Particle Detectors Overview
Particle Detectors Overview
Particle Detectors
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Contents
1 Introduction 4
1.1 The aims of particle detectors . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4
1.2 Momentum determination . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4
1.3 Energy determination . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 5
1.4 Spatial resolution . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 5
1.5 Temporal resolution . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 5
1.6 Typical spatial and temporal resolutions for common detectors . . . . . . . . . . . . . . . 5
4 Calorimeters 20
4.1 Electromagnetic versus hadronic calorimeters . . . . . . . . . . . . . . . . . . . . . . . . . 20
4.2 Homogeneous versus heterogeneous calorimeters . . . . . . . . . . . . . . . . . . . . . . . . 20
4.3 Energy resolution . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 21
4.3.1 Electromagnetic calorimeters . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 21
4.3.2 Hadronic calorimeters . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 22
4.4 Typical energy resolutions for some calorimeters . . . . . . . . . . . . . . . . . . . . . . . 22
5 Hermetic detectors 23
5.1 Introduction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 23
5.2 Layout and purpose of layers . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 23
5.3 Propagation of particles through the layers . . . . . . . . . . . . . . . . . . . . . . . . . . 24
6 Case studies 25
6.1 Drift chamber – barrel muon chambers at DELPHI . . . . . . . . . . . . . . . . . . . . . . 25
6.2 Drift chamber with magnetic field – central tracking chamber at ZEUS . . . . . . . . . . . 26
6.3 Sampling calorimeter – uranium-scintillator calorimeter at ZEUS . . . . . . . . . . . . . . 27
6.4 Hermetic detector – Compact Muon Solenoid (CMS) . . . . . . . . . . . . . . . . . . . . . 28
6.5 Ring imaging Čerenkov detector – Super-Kamiokande . . . . . . . . . . . . . . . . . . . . 29
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7 Particle identification 30
7.1 Characteristics of particle events in hermetic detectors . . . . . . . . . . . . . . . . . . . . 30
7.2 Identifying particles from the DELPHI detector at CERN’s LEP collider . . . . . . . . . . 31
7.2.1 e− e+ → e− e+ . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 31
7.2.2 e− e+ → µ− µ+ . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 32
7.2.3 e− e+ → 2 jets . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 33
7.2.4 e− e+ → 3 or 4 jets . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 34
7.2.5 e− e+ → ΛΛ̄ . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 35
7.3 Identifying particles from Super-Kamiokande events . . . . . . . . . . . . . . . . . . . . . 36
7.3.1 Electron events . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 36
7.3.2 Muon events . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 36
7.3.3 Muon decay to electron event . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 37
7.4 Identifying particles from the spark chamber at CERN’s SPS . . . . . . . . . . . . . . . . 37
w.frass@seh.oxon.org
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1 Introduction
1.1 The aims of particle detectors
The aim of a particle detector is to quantify the momenta and discover the identity of the particles that
pass through it after being produced in a collision or a decay - an ‘event’.
The event might be a collision deliberately engineered to occur within the detector leading to many
particles which in turn decay into many more, or it could be a decay that occurs naturally (in the upper
atmosphere, for example), which is then detected on Earth. The exact position in space where the event
occurs is known as the interaction point.
In order to identify every particle produced by the collision, and plot the paths they take - to ‘completely
reconstruct the event’ - it is necessary to know the mass and momentum of the particles. The mass
can be found by measuring the momentum and either the velocity or the energy.
The modern large-scale detectors used today at places such CERN, including ATLAS and LCHb, which
encompass many forms of tracking chambers and calorimeters that completely surround the interaction
point are known as ‘hermetic detectors’.
F = qvB (1)
ma = qvB (2)
v2
m = qvB (3)
r
mv
= qB (4)
r
mv p
Figure 1: A particle with velocity v entering a mag- r= = (5)
qB qB
netic field. In unit time the particle travels a distance
v around the circle and turns through an angle ω. r∝p (6)
The radius is also proportional to the mass-charge-ratio, m/q, so if two particles have the same speed,
and one is half as heavy as the other, but has twice the charge, they will both orbit with the same radius.
Since the magnetic field exerts a force perpendicular to the direction of the particle’s direction, it can do
no work on the particle, hence the particle does not lose energy as a result of this process.
Thus having established the momentum, the energy can be measured by a calorimeter and the mass of
the particle, and hence its identity, deduced.
The direction the particle curves in the magnetic field reveals its charge, since positive and negative
charges curve in opposite directions.
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1.3 Energy determination
Calorimeters rely on energy loss phenomena in order to determine the energy of the particles pass-
ing through them. In the case of detectors built specifically for calorimetry, the energy deposition is
usually in the form of electromagnetic or hadronic showers, however calorimeters exist that exploit com-
pletely different forms of energy loss. In addition, a tracking detector is sometimes also able to provide
information on energy loss.
• The precision with which a tracking detector reports the true location of a particle. The usual
measure of this precision is the square root of the variance of the probability density function that
gives the probability of getting a signal for a particle at x when it has crossed the detector at x0 :
Z 1/2 Z 1/2
σ(x0 ) = (x − x0 )2 P (x, x0 )dx ≈ (x − x0 )2 × r0 (x − x0 )dx (7)
• The ability of a tracking detector to distinguish the signals it receives due to two different particles
passing very close to each other.
Spatial resolution is also significant, albeit slightly less important, in calorimeters. This is because in
large hermetic detectors it is often necessary to associate a particle’s calorimeter hits with the track it
has left in tracking detectors - for this to work, the calorimeter has to be able to report fairly accurately
where the energy was deposited.
