4.7 Article

Representative measurement of two-dimensional reactive phosphate distributions and co-distributed iron(II) and sulfide in seagrass sediment porewaters

Journal

CHEMOSPHERE
Volume 85, Issue 8, Pages 1256-1261

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.chemosphere.2011.07.020

Keywords

Diffusive equilibration in a thin film (DET); Diffusive gradients in a thin film (DGT); Computer imaging densitometry; High resolution; Sediment heterogeneity; In situ measurement

Funding

  1. Australian Research Council [DP0559935]
  2. Griffith Centre for Coastal Management
  3. Australian Research Council [DP0559935] Funding Source: Australian Research Council

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The high degree of heterogeneity within sediments can make interpreting one-dimensional measurements difficult. The recent development and use of in situ techniques that measure two-dimensional distributions of porewater solutes have facilitated investigation of the role of spatial heterogeneity in sediment biogeochemistry. A colourimetric diffusive equilibration in thin films method has been developed that allows two-dimensional, high-resolution measurement of reactive phosphate in sediment porewaters. A method detection limit of 0.22 mu M, an effective upper limit of similar to 1000 mu M and relative standard deviations typically below 5% were achieved. This method was evaluated by deployment in seagrass (Zostera capricorni) colonised sediments, as part of combined probes with similar colourimetric methods for sulphide and iron(II). The two-dimensional, high resolution distributions obtained provide a highly representative measurement of the co-distributions of porewater solutes, allowing heterogeneous features and biogeochemical processes to be observed and interpreted. Microniches of high phosphate concentration > 100 mu M were observed throughout the distributions and were interpreted to be due to localised zones of rapid organic matter mineralisation, possibly using electron acceptors other than iron(III) oxyhydroxides (e.g. aerobic respiration) as often they did not correspond with microniches of higher Fe(II) concentration. (C) 2011 Elsevier Ltd. All rights reserved.

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