November 3, 2011 As a first line of defense, steel barrels buried deep underground are designed to keep dangerous plutonium waste from seeping into the soil and surrounding bedrock and, eventually, contaminating the groundwater. But after several thousand years, those barrels will naturally begin to disintegrate because of corrosion.
To determine what will happen to this toxic waste once its container disappears, a team of scientists at Argonne National Lab (ANL), used X-ray scattering techniques to study the way plutonium interacts with mineral surfaces on a molecular level. But the unexpected results of their tests challenge existing predictions about the way plutonium waste will behave.
"We want to be sure that nuclides (like plutonium) stay where we put them," says Moritz Schmidt, an ANL post-doctoral researcher who will present his team's work at the upcoming AVS International Symposium in Nashville, TN. Understanding how these radioactive molecules behave is "the only way we can make educated decisions about what is a sufficient nuclear waste repository and what is not," he adds.
Plutonium, with its half-life of 24 thousand years, is notoriously difficult to work with. Few labs around the world are equipped to handle its high radioactivity and toxicity, and its extremely complicated behavior around water makes modeling plutonium systems a formidable task. These challenges mean that very little is known about the element's chemistry, Schmidt says.
Plutonium's extraordinary chemistry in water also means scientists cannot directly equate it with similar elements to tell them how plutonium will behave in the environment. Other ions tend to stick to the surface of clay as individual atoms. Plutonium, on the other hand, bunches into nanometer-sized clusters in water, and almost nothing is known about how these clusters interact with clay surfaces.
To better understand how this toxic substance might respond to its environment, the Argonne team examined the interactions between plutonium ions dissolved in water and a mineral called muscovite. This mineral is structurally similar to clay, which is often considered for use in waste repository sites around the world due to its strong affinity for plutonium. Using a range of X-ray scattering techniques, the scientists reconstructed images of thin layers of plutonium molecules sitting on the surface of a slab of muscovite.
What they found was "very interesting," Schmidt says. The Argonne scientists discovered that plutonium clusters adhere much more strongly to mineral surfaces than individual plutonium ions would be expected to. The result of this strong adherence is that plutonium tends to become trapped on the surface of the clay
-and could help contain the spread of plutonium into the environment.
"In this respect, it's a rather positive effect" that his group has observed, Schmidt says; but, he adds, "it's hard to make a very general statement" about whether this would alter the rate of plutonium leaking out of its repository thousands of years from now.
Schmidt cautions that these are fundamental studies and probably will not have a direct impact on the way structures for containing plutonium are currently built; however, he stresses that this work shows the importance of studying plutonium's surface reactivity at a molecular level, with potential future benefits for nuclear waste containment strategies.
"This is a field that is only just emerging," Schmidt says.