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. 2023 Mar 29;13:5132. doi: 10.1038/s41598-023-31640-6

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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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Pictures of the salt crust in the Hele-Shaw cell. Illustration of the various stages in the evolution of the crust identified from both the crust morphology modification and evaporation rate variation. The red horizontal dashed lines are guide to the eye to see better the crust evolution and its upward migration. The white objects on the liquid–gas interface or attached to the walls (more visible in the supplementary movies) correspond to residual glass beads.