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Ana Isabel Ruiz

Researcher at Autonomous University of Madrid

Publications -  56
Citations -  950

Ana Isabel Ruiz is an academic researcher from Autonomous University of Madrid. The author has contributed to research in topics: Bentonite & Neutron diffraction. The author has an hindex of 17, co-authored 52 publications receiving 811 citations. Previous affiliations of Ana Isabel Ruiz include Complutense University of Madrid.

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Electrical properties of La1.33−xLi3xTi2O6 (0.1<x<0.3)

TL;DR: In this article, structural characterization and ionic conductivity properties of three members of the La1.33−xLi3xTi2O6 (being x=0.29, 0.21 and 0.09, respectively) perovskite type series are reported.
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Pollution profiles and physicochemical parameters in old uncontrolled landfills

TL;DR: Examination of natural clayey soils directly in contact with the waste deposited in three landfills over 12 years old in Spain finds these natural substrata are suitable for confining leachate pollution and for complying with European legislation.
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Gelatin-clay bio-nanocomposites: structural and functional properties as advanced materials.

TL;DR: The incorporation of pH indicator dyes to the montmorillonite bio-nanocomposite films allows their application for optical pH sensing and the possibility to be processed as homogeneous thin films provided of good mechanical properties and transparency.
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Voltage inactivation of Ca2+ entry and secretion associated with N- and P/Q-type but not L-type Ca2+ channels of bovine chromaffin cells

TL;DR: It seems that the N‐ and P/Q‐subtypes of calcium channels are more prone to inactivation at depolarizing voltages than the L‐subtype, and this different inactivation might occur physiologically during different patterns of action potential firing.
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The performance of natural clay as a barrier to the diffusion of municipal solid waste landfill leachates.

TL;DR: The model predicted the chloride anion diffusion and cation exchange processes for three different experiments and found that at larger space and time scales, diffusion was retarded due to the presence of more consolidated, non-mechanically disturbed clay materials at large depths in a natural clay-rock emplacement.