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. 2023 Jul 31;13:12381. doi: 10.1038/s41598-023-39347-4

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© The Author(s) 2023

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.

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(a) Topograms calculated by integrating section topograms from surface to 40-μm depth and (b) line profiles at the blue and red lines in sagittal topograms from (a). Depth was calculated as 32.2 and 30.0 μm for high and low current stress samples, respectively, using the distance between the two peaks.