Speciation of CuCl and CuCl Thiol-Amine Solutions and Characterization of Resulting Films: Implications for Semiconductor Device Fabrication.

Thiol-amine mixtures are an attractive medium for the solution processing of semiconducting thin films because of their remarkable ability to dissolve a variety of metals, metal chalcogenides, metal salts, and chalcogens. However, very little is known about their dissolution chemistry. Electrospray ionization high-resolution tandem mass spectrometry and X-ray absorption spectroscopy were employed to identify the species formed upon dissolution of CuCl and CuCl in 1-propanethiol and n-butylamine. Copper was found to be present exclusively in the 1+ oxidation state for both solutions. The copper complexes detected include copper chlorides, copper thiolates, and copper thiolate chlorides. No complexes of copper with amines were observed. Additionally, alkylammonium ions and alkylammonium chloride adducts were observed. These findings suggest that the dissolution is initiated by proton transfer from the thiol to the amine, followed by coordination of the thiolate anions with copper cations. Interestingly, the mass and X-ray absorption spectra of the solutions of CuCl and CuCl in thiol-amine were essentially identical. However, dialkyl disulfides were identified by Raman spectroscopy as an oxidation product only for the copper(II) solution, wherein copper(II) had been reduced to copper(I). Analysis of several thiol-amine pairs suggested that the dissolution mechanism is quite general. Finally, analysis of thin films prepared from these solutions revealed persistent chlorine impurities, in agreement with previous studies. These impurities are explained by the mass spectrometric finding that chloride ligands are not completely displaced by thiolates upon dissolution. These results suggest that precursors other than chlorides will likely be preferred for the generation of high-efficiency copper chalcogenide films, despite the reasonable efficiencies that have been obtained for films generated from chloride precursors in the past.