Aquatic vegetation is a crucial part of wetland and floodplain ecosystems. It stabilizes river banks (Hackney et al., 2020), protects coasts from waves and storm surges (Barbier et al., 2011), and provides habitat for fisheries (Costanza et al., 1997). Wetlands sustain themselves partially through their ability to retain and accrete sediment. However, the influence of vegetation on water motion and sediment transport is complex. On the one hand, vegetation provides additional drag, which reduces current (Kouwen & Unny, 1973), facilitating sediment deposition (Abt et al., 1994) and increasing bed elevation. On the other hand, vegetation generates turbulence (Tanino & Nepf, 2008;Xu & Nepf, 2020), which can enhance erosion (Niño & Garcia, 1996), alter the vertical distribution of suspended sediment (Tseng & Tinoco, 2021), and decrease bed elevation in the vicinity of vegetation (Norris et al., 2021;Yagci et al., 2016). Recent studies have proposed ways to incorporate the impacts of vegetation on bedload transport by considering the related process of scour hole formation (Wu et al., 2021), or by modifying the parameters of the Einstein (1950) probabilistic model (Armanini & Cavedon, 2019). A deeper understanding of sediment transport within aquatic ecosystems is still critical (Fagherazzi et al., 2017) to facilitate wetland protection and restoration projects (Paola et al., 2011).