B18-Core EXAFS
I18-Microfocus Spectroscopy
I20-Scanning-X-ray spectroscopy (XAS/XES)
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Abstract: A legacy of radioactive waste has accumulated since the late 1940s and safe containment of long lived, highly radioactive waste is crucial for the future of nuclear power. A geological disposal facility (GDF) is the preferred method for the safe disposal of radioactive wastes; a multifaceted approach, using both engineered and natural barriers, to maximise the time between the breakdown of barriers and the final interaction with the environment and subsequently people. Clay is likely form an integral part of the engineered barrier system (EBS) surrounding the waste canisters in many proposed GDFs for heat generating radioactive wastes. The clay selected for this purpose would need to have the necessary physical and chemical properties to protect the waste container against corrosion and also to limit the release of radionuclides from the waste after container failure. Clays have a number of advantageous properties, such as high sorption capacity for radionuclides, small pore structure restricting microbial activity, and stability over geological time scales. Substitution of cations (Fe2+/3+, Mg2+, Al3+) into octahedral and tetrahedral (Al3+ and Si4+) sheets give a net negative charge on the clay layers giving interlayer spaces in-between; hydrated cations balance the negative charge within the interlayer space and cause the clay to swell filling surrounding gaps/cracks, avoiding advective flow, stabilizing the canister, and making diffusion the predominant transport mechanism within the barrier. A number of challenges such as heat (from the high level wastes 160 °C), with small changes being resisted further by divalent interlayer cations. gamma irradiation was shown to generate charge defects within the clay, increasing surface potential and activating redox properties (Fe); alpha irradiation showed localised amorphisation of the clay structure with long range order maintained. Maximising the ability of the clay barrier to withstand the challenges expected in the GDF environment would allow for the strengthening of public opinion and a faster, smaller (footprint), cheaper and safer GDF for high level, heat generating, radioactive wastes to be produced.
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May 2019
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I18-Microfocus Spectroscopy
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Open Access
Abstract: Synchrotron nanoprobe X-ray absorption (XAS) studies of a potent organo-osmium arene anticancer complex in ovarian cancer cells at subcellular resolution allow detection and quantification of both OsII and OsIII species, which are distributed heterogeneously in different areas of the cells.
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May 2019
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I18-Microfocus Spectroscopy
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Diamond Proposal Number(s):
[17304]
Open Access
Abstract: We present a method for the production of polycrystalline Si (poly-Si) photonic micro-structures based on laser writing. The method consists of local laser-induced crystallization of amorphous silicon (a-Si) followed by selective etching in chemical agents that act preferentially on the a-Si material, consequently revealing the poly-Si content of the film. We have studied the characteristics of these structures as a function of the laser processing parameters and we demonstrate their potential photonic functionality by fabricating polycrystalline silicon ridge optical waveguides. Preliminary waveguide transmission performance results indicated an optical transmission loss of 9 dB/cm in these unrefined devices.
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May 2019
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I18-Microfocus Spectroscopy
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Phillip L.
Manning
,
Nicholas P.
Edwards
,
Uwe
Bergmann
,
Jennifer
Anne
,
William
Sellers
,
Arjen
Van Veelen
,
Dimosthenis
Sokaras
,
Victoria M.
Egerton
,
Roberto
Alonso-mori
,
Konstantin
Ignatyev
,
Bart E.
Van Dongen
,
Kazumasa
Wakamatsu
,
Shosuke
Ito
,
Fabien
Knoll
,
Roy A.
Wogelius
Diamond Proposal Number(s):
[12948, 11865, 9488, 8597, 7749]
Open Access
Abstract: Recent progress has been made in paleontology with respect to resolving pigmentation in fossil material. Morphological identification of fossilized melanosomes has been one approach, while a second methodology using chemical imaging and spectroscopy has also provided critical information particularly concerning eumelanin (black pigment) residue. In this work we develop the chemical imaging methodology to show that organosulfur-Zn complexes are indicators of pheomelanin (red pigment) in extant and fossil soft tissue and that the mapping of these residual biochemical compounds can be used to restore melanin pigment distribution in a 3 million year old extinct mammal species (Apodemus atavus). Synchotron Rapid Scanning X-ray Fluorescence imaging showed that the distributions of Zn and organic S are correlated within this fossil fur just as in pheomelanin-rich modern integument. Furthermore, Zn coordination chemistry within this fossil fur is closely comparable to that determined from pheomelanin-rich fur and hair standards. The non-destructive methods presented here provide a protocol for detecting residual pheomelanin in precious specimens.
