“…Direct current electrical resistivity tomography (ERT) is one of the key geophysical methods for shallow-subsurface investigations, having applications in areas such as groundwater (Dahlin, 2001;Johnson et al, 2012;Meyerhoff et al, 2014;Park et al, 2016;Greggio et al, 2018;Alshehri and Abdelrahman, 2021), mineral exploration (Badmus and Olatinsu, 2009;Bery et al, 2012;Uhlemann et al, 2018;Martínez et al, 2019), environmental monitoring and remediation (Rosales et al, 2012;Rucker et al, 2013;Gabarrón et al, 2020;Rockhold et al, 2020;Kessouri et al, 2022), and engineering problems (Dahlin, 1996;Rizzo et al, 2004;Lysdahl et al, 2017). It can also be used for large-scale deepsubsurface investigations, e.g., for geothermal systems, active volcano imaging, and tectonic studies (Storz et al, 2000;Caputo et al, 2003;Johnson et al, 2010;Richards et al, 2010).…”