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AUTHOR:

CRUICKSHANK, L.

TITLE:

Development of novel lanthanide based particle tracers for rapid monitoring of soil erosion.

YEAR:

2016

OpenAIR citation:

CRUICKSHANK, L. 2016. Development of novel lanthanide based particle tracers for rapid monitoring of soil erosion. Robert Gordon University, PhD thesis. Held on OpenAIR [online]. Available from: https://openair.rgu.ac.uk

This work was submitted to- and approved by Robert Gordon University in partial fulfilment of the following degree: Doctor of Philosophy, Faculty of Design and Technology, School of Engineering _______________________________________________________________________________________________

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Development of novel lanthanide based particle tracers for rapid monitoring of soil erosion

Laura Cruickshank

A thesis submitted in partial fulfilment of the requirements of The Robert Gordon University, Aberdeen for the degree of Doctor of Philosophy

January 2016 This research programme was carried out in collaboration with The James Hutton Institute

ii

Dedication

For my Mum and Dad, who taught me to always aim for the stars.

And for Chloe and Euan, I hope in some small way this helps teach you the same.

iii

Declaration

I hereby declare that no portion of the work referred to in this thesis has been submitted in support for an application for another degree or qualification of this or another university or other institute of learning. This is an original piece of work undertaken by myself. All results and work other than my own are clearly cited and acknowledged.

iv

Acknowledgements

I wish to express my sincere thanks to the following: Firstly I wish to express my immense gratitude to my supervisors, Simon Officer, Marc Stutter and Pat Pollard for all the support and advice given throughout the project. A special thank you to all the staff and students in the centre for research, energy and the environment for many useful discussions and much encouragement. In particular to Morgan Adams who helped to remind me that research can be fun! Thank you to the staff of the analytical chemistry labs, and engineering workshop, who were always there to give advice whenever needed. Also, to everyone at the James Hutton Institute whose help was invaluable, particularly Samia Richards for guiding me patiently through a variety of new techniques, and Evelyne DelBois who helped obtain some of the SEM images included in this thesis. Funded by the Institute for Innovation, Design and Sustainability (IDEAS) at the Robert Gordon University. Finally I would like to thank my friends and family, particularly Neil, Chloe and Euan for providing endless encouragement, patience and support. You can finally get mummy back now!

v

Abstract Soil erosion is a global problem, affecting much of the world’s agricultural land. As the world’s population increases, the pressures placed upon the land resource to provide space for food production, leisure, housing and industrial facilities also increases. Thus it is vital that the land resource is as productive as possible. As soil erosion is the major cause of soil degradation globally, it is vital that methods for accurately monitoring the degree of erosion from a site, and the effectiveness of any remediation attempts are available. Reported here is the development of a novel soil erosion particle tracer, based upon a lanthanide chelate complex doped silica particle. The luminescent lanthanide chelate complexes were comprised of 2-thenoyltrifluoroacetone (TTA) and 2-pyridinol-1-oxide (2PO) coordinated with either trivalent europium or terbium ions. These complexes were then doped into silica sol-gel particles using a core shell technique. This method resulted in the synthesis of two luminescent soil tracers, targeted to two of the key eroded soil fractions; fine silt (63-250 μm) and clay (< 1.2 μm). The behaviour of the tracers was analysed within three different soils obtained from the Glensaugh research station. They retained their luminescence when mixed with soil, and could be detected at concentrations of 10 mg tracer / kg soil using a standard benchtop fluorescence spectrometer (Perkin Elmer LS55B). Scanning electron micrographs indicated that the tracer particles interacted with the soil particles, whilst soil sedimentation experiments demonstrated that the tracer particles had a similar sedimentation pattern to natural soil particles. Soil microbial respiration studies were performed for the tracers and showed that the tracers did not significantly impact the soil microbial population. Studies of the luminescence stability of the tracer in soil over time showed that the tracer could be detected in the soil for one season (approximately 3 months). A prototype rainfall simulator, designed to simulate the kinetic energy of vi

raindrops on the surface of the soil, was developed, and used during a series of rainfall simulation experiments. These simulations were performed at two different rainfall intensities (30 and 90 mm.h-1) and both of these conditions resulted in movement of the tracer particles within the plot. This movement was both horizontal, in overland flow over the plot surface, and vertical, through the plot. The pattern of tracer movement reflected that of the soil mass moved, and as such indicated that the tracers exhibited similar transport behaviour during the erosion simulations performed. These initial simulations demonstrated that the tracers can be detected at low concentrations within the soil using standard laboratory equipment, and that they move with the eroded soil particles during simulated soil erosion experiments. As such, these tracers are excellent candidates for further study in larger scale erosion events.

