Use this URL to cite or link to this record in EThOS: https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.798121
Title: Reinterpreting turbidity : new methodologies for suspended-sediment research
Author: Kitchener, Ben G. B.
ISNI:       0000 0004 8506 5128
Awarding Body: University of Sheffield
Current Institution: University of Sheffield
Date of Award: 2019
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Abstract:
Existing instruments for turbidity measurement vary considerably in terms of the principles of operation, the physical design, and the cost to the researcher. The operational methodologies of late twentieth century turbidity instruments have led to the development of new turbidity measurement standards, and the invention of new turbidity measurement units. These measurement units are invalid and do not have a sound footing with regard to the underlying physics of the scattering and absorption of light by suspended particles. A review of the turbidity literature has shown that the proliferation of these incommensurate units of measurement throughout the physical sciences has caused extensive misinterpretation of turbidity data, particularly concerning its use as a surrogate for suspended sediment concentration (SSC). Turbidity is a complex phenomenon, and its measurement reported in terms of a single numeric quantity in some physically indeterminate units of measurement. It is not necessarily useful to reduce complex data to a single value, since this approach does not permit the researcher any a posteriori opportunity to reinterpret existing data in light of innovations in analysis methodology. This thesis proposes a new way to present turbidity data that will facilitate the cross-comparison of turbidity measurements made by different instruments on any type of suspended sediment. The creation of a new turbidity research instrument that illustrates the application of the new method for reporting turbidity data as a ratio of light attenuation values in decibels, promotes a positive change in direction away from the traditional measurement units. The design process focusses on the instrument calibration procedure. With a simple reinterpretation of the phase-function description of light scattering from suspended particles, measurements of light attenuation made at multiple angles with respect to the axis of the incident light beam, compare easily with the same measurements made using different wavelengths of incident light. This work goes on to introduce new nomenclature that requires the citing of measurement angle and wavelength of light to be an integral part of any recorded turbidity measurement. A modelling approach is used in the evaluation of the new turbidity instrument. This modelling is important for three reasons. First, it identifies which instrument parameters affect the result of a turbidity measurement - the key parameter being the mathematical function that describes the spatial divergence of the incident light beam, which is important to measurement systems that employ incoherent light sources such as LEDs, rather than to laser-based systems. Secondly, the modelling reveals two fundamental theories of light scattering due to suspended particles, both of which are required to describe adequately the turbidity of sediment-laden water. These two theories are Mie scattering and geometric optics. Mie scattering is well accounted for by the developed model - geometric optics, less so. The extent to which the model predictions diverge from the empirical data is characterised by a metric related to the backscatter fraction, and the consistency and linearity of the model is established. Ideas for the improvement of the geometric optics feature of the model are discussed, as is the third reason for the importance of numerical modelling. This third reason relates to the use of multi-parameter turbidity measurements as a means to characterise the properties of a suspended sediment. By simulating precisely the measurement response of the turbidity instrument, then it is notionally possible to infer the properties of an unknown sediment by tuning the model parameters to match the empirical response of the unknown sediment. This tuning process could reveal information pertaining to particle size and shape. Finally, potential applications for the new research instrument focus on improvements to the instrument itself and the methodology, and the further development of the turbidity data reporting nomenclature. Prototype methodologies that relate turbidity to suspended sediment concentration are suggested, which also consider ways in which the optical measurements can potentially classify the physical properties of a sediment.
Supervisor: Bateman, Mark D. ; Parsons, Anthony J. ; Wainrwight, John Sponsor: Not available
Qualification Name: Thesis (Ph.D.) Qualification Level: Doctoral
EThOS ID: uk.bl.ethos.798121  DOI: Not available
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