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Kunimitsu Morishige

Researcher at Okayama University of Science

Publications -  71
Citations -  2678

Kunimitsu Morishige is an academic researcher from Okayama University of Science. The author has contributed to research in topics: Adsorption & Capillary condensation. The author has an hindex of 28, co-authored 70 publications receiving 2523 citations.

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Freezing and melting of water in a single cylindrical pore: The pore-size dependence of freezing and melting behavior

TL;DR: In order to clarify the origin of the hysteresis between freezing and melting of pore water, this paper performed x-ray diffraction measurements of water confined inside the cylindrical pores of seven kinds of ordered mesoporous materials with different pore radii (1.2-2.9 nm).
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Capillary Critical Point of Argon, Nitrogen, Oxygen, Ethylene, and Carbon Dioxide in MCM-41

TL;DR: In this paper, the effect of temperature on adsorption isotherms of Ar, N2, O2, C2H4, and CO2 on mesoporous MCM-41 molecular sieves with different pore sizes has been measured.
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Thermal desorption and infrared studies of ammonia, amines and pyridines chemisorbed on chromic oxide

TL;DR: The thermal desorption spectra of ammonia, amines and pyridines chemisorbed on Cr2O3 as well as the infrared absorption spectra have been measured in order to elucidate the acidic properties of the surface.
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Capillary condensation of nitrogen in MCM-41 and SBA-15

TL;DR: In this paper, the exact pore sizes of the samples from comparing the experimental equilibrium pressure at 77 K with the NLDFT isotherms were determined by extrapolating a plot of the equilibrium pressure versus temperature measured above Tch.
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Nature of adsorption and desorption branches in cylindrical pores.

TL;DR: Results clearly show that in the open-ended cylindrical pores of MCM-41, capillary condensation rather than evaporation takes place near a thermodynamical equilibrium transition, as opposed to the general statement that capillary evporation can occur via a meniscus formed at the pore mouth, and, thus, takes place at equilibrium.