“…Meanwhile, it is generally accepted that solute transport is not a stochastically random process but rather dominated by structured heterogeneity, i.e., geological facies with contrasting hydraulic properties, and the spatial organization and connectivity of high‐conductivity zones [e.g., Fogg et al ., ; Zheng and Gorelick , ; Zinn and Harvey , ; Knudby and Carrera , ]; see Molz [] for a chronology of discussions and gained scientific knowledge in the past 35 years. Therefore, bi‐ and multimodal models mimicking the distribution of facies‐like discrete zones have increasingly been investigated and applied [e.g., Rubin , ; Dagan and Lessoff , ; Lessoff and Dagan , ; Dagan and Fiori , ; Fiori and Dagan , ; Ritzi et al ., ; de Marsily et al ., ; Feyen and Caers , ; Werth et al ., ; Lee et al ., ; Massabo et al ., ; Coppola et al ., ; Ramanathan et al ., ; Fiori , ; Allen‐King et al ., ; Maghrebi et al ., ; Pryshlak et al ., ; Soltanian et al ., , ; Zarlenga and Fiori , ; Zhang and Zhang , ]. In this paper, we make use of the work of Bayer et al .…”