The temporal resolution can be influenced by many properties of the detector, not limited to the material
it is made from, the size and the surface of the scintillation counter and the properties of the light guide.
The bubble chamber is now obsolete, but has been included in a few tables for comparative purposes.
1 Source: Table 28.1 of Particle Data Group 2008.
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2 Gaseous ionisation detectors
2.1 Principle of operation
The principle on which gaseous ionisation chambers work is outlined below:
A voltage is applied to the central anode (positive) and the chamber walls / cathode (negative) to create
an electric field between them. When a charged particle passes through the chamber it ionises the gas
molecules inside, along the path it takes, creating negative electrons (anions) and positive ions (cations).
The collection of these charged particles reduces the voltage across the capacitor - this in turn increases
the voltage across the resistor. This ‘pulse’ across the resistor is recorded electronically, registering a hit.
Q = CV (8)
• As mentioned above, a change in the charge causes a change in the voltage:
∆Q
∆V = (9)
C
• The change in charge is equal to the number of electrons collected by the anode. This is related to
the number of ionising events that occur, n, as the charged particle being detected passes through
the gas. If the ionisation products have sufficient energy to cause secondary ionisations, then the
charge due to the primary ionisation events (n × e) must be multiplied by the gas amplification
factor A:
Ane
Pulse height = ∆V = (10)
C
• The gas amplification factor, A, is dependent on the voltage applied.
Many different elements or compounds can be used to fill the chamber2 - but they are always gases
because the ionisation products can move to the relevant electrodes more easily in a gas than they can
in a liquid or solid.
As shown in equation (10), the pulse height is dependent on the number of ion pairs collected by the
anode. However, the number of ion pairs collected varies hugely depending on the applied voltage. So
much so, that the way a detector behaves is different in each of the voltage ranges.
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2.2 Applied detector voltage
The number of ion pairs collected varies hugely as the voltage applied to the detector (see Figure 2) is
increased. The graph below shows two curves, the curve for alpha-particles is higher than the curve for
beta-particles because of the greater number of initial ion pairs an alpha-particle is able to produce due
to its larger mass.
Figure 3: Number of ion pairs collected versus applied voltage in a gaseous ionisation chamber.
Recombination region
In this region, the voltage is insufficient to create an electric field strong enough for collection of all
the ions produced. Instead they drift too slowly towards the electrodes and recombine back to neutral
molecules before they can be collected. Obviously as the voltage is increased - more ions are collected,
but until the saturation value is reached, not all ions will be prevented from recombining. For this reason
gaseous ionisation chambers are not operated at these voltages.
Ionisation region
Somewhere around 100 V a saturation value is reached: the voltage is now sufficient to ensure collection
of all the ion pairs that the charged particle creates. However, the voltage is not yet strong enough to
cause secondary ionisation - there is no gas amplification here, hence there is no rise in the number of
ions collected.
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Proportional region
The voltage in this region produces a large potential gradient near the anode. Gas amplification is now
possible because the electrons produced by ionisation are accelerated up to speeds where they can cause
secondary ionisation - this is a Townsend avalanche. In this region the voltage pulse is proportional
to the amount of ionisation.
As the voltage is increased further, the strength of the electric field causes electrons to be released from
the cathode. This results in the Townsend avalanche spreading along the anode, whilst the positive
ions then tend to remain near where they were created. This reduces the electric field to a point where
further ionisation events are impossible: the number of ions pairs collected begins to level off again. This
is another range of voltages not used for detectors.
Geiger-Müller region
By this point the voltage is so high that once an avalanche is initiated, it continues to spread until gas
amplification becomes impossible due to a build-up of positive ions around the anode forming a dense
shield. Once the threshold has been crossed and the dense shield is formed, no more ions can be col-
lected and the graph reaches the Geiger plateau.
The number of ions required to shield the anode depends on the detector and not the charged particle
passing through it. Therefore both alpha- and beta-particles have the same Geiger plateau because once
the ion shield is in place, no more ionisation events can occur, irrespective of the charged particle under
detection.
Finally, if the voltage is increased further it is so high that once ionisation occurs there is a continuous
discharge of electricity. The Geiger plateau is the last useful range for continuously applied voltages -
anything above this cannot be used for particle detection.
Spark chambers do operate at voltages above those shown on the graph - but there is a single discharge
onto the plates - not a continuous voltage supply.
• Pulse counting ionisation chambers: each individual particle traversing the detector creates
a pulse, which is counted.
• Integrating ionisation chambers: all the pulses add and the integrated total of all the ionisation
events over a period of time is measured. This type is more commonly used.
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Ionisation chambers primarily detect charged particles through their ionisation losses. However they can
also detect neutral photons and neutrons:
• Photons can be detected because the interactions they undergo, namely photoelectric emission,
Compton scattering and pair production, all lead to the production of electrons, which are then
detected in exactly the same way as the electrons resulting from an ionisation event.
• Neutron detection is not possible in an ordinary ionisation chamber because neutrons are not
ionising. However, with the addition of a thin boron coating on the inner chamber walls, or the
use of boron triflouride gas, the following reaction takes place:
10 1 7 4
5 B + 0 n → 3 Li + 2 He + 5 e (11)
The neutron is captured by the boron atom and an energetic alpha particle is emitted along with
some electrons. The alpha particle is heavily ionising - losing all its energy in a just a few centimetres
- allowing the neutron to be detected.
Such ionisation counters are widely used in the nuclear industry. By reducing the volume or decreasing
the pressure inside the chamber, the active-volume is too small to contain the electrons produced by
gamma radiation, so only the alpha-particles due to the presence of neutrons are counted.
