“…Such a model has been employed in several different situations, such as flows in fluid-porous media systems (Breugem, Boersma & Uittenbogaard 2006; Jin & Kuznetsov 2017) and their stability analysis (Hill & Straughan 2008; Samanta 2020), fluid motion in a porous medium with slip at the macroscopic boundaries of the domain (Haddad, Al-Nimr & Sari 2007; Qayyum et al. 2015), and magnetohydrodynamic (MHD) flows (Ullah, Khan & Shafie 2017; Nandal, Kumari & Rathee 2019), among others. However, as suggested by Auriault (1980) and Allaire (1992), and further elaborated by Lasseux, Valdés-Parada & Bellet (2019) and Bottaro (2019) in a more general framework including inertial effects, the macroscopic model obtained by formal upscaling of the pore-scale equations, and validated by several numerical examples, does not correspond, in general, to the heuristic form, which relies on a separation of time scales between the pore-scale and the macroscale.…”