vii

Abbreviations AGA –

amino G acid monopotassium dye

ANOVA –

analysis of variance

ATR -

attenuated total reflection

BLD -

below limit of detection

DMSO –

dimethyl sulfoxide

D2 O –

deuterium

DOE -

design of experiments

DSC –

differential scanning colorimetry

EDXA –

energy dispersive x-ray analysis

FTIR –

Fourier Transform Infrared

HMP –

sodium hexametaphosphate solution

HOPO –

hydroxy-pyridinones

HP-Ge –

high purity – germanium

HTTA -

free 2-thenoyltrifluoroacteone

ICP-OES –

inductively coupled plasma – optical emission spectroscopy

ICP-MS –

inductively coupled plasma – mass spectrometry

IR -

Infra-red

LC-MS –

liquid chromatography- mass spectrometry

Ln3+ -

trivalent ion of the lanthanide series

viii

LOD –

limit of detection

MRI –

magnetic resonance imaging

NMR –

nuclear magnetic resonance

PMT –

photomultiplier tube

REE

-

rare earth element

REETM -

rare earth element tracer method

SAXS -

small angle x-ray scattering

SEM

scanning electron microscope

-

SEPA –

Scottish Environmental Protection Agency

TEOS –

tetraethylorthosilicate

TGA –

thermogravimetric analysis

TMOS –

tetramethoxysilane

TTA –

coordinated 2-thenoyltrifluoroacetone

2PO –

2-pyridinol-1-oxide

ix

Table of contents DEDICATION

III

DECLARATION

IV

ACKNOWLEDGEMENTS ABSTRACT

V VI

ABBREVIATIONS

VIII

LIST OF FIGURES

XIV

LIST OF TABLES

XXII

PUBLICATIONS

XXIV

CHAPTER 1 - GENERAL INTRODUCTION AND LITERATURE REVIEW 1.1 SOILS AND SOIL STRUCTURE 1.2 SOIL EROSION

1 2

3

1.2.1 Water erosion

11

1.2.2 Wind erosion

13

1.2.3 Tillage erosion

14

1.3 SUSPENDED PARTICULATE MATTER

15

1.4 METHODS OF MONITORING SOIL EROSION 1.4.1 Sediment fingerprinting

16

1.4.2 Radioisotopes as erosion tracers

17

1.4.3 Rare earth elements

19

1.4.4 Applied ions

20

1.4.5 Dyes

21

1.4.6 Physical tracers

22

1.4.7 Applied particle tracers

22

16

1.5 LANTHANIDES AND LANTHANIDE CHELATE COMPLEXES

24

1.6 SILICA SOL-GEL PARTICLES

31

1.7 RESEARCH AIMS AND THESIS OVERVIEW

36

1.5.1 Lanthanide photochemistry

1.5.2 Luminescent lanthanide complexes 1.6.1 Lanthanide complex doped sol-gels

CHAPTER 2 – SYNTHESIS AND CHARACTERISATION OF LANTHANIDE CHELATE COMPLEXES.

25 28 35

39

x

2.1 INTRODUCTION

2.1.1 The hydroxy-pyridinones 2.1.2 Quantum yield

40

40 41

2.1.3 Fluorescence lifetimes

42

2.1.4 Aim and objectives

43

2.2 MATERIALS AND METHODS

45

2.2.1 Chemicals and reagents 2.2.2 Synthesis of lanthanide chelate complexes

45

45

2.2.3 Determination of lowest triplet state

46

2.2.3 Infra-red analysis of chelate complexes

46

2.2.4 Nuclear magnetic resonance spectroscopy and Flow injection analysis.

48

2.2.5 Thermogravimetric analysis and Karl Fisher titrations

48

2.2.6 Fluorescence emission and excitation

49

2.2.7 Quantum yield and fluorescence lifetime measurement

49

2.3 RESULTS AND DISCUSSION

2.3.1 Triplet state determination 2.3.2 Infra-red analysis

50

50 52

2.3.3 Nuclear magnetic resonance

58

2.3.4 Flow injection analysis – mass spectrometry

61

2.3.5 Determination of coordinated water

63

2.3.6 Fluorescence spectroscopy

65

2.3.7 Lifetime determination

67

2.3.8 Quantum yield

69

2.4 CONCLUSIONS

73

3.1 INTRODUCTION

74

CHAPTER 3 – SYNTHESIS AND CHARACTERIZATION OF SILICA SOL-GEL PARTICLES 3.1.1 Sol-gel synthesis 3.1.2 Lanthanides doped sol-gels 3.1.3 Aim and objectives 3.2 SOL-GEL SYNTHESIS

3.2.1 Chemicals and reagents 3.2.2 Methods for particle synthesis 3.2.3 Methods for analysis of synthesised particles

3.3 RESULTS AND DISCUSSION

70 74

74 75

76

76 76 78

81

xi

3.3.1 Synthesis of silica sol-gel particles in the colloidal clay size range (