# Tracking in a nutshell

Track reconstruction is the process to recover the properties of a charged particle from a set of measurements caused by the interaction with some form of sensitive detector. The goal is to find which measurements are likely to have been caused by which particle, to group them accordingly, and to estimate the associated trajectory. Such charged particle trajectories form the basic input to the majority of higher-level reconstruction procedures in many cases.

This section provides a high-level view of a track reconstruction chain, and is largely based on 1. It gives an overview of the basic building blocks conceptually, and also connects these building blocks with the concrete implementations in the core ACTS library, where available.

## Charged particle detection

The first step in the chain to reconstruct charged particles is their detection using sensitive elements. Charged particle detection can be achieved in a variety of ways with very different technologies. It can be achieved by measuring the interaction of charged particles with matter. When this occurs, the interacting particle typically ionizes the surrounding material. Particle detectors make use of this fact by converting the resulting charge into a measurable signal in various ways.

A very common electronic detection approach is the use of semiconducting
particle detectors, often made of silicon. When a charged particle traverses
such a sensor, it ionizes the material in the depletion zone, caused by the
interface of two different semiconducting materials. The result are pairs of
opposite charges. These charge pairs are separated by an electric field and
drift toward the electrodes. At this point, an electric signal is created
which can be amplified and read out. By means of segmentation, the measured
signal can be associated with a location on the sensor. Silicon sensors are
usually segmented in one dimension (*strips*) or in two dimensions
(*pixels*) (see Fig. 2).

## Track parametrization

To express the properties of a particle’s trajectory, a choice of parameters has to be made. The parameters need to express all the relevant quantities of interest. In the presence of a magnetic field, which affects charged trajectories, the global position and momentum, as well as the charge are needed to fully specify the particle properties. In addition, a time parameter can be included. Apart from the global reference frame, track quantities often need to be represented with respect to a surface. This can be achieved with a parametrization like

although other parameter conventions exist as well. Fig. 3 illustrates this choice of parameters. \(l_0\), \(l_1\) are the local coordinates of the corresponding surface, \(\phi \in [-\pi,\pi)\) and \(\theta \in [0,\pi]\) are the angles in the transverse and longitudinal direction of the global frame, expressed with respect to the current location along the trajectory, as indicated in Fig. 3 (b). \(\theta\) is the polar angle relative to the positive \(z\)-axis, and \(\phi\) is the azimuth angle in the transverse plane. Finally, \(q/p\) combines the charge of the particle with the inverse momentum. In Fig. 3 (a), the global momentum vector \(\vec p\) is shown, which can be recovered from the parameters \(\vec x\) using \(\phi\), \(\theta\) and \(q/p\).

Aside from the nominal quantities captured in \(\vec x\), the related uncertainties and correlations need to be taken into account as well. They can be expressed as a \(5\times 5\) covariance matrix like

Here, \(\text{cov}(X,Y)\) is the covariance of variables \(X\) and \(Y\), while \(\sigma^2(X)\) are the regular variances. As the covariance matrix \(C\) is symmetric, only the upper right half is shown in the matrix above. The uncertainties associated with the local position, as well as the momentum direction are indicated in Fig. 3 (a) as an ellipse and a cone around the momentum vector \(\vec p\), respectively.

## Particle propagation

Tip

A dedicated description of the ACTS implementation of particle propagation can be found here.

A central part of track reconstruction is the ability to calculate the trajectory
of a charged particle, given its properties at a given point. This process,
called *particle propagation* or *extrapolation*, is used to predict a
particle’s properties after it has travelled a certain distance. In many cases,
the projected intersection with various types of surfaces is desired. The
trajectory of a charged particle is governed by the magnetic
field through which it travels, as well as any
material effects. In case of a homogeneous magnetic field,
and in the absence of material interaction, the particle follows a helical
trajectory. Such a helix can be calculated purely analytically, although
intersections require numerical methods nevertheless.

Often, magnetic fields are not homogeneous, however. In the presence of such changing fields, the corresponding differential equations of motions need to be solved using numerical integration techniques.

