exotic nuclei structure and reaction noyaux exotiques ... - IPN - IN2P3
exotic nuclei structure and reaction noyaux exotiques ... - IPN - IN2P3
exotic nuclei structure and reaction noyaux exotiques ... - IPN - IN2P3
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function of temperature. The recent results allow<br />
one to demonstrate that the monazite’s (LaPO 4 )<br />
point of zero charge remains constant whatever<br />
the temperature in a non-complexing medium such<br />
as NaClO 4 (pH PZC = 1.8). Moreover, microcalorimetry<br />
measurements show that the surface hydration<br />
process is exothermic, close to -0.4 J/g at<br />
30°C but it is found to depend on the temperature.<br />
Then, further study are in progress to precisely<br />
determine the variation in the enthalpy of hydration<br />
versus temperature in order to calculated the rC p<br />
associated to the <strong>reaction</strong>. In a second step, the<br />
retention of U(VI) by the hydrated surface can be<br />
investigated. A spectroscopic study is carried out<br />
by using Laser-Induced Fluorescence (LIFS), X-<br />
ray Absorption Spectroscopy (XAS) <strong>and</strong> vibrational<br />
spectroscopies (Infrared <strong>and</strong> Raman) which allows<br />
one to experimentally determine all the components<br />
involved in the sorption process. The first<br />
results obtained for lanthanum phosphate show<br />
that U(VI) is sorbed on two types of surface sites<br />
whatever the temperature. Nevertheless, the reactivity<br />
of both sites is found to be temperaturedepend<br />
since the relative proportions of the resulting<br />
surface complexes strongly change as a function<br />
of temperature. Additionally, microcalorimetric<br />
measurements are performed in order to measure<br />
the heat of sorption. The U(VI) retention by lanthanum<br />
monophosphate is an endothermic process<br />
with an associated heat of 0.3 J/g. The extensive<br />
study of these systems is under progress <strong>and</strong> a<br />
global underst<strong>and</strong>ing of the temperature effects on<br />
the U(VI) retention mechanisms by oxide-like compounds<br />
should be achieved in a near future. Then,<br />
the results will allow one to check the validity of the<br />
retention mechanisms determined at 25°C (most of<br />
the studies found in the literature) for higher temperatures<br />
(up to 150°C).<br />
culations which take place in static <strong>and</strong> vacuum<br />
conditions at T=0 K. In a first part, a (001) gibbsite<br />
face model composed of two sheets, where the<br />
deepest one was frozen to atomic bulk positions,<br />
was optimized. Geometrical relaxations clearly<br />
demonstrated the validity of this surface model to<br />
mimic the real system. In a second part, water interactions<br />
with the optimized surface model were<br />
investigated. Two adsorption modes were identified<br />
in agreement with experimental results. The<br />
first one takes place through a water molecule hydrogen<br />
<strong>and</strong> a surface oxygen (Fig. 3-a) while in the<br />
second adsorption mode, a surface hydrogen interacts<br />
with a water molecule oxygen (Fig. 3-b). The<br />
first adsorption mode was calculated as the most<br />
stable one.<br />
Gibbsite surface model Solvent<br />
2.12 Å<br />
1.85 Å<br />
O Al H<br />
Fig. 3: (001) Gibbsite face hydration.<br />
2.89 Å<br />
2.64 Å<br />
(b)<br />
Finally, the uranyl interaction with the hydrated<br />
(001) gibbsite face was simulated. Two types of<br />
adsorption mechanisms were considered: the<br />
outer sphere mechanism (Fig. 4-a) as well as the<br />
inner sphere one (Fig. 4-b).<br />
(a)<br />
Fig 2: Example of thermograms obtained for La-<br />
PO 4 hydration (top) <strong>and</strong> U(VI) sorption onto LaPO 4<br />
(bottom).<br />
Theoretical calculations<br />
In order to investigate, at the solid/liquid interface,<br />
the uranyl ion behaviour with the (001) gibbsite<br />
face, we have used an Ab-initio Molecular dynamics<br />
approach as implemented in the CPMD code<br />
(Car-Parrinello Molecular Dynamics). With this<br />
original methodology, temperature, solvent <strong>and</strong><br />
dynamic effects are explicitly taken into account in<br />
simulations which is innovator relative to usual cal-<br />
Fig. 4: Uranyl adsorption on the gibbsite face. (a)<br />
outer sphere <strong>and</strong> (b) inner sphere mechanism.<br />
Both adsorption modes were calculated as possible.<br />
The second one (inner sphere mechanism) is<br />
the most stable because of strong covalent interactions.<br />
However, even though it is the most stable<br />
one, the needed activation energy (E a ) to reach it,<br />
is not known. Therefore, in order to evaluate the<br />
gibbsite retention capability towards uranyl migration,<br />
current work are devoted to evaluate E a. This<br />
value, will be used to predict if at a given temperature<br />
the energy barrier will be able to be crossed.<br />
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