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Antonino Marco Saitta

Researcher at University of Paris

Publications -  46
Citations -  2362

Antonino Marco Saitta is an academic researcher from University of Paris. The author has contributed to research in topics: Neutron diffraction & Ab initio quantum chemistry methods. The author has an hindex of 26, co-authored 46 publications receiving 2053 citations. Previous affiliations of Antonino Marco Saitta include Pierre-and-Marie-Curie University & Institut de recherche pour le développement.

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Local structure of condensed zinc oxide

TL;DR: The high-pressure local structure of zinc oxide has been studied at room temperature using combined energy-dispersive x-ray-diffraction and xray-absorption spectroscopy experiments as mentioned in this paper.
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Variations in the work function of doped single- and few-layer graphene assessed by Kelvin probe force microscopy and density functional theory

TL;DR: In this article, the authors compare the layer thickness dependency of the measured surface potential with ab initio density functional theory calculations of the work function for substrate-doped graphene and independently find an interlayer screening length in the order of four to five layers.
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Miller experiments in atomistic computer simulations

TL;DR: It is shown that glycine spontaneously forms from mixtures of simple molecules once an electric field is switched on and formic acid and formamide are identified as key intermediate products of the early steps of the Miller reactions, and the crucible of formation of complex biological molecules.
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Superconductivity in doped sp(3) semiconductors: The case of the clathrates

TL;DR: The study of I(8)@Si-46 and of gedanken pure silicon diamond and clathrate phases doped within a rigid-band approach show that the superconductivity is an intrinsic property of the sp(3) silicon network.
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Nature of the polyamorphic transition in ice under pressure.

TL;DR: A neutron diffraction study of the transition between low-density and high-density amorphous ice (LDA and HDA) under pressure at approximately 0.3 GPa gives direct evidence of a classical first-order transition.