Hydrothermal synthesis

Hydrothermal synthesis includes the various techniques of crystallizing substances from high-temperature aqueous solutions at high vapor pressures; also termed "hydrothermal method". The term "hydrothermal" is of geologic origin.[1] Geochemists and mineralogists have studied hydrothermal phase equilibria since the beginning of the twentieth century. George W. Morey at the Carnegie Institution and later, Percy W. Bridgman at Harvard University did much of the work to lay the foundations necessary to containment of reactive media in the temperature and pressure range where most of the hydrothermal work is conducted.

Crystallization
Fundamentals
Crystal · Crystal structure · Nucleation
Concepts
Crystallization · Crystal growth
Recrystallization · Seed crystal
Protocrystalline · Single crystal
Methods and technology
Boules
Bridgman–Stockbarger method
Crystal bar process
Czochralski method
Epitaxy · Flux method
Fractional crystallization
Fractional freezing
Hydrothermal synthesis
Kyropoulos method
Laser-heated pedestal growth
Micro-pulling-down
Shaping processes in crystal growth
Skull crucible
Verneuil method
Zone melting
A synthetic quartz crystal grown by the hydrothermal method

Hydrothermal synthesis can be defined as a method of synthesis of single crystals that depends on the solubility of minerals in hot water under high pressure. The crystal growth is performed in an apparatus consisting of a steel pressure vessel called an autoclave, in which a nutrient is supplied along with water. A temperature gradient is maintained between the opposite ends of the growth chamber. At the hotter end the nutrient solute dissolves, while at the cooler end it is deposited on a seed crystal, growing the desired crystal.

Advantages of the hydrothermal method over other types of crystal growth include the ability to create crystalline phases which are not stable at the melting point. Also, materials which have a high vapour pressure near their melting points can be grown by the hydrothermal method. The method is also particularly suitable for the growth of large good-quality crystals while maintaining control over their composition. Disadvantages of the method include the need of expensive autoclaves, and the impossibility of observing the crystal as it grows if a steel tube is used.[2] There are autoclaves made out of thick walled glass, which can be used up to 300 °C and 10 bar.[3]

History
Synthetic quartz crystals produced in the autoclave shown in Western Electrics pilot hydrothermal quartz plant in 1959.

The first report of the hydrothermal growth of crystals[4] was by German geologist Karl Emil von Schafhäutl (1803–1890) in 1845: he grew microscopic quartz crystals in a pressure cooker.[5] In 1848, Robert Bunsen reported growing crystals of barium and strontium carbonate at 200 °C and at pressures of 15 atmospheres, using sealed glass tubes and aqueous ammonium chloride ("Salmiak") as a solvent.[6] In 1849 and 1851, French crystallographer Henri Hureau de Sénarmont (1808–1862) produced crystals of various minerals via hydrothermal synthesis.[7][8] Later (1905) Giorgio Spezia (1842–1911) published reports on the growth of macroscopic crystals.[9] He used solutions of sodium silicate, natural crystals as seeds and supply, and a silver-lined vessel. By heating the supply end of his vessel to 320–350 °C, and the other end to 165–180 °C, he obtained about 15 mm of new growth over a 200-day period. Unlike modern practice, the hotter part of the vessel was at the top. A shortage in the electronics industry of natural quartz crystals from Brazil during World War 2 led to postwar development of a commercial-scale hydrothermal process for culturing quartz crystals, by A. C. Walker and Ernie Buehler in 1950 at Bell Laboratories.[10] Other notable contributions have been made by Nacken (1946), Hale (1948), Brown (1951), and Kohman (1955).[11]

Uses

A large number of compounds belonging to practically all classes have been synthesized under hydrothermal conditions: elements, simple and complex oxides, tungstates, molybdates, carbonates, silicates, germanates etc. Hydrothermal synthesis is commonly used to grow synthetic quartz, gems and other single crystals with commercial value. Some of the crystals that have been efficiently grown are emeralds, rubies, quartz, alexandrite and others. The method has proved to be extremely efficient both in the search for new compounds with specific physical properties and in the systematic physicochemical investigation of intricate multicomponent systems at elevated temperatures and pressures.

Equipment for hydrothermal crystal growth

The crystallization vessels used are autoclaves. These are usually thick-walled steel cylinders with a hermetic seal which must withstand high temperatures and pressures for prolonged periods of time. Furthermore, the autoclave material must be inert with respect to the solvent. The closure is the most important element of the autoclave. Many designs have been developed for seals, the most famous being the Bridgman seal. In most cases, steel-corroding solutions are used in hydrothermal experiments. To prevent corrosion of the internal cavity of the autoclave, protective inserts are generally used. These may have the same shape as the autoclave and fit in the internal cavity (contact-type insert), or be "floating" type inserts which occupy only part of the autoclave interior. Inserts may be made of carbon-free iron, copper, silver, gold, platinum, titanium, glass (or quartz), or Teflon, depending on the temperature and solution used.

