Σφακιανάκης Αλέξανδρος
ΩτοΡινοΛαρυγγολόγος
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Κρήτη 72100
00302841026182
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alsfakia@gmail.com

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Κυριακή 11 Δεκεμβρίου 2016

Large scale syntheses of colloidal nanomaterials

Publication date: Available online 10 December 2016
Source:Nano Today
Author(s): Pearl L. Saldanha, Vladimir Lesnyak, Liberato Manna
Nanoscale materials have long promised to revolutionize science and technology, with claims being sustained by both the advances in their fabrication and by the many fundamental studies that have been carried out to date, which have revealed fascinating properties when materials dimensions shrink all the way down to a few hundreds/thousands of atoms. In this ongoing hype, on one side we have the futuristic views and promises of ubiquitous devices in which the operating units will be eventually scaled down to individual atoms or molecules. On the other side, we have the more realistic (and already unfolding) scenario represented by nanoscale materials making their way in a wide variety of applications (not always and not necessarily flagged as "high-tech") where downsizing truly brings about new or improved features that can be immediately exploited for some practical use. These applications have encompassed fields as disparate as medicine, biology, energy conversion and storage, catalysis, sensing, nanocomposite engineering, cosmetics, to cite the most popular ones. For a new technology to be pervasive and disruptive, the costs associated to the fabrication, the characterization and the assemblage of its key components have to drop quickly over time, while at the same time the material quality and the reproducibility of the various processes must keep improving. In the case of nanomaterials, we have not yet witnessed such an ubiquitous revolution, and one of the reasons is probably the lack of straightforward and reproducible synthetic protocols providing large amounts of nanomaterials and thus capable of efficient up-scaling to fulfil industrial needs. Another reason likely resides in the growing concern that nanomaterials will pose new threats to the environment, but this aspect will not be investigated here.In this review, we will touch upon the critical feature of nanomaterials science and engineering dealing with the high throughput synthesis, with a focus on materials prepared in the liquid phase, where the expertise of the authors of this review lays. As a note of caution to the reader, we will not cover in depth all existing approaches to large scale syntheses. Our discussion will be instead a broad summary of the main types of synthetic approaches developed to date, and which we believe will be useful to scientists and engineers who are approaching the fabrication of nanomaterials with an eye on their use in large-scale, industrial applications. The review has been written according to the principle "from the simple to the complex": it begins with the simplest one-batch heat-up synthesis approach, followed by hot-injection methods and ends by discussing the more sophisticated continuous flow syntheses of nanoparticles. Similarly, in each section, wherever possible, the discussion will start from simpler compounds, (for example, one-component noble metal nanocrystals), and will then move on to more complex structures (from binary to ternary and even quaternary compounds, which will be mainly metal oxides and chalcogenides).

Graphical abstract

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Title page / Editorial Board

Publication date: December 2016
Source:Cancer Epidemiology, Volume 45, Supplement 1





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Supplement title page

Publication date: December 2016
Source:Cancer Epidemiology, Volume 45, Supplement 1





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Table of contents

Publication date: December 2016
Source:Cancer Epidemiology, Volume 45, Supplement 1





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Salmonella-induced inflammasome activation in humans

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Publication date: Available online 11 December 2016
Source:Molecular Immunology
Author(s): Damien Bierschenk, Dave Boucher, Kate Schroder
Inflammasomes are macromolecular complexes that assemble upon recognition of pathogen- or danger-associated molecular patterns. Inflammasome assembly is nucleated by the oligomerisation of specific, activated pattern recognition receptors within the cytosol. Inflammasomes function as platforms for the activation of the caspase-1 protease, which in turn triggers the maturation and secretion of the pro-inflammatory cytokines IL-1β and IL-18, and initiates pyroptosis, a highly inflammatory form of lytic cell death. Recently, additional inflammatory caspases (murine caspase-11, and human caspase-4/5) were also reported to be activated upon a pyroptosis-inducing 'non-canonical inflammasome' by direct recognition of lipopolysaccharide (LPS), a pathogen-associated molecular pattern. Here we review and discuss recent advances in our understanding of inflammasome-mediated host defence against Salmonella particularly in human cells, and their implications for cellular survival and cytokine secretion.



