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The FuTure oF nuclear Fuel cycle - MIT Energy Initiative

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Repository Engineering<br />

All repositories for SNF disposal plan to use long-lived waste package designed to last thousands<br />

to hundreds of thousands of years. Because radioactivity decays with time (Figure<br />

5A.1) the waste package can provide a significant barrier to radionuclide release when the<br />

hazard is the greatest and enable the wastes to be retrieved if a problem is found in the performance<br />

of the repository.<br />

SNF and HLW generate significant decay heat that could raise repository temperatures sufficiently<br />

to accelerate degradation of the waste, waste package and geology with degradation<br />

of repository performance. This has several implications.<br />

p Repository temperatures are controlled by limiting the decay heat per waste package<br />

(that is, the quantity of SNF and HLW in each package) and spreading out the waste<br />

packages over a large underground area. Decay heat is conducted from the waste through<br />

the waste package and the rock ultimately to the earth’s surface.<br />

p Repository cost and size is partly dependent upon total SNF and HLW decay heat. <strong>The</strong><br />

greater the total heat load, the larger the number of waste packages and the more tunnels<br />

that must be constructed to spread the SNF and HLW over a large area. For the proposed<br />

YM repository, about 40 tons of SNF can be emplaced per acre of repository space. This<br />

implies about 50 acres of repository are needed to dispose of a year’s production of SNF<br />

in the U.S (~2000 tons).<br />

p Repository programs have adopted a policy of storing SNF and HLW for 40 to 60 years<br />

before disposal to reduce decay heat and thus reduce repository costs and performance<br />

uncertainties. Engineering tradeoffs determine storage times. After the first decade, the<br />

fission products strontium-90 ( 90 Sr) and cesium-137 ( 137 Cs) produce most of the decay<br />

heat. <strong>The</strong>se radionuclides have 30-year half-lives and thus the radioactivity and decay<br />

heat drops in half every 30 years. After ~50 years, the transuranic isotope 241 Am becomes<br />

the dominant source of decay heat in SNF with a half life of 470 years before decaying to<br />

Neptunium-237 ( 237 Np). <strong>The</strong> decay heat per fuel assembly initially decreases at a rapid<br />

rate and then slows down when the decay heat is controlled by 241 Am. This occurs 40 to<br />

60 years after SNF discharge—the technical basis for the storage time.<br />

Repository capacities are not limited by waste volume or mass. For some wastes there are<br />

incentives to increase waste volumes to improve repository performance. For example, liquid<br />

HLW is converted into HLW glass for disposal. 11 This increases waste volumes by a<br />

factor of three to four compared to calcining the waste; but, glass is a superior waste form<br />

with lower handling risks and is less soluble in water—resulting in better repository performance.<br />

Economics is not a major repository engineering constraint. <strong>The</strong> cost of geological disposal<br />

of HLW and SNF is a small fraction of the cost of <strong>nuclear</strong> electricity—typically a few percent<br />

of the cost of electricity.<br />

160 <strong>MIT</strong> STudy on <strong>The</strong> <strong>FuTure</strong> <strong>oF</strong> <strong>nuclear</strong> <strong>Fuel</strong> <strong>cycle</strong>

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