77 research outputs found
The imprint of thermally induced devolatilization phenomena on radon signal. Implications for the geochemical survey in volcanic areas
Thermal gradients due to magma dynamics in active volcanic areas may affect the emanating
power of the substrate and the background level of radon signal. This is particularly effective
in subvolcanic substrates where intense hydrothermal alteration and/or weathering processes
generally form hydrous minerals, such as zeolites able to store and release great amounts of
H2O (up to âŒ25 wt.%) at relative low temperatures. To better understand the role played by
thermally induced devolatilization reactions on the radon signal, a new experimental setup has
been developed for measuring in real time the radon emission from a zeolitized volcanic tuff.
Progressive dehydration phenomena with increasing temperature produce radon emissions two
orders of magnitude higher than those measured during rock deformation, microfracturing and
failure. In this framework, mineral devolatilization reactions can contribute significantly to
produce radon emissions spatially heterogeneous and non-stationary in time, resulting in a
transient state dictated by temperature gradients and the carrier effects of subsurface gases.
Results from these experiments can be extrapolated to the temporal and spatial scales of
magmatic processes, where the ascent of small magma batches from depth causes volatile
release due to dehydration phenomena that increase the radon signal from the degassing host
rock material
Rheological changes in melts and magmas induced by crystallization and strain rate
This review highlights the rheological and phase proportions variation induced by cooling events from superliquidus temperature (melt) to subliquidus temperatures. It provides a comprehensive view of the rheological response of magmatic systems undergoing dynamic cooling and shear deformation. The two main parameters which are of importance to model the rheological properties of such crystallizing systems and which are simultaneously poorly investigated so far are crystallization and strain rates. The response to relatively high deformation rates results in shear thinning behavior in partly crystallized systems under variable shear rate and it should be considered in magmatic processes. Due to the sluggish crystallization of SiO2-rich melts, data are mainly available for mafic systems, which does not allow a general reappraisal. An attempt to model available literature data for less evolved systems in dynamic scenarios and a comparison with MELTS algorithm approach (thermodynamic equilibrium conditions) is provided. Since there are difficulties in comparing experimental data gained using different methodologies, we focus mainly on data obtained with the concentric cylinder technique. This highlights the fact that a general experimental protocol is needed in order to compare and model viscosity data to predict the dynamic rheological evolution for volcanic rocks. © Académie des sciences, Paris and the authors, 2022. Some rights reserved
Incentives In Primary Care and Their Impact on Potentially Avoidable Hospital Admissions
Financial incentives in primary care have been often introduced with the purpose of improving
appropriateness of care and containing demand. We usually observe pay-for-performance programs,
but alternatives have been also implemented, such as pay-for-participation in improvement
activities and pay-for-compliance with clinical guidelines. Here, we assess the influence of different
programs which ensure extra-payments to GPs, for containing episodes of avoidable
hospitalisations. Our dataset covers patients and GPs of the Italian region Emilia-Romagna for year
2005, and we control for a wide range of factors potentially influencing GPsâ behaviour. By
separating pay-for-performance from pay-for-participation and pay-for-compliance programs, we
estimate the impact on the probability of (inappropriate) hospitalisation of financial incentives
included in contracts between GPs and the NHS. As dependent variable, we consider two different
sets of conditions, for both of which timely and effective primary care should be able to limit the
need of hospital admission. The first is based on 27 medical DRGs that Emilia-Romagna identifies
as at risk of inappropriateness in primary care, while the second refers to the internationally
recognised ACSCs (ambulatory care-sensitive conditions). We show that pay-for-performance
schemes may have a significant effect over aggregate indicators of appropriateness, while the
effectiveness of pay-for-participation schemes is adequately captured only by taking into account
subpopulations affected by specific diseases. Moreover, the same incentive scheme has fairly
