Hydrogeophysical monitoring of intense rainfall infiltration in the karst critical zone

Published: 27 August 2021| Version 1 | DOI: 10.17632/vyzmvnj8hr.1


Column 1 presents the distance along the ERT profile. Column 2 represents the pseudo-depth calculated for a gradient array using the formula developed by Dahlin and Zhou [2006]. The following columns present the apparent resistivity for each of 106 time steps (after filtering). There is 1360 values of apparent resistivity for each time step.