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. 2024 Aug 6;167(10):1175–1201. doi: 10.1007/s10533-024-01163-x

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© The Author(s) 2024

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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Fig. 10 — Monthly flow-weighted concentration versus monthly specific discharge for the summer, growing season and winter, dormant season for the (a, b) sum of base cations (SBC), (c, d) silica (SiO₂), and (e, f) acid neutralizing capacity (ANC) at Piney River (left column) and Paine Run (right column). Error bars represent 95% confidence intervals. The best fit lines for the respective seasons, inclusive of both the typical (closed circles) and atypical (open circles) water years are presented along with the associated r² and p values