Ionisation chambers are not really useful for modern particle physics experiments because they need
heavy ionisation in order to receive a signal, yet fast particles create little ionisation according to (12),
and they have a slower response time than proportional chambers. They do however, have a longer
life-time than both proportional chambers and Geiger-Müller tubes because the gas in these tends to
break down eventually.
The voltage is large enough to collect all the electrons within microseconds. The height of the voltage
pulse in a proportional chamber provides information about the energy of the incident charged particle:
pulse charge number of primary energy deposited by 1
∝ ∝ ∝ ∝ 2 (12)
height collected ionisation electrons the charged particle β
This is the biggest advantage proportional chambers have over other gaseous ionisation detectors - in
addition to tracking, they can provide information on the energy deposited by particles, which can be
used for particle identification. This works because the geometry of the detector is such that the
electric-field is insufficient to accelerate the electrons until they are micrometres from the anode: this
way all electrons generate the same sized avalanche - no matter how far they have drifted before getting
close to the anode.
The energy a particle deposits is, of course, proportional to 1/β 2 according to the Bethe formula. Once
the value of β is known, the energy can be found, if the momentum is deduced from magnetic curvature.
Unfortunately, for every electron there is an ion of chamber gas, which will gain an electron at the
cathode and thus emit a photon. All these emitted photons release electrons from the cathode via the
photoelectric effect, which will create unwanted pulses and could result in a current strong enough to
melt the wire. These photons must be absorbed by a quencher gas, typically carbon dioxide or
an organic molecule such as methane. A typical gas composition for proportional chambers is P-10
comprising 90% argon and 10% methane.
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Spatial dependence of the voltage pulse
• The work done (∆W = Force × distance), by a charge q moving through an electric-field, E is:
Z end
∆W = qE · dr (13)
start
• This change in energy is the source of the voltage pulse, ∆V . Voltage is the energy per unit charge,
therefore the change in energy equals Q × ∆V :
Z end
Q∆V = qE · dr (14)
start
• The total charge a capacitor of capacitance C can store is Q = CV0 , with V0 the applied voltage:
Z end
q
∆V = E · dr (15)
start CV0
• E is sometimes expressed as the gradient of the potential, and in any case is given by Gauss’ law:
Z start
q dV0
Voltage pulse = ∆V = dr (16)
end CV0 dr
• Recall the electric-field is not strong enough to cause an avalanche until the initial electrons are a
small distance from the anode - call this distance λ. Integrating along their paths, it can be shown
that the voltage pulse due to the electrons moving from λ to the anode is small compared to the
pulse due to the ions moving from λ to the cathode: the pulse is almost all due to the motion
of the positive ions.
Time dependence of the voltage pulse
• To find the temporal variation of the voltage pulse, substitute dV0 /dr for the electric field in (16).
• Now integrate (16), in general this time, using a boundary condition to find the constant of inte-
gration. This gives the voltage pulse in terms of r, hereby referred to as ∆V (r).
• The variable of time is introduced by considering the drift velocity. In a proportional chamber
the drift velocity is proportional to the electric-field:
dr
= v = µE (17)
dt
• Substitute for the electric field, E, in (17) and integrate (17) with respect to time; this yields a
new expression for r in terms of t. Now substitute this new expression into ∆V (r) giving ∆V (t).
• For the specific case of concentric cylinders of length l, with an inner cylinder having radius a:
−Q µCV0 t
∆V (t) = ln 1 + t ∆V (t) ∝ ln 1 + (18)
4π0 l π0 a2 t0
• The constant t0 is typically a few nanoseconds and depends on the geometry and ion mobility.
Dead time
• The longer the pulse, the longer the time before an individual wire can be used to detect another
particle - the wire’s dead time. The table below shows the dead time of some common detectors: 3
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2.4.2 Multi-wire proportional chambers (MWPCs)
The detectors discussed so far have primarily been counters - they merely detect the presence of a par-
ticle. The proportional chamber advances this by virtue of the fact the voltage pulse it measures is able
to provide information on the particle’s energy as well.
The multi-wire proportional chamber or MWPC advances this further - instead of having one anode
wire surrounded by a cathode wall or plate, multiple ‘sense wires’ are equidistantly spaced symmet-
rically between two parallel plates. Wire spacings are typically a few millimetres. A nearly uniform
electric-field develops between the cathode plates, distorted only near the sense wires.
Each wire acts as a separate counter - when a charged particle passes through the chamber leaving a
trail of electron-ion pairs, the electrons drift to the nearest wire and cause a voltage pulse. By placing
another such configuration at 90◦ to the first, thus forming a grid, and marking off the wires that produce
a pulse, the path of the charged particle is revealed.
As explained in Chapter 1, applying a magnetic field perpendicular to the direction the particle is trav-
elling in, will cause it to spiral due to the Lorentz force. This will reveal how the particle is charged and
what its momentum is.
A typical gas composition for multi-wire proportional chambers is the ‘magic gas’ mixture comprising
75% argon + 24.5% isobutane + 0.5% freon.
In order to calculate the distance an electron has travelled it is necessary to understand its velocity in
the electric-field. The uniformity of the field must be more carefully controlled than it is in a multi-
wire proportional chamber: to this end, the anode sense wires are alternated with cathode field wires
that ‘correct’ the field distortion caused by the sense wires, restoring uniformity throughout the chamber.
