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Correction: Hydrogeology Journal (2022) 30:1917–1931
In response to a Comment, several highlighted errors in the original article (Toulier et al, 2022) have been assessed and the corrections are presented here.
The double-ended arrow defining the piezometric head (H) was inappropriately drawn in the original Figures 2 and 3a. Accordingly, the length of the double-ended arrow in these figures has been extended to better represent the vertical datum, namely the sea level (z=0).
Conceptual model and technical terms for geologically-controlled confined aquifers, and unconfined aquifers (modified from Chen et al. 2018)
a Description of the free-flowing artesian well device (FFAWD) and measurement method through steps 1 to 4. b Typical pressure data set recorded by the probe over time (test on well n°8). The characteristics of free-flowing well n°8 are described in Table 1. c Design of the FFAWD
There is also a correction in the References section:
Jacob CE, Lohman SW (1952). Nonsteady flow to a well of constant drawdown in an extensive aquifer, Trans. Am. Geophys. Union, 33(4), 559– 569
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The online version of the original article can be found at https://doi.org/10.1007/s10040-022-02505-5
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Toulier, A., Lachassagne, P., Hendrayana, H. et al. Correction: A cost-effective device and methodology to compute aquifer transmissivity and piezometry from free-flowing artesian wells. Hydrogeol J 31, 849–851 (2023). https://doi.org/10.1007/s10040-023-02605-w
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DOI: https://doi.org/10.1007/s10040-023-02605-w