I18-Microfocus Spectroscopy
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Feb 2012
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I18-Microfocus Spectroscopy
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Feb 2012
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I18-Microfocus Spectroscopy
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Abstract: Recently glasses based on gallate and aluminate networks have aroused interest in laser technology, for example, for the use as the host for .Iaser active ions. As these glasses are not good glass-formers other ingredients such as silica are normally added to improve their glass abilities. In this work I have succeeded in producing these glasses without the need for these additions. The structures of these pure rare-earth gallate and aluminate glasses made by aerodynamic levita- tion and laser heating techniques have been studied including neutron and X-ray diffraction and spectroscopy. The following results have been obtained. The structures of rare-earth gallate glasses, R2Ga6012 and R3Ga5012 where R = Pr and Nd, were studied using neutron diffrac- tion with the isomorphic substitution technique. A good agreement between the structural models from MD simulation and MD-RMC for the difference functions and the full experimental data sets was achieved. The mean Ga-O coordination number was found to be 4.1(1). The results also show a mixture of 6, 7 and 8-fold coordinated sites for the rare-earth ions with an average coordination number of 7.7(1). A more detailed study using a combination of neutron diffraction, Extended X-ray Absorption Fine Structure (EXAFS), MD simulation and MD-RMC refinement was applied to obtain the detail of the local structure of Pr3Ga5012 glasses at Pr and Ga K-edges. The nucleation and phase separation in the (Y203)x(Al203)1-x glassy systems produced by an aerodynamic levitation and laser heating was studied using micro-focus EXAFS. Turbidity was found to occur in the x < 0.25 and x > 0.35 glasses. At x < 0.25, even though no large inclusions (> 1?m) were seen in the turbid glasses, a phase separation into a polycrystalline sample of YAP (x = 0.50) and pure alumina was found. It is concluded that the turbidity in glassy samples at x ? 0.25 is due to the formation of nano meter size crystallites. For x = 0.36 and 0.375 (known as YAG), a nucleation of YAG crystals as spherical inclusions was found in a glass matrix giving rise to the turbidity in these glasses. Finally, a study of the structures of BaTiAl206 glasses was made in order to understand the processes giving rise to their unusual properties. Black and opaque, and clear and transparent BaTiAb06 glasses produced by aerodynamic levitation and laser heating by fast and slow quench rates were studied. Neutron and X-ray diffraction, MD simulation, MD-RMC refinement and X-ray absorption spectroscopy have been used and combined to determine the structure of the glass especially with regard to the coordination structure around the Ti ions. Evidence is found to show that the Ti ions occur in four fold and higher fold oxygen coordinated sites while the Al ions remain to- tally four fold coordinated. Very small differences in the structure of the two glasses are observed confirming that the opacity arises largely due to a small number of optical defects in present in the same overall glass structure.
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Feb 2012
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I18-Microfocus Spectroscopy
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Diamond Proposal Number(s):
[7058]
Abstract: Results are presented from X-ray absorption spectroscopy based analysis of As, Cr, and V speciation within samples of bauxite ore processing residue (red mud) collected from the spill site at Ajka, Western Hungary.
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Mar 2012
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I18-Microfocus Spectroscopy
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Mar 2012
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I18-Microfocus Spectroscopy
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Diamond Proposal Number(s):
[6174]
Abstract: Since deposited dredged sediments are rich in metallic contaminants, they present a risk for environment. This work aims to study dredged sediments chemical composition, identify metal-carrier minerals and understand their mobility. Combining chemical and spectroscopic techniques at multi-scale for an integrative approach of trace elements (zinc, lead, iron) behaviour is therefore necessary. The global mineralogy and the chemistry of the sediment were determined by X-ray diffraction and fluorescence (XRF), respectively. Zn and Pb enriched fractions were separated using a sequential chemical extraction procedure and measured by inductively coupled plasma atomic emission and mass spectroscopy. Microanalyses using scanning electron microscopy (SEM), electron microprobe microanalysis (EPMA), combined with synchrotron radiation X-ray fluorescence (?-XRF) were carried out to characterize mineralogical phases and identify Zn and Pb carrier minerals. Iron oxyhydroxides and iron sulphides were consistently identify as Zn and Pb carriers. The assumption that carbonate fraction was the major Zn carried phase, as demonstrated by chemical extraction results, was not verified by EPMA or ?-XRF.
