• Aucun résultat trouvé

Utility of Scanning Transmission X-ray Microscopy to Investigate Chemical Composition in Perovskite Thin Films

N/A
N/A
Protected

Academic year: 2021

Partager "Utility of Scanning Transmission X-ray Microscopy to Investigate Chemical Composition in Perovskite Thin Films"

Copied!
2
0
0

Texte intégral

(1)

HAL Id: cea-03123519

https://hal-cea.archives-ouvertes.fr/cea-03123519

Submitted on 28 Jan 2021

HAL is a multi-disciplinary open access

archive for the deposit and dissemination of sci-entific research documents, whether they are pub-lished or not. The documents may come from teaching and research institutions in France or abroad, or from public or private research centers.

L’archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des établissements d’enseignement et de recherche français ou étrangers, des laboratoires publics ou privés.

Utility of Scanning Transmission X-ray Microscopy to

Investigate Chemical Composition in Perovskite Thin

Films

Haeyon Jun, Denis Tondelier, Bernard Geffroy, Jean-Eric Bourée, Sufal

Swaraj, Yvan Bonnassieux

To cite this version:

Haeyon Jun, Denis Tondelier, Bernard Geffroy, Jean-Eric Bourée, Sufal Swaraj, et al.. Utility of Scanning Transmission X-ray Microscopy to Investigate Chemical Composition in Perovskite Thin Films. Journées Nationales du Photovoltaïque, Jan 2021, Dourdan, France. 2021. �cea-03123519�

(2)

Utility of Scanning Transmission X-ray Microscopy

to Investigate Chemical Composition in Perovskite Thin Films

Haeyeon Jun1,2, Denis Tondlier1, Bernard Geffroy1,3, Jean-Eric Bourée1, Sufal Swaraj2 and Yvan Bonnassieux1

1LPICM-CNRS (UMR7647), Ecole polytechnique, IP Paris, 91128 Palaiseau, France 2Synchrotron SOLEIL, L'Orme des Merisiers Saint-Aubin, BP 48 91192 Gif-sur-Yvette Cedex

3 Université Paris-Saclay, CEA, CNRS, NIMBE, LICSEN, 91191 Gif-sur-Yvette, France

Organic–inorganic lead halide perovskites with remarkable photoelectric properties have achieved power conversion efficiencies of 25.2 %, making them a promising candidate as an emerging solar cell technology [1]–[4]. Formation of high crystalline perovskite film is necessary for stable and high efficient solar cells. Among them, vacuum-based deposition processes are profitable because highly uniform and smooth thin films can be obtained [5], [6]. Especially, characterization of evaporated perovskite thin films using various technique contribute to the accurate analysis in the physical or chemical point of view [7].

Scanning transmission X-ray microscopy (STXM) is an experimental technique based on near edge X-ray absorption fine structure (NEXAFS) spectroscopy [8]. This spectro-microscopy technique allows us to obtain quantitative chemical composition maps in bulk of materials with high spatial resolution (~ 50 nm). We have been exploring the utility of this technique in order to characterize perovskite films synthesized with evaporation techniques. In this poster, we present some strategies developed to study these materials. In particular, we have shown how the soft x-ray energy range from 270 to 750 eV, that includes the C K-edge, N K-edge, Pb N-edge and I M-edge, can be used to quantify elemental and molecular concentration[9]–[11].

Keywords

Organic–inorganic halide perovskite, Co-evaporation, Scanning transmission X-ray microscopy Reference

[1] D. B. Mitzi, C. A. Feild, Z. Schlesinger, and R. B. Laibowitz, J. Solide State chem., 114, 1. 159–163, 1995.

[2] S. D. Stranks et al., Science, 342, 10, 341–345, 2013.

[3] J. H. Noh, S. H. Im, J. H. Heo, T. N. Mandal, and S. Il Seok, Nano Lett., 13, 4, 1764–1769, 2013. [4] “NREL efficiency chart.” [Online]. Available: https://www.nrel.gov/pv/cell-efficiency.html. [5] M. Liu, M. B. Johnston, and H. J. Snaith, Nature, 501, 7467, 395–398, 2013.

[6] L. K. Ono, S. Wang, Y. Kato, S. R. Raga, and Y. Qi, Energy Environ. Sci., 7, 12, 3989–3993, 2014. [7] M. Sowinska, C. Das, K. Wojciechowski, and Z. Rouissi, ISSRNS, 15, 1, 1500962, 2016.

[8] H. Ade, Academic Press, 32, 225-262. 1998.

[9] J. Stöhr, R. Jaeger, J. Feldhaus, S. Brennan, D. Norman, and G. Apai, Appl. Opt., 19, 23, 3911, 1980. [10] C. Reverdin et al., AIP Conf. Proc., 207, 5, 207–212, 2008.

[11] M. W. Lin et al., Adv. Mater. Interfaces, 3, 17, 1–12, 2016.

Figure 1. (a) Schematic of scanning transmission X-ray microscope (b) Carbon K-edge, Nitrogen N-edge and Iodide M-edge NEXAFS spectroscopy of PbI2 and MAPbI3 perovskite film.

Figure

Figure 1. (a) Schematic of scanning transmission X-ray microscope  (b) Carbon K-edge, Nitrogen N-edge and Iodide M-edge  NEXAFS spectroscopy of PbI 2  and MAPbI 3  perovskite film.

Références

Documents relatifs

Glancing incidence X-ray reflectivity of sample # 2 (dots), an improved simulation (dotted curve) based on the result of the Fourier transform shown in figure 5, a simulation

detection will be corrected by considering a "virtual" medium having a composition obtained by the dilution of the film compound into a substrate thickness equal to

The image contrast is dominated by photoelectric absorption and scattering is negligible ; thus the resolution is only limited by the wavelength and the energy dose in the

Physios Department, Queen Elizabeth College, University of London, Campden Hill Road, London W8 7 AH, U.K. Résumé - En reconstruction d'image à trois dimensions, on a besoin

In this paper, we combine high-resolution transmission electron microscopy with x-ray absorption spectroscopy and x-ray magnetic circular dichroism (XMCD) to determine the

sample : the central part is characterized by an indigo blue uniform background ; (b) interference colors observed in the case of a sample annealed at 170 °C for

Linen bres present a composite structure oriented along the bre axis 18,21 and composed, from the inner to the outer part, of a lumen, of a secondary cell wall and of a primary

Quan- tification of the ferric/ferrous iron ratio in silicates by scanning transmission X-ray microscopy at the Fe L2,3 edges.. Contributions to Mineralogy and Petrology,