“…As a consequence of human activities (agriculture, urbanization, grazing and mining), soil organic carbon contents in fluvial soils would decrease, generating a reduction of soil stability and size of the aggregates, affecting fertility and biodiversity (Pulido‐Fernández, Schnabel, Lavado‐Contador, Miralles Mellado, & Ortega Pérez, 2013). In the long‐term, these soils could experience a lower water holding capacity, lower permeability and higher probability of crust formation, with the resulting dramatic decrease in infiltration rates (Fick, Belnap, & Duniway, 2020; Li, Li, Huang, Wang, & Zhang, 2019; Rosentreter & Root, 2019). Due to the absence of available water in the soil profile, vegetation will not be able to re‐establish resulting in high rates of overland flow and sediment yield (Manning, Julian, & Doyle, 2020; Wang et al, 2019).…”