“…In hydrogeology, the adjoint state method has been employed in many applications including interpretation of interference tests using geostastistical techniques (de Marsily et al, 1984), steady-state groundwater flow (Sykes et al, 1985;Wilson & Metcalfe, 1985), groundwater travel time uncertainty analysis (LaVenue et al, 1989), automated calibration of transmissivity fields (LaVenue et al, 1995;RamaRao et al, 1995), coupled nonlinear multiphase multicomponent flow (RamaRao & Mishra, 1996), modeling multidimensional groundwater flow (Clemo, 2007), adaptive multiscale parameterization of flow in unsaturated porous media (Hayek et al, 2008), transient groundwater flow in a bounded model domain (Lu & Vesselinov, 2015), fractured dual-porosity media (Delay et al, 2017;Fahs et al, 2014), and coupled surface water-groundwater modeling (RamaRao et al, 2017). However, few applications of the adjoint state method have been devoted to solute transport (e.g., Larbkich et al, 2014;Michalak & Kitanidis, 2004;Neupauer & Wilson, 1999, 2001Piasecki & Katopodes, 1997).…”