Effect of CH3NH3PbI3 Perovskite Cuboids Size on Ferroelectric Characteristics
Nam-Gyu Park a, Sang-Woo Kim a, Sung Kyun Kim a, Hui-Seon Kim a
a Sungkyunkwan University, South Korea, 300 Cheoncheon-dong, Jangan-gu, Suwon, 440, Korea, Republic of
International Conference on Hybrid and Organic Photovoltaics
Proceedings of International Conference on Hybrid and Organic Photovoltaics 2015 (HOPV15)
Roma, Italy, 2015 May 11th - 13th
Organizer: Filippo De Angelis
Oral, Hui-Seon Kim, presentation 045
Publication date: 5th February 2015
Size-dependent polarization characteristics of CH3NH3PbI3 perovskite cuboids were investigated by piezoresponse force microscopy (PFM). From the PFM measurement, It is found that the dipole array domain was closely overlapped with perovskite cuboids size. Unpoled (Vapp= 0 V) perovskite showed some extent of spontaneous polarization where 700 nm-sized perovskite cuboids had dipole orientation toward both (+) and (-) direction, but the dipole alignment toward (-) direction was highly enhanced with 100 nm-sized small cuboids. While dipole alignment in large perovskite cuboids (700 nm) were siginificantly dependent on the poling direction showing switchable characteristic, small perovskite cuboids (100 nm) always showed a biased-dipole alignment toward (-) direction regardless of a given poling direction (Vapp= +/- 3 V). The aligned dipole retention after a removal of external field (poling) was quite stable showing the retention time of 30 min or more. These observations suggest that crystal size is a dominant factor to determine the dipole polarization characteristics which is carefully correlated with the effective charge separation and retarded charge recombination in bulk perovskite by the aid of the developed internal electric field. In terms of an actual device level, the large crystals with positive poling provides a favorable internal electric field for the separating generated charge carrier and also inhibits carrier trapped at the boundary of dipole domain leading alleviated I-V hysteresis.

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