The graph below shows the drift velocities of common drift chamber gases as a function of the applied
electric-field:
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If the average momentum relaxation time is τ , then an electron moving in an electric-field E
experiences a force:
dp mvdrift
F = = = eE (19)
dt τ
Here, vdrift is the drift velocity of the electrons in an electric-field only:
eEτ
vdrift = (20)
m
Drift velocities under electric- and magnetic-fields
The situation becomes more complex upon the application of a uniform magnetic-field. The electrons now
drift at an angle ψ with respect to the electric-field. If the electric- and magnetic-fields are perpendicular:
tan(ψ) = ωτ (21)
The angle ψ is known as the Lorentz angle, with the cyclotron frequency, ω, given by:
eB
ω= (22)
m
In order to prove the relationship in (21), it is necessary to solve the equation of motion for an electron
in both electric- and magnetic-fields. To avoid confusion with the electric-field-only drift velocity, vdrift ,
the symbol u will be used for the electric- plus magnetic-field case.
In addition to the Lorentz force, a particle in a gas filled drift chamber is also subjected to a retarding
force proportional to its velocity −Ku:
du
m = eE + e[u × B] − Ku (23)
dt
The constant K is defined such that τ = m/K. In steady-state (23) reduces to:
e 1 e
E = u + [u × B] (24)
m τ m
Writing out the x, y and z components of the above in a matrix equation gives:
E 1/τ −ωz ωy ux
e x
Ey = ωz 1/τ −ωx uy (25)
m
Ez −ωy ωx 1/τ uz
The ω components are defined according to (22). Solve for the drift velocity, u, by inverting this matrix:
1 + ωx2 τ 2 ωz τ + ωx ωy τ 2 −ωτ + ωx ωz τ 2
ux Ex
τ −ωz τ + ωx ωy τ 2 2 2 2 e
uy = 1 + ω y τ ωx τ + ω ω
y z τ Ey (26)
1 + (ωτ )2 2 2 2 2 m
uz ωy τ + ωx ωz τ −ωx τ + ωy ωz τ 1 + ωz τ Ez
This can be written in a more accessible form with the use of the unit vectors Ê and B̂:
eEτ /m h i
u= 2
Ê + ωτ (Ê × B̂) + (ωτ )2 (Ê · B̂)B̂ (27)
1 + (ωτ )
When Ê is perpendicular to B̂ their scalar product is zero, so the last term vanishes:
eEτ /m h i
u= Ê + ωτ (Ê × B̂) (28)
1 + (ωτ )2
Remember, ψ is the angle the electrons are drifting at with respect to the electric-field, in other words
it is the angle between u and E, readily found from u · E:
eEτ /m h i
u · E = uE cos(ψ) = Ê · E + ωτ ( Ê × B̂) · E (29)
1 + (ωτ )2
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The scalar product of a vector with its own unit vector returns the modulus of that vector (Ê · E = E).
The second term is a triple-scalar-product, eligible for a cyclic-permutation:
eEτ /m h i
uE cos(ψ) = E + ωτ ( Ê × Ê) · B (30)
1 + (ωτ )2
The vector-product of a vector with itself is zero (Ê × Ê = 0), hence the last term vanishes and some
factors of E can be cancelled:
eEτ /m
u = sec(ψ) (31)
1 + (ωτ )2
Since electrons solely under the influence of an electric-field move in the direction of E and the Lorentz
angle is the angle between u and E – ψ is also the angle between u and vdrift :
eEτ /m eEτ
sec(ψ) 2
= cos(ψ) (33)
1 + (ωτ ) m
1
sec(ψ) = cos(ψ) (34)
1 + (ωτ )2
tan(ψ) = ωτ (37)
This has important practical design consequences. For a typical gas the mean free path is 0.1 µm, and
the argon-methane mix in Figure 4 has a drift velocity peaking at 5.5 cm/µs. This gives τ ≈ 0.55 ps.
With a magnetic-field of 1 Tesla, tan(ψ) = 0.1 or ψ ≈ 6◦ . Drift chambers used with magnetic fields are
often structured to follow the Lorentz angle.
If a high-voltage cathode disc is placed at the centre of the chamber an electric-field can be established
between the disc and the end-plates. The electrons that result from ionisation events in the chamber
will drift to the multi-wire end-plates - a typical drift length is around 2 metres. The arrival times of
the electrons at the end-plates determine how far they have travelled and hence the axial (z) coordinate
of the charged particle, thus allowing it to be tracked along its journey through the chamber.
Additionally, a magnetic-field is often applied in the axial direction to minimise the diffusion of the
electrons produced by the ionisation.
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2.4.5 Brief history of improvements to the proportional chamber
a Useful resource at Google Books: Particle Detection with Drift Chambers (W. Blum, W. Riegler & L. Rolandi)
Traditional Geiger-Müller tubes have a window at one end, trapping the noble gas 4 , through which
the charged particle may enter. Geiger-Müller tubes are only really used for nuclear work so are largely
concerned with alpha, beta and gamma radiation. The window is made of either:
• Glass-mantle: thicker window, which is cheaper and stronger. However, alpha particles cannot
penetrate the glass, so are not detected.
• Mica: thinner window, which is more expensive and fragile. But alpha radiation may be detected.
Neutron detection is possible using the boron trifluoride gas techniques discussed in conjunction with
ionisation chambers.
For any given detector working in the Geiger-Müller region, all particles have the same Geiger plateau.
Therefore the same number of ions are collected irrespective of the charged particle passing through the
tube. This means the voltage pulse is the same height for all particles, making particle identification im-
possible. Despite this disadvantage Geiger-Müller tubes do produce many more electrons than detectors
working in the proportional region and are thus more sensitive.