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May 2019
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I18-Microfocus Spectroscopy
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Paul A.
Wallace
,
Sarah
Henton De Angelis
,
Adrian J.
Hornby
,
Jackie E.
Kendrick
,
Stephen
Clesham
,
Felix W.
Von Aulock
,
Amy
Hughes
,
James
E. P. Utley
,
Takehiro
Hirose
,
Donald B.
Dingwell
,
Yan
Lavallee
Diamond Proposal Number(s):
[9220]
Abstract: Volcanic environments often represent structurally active settings where strain localisation can promote faulting, frictional deformation, and subsequent melting along fault planes. Such frictional melting is thermodynamically a disequilibrium process initiated by selective melting of individual mineral phases and softening of volcanic glass at its glass transition as a response to rapid frictional heating. The formation of a thin melt layer on a fault plane surface can drastically accelerate or terminate slip during fault motion. A comprehensive understanding of the physical and chemical properties of the frictional melt is required for a full assessment of slip mechanism, as frictional rheology depends on the contributions from selectively melted mineral and glass phases as well as the physical effects of restite fragments suspended in the frictional melt. Here, we experimentally investigate the impact of host-rock mineralogy on the compositional and textural evolution of a frictional melt during slip. High-velocity rotary shear (HVR) experiments were performed under controlled, volcanically relevant, coseismic conditions (1 m s−1 slip rate and 1 MPa normal stress) using three intermediate dome lavas with contrasting mineral assemblages, sampled from volcanic systems where fault friction is evident: (1) an amphibole-bearing andesite (Soufrière Hills Volcano, Montserrat); (2) an amphibole-poor dacite (Santiaguito dome complex, Guatemala); and (3) an amphibole-free andesite (Volcán de Colima, Mexico). For each sample, five HVR experiments were terminated at different stages of frictional melt evolution, namely: (1) at the onset of melting and (2) formation of a steady-state melt layer; and (3) after 5 m, (4) 10 m, and (5) 15 m of slip at steady-state conditions. Progressive mixing and homogenisation of selective, single-phase melts within the frictional melt layer through double-diffusion convection demonstrates the dependence of melt composition on slip behaviour. Amphiboles melted preferentially, leading to lower shear stress (∼1 MPa) and pronounced shear weakening during the frictional melting of amphibole-bearing lavas. The results highlight the implications of mineral assemblage on volcanic conduit flow processes, which may influence the explosivity of eruptions, and run-out distances of rapid granular flows.
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Apr 2019
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I13-1-Coherence
I18-Microfocus Spectroscopy
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Abstract: In addition to the micron and sub-micron scale atmospheric particulate identified through combined electron microscopy and characteristic x-ray (EDS) analysis (as described formerly within Chap. 8), a suite of considerably larger particles were also released into the environment—the analysis of which is herein described.
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Apr 2019
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I13-1-Coherence
I18-Microfocus Spectroscopy
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Abstract: The results of Chap. 9 identified the existence of a number of micron-scale particles of considerable density contained within the CF-01 (Unit 1) ejecta particulate. In addition to these surface and sub-surface fragments, Cs (as well as other elements, including Pb, Sr and Zr) were observed to be strongly-heterogeneous—located as spatially discontinuous regions at elevated concentrations. Despite exhibiting a spatially heterogeneous occurrence of these elements (within the Si-based particle)—the location of such constituents was shown to be concentrated greatest around the exterior circumference of the sub-mm sample.
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Apr 2019
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I18-Microfocus Spectroscopy
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Abstract: As shown previously in Chap. 7, U-containing material (alongside material of a wide range of other compositions) has been observed to exist distributed across the majority of Fukushima Prefecture. This U-rich atmospheric particulate was shown to be some of the smallest to exist (with a mean diameter of 1.07 µm), while containing the fewest additional elemental constituents (i.e. predominantly composed of just U and O).