different effects on the two sets of indicators used, with performance improvements limited to the
target explicitly addressed by the policy maker (i.e. the list of 27 DRGs). This evidence is consistent
with the idea that a âtunnel visionâ effect may occur when public authorities promote and monitor
specific sets of objectives, as proxies for more general improvements in health care practices
The Onset and Solidification Path of a Basaltic Melt by in situ Differential Scanning Calorimetry (DSC) and ex situ Investigations
The in situ differential scanning calorimetry (DSC) technique has been applied to investigate the solidification paths of a basaltic liquid. The starting glass was heated up to 1300°C, kept at this superliquidus temperature for 2 h and cooled at rates (ÎT/Ît) of 7, 60, 180, 1000, and 1800°C/h, down to 800 and 600°C. Glass transition temperature (Tg), crystallization temperature (Tx_HR) and melting temperature (Tm) were measured by in situ DSC spectra on heating. Tx measured along the cooling paths (Tx_CR) shows exothermic peaks that change from a single symmetric shape (7 and 60°C/h) to multi-component patterns (180, 1000, and 1800°C/h). The recovered products characterized by field emission gun source of the scanning electron microscopy and electron probe micro-analyzer-wavelength dispersive spectrometers show a phase assemblage of spinel (sp), clinopyroxene (cpx), melilite (mel), plagioclase (plg), and glass. Moreover, crystal size distributions (CSDs) and growth rates (Gmax and GCSD) were also determined. The crystal content slightly increases from 7 to 1800°C/h. Faceted sp are present in all the run products with an amount always <2 area%. Cpx increases from 7 to 1800°C/h, changing its texture from almost faceted to dendritic between 60 and 180°C/h. The area% of mel follows an asymmetric Gaussian trend, while plg nucleates only at 7°C/h with a content <2 area%. The coupling of DSC and SEM outcomes indicate that sp nucleate first, followed by cpx and mel (and/or plg). The increment of ÎT/Ît causes an increase of the CSD slope (m) and crystal population density per size (n0), as well as a decrease of the crystal size, for both cpx and sp. The log-linear CSD segments with different slopes at 7 and 60°C/h suggest multiple nucleation events and crystal growth by coarsening. Gmax and GCSD for cpx and sp directly measured on the actual crystallization time by DSC spectra, both increase with the increasing of ÎT/Ît. The onset temperature of crystallization (Txi) decreases as ÎT/Ît increases, following an exponential trend that defines the uppermost portion of a time-transformation-temperature-like curve. This analytical model allows us to quantitatively model the kinetic crystallization paths of dry basalts
BNaâBLi solid-solution in A-site-vacant amphiboles: synthesis and cation ordering along the ferri-clinoferroholmquistiteâriebeckite join.
Amphiboles were hydrothermally synthesized at 500 âC and 4 kbar in the system Li2O-Na2OFeO- Fe2O3-SiO2-H2O, with nominal compositions along the riebeckite [â Na2Fe3 2+ Fe2 3+Si8O22(OH)2]-ferri-clinoferroholmquistite [â Li2Fe3 2+Fe2 3+Si8O22(OH)2] join, where the exchange vector is NaLiâ1 at the B-site. Experimental products were characterized by powder XRD and SEM-EDAX, confirming very high amphibole yield along the join (>95%, plus minor quartz). The XRD patterns can be indexed in C2/m, and the refined cell parameters show linear variation as a function of composition. For the BLi end-member, the IR spectrum shows a single sharp main band centered at 3614 cmâ1, which is assigned to the FeFeFe-OH-Aâ configuration. With increasing BNa in the mineral, this band broadens and shifts 4 cmâ1 to higher frequencies. This effect can be attributed to the change in M4 site occupancy. Minor ANa (partial solid-solution toward arfvedsonite) is also observed with increasing sodium in the system. Mössbauer spectroscopy confirms the cation distribution provided by IR data, and shows that a small, but significant amount of Fe2+ occurs at M4 along the join. Infrared spectroscopy shows that the Li end-member has a very ordered structure, whereas intermediate compositions show local heterogeneities associated with the presence of two different B sites occupied by Na or Li
Rheological changes in melts and magmas induced by crystallization and strain rate
