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V - MSpace at the University of Manitoba

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years, it is considered to be one <strong>of</strong> <strong>the</strong> largest contributors to <strong>the</strong> long-term potential<br />

thre<strong>at</strong> <strong>of</strong> radioactivity from nuclear waste.<br />

The two primary fissile isotopes are 235 U and <strong>the</strong> str<strong>at</strong>egically important 239 Pu,<br />

which has a low critical mass <strong>of</strong> < 2 Kg. The 239 Pu isotope is now produced by <strong>the</strong> ton in<br />

nuclear reactors. Three grades <strong>of</strong> plutonium are commonly recognized: weapon-grade<br />

240 Pu (< 7%), fuel-grade 240 Pu (7–18%) and reactor-grade 240 Pu (18%). High-level waste<br />

from <strong>the</strong> isol<strong>at</strong>ion <strong>of</strong> 239 Pu also contains large quantities <strong>of</strong> 238 Pu, as well as heavier Pu<br />

isotopes. Isotope 238 Pu is considered to be an important fuel source and is commonly used<br />

as a source <strong>of</strong> energy in both earth and space borne s<strong>at</strong>ellites [2].<br />

These and o<strong>the</strong>r radiotoxic actinides, found in nuclear fuel processing and waste<br />

storage, pose an immedi<strong>at</strong>e and future environmental concern. Tre<strong>at</strong>ment <strong>of</strong>ten involves<br />

ei<strong>the</strong>r separ<strong>at</strong>ion for reuse or immobiliz<strong>at</strong>ion for long-term storage. The waste solutions<br />

from <strong>the</strong> processing <strong>of</strong> irradi<strong>at</strong>ed uranium fuel contain U, Np, and Pu isotopes but <strong>of</strong>ten<br />

also contain o<strong>the</strong>r isotopes represent<strong>at</strong>ive <strong>of</strong> as much as a third <strong>of</strong> <strong>the</strong> periodic table <strong>of</strong><br />

elements. U, Np, and Pu can <strong>of</strong>ten be isol<strong>at</strong>ed and purified by a combin<strong>at</strong>ion <strong>of</strong> solvent<br />

extraction, ion exchange, and precipit<strong>at</strong>ion/coprecipit<strong>at</strong>ion techniques.<br />

The separ<strong>at</strong>ion <strong>of</strong> <strong>the</strong> early actinides from <strong>the</strong>ir fission products and from each<br />

o<strong>the</strong>r is generally accomplished by adjusting <strong>the</strong> oxid<strong>at</strong>ion st<strong>at</strong>e <strong>of</strong> <strong>the</strong> actinide ion in<br />

aqueous solution to make <strong>the</strong> coordin<strong>at</strong>ion chemistry substantially different from th<strong>at</strong> <strong>of</strong><br />

<strong>the</strong> o<strong>the</strong>r species to be separ<strong>at</strong>ed.<br />

The radioactivity, toxicity, and chemical reactivity <strong>of</strong> <strong>the</strong> actinides make handling<br />

<strong>the</strong>m in <strong>at</strong>mosphere-controlled glove boxes a necessity. When high levels <strong>of</strong> penetr<strong>at</strong>ing<br />

radi<strong>at</strong>ion are encountered, manipul<strong>at</strong>ion also needs to be done with remote controls. With<br />

6

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