As with all detectors working above the ionisation region a quencher gas is necessary because of the
positive ions produced by gas amplification.
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2.6 Detectors working in the continuous discharge region: spark chambers
Spark chambers (or streamer chambers) are usually filled with helium or neon. They are gaseous
ionisation chambers, but do not have a continuous supply of electricity. Instead a charged particle
will trigger its own detection by passing through a scintillator at either end of the chamber. When
the coincidence unit receives a signal from both of the scintillators’ neighbouring photomultiplier tubes
(PMTs) it triggers the discharge of many kilovolts onto the plates. Meanwhile the particle has left a trail
of electrons and ions in the spark chamber itself. The now highly charged plates will seek to discharge
themselves via the easiest route - in this case along the trail of electrons just left by the charged particle.
Sparks fly between the plates with a loud crack showing the path the particle took.
A more detailed explanation of spark formation is now given. The huge voltage difference across the
plates accelerates the electrons so they are able to cause multiple secondary ionisations; an avalanche
quickly forms. The electrons move to the head of the avalanche, positive ions move to the tail.
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3 Solid state detectors
3.1 Silicon semiconductor detectors
3.1.1 Principle of operation
Most modern particle detectors use silicon detectors as their central tracking detector - the position
resolution possible far exceeds that which is possible in gaseous ionisation chambers:
• An individual detector module comprises silicon that has been doped to form a diode.
• When the module is reverse-biased, a depletion region is set up with an electric-field that sweeps
charge-carriers to the electrodes.
• When a charged particle passes across the silicon strip it will liberate electrons from their atoms
creating electron-hole pairs. This is analogous to a charged particle creating electron-ion pairs
when traversing a gas.
• The electric-field in the depletion region sweeps the new electron-hole pairs to the electrodes where
they are collected and that particular module records a ‘hit’.
• In contrast to gaseous detectors, silicon detectors do not track the charged particle through the
entire body of silicon - instead individual, isolated mm sized strips or µm sized pixels record
hits.
• Those modules that record hits trace out the path followed by the charged particle. The smaller
the modules, the better the spatial resolution: around 5 µm for a 300 µm thick module.
The time taken for collection decreases as the bias voltage is increased. Increasing the voltage beyond
that necessary for complete collection - over-biasing - reduces the collection time further. In a silicon
detector 300 µm thick, electrons are collected in about 10 ns and holes in about 25 ns.
Figure 8: Left: schematic diagram of a silicon detector; Right: an array of silicon detector pixels - those
which detected hits are shown highlighted and trace out the particle’s trajectory..
In constrast to gasesous ionisation detectors, the active material in solid-state detectors is much denser,
therefore every effort is made to make the silicon as thin as possible - otherwise any improvement in
resolution gained by using silicon, is negated by the effects of increased multiple scattering.
Hence the increased spatial resolution possible with silicon detectors (compared to gaseous ionisation
detectors) comes at an increased cost.
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3.1.2 Energy resolution
If the band-gap energy required to promote an electron into the conduction band and create an electron-
hole pair is Egap , the number of electron-hole pairs produced by a particle despositing energy E is:
E
N= (38)
Egap
Assuming a Poisson distribution for the number of electron-hole pairs, the fractional variance of N is:
√
σN N
= (39)
N N
The actual variance is affected by both electronic and lattice excitations. This is accounted for by the
Fano factor, F (FSi ≈ 0.1):
√ r
σN FN F
= = (40)
N N N
This can be used to find the energy resolution by substituting from (38):
r
σE F Egap
= (41)
E E
In actual fact, since silicon is an indirect semiconductor5 , Egap should also include phonon excitation to
provide the necessary momentum change. Taking this into account, at room temperature Egap = 3.67
eV. Therefore a 1 MeV charged particle will produce about 272,000 electrons. This gives σE /E = 0.06%.
However, the energy resolution is dominated by electrical noise and energy loss fluctuations in the
detector, hence the need for expensive cooling and low-noise electronics.
3.2 Scintillators
3.2.1 Principle of operation
A charged particle passing through matter will create electron-ion pairs in a gas and electron-hole pairs
in a semiconductor. In more complex substances however, the energy is manifest in excited molecules.
Those substances in which the molecules de-excite by emiting a photon are known as scintillators.
If a photon excites the molecules of a substance, which then de-excite by emitting a lower energy photon,
the substance is said to fluoresce. Absorption and emission occur over a wide range of photon energies,
which can overlap, leading to unwanted self-absorption. The greater the difference between the main
absorption and main emission energies (the Stokes’ shift), the less the amount of self-absorption.
5 The maxima of the valence band does not have the same k-space momentum as the minima of the conduction band
17
The organic substances used in detectors comprise a mixture of both scintillators and fluors. This is
because typical scintillators emit ultraviolet light which is rapidly attenuated by the scintillator itself
before it can ever be detected. The fluor acts as a wavelength-shifter: absorbing the ultraviolet light
and re-radiating it as blue light (a wavelength at which the scintillator is more transparent). Sometimes
secondary or even tertiary fluors are added to step-down the wavelength in stages.
If the fluor is added in high concentration the distance between the scintillator and the fluor is shorter
than the wavelength of light. In these cases the energy transfer from scintillator to fluor occurs by
dipole-dipole interactions, which are faster than absorption and emission, thus reducing the decay time
by an order of magnitude.
There is a threshold velocity, and hence a threshold momentum below which particles do not radiate.
