Pre-restoration sediment budget of a tidally restricted estuary reveals potential for landward transport

Unnatural tidal restrictions are common features in estuaries, often arising from agricultural practices, road construction, or drainage activities. Restrictions tend to attenuate tides landward of the structure but can induce more complex effects in the seaward direction, including modification of natural geomorphic processes. The Herring River Estuary is the site of the largest salt marsh restoration effort in the northeast United States. We deployed a suite of instruments over one year to identify the role of tidal and atmospheric processes on sediment dynamics. We find 6.2·10⁶ kg yr^-1 of sediment is exported from the system through its only channel; this seaward-directed flux indicates that the seaward Wellfleet Harbor is not a sediment source for the Herring River Estuary. The sediment floodebb differential is landward above the tidal restriction, producing a divergent, transgressive embayment. The mudflats are the primary source of this sediment, eroding at rates of 0.1 and 5.3 cm yr^-1 at the shallow and deep stations, respectively. Sediment is resuspended on the mudflats during wind events and exported from the system when landward-directed winds produced a seaward return flow. Ebb-dominated tides also yield net sediment export during calm periods. Once the tidal restriction is removed, the areas landward of the restriction may become a large sediment sink. It is possible that sediment from the embayment between the mouth and the restriction begins to move landward rather than seaward, but it is unlikely that Wellfleet Harbor would supply additional sediment. Therefore, as the subsided salt marshes landward of the tidal restriction begin to accrete sediment, it would most likely come at the expense of the seaward channel bottoms, mudflats, and salt marsh shorelines described in this study. In partitioning the sediment budget to geomorphic processes, this work presents a significant advance in the understanding of the linkage between a tidally restricted estuary and its seaward embayment. As tidal restriction removal becomes a more common restoration practice, the understanding of pre-removal baseline conditions becomes important for developing conceptual models of post-removal geomorphic evolution.