201 research outputs found

    Direct quartz-coesite transformation in shocked porous sandstone from Kamil Crater (Egypt)

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    Coesite, a high-pressure silica polymorph (pressure 3–10 GPa, temperature <3000 K), is a diagnostic feature of shock metamorphism associated with impact cratering on quartz-bearing target rocks. It is preserved as a metastable phase in sedimentary target rocks that experienced peak pressures in excess of ~10 GPa, where it typically occurs as intergranular polycrystalline aggregates of microcrystals embedded in silica glass known as “symplectic regions.” The presence of coesite in the symplectic regions of rocks experiencing shock conditions beyond the limits of the coesite stability field is a controversial issue. Through a combined scanning and transmission electron microscopy and Raman spectroscopy study of shocked quartzarenites from the 45-m-diameter Kamil Crater (southwest Egypt), we show that coesite in symplectic regions forms through direct subsolidus transformation from quartz, in contrast with the prevailing hypothesis for crystalline targets. The quartz-to-coesite transformation takes place during localized shock-wave reverberation at the beginning of the pore collapse process. Complete pore collapse generates the high temperature regimes responsible for the subsequent production of the embedding silica melts, in part at the expense of the previously formed coesite. This work documents the role of pore collapse in producing localized pressure-temperature-time gradients in shocked porous targets, as predicted by numerical models in the literature

    3D electron diffraction in nano-geology: present and perspectives

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    When working on advanced research topics in geosciences, one must often deal with small yields and cryptocrystalline polyphasic samples. Conventional optical and X-ray crystallographic tools may not be sufficient for the proper characterization of these samples. The development of efficient probes able to investigate the nanoworld becomes therefore crucial for pushing forward our understanding about the geochemical and mineralogical processes that regulate Earth and extraterrestrial environments. In the last ten years, electron diffraction (ED) evolved from a qualitative method restricted to few dedicated TEM users, to a robust protocol for phase identification and abinitio structure determination [1]. Such change has been mostly propelled by the development of routines for 3D data collection. This methodology is in principle equivalent to single-crystal X-ray diffraction, but allows sampling crystals of few tens on nanometers. We will show here some examples of recent applications of ED in geosciences, namely how to achieve an easy and relatively fast characterization of minor and cryptocrystalline phases in natural and experimental samples. We were able identify and characterize modulated phases able to carry hydrogen at upper-mantle conditions, to follow aragonite growth from the first nucleation seeds [2] and to identify mineralogical phases and polytypes in non-equilibrated extraterrestrial samples and in impact rocks [3]

    Occurrence of fungi in the potable water of hospitals: A public health threat

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    Since the last decade, attention towards the occurrence of fungi in potable water has increased. Commensal and saprophytic microorganisms widely distributed in nature are also responsible for causing public health problems. Fungi can contaminate hospital environments, surviving and proliferating in moist and unsterile conditions. According to Italian regulations, the absence of fungi is not a mandatory parameter to define potable water, as a threshold value for the fungal occurrence has not been defined. This study evaluated the occurrence of fungi in potable water distribution systems in hospitals. The frequency of samples positive for the presence of fungi was 56.9%; among them, filamentous fungi and yeasts were isolated from 94.2% and 9.2% of the samples, respectively. The intensive care unit (87.1%) had the highest frequency of positive samples. Multivariable model (p < 0.0001), the variables of the period of the year (p < 0.0001) and type of department (p = 0.0002) were found to be statistically significant, suggesting a high distribution of filamentous fungi in the potable water of hospitals. Further studies are necessary to validate these results and identify the threshold values of fungi levels for different types of water used for various purposes to ensure the water is safe for consumption and protect public health

    Epoxy Resins for Flooring Applications, an Optimal Host for Recycling Deactivated Cement Asbestos

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    Cement asbestos slates, commonly known as Eternit((R)) and still abundant in private and public buildings, were deactivated through a thermal process. The resulting deactivated cement asbestos powder (DCAP), a mixture of Ca-Mg-Al silicates and glass, was compounded with Pavatekno Gold 200 (PT) and Pavafloor H200/E (PF), two different epoxy resins (bisphenol A epichlorohydrin) for flooring applications. The addition of the DCAP filler to the PF samples causes a slight but acceptable decrease in the relevant mechanical properties (compressive, tensile, and flexural strengths) upon increasing DCAP content. The addition of the DCAP filler to pure epoxy (PT resin) causes a slight decrease in the tensile and flexural strengths with increasing DCAP content, while the compressive strength is almost unaffected, and the Shore hardness increases. The main mechanical properties of the PT samples are significantly better than those of the filler-bearing sample of normal production. Overall, these results suggest that DCAP can be advantageously used as filler in addition to, or in substitution for, commercial barite. In particular, the sample with 20 wt% of DCAP is the best performing in terms of compressive, tensile, and flexural strengths, whereas the sample with 30 wt% of DCAP shows the highest Shore hardness, which is an important property to be considered in flooring applications

