Abstract

Sedimentation is considered the most widespread contemporary, human-induced perturbation on reefs, and yet if the problems associated with its estimation using sediment traps are recognized, there have been few reliable measurements made over time frames relevant to the local organisms. This study describes the design, calibration and testing of an in situ optical backscatter sediment deposition sensor capable of measuring sedimentation over intervals of a few hours. The instrument has been reconfigured from an earlier version to include 15 measurement points instead of one, and to have a more rugose measuring surface with a microtopography similar to a coral. Laboratory tests of the instrument with different sediment types, colours, particle sizes and under different flow regimes gave similar accumulation estimates to SedPods, but lower estimates than sediment traps. At higher flow rates (9–17 cm s−1), the deposition sensor and SedPods gave estimates >10× lower than trap accumulation rates. The instrument was deployed for 39 d in a highly turbid inshore area in the Great Barrier Reef. Sediment deposition varied by several orders of magnitude, occurring in either a relatively uniform (constant) pattern or a pulsed pattern characterized by short-term (4–6 h) periods of ‘enhanced’ deposition, occurring daily or twice daily and modulated by the tidal phase. For the whole deployment, which included several very high wind events and suspended sediment concentrations (SSCs) >100 mg L−1, deposition rates averaged 19 ± 16 mg cm−2 d−1. For the first half of the deployment, where SSCs varied from <1 to 28 mg L−1 which is more typical for the study area, the deposition rate averaged only 8 ± 5 mg cm−2 d−1. The capacity to measure sedimentation rates over a few hours is discussed in terms of examining the risk from sediment deposition associated with catchment run-off, natural wind/wave events and dredging activities.

Highlights

  • All laboratory testing was conducted at the Australian Institute of Marine Science (AIMS) Sea Simulator (SeaSim) at Cape Cleveland and field work was conducted at Middle Reef in Cleveland Bay, in the turbid inner shelf reef zone of the central Great Barrier Reef (GBR) (Fig. 1)

  • The raw readings from the deposition sensor are proportional to how much light is reflected back by sediment that has fallen through the apertures and deposited on the surface of the fibre optic bundles

  • Sediment depositing on the surface of the fibre optics of each of the three sensors is converted to mass per unit area using the sediment-specific calibrations and the settled amount increases with each 10 min reading until the wiper clears the sediment

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Summary

Materials and methods

All laboratory testing was conducted at the Australian Institute of Marine Science (AIMS) Sea Simulator (SeaSim) at Cape Cleveland and field work was conducted at Middle Reef in Cleveland Bay, in the turbid inner shelf reef zone of the central GBR (Fig. 1)

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Results
Discussion

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