### Numerical integration

In ACTS, numerical integration is done using the *Runge-Kutta-Nyström* (RKN) method.
Commonly used in the variant at fourth order, the RKN method describes how to calculate a
solution to an initial value problem that can be formulated generically like

where \(y_0\) refers to the initial value of \(y\) at \(t_0\), and \(f(t,y)\) is the functional form describing the dynamics. The method then successively approximates the analytical solution \(y(t)\) in a stepwise fashion. At each step \((t_n, y_n)\), the goal is effectively to approximate the next step \(y(t_{n+1})\). Using a step size \(h\), the algorithm evaluates the function \(f\) at four points \(k_{1-4}\):

Looking at Fig. 5, the meaning of these four points in relation to the step size \(h\) can be understood. \(k_1\) is the derivative at the current location, \(k_{2,3}\) use \(k_1\) and \(k_2\) respectively to calculate two envelope derivatives at \(h/2\) and \(k_4\) uses \(k_3\) to make an estimate of the derivative at \(h\). Combining \(k_{1-4}\), \((t_{n+1},y_{n+1})\) can be calculated as the approximation of \(y(t_{n+1})\) like

by effectively averaging the four derivatives. It is apparent that the step size crucially influences the accuracy of the approximation. A large step size weakens the approximation, especially if the magnetic field changes strongly. On the other hand, a too small step size will negatively affect the execution time of the algorithm.

The Runge-Kutta-Nyström method from above can be adapted to handle second order differential equations, as is needed for the equations of motion in question,

with the global position \(\vec r\), the path element \(s\), the normalized tangent vector \(\vec T\) and the magnetic field \(\vec B(\vec r)\) at the global position. A slight modification of \(k_{1-4}\) is also required, incorporating the first derivative of \(f(s, \vec r, \vec r')\), finally leading to

A strategy exists to dynamically adapt the step size according to the magnetic field strength, with the definition of a target accuracy that the algorithm tries to achieve. Here, the step size \(h\) will successively be decreased and the approximation recalculated until the accuracy goal is achieved. Even with these additional calculations, the approach is still preferable over a consistently low step size.

### Covariance transport

Aside from the prediction of the track parameters at a given path length, a key ingredient to many dependent applications are the uncertainties in the form of the associated covariance matrix \(C\). Conversions between covariance matrices \(C^i\to C^f\) can generally be achieved like

using the Jacobian matrix

between initial and final parameters \(\vec x^i\) and \(\vec x^f\). The task therefore becomes calculating the necessary Jacobians to achieve correct transformation.

One part is the transformation between different coordinate systems, but at the same location along the trajectory. For this purpose, generic Jacobians can be calculated between each coordinate system type, and a common coordinate system. The common coordinate system used for this purpose is the curvilinear frame, which consists of the global direction angles, and a plane surface located at the track location, with the normal of the plane surface aligned with the track momentum. By using Jacobians to the curvilinear frame and the corresponding inverse matrices, conversions between any two coordinate systems can be performed.

The second part is the calculation of the evolution of the covariance matrix during the propagation between surfaces. To this end, a semi-analytical method which calculates the effective derivatives between two consecutive RKN steps can be used. By accumulating the Jacobian matrices calculated for each step, the effective Jacobian between the starting point and the destination can be obtained.

## Material effects

Charged particles interact with matter as they pass through it. Since particle detectors inevitably consist of some form or material, this effect cannot be completely avoided. By building tracking detectors as light as possible, and arranging passive components, such as services and support structures carefully, the material a particle encounters before being measured can be reduced. Charged particles traversing any form of matter undergo elastic and inelastic interactions with the atomic structure of the material, depending on the particle properties.

In elastic interactions, the particle does not lose a significant amount of energy, while its trajectory is affected. Fig. 6 shows a sketch of the way multiple Coulomb scattering affects the direction of a particle trajectory. In addition, a shift in the transverse plane relative to the incident direction can occur. As the scattering events occur in statistically independent directions, the means of both the deflection and offset tends toward zero as the number of scatters increases. Therefore, in the numerical particle propagation, this can be accounted for by simply increasing the uncertainties associated with the direction, depending on the amount of material encountered.

