806 research outputs found
An IoT-Aware Architecture for Smart Healthcare Systems
none7Over the last few years, the convincing forward steps in the development of Internet-of-Things (IoT) enabling solutions are spurring the advent of novel and fascinating applications. Among others, mainly Radio Frequency Identification (RFID), Wireless Sensor Network (WSN), and smart mobile technologies are leading this evolutionary trend. In the wake of this tendency, this paper proposes a novel, IoTaware, smart architecture for automatic monitoring and tracking of patients, personnel, and biomedical devices within hospitals and nursing institutes. Staying true to the IoT vision, we propose a Smart Hospital System (SHS) which relies on different, yet complementary, technologies, specifically RFID, WSN, and smart mobile, interoperating with each other through a CoAP/6LoWPAN/REST network infrastructure. The SHS is able to collect, in real time, both environmental conditions and patientsâ physiological parameters via an ultra-low-power Hybrid Sensing Network (HSN) composed of 6LoWPAN nodes integrating UHF RFID functionalities. Sensed data are delivered to a control center where an advanced monitoring application makes them easily accessible by both local and remote users via a REST web service. The simple proof of concept implemented to validate the proposed SHS has highlighted a number of key capabilities and aspects of novelty which represent a significant step forward compared to the actual state of art.restrictedCATARINUCCI L.; DE DONNO D.; MAINETTI L.; PALANO L.; PATRONO L.; STEFANIZZI M.; TARRICONE L.Catarinucci, Luca; DE DONNO, Danilo; Mainetti, Luca; Palano, L.; Patrono, Luigi; Stefanizzi, MARIA LAURA; Tarricone, Lucian
Hematopoietic progenitor cell liabilities and alarmins S100A8/A9-related inflammaging associate with frailty and predict poor cardiovascular outcomes in older adults
Frailty affects the physical, cognitive, and social domains exposing older adults to an increased risk of cardiovascular disease and death. The mechanisms linking frailty and cardiovascular outcomes are mostly unknown. Here, we studied the association of abundance (flow cytometry) and gene expression profile (RNAseq) of stem/progenitor cells (HSPCs) and molecular markers of inflammaging (ELISA) with the cardiorespiratory phenotype and prospective adverse events of individuals classified according to levels of frailty. Two cohorts of older adults were enrolled in the study. In a cohort of preâfrail 35 individuals (average age: 75Â years), a physical frailty score above the median identified subjects with initial alterations in cardiorespiratory function. RNA sequencing revealed S100A8/A9 upregulation in HSPCs from the bone marrow (>10âfold) and peripheral blood (>200âfold) of individuals with greater physical frailty. Moreover higher frailty was associated with increased alarmins S100A8/A9 and inflammatory cytokines in peripheral blood. We then studied a cohort of 104Â more frail individuals (average age: 81Â years) with multidomain health deficits. Reduced levels of circulating HSPCs and increased S100A8/A9 concentrations were independently associated with the frailty index. Remarkably, low HSPCs and high S100A8/A9Â simultaneously predicted major adverse cardiovascular events at 1âyear followâup after adjustment for age and frailty index. In conclusion, inflammaging characterized by alarmin and proâinflammatory cytokines in preâfrail individuals is mirrored by the pauperization of HSPCs in frail older people with comorbidities. S100A8/A9 is upregulated within HSPCs, identifying a phenotype that associates with poor cardiovascular outcomes
DInSAR Analysis and Analytical Modeling of Mount Etna Displacements: The December 2018 VolcanoâTectonic Crisis
We investigate the 24â27 December 2018 eruption of Mount Etna occurred from fissures located on the volcano eastern flank and accompanied by a seismic swarm, which was triggered by the magma intrusion and continued for weeks after the end of the eruption. Moreover, this swarm involved some of the shallow volcanoâtectonic structures located on the Mount Etna flanks and culminated on 26 December with the strongest event (ML 4.8), occurred along the Fiandaca Fault. In this work, we analyze seismological data and Sentinelâ1 Differential Interferometric Synthetic Aperture Radar (DInSAR) measurements, the latter inverted through analytical modeling. Our results suggest that a dike source intruded, promoting the opening of the eruptive fissures fed by a shallower dike. Moreover, our findings indicate that the activation of faults in different sectors of the volcano may be considered as a response to accommodate the deformations induced by the magma volumes injection.Published5817-58275V. Processi eruttivi e post-eruttiviJCR Journa
The RING GPS network: a research geodetic infrastructure to study plate boundary deformation in the Central Mediterranean
We present the INGV (Italian National Institute of Geophysics and Volcanology) geodetic research infrastructure
and related facilities, dedicated to the observation and monitoring of current deformation of the plate boundary
between Africa and Eurasia. The recent increase of continuous GPS (CGPS) stations in the Central Mediterranean
plate boundary zone offers the opportunity to study in detail the present-day kinematics of this actively deforming
region. For answering all the open questions related to this complex area, INGV deployed a permanent, integrated
and real-time monitoring CGPS network (RING) all over Italy. The RING network (http:/ring.gm.ingv.it) is now
constituted by more than 150 stations. All stations have high quality GPS monuments and most of them are
co-located with broadband or very broadband seismometers and strong motion sensors. The RING CGPS sites
