Abstract

Suspended cohesive sediments form aggregates or ‘flocs’ and are often closely associated with carbon, nutrients, pathogens and pollutants, which makes understanding their composition, transport and fate highly desirable. Accurate prediction of floc behaviour requires the quantification of 3-dimensional (3D) properties (size, shape and internal structure) that span several scales (i.e. nanometre [nm] to millimetre [mm]-scale). Traditional techniques (optical cameras and electron microscopy [EM]), however, can only provide 2-dimensional (2D) simplifications of 3D floc geometries. Additionally, the existence of a resolution gap between conventional optical microscopy (COM) and transmission EM (TEM) prevents an understanding of how floc nm-scale constituents and internal structure influence mm-scale floc properties. Here, we develop a novel correlative imaging workflow combining 3D X-ray micro-computed tomography (μCT), 3D focused ion beam nanotomography (FIB-nt) and 2D scanning EM (SEM) and TEM (STEM) which allows us to stabilise, visualise and quantify the composition and multi-scale structure of sediment flocs for the first time. This new technique allowed the quantification of 3D floc geometries, the identification of individual floc components (e.g., clays, non-clay minerals and bacteria), and characterisation of particle-particle and structural associations across scales. This novel dataset demonstrates the truly complex structure of natural flocs at multiple scales. The integration of multi scale, state-of-the-art instrumentation/techniques offers the potential to generate fundamental new understanding of floc composition, structure and behaviour.

Highlights

  • Cohesive fine-grained sediments and mixed sediments in suspension influence a wide array of environmental processes and material transfers, including the transport, fate and effect of carbon, nutrients, microbiota and pollutants within lakes, rivers, estuaries and the marine environment (Azam & Long 2001; Rusconi et al 2014; Rummel et al 2017)

  • The aim of this study is to develop a correlative workflow that enables observation, characterisation and quantification of natural suspended sediment floc structure and composition from the mm to nm-scale for the first time

  • Reconstruction greyscale contrast (16-bit pixel depth, e.g., 65,536 greyscales) between the flocs, surrounding resin and aluminium fiducial markers was sufficient to allow segmentation based on simple thresholding

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Summary

Introduction

Cohesive fine-grained sediments and mixed sediments in suspension influence a wide array of environmental processes and material transfers, including the transport, fate and effect of carbon, nutrients, microbiota (including pathogens) and pollutants within lakes, rivers, estuaries and the marine environment (Azam & Long 2001; Rusconi et al 2014; Rummel et al 2017). Understanding the composition and behaviour of cohesive and mixed sediments is a major issue for the management of aquatic environments In suspension this biotic and abiotic particulate matter forms loosely bound, complex and fragile aggregates, or ‘flocs’. An understanding of floc composition and particle associations provides a mechanistic understanding of e.g., pathogen and pollutant transport and elucidates microbial dynamics (Liss 2002). Obtaining such empirical data is challenging since flocs are inherently fragile and their properties often span several spatial scales, i.e. nm to mm-scale. A major challenge is the development of methods that enable empirical observation and 77 accurate quantification of floc characteristics, correlated across multiple length scales

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