ADVANCING METHODS FOR APPORTIONING THE SOURCES OF SEDIMENT IN RIVERS: COMBINING SPECTROSCOPY AND STABLE ISOTOPES WITH BAYESIAN MIXING MODELS

Cooper, Richard (2015) ADVANCING METHODS FOR APPORTIONING THE SOURCES OF SEDIMENT IN RIVERS: COMBINING SPECTROSCOPY AND STABLE ISOTOPES WITH BAYESIAN MIXING MODELS. Doctoral thesis, University of East Anglia.

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Abstract

Sediment fingerprinting is a commonly employed technique for estimating sediment contributions from various eroding terrestrial sources to fluvial sediment load via a mixing model approach. However, there remain significant shortcomings in sediment fingerprinting practice, specifically relating to difficulties in producing high-temporal resolution apportionment estimates, inconsistencies in mixing model uncertainty representation, and a lack of attention given to organic matter provenance. Addressing these deficiencies, a combined X-ray fluorescence spectroscopy (XRFS) and diffuse reflectance infra-red Fourier transform spectroscopy (DRIFTS) approach is developed to rapidly, accurately and non-destructively analyse suspended particulate matter (SPM) geochemistry directly from sediment covered quartz fibre filter (QFF) papers at masses as low as 3 mg. An improved Bayesian source apportionment mixing model is then developed which allows for full characterisation of spatial geochemical variability, instrument precision and residual error, to yield a realistic and coherent assessment of the uncertainties associated with sediment fingerprinting estimates. Lastly, a novel application of a coupled molecular and δ2H and δ13C compound-specific isotope analysis (CSIA) of leaf wax n-alkane biomarkers is conducted to demonstrate the apportionment of plant-specific organic matter contributions to streambed sediments. Employing these developments in conjunction with automatic water samplers, high-temporal resolution SPM source apportionment estimates are derived throughout the progression of numerous storm events in a lowland agricultural catchment, revealing significant temporal variability in SPM provenance at 60- and 120-min resolution. Lower resolution, weekly, baseflow sampling is also performed, revealing distinct seasonal cycles in SPM geochemistry and sediment source apportionment over a 23-month period. Collectively, the developments presented in this thesis significantly advance sediment fingerprinting research by enabling organic and inorganic fluvial sediment fractions to be quantitatively apportioned at both low- and high-temporal resolution within realistic levels of uncertainty, thereby enhancing our understanding of sediment dynamics under a range of instream hydrological conditions.

Item Type: Thesis (Doctoral)
Faculty \ School: Faculty of Science > School of Environmental Sciences
Depositing User: Mia Reeves
Date Deposited: 19 Jun 2015 11:08
Last Modified: 19 Jun 2015 11:08
URI: https://ueaeprints.uea.ac.uk/id/eprint/53376
DOI:

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