The niobium phosphate bronze β-K2Na2− xNb8P5O34, second form of the first member of the series (K3Nb6P4O26) n KNb2PO8

In this case, the pseudo-solid, coexisting with a low-density phase, can be strongly compressed; the molecules lay certainly flat on the graphite at first and

Even when we consider diffraction from a very small crystal, where the shapes of diffraction spots are only determined by the mosaicity distribution of the crystal, the

hexagonal and more concentrated phases- from the parameters of the two-dimensional latice perpendicular to the axis of the molecules. When the critical concen- tration C~ is

intensities between the diffraction satellites in the rocking curve near the K absorption edge of Ga due to the change in the x-ray penetration depth into the crystal and an

The refinement of the structure must be done by including reconstruction/relaxation in the underlying Si-substrate, but the main features contained in the x-ray

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Mesoscale variability in updraft velocities in combination with pure homogeneous freezing processes accounts for most of the observed variance in number densities of ice crystals.

Supporting the Time Resolved data with Molecular Dynamics simulations, static diraction data and the experimental study of the pure solvent response to ultrafast heating,