82 research outputs found
DIS Structure Functions in Lattice QCD
In this talk I present the complete 1-loop perturbative computation of the
renormalization constants and mixing coefficients of quark and gluon lattice
operators of rank two and three whose hadronic elements enter in the
determination of the first and second moment of Deep Inelastic Scattering
Structure Functions, making use of the nearest-neighbor improved
``clover-leaf'' lattice QCD action.
To perform the huge amount of calculations required for the evaluation of all
the relevant Feynman diagrams, extensive use of symbolic manipulation languages
like Schoonschip and Form has been made.Comment: Talk presented at LATTICE96(theoretical developments) by S. Capitani;
3 pages, LaTeX and espcrc2.sty (included
High-precision computation of two-loop Feynman diagrams with Wilson fermions
We apply the coordinate-space method by Luescher and Weisz to the computation
of two-loop diagrams in full QCD with Wilson fermions on the lattice. The
essential ingredient is the high-precision determination of mixed
fermionic-bosonic propagators.Comment: Talk presented at Lattice '97 (Theoretical Developments), Edinburgh
(UK), July 1997. LaTeX2e, 3 pages, uses espcrc2. Report DESY 97-18
Deep Inelastic Scattering in Improved Lattice QCD. II. The second moment of structure functions
In this paper we present the 1-loop perturbative computation of the
renormalization constants and mixing coefficients of the lattice quark
operators of rank three whose hadronic elements enter in the determination of
the second moment of Deep Inelastic Scattering (DIS) structure functions.
We have employed in our calculations the nearest-neighbor improved
``clover-leaf'' lattice QCD action. The interest of using this action in Monte
Carlo simulations lies in the fact that all terms which in the continuum limit
are effectively of order ( being the lattice spacing) have been
demonstrated to be absent from on-shell hadronic lattice matrix elements. We
have limited our computations to the quenched case, in which quark operators do
not mix with gluon operators.
We have studied the transformation properties under the hypercubic group of
the operators up to the rank five (which are related to moments up to the
fourth of DIS structure functions), and we discuss the choice of the operators
considered in this paper together with the feasibility of lattice computations
for operators of higher ranks.
To perform the huge amount of calculations required for the evaluation of all
the relevant Feynman diagrams, we have extensively used the symbolic
manipulation languages Schoonschip and Form.Comment: 30 pages, latex + elsart + feynman (complete postscript file
available upon request to [email protected]); submitted to
Nuclear Physics
Particulate Matter Contamination of Bee Pollen in an Industrial Area of the Po Valley (Italy)
The global demand for bee pollen as a dietary supplement for human nutrition is increasing. Pollen, which comprises proteins and lipids from bees' diets, is rich in essential amino acids, omega fatty acids, and bioactive compounds that can have beneficial effects on human health. However, bee pollen may also contain contaminants due to environmental contamination. To date, data on bee pollen contamination by environmental pollutants refer almost exclusively to pesticides and heavy metals, and very little information is available on the potential contamination of bee pollen by airborne particulate matter (PM), a ubiquitous pollutant that originates from a wide range of anthropogenic sources (e.g., motor vehicles, industrial processes, agricultural operations). In the present study, pollen grains collected by forager bees living in an industrial area of the Po Valley (Northern Italy) were analyzed for contamination by inorganic PM. The morpho-chemical characterization of inorganic particles using SEM/EDX allowed us to identify different emission sources and demonstrate the potential risk of PM entering the food chain and exposing bees to its ingestion
TEM-EDS microanalysis: Comparison among the standardless, Cliff & Lorimer and absorption correction quantification methods
Supplementary material associated with this article can be found, in
the online version, at doi:10.1016/j.ultramic.2023.113845Available quantification methods for energy dispersive X-ray microanalysis in transmission electron microscopy, such as the standardless method (SLM), the Cliff-Lorimer approximation (CLA) and the absorption correction method (ACM), are compared. As expected, the CLA and ACM give superior results with respect to the SLM. As far as absorption can be considered negligible, CLA and ACM perform similarly. However, starting from mass-thickness of the order of 22 Ă 10â6 g/cm2, absorption become significant and the ACM gives better results. More accurate analyses can be obtained with the ACM if distinct kO/Si factors are determined for light and heavy minerals, respectively, placing a divide at 2.90 g/cm3. Caution must be used when k-factors are derived indirectly from minerals with very different structure/chemistry, suggesting that separate k-factors data sets are required for accurate EDS quantification, at least for the major and diverse broad classes of minerals. Element diffusion of monovalent cations and channelling effects may represent a complication, especially in very anisotropic minerals such as phyllosilicates, where these two phenomena may occur together
High-temperature study of basic ferric sulfate, FeOHSO 4
AbstractWe report in this paper a new crystal-chemical study of synthetic basic ferric sulfate FeOHSO4. The structure solution performed by the Endeavour program, from new X-ray powder diffraction (XRPD) data, indicated that the correct space group of the monoclinic polytype of FeOHSO4 is C2/c. Selected Area Electron Diffraction (SAED) patterns are also consistent with this structure solution. The arrangement of Fe and S atoms, based on linear chains of Fe3+ octahedra cross-linked by SO4 tetrahedra, corresponds to that of the order/disorder (OD) family. The positions of the hydrogen atoms were located based on DFT calculations. IR and Raman spectra are presented and discussed according to this new structure model. The decomposition of FeOHSO4 during heating was further investigated by means of variable temperature XRPD, thermogravimetry, and differential thermal analysis as well as IR and Raman spectroscopies
Astronomical silicate nanoparticle analogues produced by pulsed laser ablation on olivine single crystals
Silicate nanoparticles, otherwise referred to as very small grains (VSGs) [1], occur in various
astrophysical environments. These grains experience substantial processing (e.g., amorphization)
during their lifetime in the diffuse interstellar medium due to events such as grain-grain collisions
and irradiation [2]. Moreover, several studies have pointed out that the main building blocks of
these silicates are O, Si, Fe, Mg, Al and Ca, all elements that are among the principal constituents of
the Earthâs surface [3], thus leading to the name âastronomical silicatesâ. However, the structure
and chemical evolution together with the origin of these grains are still poorly understood and
intensively debated [4,5].