acquire at 1Hz and 30s sampling rates (some of them acquire at 10 Hz) and are connected in real-time to the
INGV acquisition centers located in Roma and Grottaminarda. Real-time GPS data are transmitted using different
systems, such as satellite systems, Internet, GPRS/UMTS and wireless networks. The differentiation of data
transmission type and the integration with seismic instruments makes this network one of the most innovative
CGPS networks in Europe. Furthermore, the INGV data acquisition centers acquire, archive and analyze most
of the Italian CGPS stations managed by regional or national data providers (such as local Authorities and
nation-wide industries), integrating more than 350 stations of the CGPS scientific and commercial networks
existing in the Italian region. To manage data acquisition, storage, distribution and access we developed dedicated
facilities including new softwares for data acquisition and a web-based collaborative environment for management
of data and metadata. The GPS analysis is carried out with the three main geodetic-quality softwares used in the
GPS scientific community: Bernese GAMIT an GIPSY-OASIS. The resulting daily solutions are aligned to the
ITRF2005 reference frame. Stable plate reference frames are realized by minimizing the horizontal velocities at
sites on the Eurasia and Nubia plates, respectively. The different software-related solutions consistency RMS is
within 0.3 mm/yr (Avallone et al., 2010). The solutions are then evaluated with regard to the numerous scientific
motivations behind this presentation, ranging from the definition of strain distribution and microplate kinematics
within the plate boundary, to the evaluation of tectonic strain accumulation on active faults. The RING network
is strongly contributing to the definition of GPS velocity field in the Italian region, and now is able to furnish
a newly and up to date view of this actively deforming part of the Nubia-Eurasia plate boundary. INGV is now
aiming to make the RING (and integrated CGPS networks) data and related products publicly available for the
scientific community. We believe that our network represents an important reality in the framework of the EPOS
infrastructure and we strongly support the idea of an European research approach to data sharing among the
scientific community. We will present (a) the current CGPS site distribution, (b) the technological description of
the data acquisition, storage and distribution at INGV centers, (c) the results of CGPS data analysis, and (d) the
planned data access for the scientific community.PublishedVienna, Geophysical Research Abstracts
Vol. 13, EGU2011-8626, 20111.9. Rete GPS nazionale3.2. Tettonica attivaope
The RING GPS network: a research geodetic infrastructure to study plate boundary deformation in the Central Mediterranean
We present the INGV (Italian National Institute of Geophysics and Volcanology) geodetic research infrastructure
and related facilities, dedicated to the observation and monitoring of current deformation of the plate boundary
between Africa and Eurasia. The recent increase of continuous GPS (CGPS) stations in the Central Mediterranean
plate boundary zone offers the opportunity to study in detail the present-day kinematics of this actively deforming
region. For answering all the open questions related to this complex area, INGV deployed a permanent, integrated
and real-time monitoring CGPS network (RING) all over Italy. The RING network (http:/ring.gm.ingv.it) is now
constituted by more than 150 stations. All stations have high quality GPS monuments and most of them are
co-located with broadband or very broadband seismometers and strong motion sensors. The RING CGPS sites
acquire at 1Hz and 30s sampling rates (some of them acquire at 10 Hz) and are connected in real-time to the
INGV acquisition centers located in Roma and Grottaminarda. Real-time GPS data are transmitted using different
systems, such as satellite systems, Internet, GPRS/UMTS and wireless networks. The differentiation of data
transmission type and the integration with seismic instruments makes this network one of the most innovative
CGPS networks in Europe. Furthermore, the INGV data acquisition centers acquire, archive and analyze most
of the Italian CGPS stations managed by regional or national data providers (such as local Authorities and
nation-wide industries), integrating more than 350 stations of the CGPS scientific and commercial networks
existing in the Italian region. To manage data acquisition, storage, distribution and access we developed dedicated
facilities including new softwares for data acquisition and a web-based collaborative environment for management
of data and metadata. The GPS analysis is carried out with the three main geodetic-quality softwares used in the
GPS scientific community: Bernese GAMIT an GIPSY-OASIS. The resulting daily solutions are aligned to the
ITRF2005 reference frame. Stable plate reference frames are realized by minimizing the horizontal velocities at
sites on the Eurasia and Nubia plates, respectively. The different software-related solutions consistency RMS is
within 0.3 mm/yr (Avallone et al., 2010). The solutions are then evaluated with regard to the numerous scientific
motivations behind this presentation, ranging from the definition of strain distribution and microplate kinematics
within the plate boundary, to the evaluation of tectonic strain accumulation on active faults. The RING network
is strongly contributing to the definition of GPS velocity field in the Italian region, and now is able to furnish
a newly and up to date view of this actively deforming part of the Nubia-Eurasia plate boundary. INGV is now
aiming to make the RING (and integrated CGPS networks) data and related products publicly available for the
