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Correction: Double-peaked breakthrough curves as a consequence of solute transport through underground lakes: a case study of the Furfooz karst system, Belgium

Abstract : There was an error in the fluorimeter data computing for tracer test 1 (Q= 20 l/s) at site 4. Indeed, due to a misinterpretation of the fluorimeter recording, some data should appear as interpolated. This interpolation was based, namely, on the comparison with other tracer test results. Figure 4 is corrected here with the interpolated data appearing as a red dotted line (top graph, see `interpolated data'). In consequence, the recovery rate (39.9%) calculated in Table 1 is an estimation based on the interpolated data. A note has been added to Table 1. Correction: Hydrogeology Journal (2018) 26:641-650 https://doi.org/10.1007/s10040-017-1671-4
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https://hal-insu.archives-ouvertes.fr/insu-03665949
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Submitted on : Thursday, May 12, 2022 - 10:52:45 AM
Last modification on : Friday, May 13, 2022 - 12:02:43 PM

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Lorraine Dewaide, Pauline Collon, Amaël Poulain, Gaëtan Rochez, Vincent Hallet. Correction: Double-peaked breakthrough curves as a consequence of solute transport through underground lakes: a case study of the Furfooz karst system, Belgium. 2019, pp.3109-3111. ⟨10.1007/s10040-019-02044-6⟩. ⟨insu-03665949⟩

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