This threshold is different for different particles. This is the principle of the threshold Čerenkov
detector:
mβc
p = γmv = p (43)
1 − β2
Using the condition for Čerenkov radiation, β = 1/n, gives:
mc/n
pthreshold = √ (44)
1 − n−2
18
In an air filled detector (nair = 1.0003) the threshold for pions is 5 GeV/c, but the threshold for kaons
is 20 GeV/c. Therefore in the range 5 – 20 GeV/c pions radiate but kaons do not, allowing them to be
distinguished. Below 5 GeV/c neither pions nor kaons radiate, and above 20 GeV/c they both radiate.
The detector is therefore only useful in the range 5 – 20 GeV/c.
Modern Čerenkov detectors have 4π coverage of the radiating material with photomultiplier tubes. These
detectors produce rings where the light-cone intersects the PMT-lined wall of the chamber and are known
as Ring Imagining Čerenkov detectors (RICH), see Section 7.3.
3.3.2 Calorimetry
Čerenkov detectors can be used as calorimeters because the amount of light produced is proportional to
the total energy of the incident particle, E0 :
Z track length
Number of emitting
(Amount of light) ∝ dL (45)
0 particles at distance L
The number of particles after N radiation lengths is 2N . Convert the integral over dL to an integral over
dN using the fact that the track length is the number of radiation lengths (L = X0 N → dL = X0 dN ).
The integral’s upper limit is now the number of radiation lengths at which the shower stops, NC :
Z NC
(Amount of light) ∝ 2N X0 dN (46)
0
NC
2N
(Amount of light) ∝ X0 (47)
ln 2 0
X0 NC
(Amount of light) ∝ 2 −1 (48)
ln 2
The critical value of N , namely NC , can be converted into a critical energy. The initial energy E0 is
shared between however many particles there are after N radiation lengths:
E0 E0
EN = → EC = (49)
2N 2NC
This means equation (48) can be re-written as:
X0 E0
(Amount of light) ∝ −1 (50)
ln 2 EC
Finally, since E0 EC :
Energy of
(Amount of light) ∝ (52)
incident particle
19
4 Calorimeters
4.1 Electromagnetic versus hadronic calorimeters
Calorimeters use partial or total absorption of particles and their showers to measure their energy.
Calorimeters are typically composed of small cells aligned along the direction of the incident particle,
stacked up in towers. The alignment of these towers usually varies around the detector in order to
maximise the probability of encompassing the shower at a given angle.
Electrons, photons, and indeed π 0 mesons, which decay into photons, all produce electromagnetic show-
ers. These showers are relatively compact and have a short shower-depth, therefore they are readily con-
tained in a short distance by electromagnetic calorimeters. The size of an electromagnetic shower,
and hence an electromagnetic calorimeter, is governed by the radiation length, X0 .
Hadronic showers are generally much larger and their shape fluctuates hugely from one event to another,
hence hadronic calorimeters are larger than their electromagnetic counterparts. Indeed, the response
is lower and the resolution is worse for hadrons in a hadronic calorimeter compared to electrons of the
same energy in an electromagnetic calorimeter.
Most hermetic detectors use a calorimetry system that comprises both types of calorimeter. In such a
composite calorimeter the electromagnetic calorimeter is always the first layer the particles encounter
because whilst the heavy hadrons can pass through to the hadronic calorimeter beyond, electrons and
photons would never reach their designated calorimeter if the hadronic calorimeter came first.
Although hadrons might start showering in the electromagnetic calorimeter, they can only be fully con-
tained by the hadronic calorimeter. This is where all but the tiny fraction of energy hadrons lost in the
electromagnetic calorimeter, is deposited.
In light of the above, the absorber material in an electromagnetic calorimeter should ideally maximise
the hadronic interaction length (so as many hadrons can pass through with minimal interaction as
possible) and minimise the radiation length (so the electromagnetic shower is fully developed within the
electromagnetic calorimeter). The ratio λ/X0 approximately satisfies: λ/X0 ∝ Z 1.3 . Maximising this
ratio means using high-Z materials like tungsten (Z = 74), lead (Z = 82) or uranium (Z = 92).
The length and width of hadronic showers means The materials suitable for both
Particles hadronic calorimeters have to be of the sampling type, these roles can only be used in
but electromagnetic calorimeters can also be sampling. electromagnetic calorimeters.
20
4.3 Energy resolution
The accuracy with which a calorimeter reports the energy of a particle is usually expressed as a fraction
of the particle’s energy, E, and comprises four separate contributions added in quadrature:
1
Instrumental ∝ E The effect of noise and stray capacitance is This contribution tends to
largely energy independent, hence the rela- dominate at low energies.
tive contribution (σ/E) scales as 1/E.
Systematic constant Systematic errors include calibration er- This contribution usually
rors and non-uniformity of the calorime- sets the limit for perfor-
ter. Non-uniformity at high energies can mance at high energies.
limit accuracy to no-better than 2%. Usu-
ally, some average fraction of the energy
leaks out of the calorimeter as it fails to
completely contain the shower. These scale
with energy, hence the relative contribution
is energy independent.
q
∆E
Sampling ∝ E In sampling calorimeters the sampling fluc- This is only of significance
tuations have to be added, with ∆E the in sampling calorimeters.
energy loss of one particle in one layer.
σ electromagnetic r
1000∆E
≈ 4% (55)
E sampling E
√
Total energy resolution below σ/ E = 1% is easily achieved in homogeneous electromagnetic calorime-
ters. Such results are more difficult to achieve in an electromagnetic sampling calorimeter.
