The phrase "hydrothermal method" refers to a variety of processes used to crystallise compounds from highly heated aqueous solutions at high vapour pressures. Hydrothermal is a word with geology roots. Hydrothermal phase equilibria have been researched by geochemists and mineralogists since the turn of the twentieth century. The majority of the work was done by George W. Morey at the Carnegie Institution and Percy W. Bridgman at Harvard University to create the groundwork essential for the confinement of reactive media in the temperature and pressure range where the majority of hydrothermal research is done. A technique for creating single crystals that relies on the solubility of minerals in hot water under intense pressure is known as hydrothermal synthesis.
Stanislaw Dzwigaj
Sorbonne University, France
Thomas J Webster
Brown University, United States
Dai Yeun Jeong
Asia Climate Change Education Center, Korea, Republic of
Sergey Suchkov
N.D. Zelinskii Institute for Organic Chemistry of the Russian Academy of Sciences, Russian Federation
Jiri Dedecek
J Heyrovsky Institute of Physical Chemistry , Czech Republic
Vladimir G Chigrinov
Hong Kong University of Science and Technology, Russian Federation
Osman Adiguzel
Firat University, Turkey
Uday Som
Shizuoka University, Japan
Rabeharitsara Andry Tahina
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