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Adriana Vásquez-Ramírez

Publications and source records attributed to Adriana Vásquez-Ramírez.

3 recordsLinked to original sources

The ARTI Framework: Cosmic Rays Atmospheric Background Simulations

ARTI is a complete framework designed to simulate the signals produced by the secondary particles emerging from the interaction of single, multiple and even, the complete flux of primary cosmic rays with the atmosphere. These signals are simulated for any particle detector located at any place (latitude, longitude and altitude), including the real-time atmospheric, geomagnetic and detector conditions. Formulated through a sequence of codes written in C++, Fortran, Bash and Perl, it provides an easy-to-use integration of three different simulation environments: magnetocosmic, CORSIKA and Geant4. These tools evaluate the geomagnetic field effects on the primary flux, the atmospheric showers of cosmic rays and the detectors' response to the secondary flux of particles. In this work, we exhibit the usage of the ARTI framework by calculating the total expected flux of signals at eight selected sites of the Latin American Giant Observatory, a cosmic ray Observatory located in Latin America covering a wide range altitudes, latitudes and geomagnetic rigidities. ARTI also calculates the flux of signals expected during the sudden occurrence of a gamma-ray burst or the flux of energetic photons originating in steady gamma sources. It also compares these fluxes with the expected background to detect these phenomena in a single water Cherenkov detector deployed in high altitude sites. Even more, by using ARTI, it is possible to calculate in a very precise way the expected flux of high energetic muons and other secondaries on the ground and to inject it over a geological structure for muography applications.

astro-ph.IM↗

Calibration and first measurements of MuTe: a hybrid Muon Telescope for geological structures

In this work, we describe the calibration and first measurements in the commissioning of MuTe, a hybrid Muon Telescope with two subdetectors --a scintillator hodoscope and a Water Cherenkov Detector (WCD)-- for imaging the inner structures of Colombian volcanoes. The hodoscope estimates the trajectories of particles impinging on the front and rear panel, while the WCD acts as a calorimeter for the through going charged particle. MuTe combines particle identification techniques so as to discriminate noise background from data. It filters the primary noise sources for muography, i.e., the EM-component ($e^{\pm}$) of Extensive Air Showers (EAS) and scattered/upward-coming muons. The WCD identifies Electrons/positrons events by their deposited energy identifies, while scattered and backward muons are rejected using a pico-second Time-of-Flight(ToF) system. Muon generated events were found in the deposited energy deposited range of ($144$MeV$ < E_d <$ 400MeV), represent only about the 40$\%$ of the WCD-hodoscope acquired events. The other 60$\%$ of data is composed by ($e^{\pm}$) events under 144 MeV and multiparticle events above 400 MeV. Subsequently, low-momentum muons ($<$ 1 GeV/c), which are scattered by the volcano surface, measures a ToF $>$ 3.3 ns for traversing one meter length.

physics.ins-det↗

Convection and cracking stability of spheres in General Relativity

In the present paper we consider convection and cracking instabilities as well as their interplay. We develop a simple criterion to identify equations of state unstable to convection, and explore the influence of buoyancy on cracking (or overturning) for isotropic and anisotropic relativistic spheres. We show that a density profile $ρ(r)$, monotonous, decreasing and concave , i.e. $ρ' < 0$ and $ρ'' < 0$, will be stable against convection, if the radial sound velocity monotonically decreases outward. We also studied the cracking instability scenarios and found that isotropic models can be unstable, when the reaction of the pressure gradient is neglected, i.e. $δ\mathcal{R}_p = 0$; but if it is considered, the instabilities may vanish and this result is valid, for both isotropic and anisotropic matter distributions.

gr-qc↗