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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 />

128

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