“…Classical Fickian diffusion partial differential equation (PDE) governs the scaling limit of the random walk where the underlying particle jumps have a finite variance, which leads to a normal diffusion characterized by a linear growth of the mean‐squared displacement (MSD) in time
1 . In many scenarios, for example, the transport of solutes in heterogeneous porous media, the diffusion is anomalous and is characterized by a power‐law growth of the MSD in time
for
, which corresponds to the subdiffusion processes modeled by the following time‐fractional PDE (FPDE)
1–11 . Here,
is the Caputo fractional differential operator defined by
12 …”