. should be discussed. release? Scenarios leading to inadvertant release should be described.<br />

4.e.6 p. 3.6.4 4.e.10 p. 3.6.20<br />

The sediment thickness is reported to be 50 to 100 meters, while in Under the discussion <strong>of</strong> the water column, it should be recognized that<br />

Table 3.6.1 it is given as 100'to 300 meters. while the water column may not provide a barrier to migration, its<br />

enormous capability to dilute such releases below significant concentrations<br />

4.e.7 p. 3.6.4 cannot be overlooked as a mitigative feature (See comment 4.e.9).<br />

A statement is made regarding waste disposal in trenches: "...a plate<br />

being subducted would have moved only tens <strong>of</strong> kilometers during that time 4.e.11 p. 3.6.21<br />

(250 to 500 thousand years) and would not be subducted fast enough for The research and development costs to support the penetrometer emplacement<br />

waste disposal purposes." This conclusion does not follow from the concept are quoted as $250 million, on page 3.6.21, and as $60 million on<br />

discussion proceeding it in the same paragraph. page 3.6.31. The components <strong>of</strong> each figure should be given. What is the<br />

meaning <strong>of</strong> "state-<strong>of</strong>-the-art" (Figure 3.6.1) referring to penetrometer<br />

a. How far would the waste have to move during that time to be subducti emplacement, given the quarter <strong>of</strong> a billion dollar research and<br />

fact enough-for waste disposal purposes? Reference? development cost estimate?<br />

b. What might the impact be <strong>of</strong> the waste not being subducted fast 4.e.12 p. 3.6.24<br />

enough? It should be made clear that tsunamis could pose no danger to a ship that<br />

was not in shallow, near shore waters, or near the source <strong>of</strong> tsunami.<br />

Even a large tsunami would probably not be noticed by a ship in mid-ocean

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