Structural properties of molten dilute aluminium-transition metal alloys.

The short-range order in liquid binary Al-rich alloys (Al-Fe, Al-Ti) was studied by x-ray diffraction. The measurements were performed using a novel containerless technique which combines aerodynamic levitation with inductive heating. The average structure factors, S(Q), have been determined for various temperatures and compositions in the stable liquid state. From S(Q), the pair correlation functions, g(r), have been calculated. The first interatomic distance is nearly temperature-independent, whereas the first-shell coordination number decreases with increasing temperature for all the alloys investigated. For the Al-Fe alloys, room-temperature scanning electron microscropy (SEM) studies show the formation of a microstructure, namely the existence of Al(13)Fe(4) inclusions in the Al matrix.

[Synchrotron radiation techniques for structural characterisation of biological entities: an example with renal stone analysis]. / Les techniques de rayonnement synchrotron au service de la caractérisation d'objets biologiques: un exemple d'application, les calculs rénaux.

This paper describes the opportunities given by the synchrotron radiation techniques regarding the structural characterisation of biological entities. After a short recall on the characteristics of the synchrotron radiation, are described the experimental devices based on fluorescence X, wide angle X-ray scattering and X-ray absorption spectroscopy, which may applied for biological samples, especially in the field of stone analysis. Recent progresses in medical research using synchrotron radiation will be also discussed.

Heavy elements in urinary stones.

The presence and role of heavy metals in urinary stones is debated. We investigated the distribution of trace heavy metals in 78 calculi of well-defined composition by means of microfluorescence X analysis using synchrotron radiation. Seven elements were identified, the most abundant being Zn and Sr which together accounted for 91% of the heavy metal content of stones. The other heavy metals were Fe, Cu, Rb, Pb and Se. Zn and Sr were virtually confined to calcium-containing stones, whereas only trace amounts were found in uric acid or cystine stones. Among calcium stones, Zn and Sr were more abundant in calcium phosphate than in calcium oxalate stones and, in the latter, in weddellite than in whewellite stones. Fe, Cu and Rb were much less abundant and also found mainly in calcium stones. Pb was significantly less abundant than in previous studies, thus suggesting a rarefaction of Pb in the environment, and appreciable amounts of Se were found only in cystine stones. In conclusion, the preponderance of Zn and Sr, both bivalent ions, in calcium-containing stones suggests a substitution process of calcium by metal ions with similar charge and radius rather than a contribution of the metals to stone formation. Further studies are needed to examine the relationships between urine concentration in calcium or other solutes and the amount of Zn and Sr in calcium stones.