    Bioética e direitos fundamentais: a recusa às transfusões de sangue pelas Testemunhas de Jeová

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    This paper will examine the Institute of Bioethics and fundamental rights in the face of the refusal of blood transfusions by Jehovah's Witnesses. Based on investigating the motives involved in this decision and what legal support they have for their will to be recognized. It is a right provided for in the Federal Constitution that guarantees the patient's autonomy to avail himself of his existential choices, however, that is in conflict with the divergent position of the doctors who seek the judicial route to impose on the patient the use of hemotherapy against his will , provoking state intervention based on the claim that the individual's decision causes the collision of fundamental principles, such as the right to life and the right to religious freedom. For this, we studied bibliographies, laws of the current legal order, articles and jurisprudence, what remained for demonstrating the non-occurrence of a collision of fundamental rights, bearing in mind that Jehovah's Witnesses do not want to have their right to life, for religious reasons, but to guarantee it in its integral form by accepting the use of alternative methods. The existence of legitimacy in refusing blood transfusions based on fundamental principles, especially on the right to life, made possible by the recognition of blood as a risk treatment and the use of alternatives to blood transfusion.Trabalho de Conclusão de Curso (Graduação)Este trabalho analisará o instituto da Bioética e direitos fundamentais diante da recusa das transfusões de sangue pelas Testemunhas de Jeová. Tendo por base investigar os motivos que envolvem essa decisão e qual o respaldo legal possuem para que se reconheça a sua vontade. Trata-se de direito previsto na Constituição Federal que garante a autonomia do paciente de se valer de suas escolhas existenciais, porém que se choca com o divergente posicionamento dos médicos que buscam a via judicial para impor ao paciente o uso da hemoterapia contra sua vontade provocando a intervenção estatal fundamentada na alegação de que a decisão do indivíduo causa a colisão de princípios fundamentais (direito à vida versus direito à liberdade religiosa). Para isso, foram estudadas bibliografias, leis do ordenamento jurídico vigente; artigos e jurisprudências; que restaram por demonstrar a não ocorrência de colisão de direitos fundamentais, tendo em vista que as Testemunhas de Jeová não querem dispor de seu direito à vida, por fundamento religioso, e sim de garanti-lo em sua forma integral por aceitar a utilização de melhores métodos. Portanto, comprovando-se a existência de legitimidade na recusa às transfusões de sangue com base nos princípios fundamentais, principalmente no direito à vida, possibilitada pelo reconhecimento do sangue como um tratamento de risco e a utilização de alternativas a estes

    First detection of severe acute respiratory syndrome coronavirus 2 on the surfaces of tourist-recreational facilities in Italy

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    A Coronavirus disease (COVID-19), caused by a new virus called severe acute respiratory syndrome coronavirus 2 (SARS-CoV-2), spreads via direct contact through droplets produced by infected individuals. The transmission of this virus can also occur via indirect contact if objects and surfaces are contaminated by secretions from individuals with COVID-19 or asymptomatic carriers. Environmental contamination with SARS-CoV-2 is high in hospital settings; on the contrary, surface contamination in non-healthcare settings is still poorly studied. In this study, the presence of SARS-CoV-2 on the surfaces of 20 tourist-recreational facilities was investigated by performing a total of 100 swabs on surfaces, including refrigerator handles, handrails, counters, tables, and bathroom access doors. Six (6%) swabs from four (20%) tourist-recreational facilities tested positive for SARS-CoV-2; the surfaces that were involved were toilet door handles, refrigerator handles, handrails, and bar counters. This study highlights that SARS-CoV-2 is also present in non-healthcare environments; therefore, in order to limit this worrying pandemic, compliance with behavioral rules and the adoption of preventive and protective measures are of fundamental importance not only in healthcare or work environments but also in life environments