On the other hand, there are interactions during which the particle loses some of its energy. Relevant processes here are ionization, as well as bremsstrahlung for light particles like electrons. For hadronic particles, hadronic interactions with the nuclei of surrounding material is another process of interest. In such hadronic interactions, the incoming particle often disintegrates, and does not propagate further. Since the size of ionization losses only fluctuates to a small degree for thin layers of material, they can usually be accounted for by reducing the trajectory energy correspondingly. For bremsstrahlung, where fluctuations are much larger and the effect cannot be modelled adequately with a Gaussian distribution, dedicated techniques are needed (see Gaussian Sum Filter (GSF)).

Two main approaches are implemented in ACTS. The first approximates the material interaction by using a description that averages the real material onto thin surfaces across the detector (more on this in Geometry and material modelling). When the propagation encounters such a surface, it retrieves the material properties, and executes parametrized modifications to the particle properties and uncertainties. In the second approach, material effects are continuously incorporated during propagation, rather than at discrete locations. The latter approach is especially suited for propagation through volumes of dense material, where the discretization of the material distribution will not work as well.

## Geometry and material modelling

Tip

A dedicated description of the ACTS implementation of the tracking geometry model can be found here.

A detailed model of the geometry of an experiment is required for tracking. In many cases, external information is needed to associate a sensitive element with a position and rotation in the laboratory frame. In case of silicon sensors, the intrinsic information captured by the sensor is restricted to the measurement plane. Using a transformation matrix, this local measurement can be turned into a global one.

Full simulation using tools like Geant4 are frequently used in HEP.
It includes its own geometry
description framework. For the precise simulation of particle interactions
with the detector, this geometry modelling
is highly detailed. Even very small details of the
physical hardware can be crucial, and are often included in the geometry
description. An example for this are readout chips on silicon sensors, or cooling
elements. Fig. 7 (a) shows a sketch of such a detailed
geometry description. Shown as an example is a *layer* of silicon
sensors in a barrel configuration. The green rectangles represent the actual
sensitive surfaces, while other elements include cooling, readout and other components.

In the majority of cases in track reconstruction, this detailed geometry is unnecessary. During track reconstruction, the aforementioned associated information needs to be accessible for measurements, so all sensitive elements need to be included in some form. Passive elements, on the other hand, are only required to factor in material interaction effects (see Particle propagation). Moreover, the fully detailed geometry comes at the disadvantage of introducing significant overhead during navigation. In this process, an algorithm attempts to figure out which elements the particle propagation needs to target, as the trajectory is likely to intersect them. With a geometry description this precise, the navigation process becomes a significant performance bottleneck.

As a compromise between modelling accuracy and performance, ACTS uses a simplified geometry model. It focusses on the sensitive elements, which are strictly needed, while passive elements are discarded from the explicit description and approximated. Fig. 7 (b) shows such a simplified geometry. Here, the sensitive elements are still shown in green, and other elements are greyed out, indicating that they are discarded. The sensitive elements are then grouped into layers, as sketched in Fig. 8. How exactly the grouping occurs depends on the concrete experiment geometry. In some cases, the layers have the shape of cylinder surfaces with increasing radii. This example is shown in the figure in the transverse plane at radii \(r_{1,2,3}\). In the endcaps, where modules are often arranged on disks, these are used as the layer shape. An illustration of endcap disk layers can be found in Fig. 9, where six disks are located at six distinct positions in \(\pm z_{1,2,3}\), and shown in different colors.

During particle propagation, the navigation makes use of this layer system. Each layer contains a binned structure, which maps a bin to a set of sensitive surfaces that overlap with the bin area. This is illustrated in Fig. 10, where the left picture shows the sensitive surface structure of an exemplary endcap disk. The picture on the right overlays the binning structure that can be used to enable fast retrieval of compatible sensitive surfaces. By performing a simple bin lookup, the navigation can ascertain which sensors it needs to attempt propagation to.

Furthermore, layers are grouped into volumes. Each volume loosely corresponds to a region of the detector. Volumes are set up such that their boundary surfaces always touch another volume. An exception to this is the outermost volume. Each volume’s boundary surfaces store which volume is located on their other side, essentially forming portals between the volumes. This glueing enables the geometry navigation between volumes. When the propagation has finished processing a set of layers, it attempts to target the boundary surfaces. Once a boundary surface is reached, the active volume is switched, and the next set of layers is processed.

