Hydrogeology JournalDOI 10.1007/s10040-005-0010-3
Captions of Figs. 1 and 2 should have been formulated as follows:
Figure 1. a Location of the study site at Norville in the lower Seine Valley, France; b geomorphological three-dimensional diagram of the Bebec-Hannetot karstic system (Reprinted from Journal of Hydrology, 260, Massei N, Lacroix M, Wang HQ, Mahler BJ, Dupont JP, Transport of suspended solids from a karstic to an alluvial aquifer: the role of the karst/alluvium interface, 88–101, Copyright (2002), with permission from Elsevier).
Figure 2. Residence time distribution for each tracer test (peak areas = 1). Residence time distributions ordinates are H(t) = tracer flux/recovered mass (Reprinted from Journal of Hydrology, 275, Massei N, Wang HQ, Dupont JP, Rodet J, Laignel B, Assessment of direct transfer and resuspension of particles during turbid floods at a karstic spring, 109–121, Copyright (2003), with permission from Elsevier).
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Massei, N., Wang, H.Q., Field, M.S. et al. Interpreting tracer breakthrough tailing in a conduit-dominated karstic aquifer. Hydrogeol J 14, 1028 (2006). https://doi.org/10.1007/s10040-006-0093-5
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DOI: https://doi.org/10.1007/s10040-006-0093-5