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Salmonella-induced inflammasome activation in humans

S01615890.gif

Publication date: Available online 11 December 2016
Source:Molecular Immunology
Author(s): Damien Bierschenk, Dave Boucher, Kate Schroder
Inflammasomes are macromolecular complexes that assemble upon recognition of pathogen- or danger-associated molecular patterns. Inflammasome assembly is nucleated by the oligomerisation of specific, activated pattern recognition receptors within the cytosol. Inflammasomes function as platforms for the activation of the caspase-1 protease, which in turn triggers the maturation and secretion of the pro-inflammatory cytokines IL-1β and IL-18, and initiates pyroptosis, a highly inflammatory form of lytic cell death. Recently, additional inflammatory caspases (murine caspase-11, and human caspase-4/5) were also reported to be activated upon a pyroptosis-inducing 'non-canonical inflammasome' by direct recognition of lipopolysaccharide (LPS), a pathogen-associated molecular pattern. Here we review and discuss recent advances in our understanding of inflammasome-mediated host defence against Salmonella particularly in human cells, and their implications for cellular survival and cytokine secretion.



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Isotopic (C–O–S) geochemistry and Re–Os geochronology of the Haobugao Zn–Fe deposit in Inner Mongolia, NE China

Publication date: April 2017
Source:Ore Geology Reviews, Volume 82
Author(s): Yuan Liu, Si-Hong Jiang, Leon Bagas, Ning Han, Chun-Liang Chen, Huan Kang
The Haobugao Zn–Fe deposit is a typical skarn deposit located in the southern part of the Great Xing'an Range that hosts polymetallic mineralization over a large region. The main ore minerals at the deposit include sphalerite, magnetite, galena, chalcopyrite and pyrite, and the main gangue minerals include andradite, grossular garnet, hedenbergite, diopside, ilvaite, calcite and quartz. There are broadly two mineralizing periods represented by the relatively older skarn and younger quartz–sulfide veins. In detail, there are five metallogenic stages consisting of an early skarn, late skarn, oxide, early quartz–sulfide, and late quartz–sulfide–calcite stages. Electron microprobe analyses show that the garnet at the deposit varies in composition from And97.95Gro0.41Pyr1.64 to And30.69Gro66.69Pyr2.63, and pyroxene is compositionally in the diopside–hedenbergite range (i.e. Di90.63Hd8.00Jo1.37–Hd88.98Di4.53Jo6.49). Petrographic observations and electron microprobe analyses indicate that the sphalerite has three generations ([Zn0.93Fe0.08]S–[Zn0.75Fe0.24]S). The Zn associated with the first generation sphalerite replaced Cu and Fe of early xenomorphic granular chalcopyrite (i.e. [Cu1.01Fe1.03]S2–[Cu0.99Fe0.99]S2), and part of the first generation sphalerite is coeval with late chalcopyrite (i.e. [Cu0.96Fe0.99Zn0.03]S2–[Cu1.00Fe1.03Zn0.01]S2). Magnetite has a noticeable negative Ce anomaly (δCe=∼0.17 to 0.54), which might be a result of the oxidized ore-fluid. Thirty δ34SV-PDB analyses of sulfides from the ore range from −2.3 to −0.1‰ in value, which are indicative of a magmatic source. The δ13C‰ and δ18O‰ values for calcite from the ore formed at quartz–sulfide–calcite stage vary from −9.9 to −5.5‰ and from −4.2 to 1.1‰, respectively, contrasting with δ13C‰ (2.9–4.8‰) and δ18O‰ (9.8–13.9‰) values for calcite from marble. It is suggested that the ore-forming fluid associated with late stage of mineralization was predominantly magmatic in origin with some input of local meteoric water.Molybdenite from the Haobugao deposit defines an isochron age of 142±1Ma, which is interpreted as the mineralization age being synchronous, within error, with the zircon U–Pb ages of 140±1, 141±2, and 141±1Ma for granite at the deposit. These data and characteristics of lithology and mineralization further show that the Zn–Fe mineralization is temporally and spatially related to the emplacement of granite in an extensional tectonic setting during the Mesozoic.

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