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Mar 2012
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I18-Microfocus Spectroscopy
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Diamond Proposal Number(s):
[876]
Open Access
Abstract: In this thesis two analyses are performed to understand the intrinsic ability of
bulk
metallic glasses (
BMGs
)
to deform plastically, based on their elastic properties. In the first of
these, a Blackman diagram is utilised, which plots the ratios of second order elastic constants
C
12
/
C
11
and
C
44
/
C
11
. Two physically meaningful conditions are
represented
on such a p
lot
:
1)
proximity to the Born mechanical instability criterion
,
and
2)
deviation from the zero Cauchy
relationship (
C
12
=
C
44
), which indicates whether central or non
-
central forces govern material
behaviour.
Those alloys with greatest tendency for plastic s
train are found closest to the Born
condition, which is also found to correspond to BMGs with a large kinetic glass fragility
index,
m
. Additionally, that plastic alloys exhibit the largest positive deviation from the
Cauchy condition suggests that non
-
dir
ectional bonding is a feature of deformable BMGs.
In the second anaylsis, three isomechanical groups are found to exist when a
representative group of 33 BMGs was studied, by plotting the Young’s (
E
) and shear (
G
)
moduli
versus
k
b
T
g
/
Ω
(Botlzmann constant,
glass transition temperature and atomic volume
respectively). An analysis of covariance reveals that the
variation
in
the
gradient between
each group on such plot
s
are statistically meaningful, indicating
fundamental
differences in
both
bonding
and
structure
.
These are rationalis
ed as resulting from the extent of non
-
directional bonding and the ability for enhanced structure diversity in the potential energy
landscapes (PELs) of fragile glass formers, in com
parison to strong glass formers.
This
abili
ty for structure variation in the liquid state
can be translated to the solid state via the non
-
ergodicity parameter,
α
.
This ability for an enhancement in the variety of local minima in the PEL of fragile
glass formers is further studied by comparing the
ability of high, low and intermediate
m
BMGs to retain a low modulus and low surface
hardness
during suction casting in copper
dies, observed
by performing
nanoindentation traverses a
cross
the cross
-
section of
as
-
cast
rods. The
most
fragile
alloy (
Pd
77.5
S
i
16.5
Cu
6
)
is found to show the greatest propensity
to
retain
a soft surface, while the effec
t is most limited in the
strong composition (
Ce
70
Al
10
Cu
10
Ni
10
)
.
Finally,
the
extended x
-
ray absorption fine structure (EXAFS)
method
is used to understand
the sourc
e of the mech
a
nical homogeneity
observed
across the as
-
cast rods, which is
found
to
potentially
not
be controlled by
nearest neighbour
s. Instead, cluster rotation may control the
variable mechanical properties (including plastic yield), and so length scale
s beyond the first
atomic shell appear to be critical.