This review highlights the rheological and phase proportions variation induced by cooling events from superliquidus temperature (melt) to subliquidus temperatures. It provides a comprehensive view of the rheological response of magmatic systems undergoing dynamic cooling and shear deformation. The two main parameters which are of importance to model the rheological properties of such crystallizing systems and which are simultaneously poorly investigated so far are crystallization and strain rates. The response to relatively high deformation rates results in shear thinning behavior in partly crystallized systems under variable shear rate and it should be considered in magmatic processes. Due to the sluggish crystallization of SiO-rich melts, data are mainly available for mafic systems, which does not allow a general reappraisal. An attempt to model available literature data for less evolved systems in dynamic scenarios and a comparison with MELTS algorithm approach (thermodynamic equilibrium conditions) is provided. Since there are difficulties in comparing experimental data gained using different methodologies, we focus mainly on data obtained with the concentric cylinder technique. This highlights the fact that a general experimental protocol is needed in order to compare and model viscosity data to predict the dynamic rheological evolution for volcanic rocks
Infra red spectroscopy of the regulated asbestos amphiboles
Vibrational spectroscopies (Fourier Transform Infra Red, FTIR, and Raman) are exceptionally valuable tools for the identification and crystal\u2013chemical study of fibrous minerals, and asbestos amphiboles in particular. Raman spectroscopy has been widely applied in toxicological studies and thus a large corpus of reference data on regulated species is found in the literature. However, FTIR spectroscopy has been mostly used in crystal\u2013chemical studies and very few data are found on asbestos amphiboles. This paper is intended to fill this gap. We report new FTIR data collected on a suite of well-characterized samples of the five regulated amphibole species: anthophyllite, amosite, and crocidolite, provided by the Union for International Cancer Control (UICC) Organization, and tremolite and actinolite, from two well-known occurrences. The data from these reference samples have been augmented by results from additional specimens to clarify some aspects of their spectroscopic features. We show that the FTIR spectra in both the OH-stretching region and in the lattice modes region can be effective for rapid identification of the asbestos type
A new approach to deposit homogeneous samples of asbestos fibres for toxicological tests in vitro
In this paper we describe the results obtained with a novel method to prepare depositions of asbestos fibres for toxicological tests in vitro. The technique is based on a micro-dispenser, working as an inkjet printer, able to deposit micro-sized droplets from a suspension of fibres in a liquid medium; we used here a highly evaporating liquid (ethanol) to reduce the experimental time, however other solvents could be used. Both the amount and spatial distribution of fibres on the substrate can be controlled by adjusting the parameters of the micro-dispenser such as deposition area, deposition time, uniformity and volume of the deposited liquid. Statistical analysis of images obtained by optical and scanning electron microscopy shows that this technique produces an extremely homogeneous distribution of fibers. Specifically, the number of deposited single fibres is maximized (up to 20 times), a feature that is essential when performing viability tests where agglomerated or untangled fibrous particles need to be avoided
EV20-mediated delivery of cytotoxic auristatin MMAF exhibits potent therapeutic efficacy in cutaneous melanoma.
Abstract Cutaneous melanoma is one of the cancers with the fastest rising incidence and in its advanced metastatic form is a highly lethal disease. Despite the recent approval of several new drugs, the 5-year overall survival rate for advanced cutaneous melanoma is still below 20% and therefore, the development of novel treatments remains a primary need. Antibody-Drug Conjugates are an emerging novel class of anticancer agents, whose preclinical and clinical development has recently seen a remarkable increase in different tumors, including melanoma. Here, we have coupled the anti-HER-3 internalizing antibody EV20 to the cytotoxic drug monomethyl auristatin F (MMAF) to form a novel antibody-drug conjugate (EV20/MMAF). In a panel of human melanoma cell lines, this novel ADC shows a powerful, specific and target-dependent cell killing activity, independently of BRAF status. Efficacy studies demonstrated that a single administration of EV20/MMAF leads to a long-lasting tumor growth inhibition. Remarkably, the effect of this novel ADC was superior to the BRAF inhibitor vemurafenib in preventing kidney, liver and lung melanoma metastases. Overall, these results highlight EV20/MMAF as a novel ADC with promising therapeutic efficacy, warranting extensive pre-clinical evaluation in melanoma with high levels of HER-3 expression
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