21
4.3.2 Hadronic calorimeters
In hadronic calorimeters the statistical errors result from fluctuations in energy deposition due to energy
loss through non-hadronic mechanisms such as photons and leptons from pion decay and slow neutrons.
These fluctuations that arise in hadronic calorimeters are much larger than the main statistical errors in
electromagnetic calorimeters:
σ hadronic 45%
≈ √ (56)
E statistical E
Compensating calorimeters are hadronic calorimeters with enhancements such as adjusted absorber
layer and active layer widths and U-238 absorbers for slow neutron capture. These calorimeters reduce
the statistical errors by around 20%:
σ compensating 25%
≈ √ (57)
E statistical E
All hadronic calorimeters are sampling, but the contribution to the total energy resolution due to sam-
pling effects is small compared to the statistical errors:
σ hadronic r
1000∆E
≈ 9% (58)
E sampling E
Typical values of energy resolutions for various hadronic calorimeters are given below: 7
22
5 Hermetic detectors
5.1 Introduction
The modern particle detectors in use today in accelerators such as the Large Electron Positron collider at
CERN8 or HERA9 at DESY10 are hermetic detectors. These are detectors designed to cover as much
of the solid angle around the interaction point (IP) as possible – to hermetically encompass it. This is
nearly always accomplished with a cylindrical barrel around the beam-pipe along which the accelerated
particles travel with end-caps sealing in both ends of the barrel. The accelerators and detectors are
often situated underground in order to provide the maximal shielding possible from natural radiation
such as cosmic rays that would otherwise mask the events taking place inside the detector.
• Large magnet: this produces a magnetic field strong enough to curve the tracks of
charged particles in the tracking detector, allowing their momentum to calculated.
• Electromagnetic calorimeter (ECAL): this measures the shower energy of elec-
trons and photons.
Figure 9: ATLAS (A Toroidal LHC ApparatuS) detector at CERN, a transverse slice is shown above.
8 French:
Conseil Europeen pour la Recherche Nucleaire (European Council for Nuclear Research)
9 German:
Hadron-Elektron-RingAnlage (Hadron-Electron Ring Accelerator)
10 German: Deutsches Elektronen Synchrotron (German Electron Synchrotron)
23
5.3 Propagation of particles through the layers
Particles can be identified by their energy loss, curvature in magnetic fields and Čerenkov radiation.
However, the identity of a particle can be significantly narrowed down by simply examining which parts
of the detector it deposits energy in:
• Photons (γ): Neutral photons leave no tracks in the CTD but produce an electromagnetic shower
in the ECAL.
• Electrons and positrons (e− , e+ ): Charged electrons and positrons leave tracks in the CTD
and produce a shower in the ECAL.
• Muons (µ− , µ+ ): Muons leave tracks in all the detectors - they are the only particles to reach
the muon chambers.
• Charged hadrons (p, π ± , K ± ): Charged hadrons leave tracks in all the detectors up to the
HCAL where they shower and deposit all their energy.
• Neutral hadrons (n, KL0 ): Neutral hadrons leave no tracks in any of the detectors and then they
shower in the HCAL. KS0 mesons are not listed here because they decay before ever reaching the
hadronic calorimeter.
A full description of the signature characteristic of all types of particle can be found in Section 7.1. For
now, the above facts are summarised in the diagram below:
Figure 10: Overview of the signatures left in a hermetic detector by detectable particles.
24
6 Case studies
6.1 Drift chamber – barrel muon chambers at DELPHI
Figure 11: Diagram of a single sector showing the relative positions of the three layers in the barrel.
Field-strength: 400 V cm−1 Figure 12: The DELPHI detector. Some of the
muon chamber detectors are visible. These are the
Drift velocity: 46 µm ns−1 long, flat, pieces of aluminium outside the hadron
calorimeter.
Spatial σrφ = 1 mm (drift time)
resolution: σz = 10 mm (delay line)
25
6.2 Drift chamber with magnetic field – central tracking chamber at ZEUS
Figure 13: Diagram of the two types of superlayer within ZEUS’ central tracking chamber.
26
6.3 Sampling calorimeter – uranium-scintillator calorimeter at ZEUS
Hermiticity: 99.7%
σE 18%
Electromagnetic E = √
E
⊕ 1%
energy resolution:
σE 35%
Hadronic E = √
E
⊕ 2%
energy resolution:
σtiming 1.5
Time resolution: E =√ E
⊕ 0.5 ns
for E measured in GeV.
Figure 16: A ZEUS FCAL module.
Figure 17: Wavelength shifter installation of a Figure 18: The ZEUS barrel calorimeter after
central calorimeter module. dismantling had started.
Overview of the three main sections of the calorimeter. Remember, λ is the absorption length:
27
6.4 Hermetic detector – Compact Muon Solenoid (CMS)
Figure 19: The arrangement of the CMS. In the middle, under the so-called barrel there is a man for
scale. (HCAL = hadron calorimeter, ECAL = electromagnetic calorimeter)
Figure 20: A slice of the CMS showing how e± , µ± , hadrons, neutrons and photons traverse the detector.
28
6.5 Ring imaging Čerenkov detector – Super-Kamiokande
Figure 22: View of the Super-Kamiokande detector in the Mozumi Mine in Hida’s Kamioka area.
29
7 Particle identification
7.1 Characteristics of particle events in hermetic detectors
The table below outlines the tracks and shower types expected for a variety of different particle events:
In the ‘Tracks’ column the abbreviations used are: P for Primary vertices in the central tracking chamber,
S for Secondary vertices in the central tracking chamber and µ for vertices in the muon chamber.
