4,456 research outputs found
ATLAS RPC offline monitoring and data quality assessment
In this work several aspects of ATLAS RPC offline monitoring and data quality
assessment are illustrated with cosmics data selected by RPC trigger. These
correspond to trigger selection, front-end mapping, detection efficiency and
occupancy, which are studied in terms of low level quantities such as: RPC
off-line hits and standalone tracks. The tools and techniques presented are
also extended to the forthcoming LHC p-p beam collisions.Comment: Poster section at ICHEP08, Philadelphia, USA, July 2008. 3 pages,
LaTeX, 3 eps figure
Risk factors for mortality from imported falciparum malaria in the United Kingdom over 20 years: an observational study
Objectives To determine which travellers with malaria are at greatest risk of dying, highlighting factors which can be used to target health messages to travellers.
Design Observational study based on 20 years of UK national data.
Setting National register of malaria cases.
Participants 25 054 patients notified with Plasmodium falciparum malaria, of whom 184 died, between 1987 and 2006.
Main outcome measures Comparison between those with falciparum malaria who died and non-fatal cases, including age, reason for travel, country of birth, time of year diagnosed, malaria prophylaxis used.
Results Mortality increased steadily with age, with a case fatality of 25/548 (4.6%) in people aged >65 years, adjusted odds ratio 10.68 (95% confidence interval 6.4 to 17.8), P<0.001 compared with 18–35 year olds. There were no deaths in the ≤5 year age group. Case fatality was 3.0% (81/2740 cases) in tourists compared with 0.32% (26/8077) in travellers visiting friends and relatives (adjusted odds ratio 8.2 (5.1 to 13.3), P<0.001). Those born in African countries with endemic malaria had a case fatality of 0.4% (36/8937) compared with 2.4% (142/5849) in others (adjusted odds ratio 4.6 (3.1 to 9.9), P<0.001). Case fatality was particularly high from the Gambia. There was an inverse correlation in mortality between region of presentation and number of cases seen in the region (R2=0.72, P<0.001). Most delay in fatal cases was in seeking care.
Conclusions Most travellers acquiring malaria are of African heritage visiting friends and relatives. In contrast the risks of dying from malaria once acquired are highest in the elderly, tourists, and those presenting in areas in which malaria is seldom seen. Doctors often do not think of these as high risk groups for malaria; for this reason they are important groups to target in pre-travel advice
Le Fumarole di Vulcano
In tempi storici l’Isola di Vulcano è stata interessata da numerose eruzioni. Come già detto l’ultima
attività vulcanica è avvenuta fra il 1888 e il 1890. Da allora l’attività del vulcano è caratterizzata dalla presenza di numerose aree fumarolizzate..
ATLAS RPC Quality Assurance results at INFN Lecce
The main results of the quality assurance tests performed on the Resistive
Plate Chamber used by the ATLAS experiment at LHC as muon trigger chambers are
reported and discussed.
Since July 2004, about 270 RPC units has been certified at INFN Lecce site
and delivered to CERN, for being integrated in the final muon station of the
ATLAS barrel region.
We show the key RPC characteristics which qualify the performance of this
detector technology as muon trigger chamber in the harsh LHC enviroments.
These are dark current, chamber efficiency, noise rate, gas volume
tomography, and gas leakage.Comment: Comments: 6 pages, 1 table, 9 figures Proceedings of XXV Physics in
Collision-Prague, Czech Republic, 6-9 July 200
MODELING OF THE THERMAL STATE OF MT. VESUVIUS FROM 1631 AD
The last eruptive event at Mt. Vesuvius occurred in 1944 AD, ending a cycle of continuous
eruptive activity started with the sub-plinian event of 1631 AD. The aim of this research is i) to
model the thermal evolution of the volcanic system from 1631 AD up to the present and ii) to
investigate the possible process leading the volcano to the current state of quiescence. A finiteelement
software is employed to solve the time-dependent energy equation and obtain the thermal
field in the volcanic edifice and the surrounding medium. Volcanological, petrological and
geophysical constraints are used to define the crustal structure beneath the volcanic edifice, the
magma supply system active since 1631 AD, and the physico-chemical conditions of magma.