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Mar 2012
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I18-Microfocus Spectroscopy
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Diamond Proposal Number(s):
[4842]
Abstract: Timescales of magma chamber assembly and recharge are investigated here by applying 1D and 2D diffusion modeling techniques to high-resolution maps of titanium in quartz from a large-volume ignimbrite eruption in the Taupo Volcanic Zone, New Zealand. We compare quartz zonation patterns and associated diffusion timescales from the ?340?ka Whakamaru super-eruption (magma volume ?1000?km3) with the Younger Toba Tuff super-eruption, 74?ka (2000?km3), Sumatra, and the smaller volume ?50?ka Earthquake Flat eruption (10?km3), Okataina Caldera Complex, New Zealand. Two principal timescales are presented: that of chamber recharge and eruption triggering events, and that of magma generation (involving long-term assembly, stirring and reactivation). Synchrotron micro-X-ray fluorescence maps of core–rim quartz transects provide a high-resolution record of magma chamber conditions throughout quartz crystallization. Quartz crystals from the Whakamaru magma display complex zonation patterns indicating fluctuating pressure–temperature conditions throughout the crystallization history. Toba and Earthquake Flat, in contrast, display simple quartz-zoning patterns and record slightly longer periods of crystal residence in the chamber that fed the eruption. We apply Lattice Boltzmann 2D diffusion modeling to reconstruct the timescales of quartz crystal zonation, accounting for crystal boundary complexities. Quartz crystal orientation is also accounted for by using geometry constraints from the synchrotron data. Our calculations suggest that crystal-mush reactivation for the main Whakamaru magma reservoir occured over a period of the order of 103–104 years. Both the Earthquake Flat and Toba eruptions experienced a significant recharge event (causing a temperature and pressure change), which occurred within ?100 years of eruption. In comparison, the complex Whakamaru quartz zoning patterns suggest that the magma body experienced numerous thermal and compositional fluctuations in the lead-up to eruption. The final magma recharge event, which most probably triggered the eruption, occurred within ?10–60 years of the eruption. Even though the volume of these systems spans two orders of magnitude, there does not appear to be a relationship between magma volume and diffusion timescale, suggesting similar histories before eruption.
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Apr 2012
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I18-Microfocus Spectroscopy
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Abstract: X-ray Absorption Fine Structure techniques have been used on Comet Wild2/81P tracks from the Stardust mission. Fe-XANES and EXAFS have been performed on aerogel sections from Tracks 41 and 162 as well as the mid and terminal positions of Track 134. This is the first use of EXAFS in the study of early Solar System materials. With EXAFS, we have measured FeO and FeS bond lengths and thus, together with complementary XANES measurements, identified Fe-rich phases. In particular, we show that ferric-rich phases in 2 Tracks (41, 162) have FeO bond 1st shell bond lengths of 1.992.01 Å and Fe K absorption edge and pre edge centroid positions consistent with being hematite-dominated grains. These iron oxides can be clearly distinguished from a magnetite grain, present in Track 134. We also demonstrate the identification of the Mg-rich end member olivine using EXAFS with XANES in Track 162. The terminal grain of Track 134 is pyrrhotite, its first atomic shell has an FeS structure, with 4 nearest neighbouring S atoms at a distance of 2.29 ± 0.05 Å. Our XANES results show the presence of Fe3+-bearing grains along the Stardust tracks and suggest either flash-cooling of an FeSSiOO2 gas during capture or the presence of a FeNiSO melt along the cometary tracks during impact capture in the aerogel, rather than the capture process being solely associated with reduction of cometary phases. Accurate determination of Comet Wild2 redox conditions requires the identification of phases, in particular terminal grains, which have not experienced this melting. For instance, the larger hematite-rich grains (>10 μm) are more likely to be cometary in origin. EXAFS provides a valuable new analytical technique to study fine-grained early Solar System materials.
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Apr 2012
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I18-Microfocus Spectroscopy
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Diamond Proposal Number(s):
[6303]
Abstract: Tris(8-quinolinolato)gallium(III) (1, KP46) is a very promising investigational anticancer drug. Its interaction with serum proteins, elemental distribution, and coordination in tissue were investigated with X-ray absorption (XAS) methods. Model compounds with mixed O, N, and/or S donor atoms are reported. The coordination and structure of 1 in cell culture medium (minimum essential medium, MEM) and fetal calf serum (FCS) were probed by XANES and EXAFS. The interaction of 1 with the serum proteins apotransferrin (apoTf) and human serum albumin (HSA) was addressed as well. By application of micro-XAS to tissue samples from mice treated with 1, the gallium distribution pattern was analyzed and compared to those of physiological trace elements. The complex 1 turned out to be very stable under physiological conditions, in cell culture media and in tissue samples. The coordination environment of the metal center remains intact in the presence of apoTf and HSA. The gallium distribution pattern in tumor and liver tissue revealed high similarities to the distribution patterns of Zn and Fe, minor similarities to Cu and Ni, and no similarity to Ca.
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Jun 2012
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