scientific community. We believe that our network represents an important reality in the framework of the EPOS
infrastructure and we strongly support the idea of an European research approach to data sharing among the
scientific community. We will present (a) the current CGPS site distribution, (b) the technological description of
the data acquisition, storage and distribution at INGV centers, (c) the results of CGPS data analysis, and (d) the
planned data access for the scientific community
Les droits disciplinaires des fonctions publiques : « unification », « harmonisation » ou « distanciation ». A propos de la loi du 26 avril 2016 relative à la déontologie et aux droits et obligations des fonctionnaires
The production of tt⟠, W+bb⟠and W+cc⟠is studied in the forward region of protonâproton collisions collected at a centre-of-mass energy of 8 TeV by the LHCb experiment, corresponding to an integrated luminosity of 1.98±0.02 fbâ1 . The W bosons are reconstructed in the decays WââÎœ , where â denotes muon or electron, while the b and c quarks are reconstructed as jets. All measured cross-sections are in agreement with next-to-leading-order Standard Model predictions.The production of , and is studied in the forward region of proton-proton collisions collected at a centre-of-mass energy of 8 TeV by the LHCb experiment, corresponding to an integrated luminosity of 1.98 0.02 \mbox{fb}^{-1}. The bosons are reconstructed in the decays , where denotes muon or electron, while the and quarks are reconstructed as jets. All measured cross-sections are in agreement with next-to-leading-order Standard Model predictions
Measurement of the ratios of branching fractions and
The ratios of branching fractions
and are measured, assuming isospin symmetry, using a
sample of proton-proton collision data corresponding to 3.0 fb of
integrated luminosity recorded by the LHCb experiment during 2011 and 2012. The
tau lepton is identified in the decay mode
. The measured values are
and
, where the first uncertainty is
statistical and the second is systematic. The correlation between these
measurements is . Results are consistent with the current average
of these quantities and are at a combined 1.9 standard deviations from the
predictions based on lepton flavor universality in the Standard Model.Comment: All figures and tables, along with any supplementary material and
additional information, are available at
https://cern.ch/lhcbproject/Publications/p/LHCb-PAPER-2022-039.html (LHCb
public pages
Multidifferential study of identified charged hadron distributions in -tagged jets in proton-proton collisions at 13 TeV
Jet fragmentation functions are measured for the first time in proton-proton
collisions for charged pions, kaons, and protons within jets recoiling against
a boson. The charged-hadron distributions are studied longitudinally and
transversely to the jet direction for jets with transverse momentum 20 GeV and in the pseudorapidity range . The
data sample was collected with the LHCb experiment at a center-of-mass energy
of 13 TeV, corresponding to an integrated luminosity of 1.64 fb. Triple
differential distributions as a function of the hadron longitudinal momentum
fraction, hadron transverse momentum, and jet transverse momentum are also
measured for the first time. This helps constrain transverse-momentum-dependent
fragmentation functions. Differences in the shapes and magnitudes of the
measured distributions for the different hadron species provide insights into
the hadronization process for jets predominantly initiated by light quarks.Comment: All figures and tables, along with machine-readable versions and any
supplementary material and additional information, are available at
https://cern.ch/lhcbproject/Publications/p/LHCb-PAPER-2022-013.html (LHCb
public pages
Study of the decay
The decay is studied
in proton-proton collisions at a center-of-mass energy of TeV
using data corresponding to an integrated luminosity of 5
collected by the LHCb experiment. In the system, the
state observed at the BaBar and Belle experiments is
resolved into two narrower states, and ,
whose masses and widths are measured to be where the first uncertainties are statistical and the second
systematic. The results are consistent with a previous LHCb measurement using a
prompt sample. Evidence of a new
state is found with a local significance of , whose mass and width
are measured to be and , respectively. In addition, evidence of a new decay mode
is found with a significance of
. The relative branching fraction of with respect to the
decay is measured to be , where the first
uncertainty is statistical, the second systematic and the third originates from
the branching fractions of charm hadron decays.Comment: All figures and tables, along with any supplementary material and
additional information, are available at
https://cern.ch/lhcbproject/Publications/p/LHCb-PAPER-2022-028.html (LHCb
public pages
Observation of the B0 â Ï0Ï0 decay from an amplitude analysis of B0 â (Ï+Ïâ)(Ï+Ïâ) decays
Protonâproton collision data recorded in 2011 and 2012 by the LHCb experiment, corresponding to an integrated luminosity of 3.0 fbâ1 , are analysed to search for the charmless B0âÏ0Ï0 decay. More than 600 B0â(Ï+Ïâ)(Ï+Ïâ) signal decays are selected and used to perform an amplitude analysis, under the assumption of no CP violation in the decay, from which the B0âÏ0Ï0 decay is observed for the first time with 7.1 standard deviations significance. The fraction of B0âÏ0Ï0 decays yielding a longitudinally polarised final state is measured to be fL=0.745â0.058+0.048(stat)±0.034(syst) . The B0âÏ0Ï0 branching fraction, using the B0âÏKâ(892)0 decay as reference, is also reported as B(B0âÏ0Ï0)=(0.94±0.17(stat)±0.09(syst)±0.06(BF))Ă10â6
- âŠ