Study of Cosmic Rays
Profgesor: Mario Edoardo Bertaina Students: Morari Eugen Gramă Vasile
Study of Cosmic Rays Profgesor: Mario Edoardo Bertaina Students: - - PowerPoint PPT Presentation
Study of Cosmic Rays Profgesor: Mario Edoardo Bertaina Students: Morari Eugen Gram Vasile Objectives 1 What are cosmic rays? Origins of Cosmic Rays & Compositjon 2 3 3 Scintjllators & Photomultjplyers CORSIKA (COsmic Ray
Profgesor: Mario Edoardo Bertaina Students: Morari Eugen Gramă Vasile
What are cosmic rays?
1 2 3 3
CORSIKA (COsmic Ray SImulatjons for KAscade)
4 4
Measurement chain (ADC, TDC, DISCRIMINATOR)
5
Origins of Cosmic Rays & Compositjon Scintjllators & Photomultjplyers
6
Efjcience dependence
Results & Conclusions
7
distant galaxies. Upon impact with the Earth's atmosphere, cosmic rays can produce showers of secondary partjcles that sometjmes reach the surface.
Of primary cosmic rays, which originate outside of Earth's atmosphere, about 99% are the nuclei of well-known atoms (stripped of their electron shells), and about 1% are solitary electrons (similar to beta partjcles). Of the nuclei, about 90% are simple protons (i.e., hydrogen nuclei); 9% are alpha partjcles, identjcal to helium nuclei; and 1% are the nuclei of heavier elements, called HZE ions. A very small fractjon are stable partjcles of antjmatuer, such as positrons or antjprotons. The precise nature of this remaining fractjon is an area of actjve
alpha partjcles has failed to detect them.
EAS – array - roof
SCINT - MTEL
Measurement chain
The signal coming from each detector is taken via cables to the reading electronics
the floor of the building; the signal then passes into an amplifier which has two simplified
and is simultaneously split; the first signal is discriminated and is in turn split into two signals,
which the first is delayed and provides the stop of the TDC, while the second is sent to the
Input: analog signal Discrimination threshold Output: logic signal when the threshold is exceeded
Measure chain: TDC
Time to digital converter
Measure the differences between the arrival times
From these we get the direction of arrival
Measure the charge of analog signals in time given by a "gate" (logic signal)
It tells us "how big" is a signal, Proportional to n. of particles that pass through the scintillator
because it has been observed that a delay equal to 1 ns corresponds to 4 channels on the TDC spectrum.
removal of signal cables and relative connecters and a first comparison was made between the average TDC values
to 15 ns and are connected to one another by means of conectors, each furnishing a delay equal to 0,5 ns.
(Time to Digital Converter): determines the tjme interval between two signal pulses (start and stop signal). The measurement is started and stopped when the rising or falling edge of a signal exceeds a certain threshold
calibratjon procedure consists in introducing a known delay to the start or stop signal using a cable whose length determines a signal delay of 15 ns (travel tjme of 5 ns / m for 3 m)
response is verifjed by applying increasingly large delays to the stop signal (from 3ns to 41 ns)
gradually connectjng difgerent cables using I- connectors.
value, 1000 events were acquired
Angular distribution of the beam according to the angle θ
The swarm incidence directjons can be derived from the data
The angular distributjon follows the following law: y = p0sin (θ) cos (θ) and -p1 / cos (θ) p0 is proportjonal to the number
p1 = x0 / λ x0 = radiatjon length defjned as the average distance in which a partjcle remains with an energy equal to 1 / e. λ = average thickness of the atmosphere crossed by the partjcle.
Angular distribution of the beam according to the angle Φ
hypothesis of isotropic irradiatjon.
every directjon (Φ), while the inclinatjon (θ) of the swarm with respect to the vertjcal follows a well-defjned distributjon.
From the fjgure we can see that these events are distributed in a rather isotropic way around the point of coordinates L (½, ½, 0) The distributjon obtained is in line with that expected around the central detector There is a slight anisotropy due to: 1) the 5 statjons in concrete do not form a perfect square; 2) the scintjllator 2 is not very effjcient; 3) the scintjllator 5 operates at a higher voltage than that set during the data socket
the scintjllators, it will produce an electrical pulse from each.
assume that these “coincidences” have been produced by a charged partjcle passing through scintjllators.
been detected.
passed through the fjve scintjllators in a given tjme.
property of luminescence, when excited by ionizing radiatjon. Luminescent materials, when struck by an incoming partjcle, absorb its energy and scintjllate, (i.e. re-emit the absorbed energy in the form of light).Sometjmes, the excited state is metastable, so the relaxatjon back down from the excited state to lower states is delayed (necessitatjng anywhere from a few nanoseconds to hours depending on the material): the process then corresponds to either one of two phenomena, depending on the type of transitjon and hence the wavelength of the emitued optjcal photon: delayed fmuorescence or phosphorescence, also called afuer-glow.
class
vacuum tubes, and more specifjcally vacuum phototubes, are extremely sensitjve detectors of light in the ultraviolet, visible, and near-infrared ranges of the electromagnetjc spectrum. These detectors multjply the current produced by incident light by as much as 100 million tjmes (i.e., 160 dB), in multjple dynode stages, enabling (for example) individual photons to be detected when the incident fmux of light is low.
CORSIKA (COsmic Ray SImulatjons for KAscade)
CORSIKA is a program for detailed simulatjon of extensive air showers initjated by high energy cosmic ray partjcles the partjcles are tracked through the atmosphere untjl their energy decreases below a certain threshold (because of reactjons with the air nuclei or decay) into this program all the known processes that infmuence physical parameters of a shower are included
Lateral distribution of a single event (KASCADE- Grande)
The sum of the last triggers is: 0.75 events/min
We have seen that charged partjcles fmy from the universe into our atmosphere where they collide with air molecules producing air showers. We have also seen how measuring the secondary partjcles gives informatjon about the primary partjcle and how special relatjvity explains that briefmy living partjcles can stjll reach the earth because of their slow running proper