Abstract

Understanding the effects of sediment disturbances on nutrient loadings is important for the management of estuarine settings. This study investigated the initial influence of sediment disturbance on water column nutrient concentrations in a shallow estuarine setting within the Gold Coast Broadwater, using a laboratory-based approach. Undisturbed sediment cores (200 mm Ø × 330 mm length, plexiglass) were incubated before and after being subjected to a disturbance event, to investigate the effect on the immediate and subsequent short-term water column nutrient concentrations. Sediment NH4+bio and PO43−bio concentrations ranged from 150 to 478 and 1.50 to 8.56 nmol g−1 dry wt, respectively. Water column NH4+ concentrations underwent the greatest increase (>1000% or approx. 14 times greater) immediately following disturbance, with mean effluxes increasing by >300%. Thereafter, water column NH4+ concentrations and efflux rates declined to near initial pre-disturbance concentrations. Water column NH4+ concentrations accounted for 0.58%–5.50% of the depth-integrated sediment NH4+bio concentration, indicating mobilization of the sediment bound exchangeable NH4+. The observed changes in PO43− concentrations and fluxes were much lower in comparison to those observed for N-species. Following disturbance, increases in the water column PO43− concentration accounted for 7.16%–8.22% depth-integrated sediment bioavailable PO43− at +1 and +2 hours, and 5.65% at +7 hours, respectively. These results provide important insight into the potential implications of disturbance events, such as vessel activities and dredging operations, within the case study region, providing information for potential management options and relevant water quality concerns.

Highlights

  • Estuarine surface sediments typically accumulate high loads of organic matter and are regions of intense microbial activity and nutrient cycling

  • The results from this study provide an approximation of resultant water column nutrient conditions within Saltwater Creek, providing insight for potential management options and relevant water quality concerns

  • The exchangeable NH4+ measured for a particular volume of sediment can be used as a theoretical maximum for NH4+ that could potentially be released during sediment disturbance and resuspension events

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Summary

Introduction

Estuarine surface sediments typically accumulate high loads of organic matter and are regions of intense microbial activity and nutrient cycling They are often characterised by high concentrations of soluble nitrogen and phosphorus from the remineralisation of deposited organic matter and anthropogenic sources [1,2], becoming additional nutrient sources to overlying waters [3]. This exchange of nutrients across the sediment water interface (SWI) modifies both sediment nutrient pools (pore water, exchangeable/adsorbed, and strongly bound) and water column conditions [4,5]. These anthropogenic activities can induce negative impacts on the water quality, altering suspended sediment and nutrient loadings [10,12,13,14], in addition to modifying the biology of fauna present in bottom sediments [15], as well as water column communities [11,16]

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