The aim of this study is the simulation of space weathering processes on olivine single
crystals by liquid phase pulsed laser ablation (LP-PLA). The study of the resulting structure of both
the target and the ablated material together with their chemical evolution has been carried out by a
multiple technique characterization. In particular, spectroscopy and dynamic light scattering
measurements, analyses of the electrostatic properties and reactivity to acids and bases on the
obtained colloidal solutions of the ablated nanoproducts have been performed and coupled with highresolution transmission electron microscopy (HR-TEM).
Selected olivine target crystals (Fo87) from the SĂŁo Miguel island (Azores) were analyzed
by Scanning Electron Microscopy (SEM) and Energy Dispersive X-ray spectroscopy (EDX). LP-PLA
experiments were performed with a Nd:YAG laser focused via a singlet lens onto the surface of the
target, which was fixed at the bottom of a polystyrene box filled with 4 ml of deionized water (type
1) to immerge it completely. Laser pulses of 5 ns and 100 mJ simulate the timeframe and energy
exchange occurring during grain-grain interstellar collisions [6] and they generate a plasma plume
at the crystal/liquid interface. The rapid cooling induced by the confining liquid layer brings about
the condensation of the chemical vapor it contains with production of a colloidal solution of
nanoparticles. These solutions were analyzed by dynamic light scattering techniques and optical
absorption spectroscopy in the range from 200 nm to 1100 nm (6.20 eV - 1.13 eV). Absorption
measurements on the colloidal solutions have been compared against reference colloidal solutions
dispersed in deionized water (i.e. mesoporous silica [SiO2] nanoparticles, brucite [Mg(OH)2]
nanoparticles, aluminum hydroxide [Al(OH)3] nanoparticles, chrysotile [Mg3Si2O5(OH)4] nanotubes,
and synthetic forsterite [Mg2SiO4] nanoparticles). Moreover, additional absorption analyses have
been carried out as a function of the addition of known aliquots of sulfuric acid and sodium
hydroxide solutions. TEM/EDS analyses were then performed on the ablated nanoparticles deposited
via electrophoresis on C-coated Cu grids and compositional variations of the ablated target were
determined by X-ray photo-emission spectroscopy analyses.
The size distribution of LP-PLA synthesized nanoparticles is typically multimodal due to
aggregation phenomena. Aggregation is consistent with the measured ζ-potential, which is negative
with a relatively low absolute value, within the range 30-50 mV. Nonetheless, a recurrent mode is
centered at about 2 nm (hydrodynamic diameter) and it is consistent with the measured size
distribution obtained by transmission electron microscopy analysis (average nanoparticles diameter
around 3-5 nm). Optical absorption measurements on the ejected material show a main band
around 215 nm. This feature is very similar to the âB2 bandâ reported in several studies on silica
glass [7] and ascribed to oxygen vacancies, but its nature is still far to be fully understood. We also
found that this feature at 215 nm is very common among both Si and Mg compounds (e.g., Sioxide, Mg-hydroxide, chrysotile). Moreover, additional absorption bands in the range 240-350nm are
observed suggesting the formation of new space weathering products as result of the ablation
process.
Therefore, these results suggest that substantial chemical processing might be expected
during space weathering of âtypicalâ interstellar grains into VSGs. Moreover, coupling these
experimental results with remote sensing datasets will provide fundamental information about the
origin and evolution of these silicate grains
SILICATE NANOPARTICLES PRODUCED BY LABORATORY SIMULATED SPACE WEATHERING OF OLIVINE SINGLE CRYSTALS
Silicate nanoparticles, otherwise
referred to as very small grains (VSGs) [1], occur in
the interstellar medium. These grains experience a
strong structural modification during their lifetime in
the diffuse interstellar medium, due to events such as
grain-grain collisions and irradiation. Grain
amorphization is one of the major effects, transforming
crystalline dust concentrated in star envelopes into
amorphous silicate grains populating the interstellar
medium [2]. Moreover, several studies have pointed
out that the main building blocks of these silicates are
O, Si, Fe, Mg, Al and Ca, all elements that are among
the principal constituents of the Earthâs surface [3],
thus leading to the name âastronomical silicatesâ.
However, the structure and chemical evolution
together with the origin of these grains are still poorly
understood and intensively debated [4,5].
The aim of this study is the simulation of space
weathering processes by liquid phase pulsed laser
ablation (LP-PLA) on olivine single crystals. We adopt
a multiple technique characterization, taking advantage
of optical spectroscopy analyses and high- resolution
transmission electron microscopy (HR-TEM), to shed
light on the structure and chemical evolution of the
ablated material
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