Methods

Temperature-difference method

This is the most extensively used method in hydrothermal synthesis and crystal growing. Supersaturation is achieved by reducing the temperature in the crystal growth zone. The nutrient is placed in the lower part of the autoclave filled with a specific amount of solvent. The autoclave is heated in order to create two temperature zones. The nutrient dissolves in the hotter zone and the saturated aqueous solution in the lower part is transported to the upper part by convective motion of the solution. The cooler and denser solution in the upper part of the autoclave descends while the counterflow of solution ascends. The solution becomes supersaturated in the upper part as the result of the reduction in temperature and crystallization sets in.

Temperature-reduction technique

In this technique crystallization takes place without a temperature gradient between the growth and dissolution zones. The supersaturation is achieved by a gradual reduction in temperature of the solution in the autoclave. The disadvantage of this technique is the difficulty in controlling the growth process and introducing seed crystals. For these reasons, this technique is very seldom used.

Metastable-phase technique

This technique is based on the difference in solubility between the phase to be grown and that serving as the starting material. The nutrient consists of compounds that are thermodynamically unstable under the growth conditions. The solubility of the metastable phase exceeds that of the stable phase, and the latter crystallize due to the dissolution of the metastable phase. This technique is usually combined with one of the other two techniques above.

See also

References
  1. The earliest occurrence of the word "hydrothermal" appears to be: Sir Charles Lyell, A Manual of Elementary Geology … , 5th ed. (Boston, Massachusetts: Little, Brown, and Company, 1855), page 603: "The metamorphic theory [requires us to affirm] that an action, existing in the interior of the earth at an unknown depth, whether thermal, hydro-thermal, … "
  2. O'Donoghue, M. (1983). A guide to Man-made Gemstones. Great Britain: Van Nostrand Reinhold Company. pp. 40–44. ISBN 0-442-27253-7.
  3. Schubert, Ulrich. and Hüsing, Nicola. (2012) Synthesis of inorganic materials Weinheim: Wiley-VCH, page 161
  4. For a more detailed history of hydrothermal synthesis, see: K. Byrappa and Masahiro Yoshimura, Handbook of Hydrothermal Technology (Norwich, New York: Noyes Publications, 2001), Chapter 2: History of Hydrothermal Technology.
  5. Schafhäutl (1845) "Die neuesten geologischen Hypothesen und ihr Verhältniß zur Naturwissenschaft überhaupt" (The latest geological hypotheses and their relation to science in general), Gelehrte Anzeigen (published by: die königliche Bayerische Akademie der Wissenschaften (the Royal Bavarian Academy of Sciences)), 20 : 557, 561-567, 569-576, 577-596. On page 578, he states: "5) Bildeten sich aus Wasser, in welchen ich im Papinianischen Topfe frisch gefällte Kieselsäure aufgelöst hatte, beym Verdampfen schon nach 8 Tagen Krystalle, die zwar mikroscopisch, aber sehr wohl erkenntlich aus sechseitigen Prismen mit derselben gewöhnlichen Pyramide bestanden." ( 5) There formed from water in which I had dissolved freshly precipitated silicic acid in a Papin pot [i.e., pressure cooker], after just 8 days of evaporating, crystals, which albeit were microscopic but consisted of very easily recognizable six-sided prisms with their usual pyramids.)
  6. R. Bunsen (1848) "Bemerkungen zu einigen Einwürfen gegen mehrere Ansichten über die chemisch-geologischen Erscheinungen in Island" (Comments on some objections to several views on chemical-geological phenomena in Iceland), Annalen der Chemie und Pharmacie, 65 : 70-85. On page 83, Bunsen mentions crystallizing the carbonate salts of barium, strontium, etc. ("die kohlensauren Salze der Baryterde, Strontianerde, etc.").
  7. See:
  8. "Hydrothermal Crystal Growth - Quartz". Roditi International. Retrieved 2006-11-17.
  9. Giorgio Spezia (1905) "La pressione è chimicamente inattiva nella solubilità e ricostituzione del quarzo" (Pressure is chemically inactive in the solubility and reconstitution of quartz), Atti della Reale Accademia delle scienze di Torino (Proceedings of the Royal Academy of Sciences in Turin), 40 : 254-262.
  10. McWhan, Denis McWhan (2012). Sand and Silicon: Science That Changed the World. Oxford Univ. Press. p. 11. ISBN 978-0199640270.
  11. Laudise, R.A. (1958). R.H. Doremus; B.W. Roberts; D. Turnbull (eds.). Growth and perfection of crystals. Proceedings of an International Conference on Crystal Growth held at Cooperstown, New York on August 27–29, 1958. Wiley, New York. pp. 458–463.
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