    JLB: a flexible and effective device in critical patients. Review of clinical cases

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    JLB catheter (Deltamed Inc) is an alternative way to manage difficult venous access; it is placed under US-guidance in large bore veins, with an easy-sterile approach. Internal jugular vein (IJV) is the first choice for cannulation, followed by subclavian or deep upper-arm veins. The catheter is available in different lengths and gauges, it allows high flow rates and can be left in place up to 30 days. From June 2015 to March 2017, JLB has been positioned in 409 patients: in 354 as primary access in IJV, brachial or subclavian vein; in 55 cases JLB became an introducing line for the Seldinger guidewire and further CVC positioning. All clinical cases were reviewed selecting those with greater clinical relevance. We report 8 cases in which JLB resulted determinant for the patient treatment: a 16 years old obese girl born with perinatal distress, a 78 years old obese woman with hemorrhagic shock caused by gastrointestinal bleeding, a 40 years old man with severe hypokalemia, a 30 years old man with severe sepsis, a 40 years old man with Becker’s muscular dystrophy and severe sepsis, a 40 years old man with multiple myeloma who had to carry out cycles of chemotherapy, a 76 years old man with CMV pancolitis and myelofibrosis who needed parenteral nutrition, antiviral therapy and frequent blood and platelets transfusion. Moreover, it has been useful in elderly patients who needed to carry out palliative care for seniority or cancer lasting up to 30 days . In our experience the JLB catheter is safe, easy to place, quick and cost –effective. It is a valid solution either in unstable patients requiring an immediate access in emergency and stable patients with difficult venous access, in which invasive devices can be considered an over-treatment

    Fossil micrometeorites from Monte dei Corvi: Searching for dust from the Veritas asteroid family and the utility of micrometeorites as a palaeoclimate proxy

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    We searched late Miocene sedimentary rocks in an attempt to recover fossil micrometeorites derived from the Veritas asteroid family. This study was motivated by the previous identification of a pronounced 3He peak (4-5x above background) within marine sediments with ages between ∼8.5–6.9 Ma ago (Montanari et al., 2017. GSA Bulletin, 129:1357–1376). We processed 118.9 kg of sediment from the Monte dei Corvi beach section (Italy), the global type-section for the Tortonian epoch (11.6–7.2 Ma). Samples were collected both before and within the 3He peak. Although a small number of iron-rich (I-type) fossil micrometeorites were recovered from each horizon studied (Ntotal = 20), there is no clear difference between the pre- and intra- 3He peak samples. All micrometeorites are compositionally similar, and three out of five horizons yielded similar abundances and particle sizes. Micrometeorites extracted from sediments at the base of the 3He peak were exclusively small (ø 3He values were relatively large (ø 3He signature combined with the absence of fossil micrometeorites or extraterrestrial spinels (Boschi et al., 2019, Spec. Pap. Geol. Soc. Am. 542:383–391) unambiguously related to the Veritas event suggests that the Veritas family is composed of highly friable materials that rarely survive on the sea floor to become preserved in the geological record. Our data supports the existing hypothesis that the Veritas asteroid family is an aqueously altered carbonaceous chondrite parent body, one that contains minimal native metal grains or refractory Cr-spinels. The low yield of fossil micrometeorites at Monte dei Corvi is attributed to loss of particles by dissolution whilst they resided on the sea floor but also due to high sedimentation rates leading to dilution of the extraterrestrial dust flux at this site. As with other fossil micrometeorite collections (e.g. Cretaceous chalk [Suttle and Genge, EPSL, 476:132–142]) the I-type spherules have been altered since deposition. In most particles, both magnetite and wüstite remain intact but have been affected by solid state geochemical exchange, characterised by partial leaching of Ni, Co and Cr and implantation of Mn, Mg, Si and Al. In some particles Mn concentrations reach up to 16.6 wt%. Conversely, in some micrometeorites wüstite has been partially dissolved, or even replaced by calcite or ankerite. Finally, we observe evidence for wüstite recrystallisation, forming a second generation of magnetite. This process is suggested to occur by oxidation during residence on the seafloor and has implications for the use of fossil I-type micrometeorites as a potential proxy for probing Earth’s upper atmospheric composition (oxidative capacity) in the geological past. However, solutions to the limitations of post-depositional recrystallisation are suggested. Fossil I-type spherules remain a potential tool for palaeo-climatic studies
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