30
7.2 Identifying particles from the DELPHI detector at CERN’s LEP collider
The images below are real events from the DEtector with Lepton, Photon and Hadron Identification
(DELPHI) at the Large Electron Positron (LEP) collider at CERN. 11
7.2.1 e− e+ → e− e+
TD TE TS TK TV ST PA
DELPHI Interactive Analysis Act
1 20 0 2 0 0 0
Beam: 45.6 GeV Run: 39265 DAS : 5-Jul-1993 ( 41) ( 22) ( 0) ( 3) ( 0) ( 0) ( 0)
14:21:08 0 0 0 0 0 0 0
Proc: 4-May-1994 Evt: 4754 Scan: 2-Jun-1994 Deact
( 0) ( 2) ( 0) ( 4) ( 0) ( 0) ( 0)
Z
X
Figure 24: e− e+ → e− e+
Detector Observation
Central vertex detectors Two tracks back to back
11 Source: http://delphiwww.cern.ch/delfigs/events/z0ps/z0maxen.html
31
7.2.2 e− e+ → µ− µ+
TD TE TS TK TV ST PA
DELPHI Interactive Analysis Act
26 29 0 2 0 0 0
Beam: 45.6 GeV Run: 26154 DAS : 25-Aug-1991 ( 28) ( 29) ( 0) ( 2) ( 3) ( 0) ( 0)
21:36:22 0 0 0 0 0 0 0
Proc: 1-Oct-1991 Evt: 1417 Scan: 19-Feb-1992 Deact
( 0) ( 2) ( 0) ( 2) ( 0) ( 0) ( 0)
Z
X
Figure 25: e− e+ → µ− µ+
Detector Observation
Central vertex detectors Two tracks back to back
32
7.2.3 e− e+ → 2 jets
TD TE TS TK TV ST PA
DELPHI Interactive Analysis Act
14 72 0 17 0 0 0
Beam: 45.6 GeV Run: 26154 DAS : 25-Aug-1991 ( 93) (133) ( 0) ( 23) ( 18) ( 0) ( 0)
21:47:02 0 0 0 0 0 0 0
Proc: 1-Oct-1991 Evt: 3018 Scan: 19-Feb-1992 Deact
( 0) ( 13) ( 0) ( 23) ( 12) ( 0) ( 0)
Z
X
Detector Observation
Central vertex detectors Two narrow jets in opposite directions
33
7.2.4 e− e+ → 3 or 4 jets
TD TE TS TK TV ST PA
DELPHI Interactive Analysis Act
1 207 0 26 0 0 0
Beam: 45.6 GeV Run: 26154 DAS : 25-Aug-1991 (158) (207) ( 0) ( 40) ( 0) ( 0) ( 0)
21:37:20 0 0 0 0 0 0 0
Proc: 1-Oct-1991 Evt: 1580 Scan: 27-May-1994 Deact
( 0) ( 6) ( 0) ( 27) ( 0) ( 0) ( 0)
Z
X
Detector Observation
Central vertex detectors A total of 21 different particles seen
34
7.2.5 e− e+ → ΛΛ̄
+
+ ++ +
+
+
+ +++
+
++ +
+ +
++++ +
+ +
+
O + +
+
+
+
+
+ +
+
+
Figure 28: e− e+ → Λ Λ̄
In this event there is a high momentum Λ Λ̄ pair with a small rapidity difference. The lambdas are shown
as dashed lines, the outgoing pions as red solid lines and the protons as blue ones. Although there were
no track elements reconstructed in the inner detector (intermediate precision tracking) for the Λ that
decayed within it (at a radius of 17.9 cm), the vertex has been reconstructed.
The tracks belonging to the other Λ decaying at a radius of 4.4 cm have three associated vertex detector
hits.
Three other tracks which are very close to the two lambdas have been erased to make the lambda vertices
easier to see.
35
7.3 Identifying particles from Super-Kamiokande events
The colours in the images 12 below represent the time of arrival of light to individual photomultiplier
tubes (PMTs). Short wavelengths (violet and blue) correspond to early arrival times and long wave-
lengths (orange and red) to late arrival times. A window on the time of light of 30 ns has been applied
to eliminate noise and scattered reflected light. The histogram on the right shows the time charge dis-
tribution before the applying the window on the time of flight. The size of a given square representing
a PMT corresponds to the amount of observed light. There is a maximum size such that squares are
always smaller than the distance between PMTs.
7.3.1 Electron events
The fuzzy ring with all signals received at
roughly the same time (the ring is more or less
all the same green colour) is an electron event.
36
7.3.3 Muon decay to electron event
The mean lifetime of a muon is around 2 µs.
Since PMTs can record on the nanosecond scale,
muons could be observed to decay into electrons
and neutrinos according to: µ → e− + ν̄e + νµ .
Figure 32: A proton-antiproton interaction at 540 GeV observed using a spark chamber at CERN’s Super
Proton Synchrotron (SPS) facility in 1982. The identity of the particles produced is anyone’s guess.
37
References
Gaseous ionisation detectors
Data sources: D. Green, The Physics of Particle Detectors (Cambridge University Press, 2000)
W. Blum, W. Riegler & L. Rolandi, Particle Detection with Drift Chambers (Springer-Verlag, 2008)
http://ikpe1101.ikp.kfa-juelich.de/briefbook_part_detectors/PH14pp.html
Spark chambers
Data source: http://www.ep.ph.bham.ac.uk/general/outreach/SparkChamber/text4h.html
Hermetic detectors
Data source: http://www.lancs.ac.uk/users/spc/teaching/py364/introduction.html
38