Chemical transport reaction

In Chemistry, a chemical transport reaction describes a process for purification and crystallization of non-volatile solids. The process is also responsible for certain aspects of mineral growth from the effluent of volcanoes. The technique is distinct from chemical vapor deposition, which usually entails decomposition of molecular precursors (e.g. SiH₄ → Si + 2H₂) and which gives conformal coatings.

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The technique, which was popularized by Schäfer,^[1] entails the reversible conversion of nonvolatile chemical compounds into volatile derivatives.^[2] The volatile derivative migrates throughout a sealed reactor, typically a sealed, evacuated glass tube heated in a tube furnace. Elsewhere in the tube where the temperature is held at a different temperature, the volatile derivative reverts to the parent solid and the transport agent is released. The transport agent is thus catalytic. The technique requires that the two ends of tube (which contains the sample to be crystallized) be maintained at different temperatures. So-called two-zone tube furnaces are employed for this purpose.

Cases of the exothermic and endothermic reactions of the transporting agent

Transport reactions are classified according to the thermodynamics of the reaction between the solid and the transporting agent. When the reaction is exothermic, then the solid of interest is transported from the cooler end (which can be quite hot) of the reactor to a hot end, where the equilibrium constant is less favorable and the crystals grow. The reaction of molybdenum dioxide with the transporting agent iodine is an exothermic process, thus the MoO₂ migrates from the cooler end (700 °C) to the hotter end (900 °C):

MoO₂ + I₂ MoO₂I₂ ΔH_rxn < 0 (exothermic)

Using 10 milligrams of iodine for 4 grams of the solid, the process requires several days.

Alternatively, when the reaction of the solid and the transport agent is endothermic, the solid is transported from a hot zone to a cooler one. For example:

Fe₂O₃ + 6 HCl Fe₂Cl₆ + 3 H₂O ΔH_rxn > 0 (endothermic)

The sample of iron(III) oxide is maintained at 1000 °C, and the product is grown at 750 °C. HCl is the transport agent. Crystals of hematite are reportedly observed at the mouths of volcanoes because of chemical transport reactions whereby volcanic hydrogen chloride volatalizes iron(III) oxides.^[3]

Halogen lamp

A similar reaction like that of MoO₂ is used in halogen lamps. The tungsten is evaporated from the tungsten filament and converted with traces of oxygen and iodine into the WO₂I₂, at the high temperatures near the filament the compound decomposes back to tungsten oxygen and iodine. ^[4]

WO₂ + I₂ WO₂I₂ ΔH_rxn < 0 (exothermic)

References

1. ^ Günther Rienäcker, Josef Goubeau (1973). "Professor Harald Schäfer". Zeitschrift für anorganische und allgemeine Chemie 395 (2-3): 129-133. doi:10.1002/zaac.19733950202.
2. ^ Schäfer, H. "Chemical Transport Reactions" Academic Press, New York, 1963.
3. ^ P. Kleinert, D. Schmidt (1966). "Beiträge zum chemischen Transport oxidischer Metallverbindungen. I. Der Transport von α-Fe₂O₃ über dimeres Eisen(III)-chlorid". Zeitschrift für anorganische und allgemeine Chemie 348 (3-4): 142 - 150. doi:10.1002/zaac.19663480305.
4. ^ J. H. Dettingmeijer, B. Meinders (1968). "Zum system W/O/J. I: das Gleichgewicht WO₂, f + J₂, g = WO₂J₂,g". Zeitschrift für anorganische und allgemeine Chemie 357 (1-2): 1 - 10. doi:10.1002/zaac.19683570101.