Care has to be taken to correctly model the passive material, that is
initially discarded with non-sensitive elements. For the material effects to
be correctly taken into account during particle propagation, the material is
projected onto dedicated material surfaces. These material surfaces are
spread across the detector geometry. Each layer is created with two
*approach surfaces* on either side. Their distance can be interpreted as
the thickness of the layer in question. Examples of these approach surfaces
can be found in Fig. 7, at the inner and outer radius.
Approach surfaces, and the boundary surfaces between volumes mentioned before,
are candidates to receive a projection of the surrounding material.
Additional artificial material layers can also be inserted to receive
projected material.

The projection procedure (see Material and Howto run the material mapping and validation) works by extrapolating test particles using the fully detailed simulation geometry. During the extrapolation, the material properties of the geometry are sampled in small intervals. Subsequently, the same test particle is extrapolated through the tracking geometry. All material samples are then assigned and projected onto the closest material surface. Finally, the projection is averaged. The exact number and placement of the material surfaces has to be optimized to yield a sufficiently accurate representation of the inactive material in the detector.

The numerical integration uses these projected material surfaces. Whenever such a surface is encountered in the propagation, the material properties are retrieved, and the corresponding modifications to the trajectory are executed. In case material is supposed to be integrated in a continuous way (as mentioned in Particle propagation), volumes can also store an effective volumetric material composition, which is queried by the numerical integration when needed. As the actual physical location of the detection hardware can vary over time, possible misalignment of the sensors needs to be handled correctly.

## Clustering

Tip

See Clustering for information of the implementation of clustering in the core library.

The actual track reconstruction procedure itself starts with the conversion of
raw inputs that have been read out from the detector. In case of silicon
detectors, the readout can either be performed in a binary way, only recording
which segments fired, or the amount of charges measured in the segment can be
recorded, e.g. via *time-over-threshold* readout. In all cases, the readout is
attached to an identifier uniquely locating the segment on the corresponding
sensor.

As a next step, these raw readouts need to be *clustered*, in order to
extract an estimate of where particles intersect with the sensor. The general
strategy of clustering algorithms follows the Connected Component Analysis (CCA)
approach, where subsets of segments are successively grouped into clusters.
In case of the Pixel detector, this clustering occurs in two dimensions,
corresponding to the segmentation of its sensors. Here, the CCA can
either consider all eight surrounding pixels as neighboring a central one, or
only consider the four non-diagonal ones, as shown in
Fig. 11. The figure only shows the simplest possible
cluster starting from the central pixel. In reality, the CCA will iteratively
continue from the pixels on the cluster edges.

Subsequently, the effective cluster position needs to be estimated. Multiple factors play a role here. First of all, the average position of the cluster can be calculated either using only the geometry position of the segments,

or be weighted by the charge collected in each segment:

Here, \(\vec l_i\) is the local position of the \(i\)-th segment while \(q_i\) is its charge.

An illustration of the clusterization can be found in Fig. 12, where a pixel sensor is shown to be intersected by a charged particle, entering on the lower left and exiting on the top right. Three cells shown with a red frame receive energy from the particle, but the amount is under the readout threshold. Four other cells receive energy above the threshold and are read out. The clustering will then group these four cells into a cluster, and subsequently estimate the cluster position based on the energy deposited in the cells. In case no charge information is not available for a given detector, the calculation is purely geometric.

Another factor that needs to be accounted for is the drift direction of the
created charges. In addition to the collection field of the sensor itself,
the surrounding magnetic field modifies the drift direction by the
*Lorentz-angle* \(\theta_\text{L}\). Depending on the field strength, this
additional angle can cause segments to be activated that would otherwise not
be geometrically within reach of the charges. Other effects, such as the fact
that the modules are not perfectly flat, as the geometry description assumes,
or cross-talk between readout channels, also play a role at this stage.

In the presence of high event activity, particle intersections on single sensors can be close enough to one another to result in clusters that are not clearly separated from each other. This circumstance can be somewhat mitigated by allowing tracks to share clusters with other particles, which comes at the price of allowing duplicated tracks to some extent. Additionally, merged clusters typically feature worse position resolution, which manifests itself since it negatively affects the final fit of the track.

