Albert Danon
7 Papers
26 Citations
Albert Danon is an academic researcher. The author has contributed to research in topics: Thermal desorption spectroscopy & Thermal decomposition. The author has an hindex of 4, co-authored 7 publications.
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Papers
Comprehensive Study of the Ceria–H2 System: Effect of the Reaction Conditions on the Reduction Extent and Intermediates
TL;DR: The interaction of hydrogen with ceria is a fundamental process of high importance for various catalytic reactions as mentioned in this paper, and theoretical calculations have been performed to identify the elementary steps in this process.
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Measuring the water content in freshly-deposited fingermarks.
Or Keisar,Yair Cohen,Y. Finkelstein,Natalie Kostirya,Roey Ben-David,Albert Danon,Ze'ev Porat,Joseph Almog +7 more
TL;DR: The measurements indicate the occurrence of a broad 20-70% water content in freshly-deposited fingermarks, unlike the traditional narrow-range values of 98-99% and the limiting value of 20wt.% suggested by Kent.
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The role of surface coarsening and sintering during thermal decomposition of titanium hydride
Roey Ben David,Roey Ben David,Y. Finkelstein,Einat Nativ-Roth,Albert Danon,D. Cohen,Eugen Rabkin +6 more
TL;DR: In this article, mass spectrometers were used to study the non-isothermal hydrogen desorption from as-received and pre-oxidized TiH2 powder samples.
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Thermal desorption kinetics of H2O and H2 from rapidly solidified Al-Zn-Mg alloy powders
TL;DR: In this paper, the thermal desorption of water and hydrogen from a rapidly solidified Al-Zn-Mg alloy powder was studied by means of temperature-programmed Desorption Mass Spectrometer (TPD-MS) by applying the Kissinger formalism.
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A new route of oxygen isotope exchange in the solid phase: demonstration in CuSO4.5H2O.
TL;DR: Temperature-programmed desorption mass spectrometry measurements on copper sulfate pentahydrate reveal an unambiguous occurrence of efficient oxygen isotope exchange between the water of crystallization and the sulfate in its CuSO(4) solid phase, and questions the common conviction of unfeasible oxygen exchange under geothermic conditions.
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