Thermodynamic properties of magma and wall rocks have been evaluated from well-established
thermo-chemical compilations and data from the literature. It is shown that heat transfer due to
magma degassing is required in addition to the heat conduction in order to obtain transient depthtemperature
fields consistent with geochemical observations, high crustal magnetization, and rigid
behavior of the shallow crust as indicated by geophysical data. Surface data of carbon dioxide soil
flux coming out from the Mt. Vesuvius crater are taken to constrain such an additional heat flux. The
agreement between modeled and measured temperatures at the crater since 1944 AD proves the
consistency of the model. It is concluded that the present state of quiescence of Mt. Vesuvius is
mostly a consequence of the absence of magma supply from the deep reservoir into the shallower
system. This allows the cooling of residual magma left within the volcanic conduit and the transition
from continuous eruptive activity to the condition of conduit obstruction. In this scenario, the
hydrothermal system may have developed subsequent to the cooling of the magma within the
conduit. Our findings are a direct consequence of the high concentration of CO2 in the most mafic
Vesuvian magmas: the low solubility of CO2, with respect to H2O, enables a high mass flux of
carbon dioxide through the volcanic edifice. The results of this study are relevant for hazard
assessment at Vesuvius and indicate directions for further investigation, such as the role of the
hydrothermal system on the thermal energy budget of the volcanic system and its relationships with
fluids released by crustal structures likely to host the magmatic reservoir. In general, the role of the
high concentration of carbon dioxide in magmas should be more questioned and investigated when
studying the behavior of volcanic systems, particularly in South Italy volcanoes
Search for new phenomena in high-mass diphoton final states using 37 fb(-1) of proton-proton collisions collected at root(s) = 13 TeV with the ATLAS detector
Searches for new phenomena in high-mass diphoton final states with the
ATLAS experiment at the LHC are presented. The analysis is based on pp
collision data corresponding to an integrated luminosity of 36.7 fb(-1)
at a centre-of-mass energy root s = 13 TeV recorded in 2015 and 2016.
Searches are performed for resonances with spin 0, as predicted by
theories with an extended Higgs sector, and for resonances with spin 2,
using a warped extra-dimension model as a benchmark model, as well as
for non-resonant signals, assuming a large extra-dimension scenario. No
significant deviation from the Standard Model is observed. Upper limits
are placed on the production cross section times branching ratio to two
photons as a function of the resonance mass. In addition, lower limits
are set on the ultraviolet cutoff scale in the large extra-dimensions
model. (C) 2017 The Author(s). Published by Elsevier B.V
Measurements of top quark spin observables in tt events using dilepton final states in root s=8 TeV pp collisions with the ATLAS detector
Measurements of top quark spin observables in tt events are presented
based on 20.2 fb(-1) of root s = 8TeV proton-proton collisions recorded
with the ATLAS detector at the LHC. The analysis is performed in the
dilepton final state, characterised by the presence of two isolated
leptons ( electrons or muons). There are 15 observables, each sensitive
to a different coefficient of the spin density matrix of tt production,
which are measured independently. Ten of these observables are measured
for the first time. All of them are corrected for detector resolution
and acceptance effects back to the parton and stable-particle levels.
The measured values of the observables at parton level are compared to
Standard Model predictions at next-to-leading order in QCD. The
corrected distributions at stable-particle level are presented and the
means of the distributions are compared to Monte Carlo predictions. No
significant deviation from the Standard Model is observed for any
observable
Search for new phenomena in events containing a same-flavour opposite-sign dilepton pair, jets, and large missing transverse momentum in root s=13 TeV pp collisions with the ATLAS detector
Two searches for new phenomena in final states containing a same-flavour
opposite-sign lepton (electron or muon) pair, jets, and large missing
transverse momentum are presented. These searches make use of
proton-proton collision data, collected during 2015 and 2016 at a
centre-of-mass energy root s = 13 TeV by the ATLAS detector at the large
hadron collider, which correspond to an integrated luminosity of 14.7
fb(-1). Both searches target the pair production of supersymmetric
particles, squarks or gluinos, which decay to final states containing a
same-flavour opposite-sign lepton pair via one of two mechanisms: a
leptonically decaying Z boson in the final state, leading to a peak in
the dilepton invariant-mass distribution around the Z boson mass; and
decays of neutralinos (e.g.. (chi) over tilde (0)(2) -> l(+)l(-1)(chi)
over tilde (0)(1)), yielding a kinematic endpoint in the dilepton
invariant-mass spectrum. The data are found to be consistent with the
Standard Model expectation. Results are interpreted in simplified models
of gluino-pair (squark-pair) production, and provide sensitivity to
gluinos (squarks) with masses as large as 1.70 TeV (980 GeV)
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