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

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14 15<br />

43. (Page 3.1.40, physical protection) This part makes sense if it 49. (Page 3.1.49, third paragraph) "Flow rates and velocities <strong>of</strong><br />

refers to physical protection during the operational phase <strong>of</strong> the ground water that are insignificant over a 50 year period will have to<br />

repository. The first paragraph on page 3.1.41 is self-contradictory. be considered in terms <strong>of</strong> hundreds to thousands <strong>of</strong> years." This<br />

It states that the waste would be essentially unavailable after statement should be further discussed.<br />

placement in the geological repository. Because the operational<br />

controls will cease to exist long before any appreciable decay <strong>of</strong> 50. (Page 3.1.52, item four) It seems unreasonable to limit the<br />

plutonium-239, the protection must be inherent in the inaccessibility search for an optimal site to areas with "availability <strong>of</strong> title".<br />

<strong>of</strong> the waste in the repository and the massive effort that would be Surely this is an area where eminent domain is appropriate.<br />

required to remove it.<br />

51. (Page 3.1.52, last sentence) There is an unwarranted belief that<br />

44. (Page 3.1.41, third bullet) Comparison <strong>of</strong> acceptable consequences all problems can be solved by major efforts. Investigations into a<br />

from radiation in comparison with those from automobile accidents is basic research area, such as this appears to be, do not necessarily<br />

invalid. There are two primary aspects to the establishment <strong>of</strong> bases: have satisfactory outcomes. The research must first be performed<br />

before opinions as to its results are valid.<br />

1. How much will society accept on an absolute basis;<br />

2. How much better than this can the technology provide? 52. (Page 3.1.54, item two) The chemically separated high-level waste<br />

to be considered must include the iodine-129 (and the other volatiles<br />

45. (Page 3.1.41, last bullet) The use <strong>of</strong> adsorption coefficients and transuranics) which are excluded from discharge to the atmosphere<br />

from one set <strong>of</strong> Hanford subsoils, measured under laboratory conditions, from the fuel.reprocessing plant by EPA's Uranium Fuel Cycle regulations<br />

is not an adequate basis for scoping the effect <strong>of</strong> adsorption. There (40 CFR 190.10(b)).<br />

are some substantial differences between the adsorption coefficients <strong>of</strong><br />

the Hanford Subsoil and <strong>of</strong> those given on page K-20 <strong>of</strong> the <strong>Waste</strong> 53. (Page 3.1.54, item three, last sentence) Unless the actinides<br />

Isolation Pilot Plant EIS (DOE/EIS-0026-D), for example. from chemically separated high-level waste are recycled, they must be<br />

disposed <strong>of</strong> as waste and would still require consideration in this<br />

46. (Page 3.1.47 - 5th paragraph, last sentence) Isotopic age Environmental Impact Statement. Even if one assumes recycling <strong>of</strong><br />

province boundaries should be added to the list <strong>of</strong> areas to be avoided uranium and plutonium, one eventually reaches the point where recycling<br />

in the preliminary selection <strong>of</strong> repository areas, is not economically feasible and the transuranics must then be disposed<br />

as waste.<br />

47. (Page 3.1.48, near bottom) The first statement under ground water<br />

implies that a repository can be sited in conjunction with a useful 54. (Page 3.1.55, second paragraph) The leach rates <strong>of</strong> spent fuel in<br />

ground water source without affecting its quality. Since EPA analysis room temperature deionized water are irrelevant. The leach rates <strong>of</strong><br />

has shown that ground water can be significantly contaminated by a spent fuel in typical ground waters at temperatures to be expected in<br />

single drilling event, it is important that the repository should not spent fuel repositories are more important.<br />

be situated where it can affect a useful ground water resource.<br />

55. (Page 3.1.59, second paragraph) The canister could prevent ground<br />

48. (Page 3.1.49) The chemical nature <strong>of</strong> any aquifers around a water intrusion for a period provided that there was no disruptive<br />

repository should be briefly discussed. Reducing aquifers greatly event which would destroy the canister. Such disruption would be<br />

limit the solubility <strong>of</strong> U, Pu, Np, and Tc. Sorption <strong>of</strong> these elements expected in gas, oil, or mineral exploration. It therefore seems that<br />

would provide a further reduction in the amount <strong>of</strong> nuclides reaching it would be impossible to maintain canister integrity from credible<br />

people, and sorption <strong>of</strong> the reduced states <strong>of</strong> these elements is higher accidents for a significant time period.<br />

than sorption <strong>of</strong> the oxidized states. This oxidation-reduction<br />

consideration should be briefly discussed. 56. (Page 3.1.59, third paragraph) Reliance on the canister alone for<br />

long-term containment seems unwarranted, as indicated in the previous<br />

comment. This does not mean that canisters which would be durable in<br />

the absence <strong>of</strong> an intrusive event or traumatic geological events should<br />

not be developed.

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