Growing crystals from a molten bath made mostly of one of the crystal’s own ingredients – extra selenium, for example – much as sugar crystals grow from a cooling syrup. Because the bath is part of the crystal already, no foreign solvent atoms get trapped inside.
Going deeper
Self-flux growth dissolves a compound in a melt of one of its own elements – here excess selenium for WSe2 – and grows crystals by cooling very slowly. Because the solvent is part of the crystal, no foreign atoms can be taken up from it.
How it works
Flux growth dissolves the ingredients of a crystal in a molten solvent, the flux, well below the temperature at which the compound itself would melt. On slow cooling, the solubility falls and crystals nucleate and grow close to equilibrium, often with well-formed facets. fluxes such as tin, gallium or indium are common for intermetallic compounds.
Self-flux growth is the special case in which the flux is one of the crystal’s own elements: excess selenium for WSe2, excess tellurium for tellurides. The components are sealed in a quartz ampoule, heated until they dissolve, held, and cooled over days or weeks. At the end, the remaining liquid is poured or spun off through a filter while still hot, or the leftover is removed afterwards by evaporation.
Why the crystals are cleaner
The most common alternative for crystals, , carries material through the gas phase with a transport agent such as iodine. It is faster, but the agent can end up inside the crystal, and growth happens further from equilibrium. A self-flux has no foreign solvent to incorporate, grows slowly, and keeps the crystal in chalcogen-rich conditions.
The difference is measurable. In a study of transition-metal diselenides combining scanning tunnelling and , the dominant intrinsic defects were metal and chalcogen antisites rather than , and controlling the synthesis cut their density from above 1013 to below 1011 per cm2, with emission efficiency rising about a hundred-fold.
Costs and pitfalls
The price is time and yield: a run can take weeks, and the crystals are usually millimetres across. Droplets of flux can stick to surfaces or be trapped inside, and they have to be removed before . Not every compound works: the must allow the wanted phase to crystallise first from a melt rich in one component.
Chalcogens have high vapour pressures at growth temperatures, so sealed ampoules are under pressure and can burst; thick-walled quartz, limited fill amounts and careful heating are part of the method. Crystal quality is judged by defect counts from , linewidths and, for metals, the ratio of room-temperature to low-temperature resistance.
For specialists
Crystal growth from a melt rich in one of the crystal’s own constituents, such as excess selenium for WSe2.