20–23 Sept 2023
Metropol Lake Resort, Ohrid
Europe/Skopje timezone

Cyclic voltammetry study of DMAPbI3 Perovskite Material

Not scheduled
20m
Metropol Lake Resort, Ohrid

Metropol Lake Resort, Ohrid

Poster presentation

Speaker

Jeta Sela (Department of Chemistry, Faculty of Natural Sciences and Mathematics, University of Tetovo, Tetovo, North Macedonia)

Description

In the last decade, the most investigated perovskite materials are the hybrid organic-inorganic perovskites (HOIPs) due to their optoelectronic properties and possible application in production of photovoltaics. As a result, there is a continuous ongoing search for new ones, but also a thorough investigation of the properties of already known HOIPs. Here we present the cyclic voltammetry study of dimethylammonium lead iodide (DMAPbI3).
A slightly modified synthesis of DMAPbI3 than the one described in the literature was performed. Stoichiometric amounts of lead iodide (PbI2) and dimethylammonium iodide (DMAI) were dissolved in acetonitrile, followed by temperature controlled evaporation at 60 °C. This lead to the formation of DMAPbI3 yellow crystalline powder. The identification and purity of the obtained compound was confirmed by PXRD, vibrational spectroscopy, and SEM/EDX analysis.
Cyclic voltammetry studies of DMAPbI3 were conducted in dichloromethane (DCM) and tetrabutylammonium chloride (TBAC) as the electrolyte. A paraffin-impregnated graphite electrode (PIGE) was utilized as the working electrode, on which the perovskite microparticles were immobilized. The electrochemical activity of DMAPbI3 is evident through an intense, wide, and irreversible anodic peak that initiates at -0.153 V. The voltammograms recorded with lower scan rates revealed that this peak is complex consisting the oxidation of DMAPbI3 constituents. The organic cation (DMA+) exhibits oxidation to various oxidation states, including the possibility of being oxidized to CO2. The lead ion can undergo oxidation to form lead oxide, while the iodide ion can undergo oxidation to different oxidation numbers, but most probably to elemental iodine. However, the quantity of elemental iodine produced is minimal, making it difficult to detect. The observed vague and small reduction peak may be attributed to some of these by-products, rather than originating from the perovskite itself.

Primary authors

Arianit Reka (Department of Chemistry, Faculty of Natural Sciences and Mathematics, University of Tetovo, Tetovo, North Macedonia) Jeta Sela (Department of Chemistry, Faculty of Natural Sciences and Mathematics, University of Tetovo, Tetovo, North Macedonia) Mr Leon Stojanov (Institute of Chemistry, Faculty of Natural Sciences and Mathematics, Ss. Cyril and Methodius University, Skopje, North Macedonia) Miha Bukleski (Ss. Cyril and Methodius University, Faculty of Natural Sciences and Mathematics, Institute of Chemistry) Sandra Dimitrovska-Lazova (Ss. Cyril and Methodius University, Faculty of Natural Sciences and Mathematics, Institute of Chemistry) Slobotka Aleksovska (Institute of Chemistry, Faculty for Natural Sciences and Mathematics, University St. Cyril and Methodius) Valentin Mirceski (Ss Cyril and Methodius” University in Skopje)

Presentation materials