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Apr 2019
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I18-Microfocus Spectroscopy
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Diamond Proposal Number(s):
[15353]
Abstract: Both cobalt (Co) and nickel (Ni) substitute for Fe in goethite (α-FeOOH) as well as adsorb on goethite. Co and Ni-rich goethite are the dominant ore mineral in oxide-type laterite deposits. A quantitative understanding of the aqueous solubility of Ni- and Co-rich goethite would help in modelling the formation of laterites and developing methods for metal extraction. In this contribution, we determined the aqueous solubility of substituted nickel and cobalt goethite in both the binary and ternary systems as a function of pH < 1 to 5 and varying concentrations found in Ni laterites. We found the dependency of the solubility product (Ksp) of goethite to the type of incorporated ion, concentrations, and pH. The solubility of Ni substituted goethite increases with increasing pH and increasing Ni substitution. A similar trend is observed for Co, although its substitution in goethite appears to increase the stability of goethite. Ksp increases with increasing Ni and Co substitution in bi-metal (Ni and Co) goethite, and are generally low compared to those of single metal substituted goethite with the same concentration. These findings have some implication for substitution mechanism and Ni and Co extraction from laterites and soils. The Ni(OH)2-Co(OH)2-FeOOH solid solution simulation with PHREEQC is inconsistent with our experimental data and reveals “nonideality” of mixing systems with different chemical and thermodynamic properties as end members, but attained equilibrium with goethite at lower pH.
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Apr 2019
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I18-Microfocus Spectroscopy
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Diamond Proposal Number(s):
[14113, 16234]
Abstract: The local and systemic dissemination of implant-related derivatives into the body is of great
interest to human health. Biological exposures of metal micro/nano-particles, complexes and
soluble ions, generated as a consequence of in-service degradation of metallic prosthetics, can
result in severe adverse tissues reactions. However, individual reactions are highly variable and
are not easily predicted, due to in part a lack of understanding of the properties of the metalstimuli
which dictates cellular interactions and toxicity. However, interrogating ultra-dilute
metals within fragile, hydrated biological tissues without influencing the native physical and/or
chemical composition is challenging. Therefore, a drive for more advanced characterisation
techniques of the exogenous metallic particles is required. Here, synchrotron-based X-ray
fluorescence spectroscopy (XRF) and X-ray absorption near edge structure (XANES) were
deployed to investigate the quantitative spatial distribution and local chemistry of implant-related
metal particles within soft tissues. Analytical and experimental steps were outlined and improved
when using XRF for greater accuracy in quantification. This included the implications of the
matrix composition, the effects of saturation and how the instability in the flux and beam profile
affected the measurement. Two post-analytical algorithms were generated to reduce the effects of
image artefacts observed frequently in micro-focus XRF images. These methodological advances
will have significant positive impact on quantitative XRF. Specifically, the quantitative XRF
imaging displayed within this thesis, combined in a multi-institution research effort, influenced
the future use of specific metallic implants. The chemistry of exogenous implant-related particles
was also investigated, for the first time, using a XANES mapping approach. This enabled twodimensional
chemical imaging at a high spatial resolution, allowing superior chemical
discrimination of small, isolated, heterogenous features. This method highlighted the unreported
variability in metal chemistry associated with orthopaedic implants, which may alter the
perceived toxicity of implant derivatives. The results shown within this thesis outline the
advantages of using a XANES mapping approach over conventional spectroscopy methods and
should be considered when interrogating chemical species of metals in biological environments.
Finally, a novel approach to co-locative analysis between exogenous metal particles and the
underlying cellular content was developed using a lanthanide-antibody conjugate with XRF. This
allowed simultaneous imaging of the native elemental distributions and biological epitopes. The
development of this imaging modality is promising for understanding spatial relationships
between such components. Collectively, advances within these interrogation methods applied to
implant- related products will ultimately help our understanding of associated immunological
responses and will generate more appropriate biological exposure models. Additionally, the
advantages reported from the development of these techniques can be applied to an array of
samples types in many areas of science.
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Apr 2019
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