Hostname: page-component-74656f9884-8rzl6 Total loading time: 0 Render date: 2026-11-06T05:59:38.613Z Has data issue: false hasContentIssue false

Nano-scale compositional analysis of surfaces and interfaces in earth-abundant kesterite solar cells

Published online by Cambridge University Press:  02 November 2016

Kasra Sardashti
Affiliation:
Materials Science Program, University of California–San Diego, La Jolla, CA 92093, USA; and Department of Chemistry and Biochemistry, University of California–San Diego, La Jolla, CA 92093, USA
Dennis Paul
Affiliation:
Physical Electronic, Inc., Chanhassen, MN 55317, USA
Chuck Hitzman
Affiliation:
Stanford Nano Shared Facilities, Stanford, CA 94305, USA
John Hammond
Affiliation:
Physical Electronic, Inc., Chanhassen, MN 55317, USA
Richard Haight
Affiliation:
IBM T J Watson Research Center, Yorktown Heights, NY 10598, USA
Andrew C. Kummel*
Affiliation:
Department of Chemistry and Biochemistry, University of California–San Diego, La Jolla, CA 92093, USA
*
a) Address all correspondence to this author. e-mail: akummel@ucsd.edu

Abstract

Kesterite Cu2ZnSn(S,Se)4 (CZTSSe) absorbers are considered promising alternatives to commercial thin film technologies including CdTe and Cu(In,Ga)Se2 (CIGSe) owing to the earth abundance and non-toxicity of their constituents. However, to be competitive with the existing technologies, the photovoltaic performance of CZTSSe solar cells needs to be improved beyond the current record conversion efficiency of 12.6%. In this study, nanoscale elemental mapping using Auger nanoprobe microscopy (NanoAuger) and nano secondary ion mass spectrometry (NanoSIMS) are used to provide a clear picture of the compositional variations between the grains and grain boundaries in Cu2ZnSn(S,Se)4 kesterite thin films. NanoAuger measurements revealed that the top surfaces of the grains are coated with a Zn-rich (Zn,Sn)Ox layer. While thick oxide layers were observed at the grain boundaries, their chemical compositions were found to be closer to SnOx . NanoSIMS elemental maps confirmed the presence of excess oxygen deeper within the grain boundary grooves, as a result of air annealing of the CZTSSe films.

Keywords

Information

Type
Invited Feature Paper
Copyright
Copyright © Materials Research Society 2016 
Figure 0

FIG. 1. Secondary electron micrograph and NanoAuger elemental maps for Cu, Zn, Sn, Se, and O measured on as-inserted CZTSSe surface after 10 min air anneal at 350 °C. The scan size is 2 × 2 µm2. Grain boundaries have higher concentrations of Sn and O compared to the top surfaces of the grains. There is a void from which very small Auger signals were detected. Therefore, this void appeared as a dark region in all the five elemental maps.

Figure 1

FIG. 2. (a) Secondary electron micrograph and O elemental map for air-annealed CZTSSe surface with the position of the horizontal line trace shown by the dotted lines. (b) Peak-to-peak intensities for Cu, Zn, Sn, and O, normalized to the relative sensitivity factors (RSFs), along the line traces shown in (a). The line traces show that the variations in peak-to-peak intensities between the grains and grain boundaries are only 20–40%. Therefore, darker or brighter regions in the elemental maps do not correspond to full depletion or accumulation of the elements.

Figure 2

FIG. 3. Secondary electron micrograph and NanoAuger elemental maps for Cu, Zn, Sn, Se, and O measured on air-annealed CZTSSe surface after 30 s of Ar+ sputtering with 0.5 kV ion beam energy and 600 nA filament current. The scan size for these measurements is 3 × 3 µm2. Similar to the as-inserted sample, grain boundaries appear to have larger concentrations of Sn and O.

Figure 3

FIG. 4. (a) Secondary electron micrograph and Sn elemental map for air-annealed CZTSSe top surface after 30 s of Ar+ sputtering. (b) Auger survey spectra for area 1 (grain) and point 2 (grain boundary). Elemental compositions calculated from the Auger spectra are shown in the boxes on the bottom right of the spectra.

Figure 4

FIG. 5. (a) Secondary electron micrograph of air-annealed CZTSSe surface before Ar+ sputtering. The area chosen for spectroscopy is marked by the yellow box. (b) Elemental ratios calculated for Cu, Zn, Sn, S, Se, and O in area 1 before (red) and after (blue) Ar+ sputtering. (c) Sn MNN Auger peak before and after surface oxide removal by Ar+ sputtering. (d) Zn LMM Auger peak before and after surface oxide removal by Ar+ sputtering. For both (c) and (d) Auger peaks are in absolute mode and the peak intensities are normalized to the maximum intensities. It should be noted that the left shoulder for sputtered surface seems to be larger than the as-inserted surface. This background increase could be due to the overlap between Cu1 and Zn1 Auger peaks, particularly considering the increase in [Cu] after sputtering.

Figure 5

FIG. 6. Planar secondary electrons and elemental maps for O, S, and Se for three different frames measured by NanoSIMS (Cs+ source) on air-annealed CZTSSe surfaces at 3 different times during the profiling. Frame 1, 2, and 3 are subsequently showing deeper layers on the sample surface. O is present at the GBs of the air-annealed sample after more than 3 min of depth profiling (equivalent to 70–100 nm of CZTSSe removal).

Figure 6

FIG. 7. Planar secondary electrons and elemental maps for O, S, and Se measured by NanoSIMS (Cs+ source) on (a) hard-baked (HB) and (b) air-annealed (HB + AA) CZTSSe surfaces. Data has been integrated over 7 measurement frames. According to the O maps, air annealing the sample resulted in significantly higher O content at the GBs.