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Alejandro Fernandez-Martinez

Researcher at University of Savoy

Publications -  104
Citations -  3953

Alejandro Fernandez-Martinez is an academic researcher from University of Savoy. The author has contributed to research in topics: Chemistry & Crystallization. The author has an hindex of 29, co-authored 90 publications receiving 3095 citations. Previous affiliations of Alejandro Fernandez-Martinez include Joseph Fourier University & Lawrence Livermore National Laboratory.

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Microscopic Evidence for Liquid-Liquid Separation in Supersaturated CaCO3 Solutions

TL;DR: This study uses molecular dynamics simulations to probe the structure, dynamics, and energetics of hydrated CaCO3 clusters and lattice gas simulations to explore the behavior of cluster populations before nucleation and predicts formation of a dense liquid phase through liquid-liquid separation within the concentration range in which clusters are observed.
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Selenium environmental cycling and bioavailability: a structural chemist point of view

TL;DR: In this article, a review of the important advances made during these last years in the mechanistic understanding of processes which govern selenium cycling and bioavailability, such as adsorption at the mineral/water interface, precipitation of elemental Selenium, or bioavailability of nanoscaled precipitates, is presented.
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Electron transfer at the mineral/water interface: Selenium reduction by ferrous iron sorbed on clay

TL;DR: In this article, the authors investigated the long-term kinetics of selenite ( Se(IV)O 3 - ) sorption to montmorillonite in the presence of Fe2+ under anoxic conditions.
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Recovery of Rare Earth Elements and Yttrium from Passive-Remediation Systems of Acid Mine Drainage

TL;DR: The findings suggest that the proposed AMD remediation process can represent a modest but suitable REY source, and the IPB could function as a giant heap-leaching process of regional scale in which rain and oxygen act as natural driving forces with no energy investment.
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X-ray absorption and photoelectron spectroscopy investigation of selenite reduction by FeII-bearing minerals

TL;DR: Comparison of these spectroscopic results with thermodynamic equilibrium modeling provides evidence that the nature of reduction end product in these FeII systems is controlled by the concentration of HSe(-); Se0 forms only at lower HSe(-) concentrations related to slower HSeO3(-) reduction kinetics.