## Spacepoint formation

The basic input to most forms of pattern recognition algorithms for tracking are space points, which need to be assembled from the raw measurements. To this end, the raw measurements are combined with information provided by the geometry description, such as the location and rotation of the sensors. In this way, the locations, which are restricted to be local to the sensor surfaces intrinsically, can be converted into three dimensional points in space. See Spacepoint formation for a description of the implementation of spacepoint formation in the core library.

Fig. 13 shows an illustration of the information that is consumed for a pixel measurement. Shown are three clusters on a sensor, which are caused by three tracks intersecting it. The corresponding cluster positions are indicated as well, and can be converted to global positions using the inverse of the global-to-local transformation matrix, that is provided by the geometry description.

In strip detectors, on the other hand, only a single dimension is segmented, and an individual measurement is therefore only constrained in one direction on the surface. However, usually the strip modules are mounted in pairs, with a stereo angle rotation between the pairs. To form global space points, measurements from both sensors of a pair need to be combined. Due to the stereo angle, a two dimensional location on the orthogonal projection plane relative to the two parallel pairs can be found. Using the global transformations of the pair, the combined measurement location can be converted to global coordinates. If multiple measurements are located on a stereo pair of strip sensors, there exists an ambiguity on how to combine strips to form space points, which has to be resolved.

## Seeding

The next step after space point formation is pattern recognition, which be implemented in various ways. Global methods exist which attempt to cluster space points, such as conformal mapping. In this approach, the space points are transformed into a feature parameter space that reveals patterns for hits belonging to the same track. In the specific example of a Hough transform, a parameter space \(\left(\phi, q/p_\mathrm{T}\right)\) is used. As a result, each space point is effectively transformed into a line, as a series of combinations of these parameters would lead to the same space point. The lines from a set of space points of a single track will intersect in one common area. Such an intersection can be used to identify which space points originate from the same track. However, this task grows in complexity as detector activity increases and is susceptible to material effects. See Track Seeding for a description of the seeding implementation in the core library.

Another group of approaches is the one of seeding and track following. These algorithms differ from the global ones in that they evaluate individual combinations of space points, and successively explore the events. One algorithm from this group is the cellular automaton that iteratively forms chains of space points going from one layer to the next.

The main approach in ACTS is an algorithm that operates on coarse subdivisions of the detector is used. This seeding algorithm attempts to find triplets of space points from increasing radii which are likely to belong to the same track. It achieves this by iterating the combinatorial triplets and successively filtering them. Filtering is performed based on the momentum and impact parameters, which the algorithm attempts to estimate for each triplet.

Under the assumption of a homogeneous magnetic field along the \(z\)-axis, charged particles should follow helical trajectories. In the transverse plane, the motion is circular, while it is a straight line in the \(rz\)-plane. The transverse impact parameter and momentum can be estimated from the radius of the circle in the transverse plane like

with the circle center \((c_x, c_y)\) and radius \(\rho\). The transverse momentum can be related to available quantities like

with the charge \(q\) and the magnetic field \(B\). An intersection between the straight line in the \(rz\)-plane with the \(z\)-axis gives an estimate of the longitudinal impact parameter. An illustration of seeds in the transverse plane is found in Fig. 14. Note that seeds can incorporate hits spread across all of the layers shown, although this can be a configuration parameter.

## Track finding and track fitting

In the track seeding and following approach, track candidates are built from
the initial seeds. One method implemented in ACTS, the Combinatorial Kalman
Filter (CKF), uses the *Kalman formalism*.
Originally developed for monitoring and steering mechanical systems, it can
also be used to iteratively calculate a track estimate. After a set of track
candidates has been assembled and filtered (see Ambiguity resolution), an
additional track fit is usually performed to extract the best estimate of the
track. The Kalman formalism can also be used for this, with the addition of a
smoothing step that has certain benefits. Other fit strategies exist, such as
a global \(\chi^2\) fit that minimizes the distances between track-sensor
intersections and measurements on all sensors at the same time. One drawback of
this method is the necessity to invert very large matrices, which is
computationally expensive.

In a track fit, the Kalman formalism can be shown to yield optimal estimates for Gaussian uncertainties. This assumption breaks down when effects like bremsstrahlung come into play. An extension of the Kalman Filter (KF) exists that relies on the individual propagation of a set of trajectories, instead of a single one, to model these biased uncertainties by a sum of Gaussian components. This Gaussian Sum Filter (GSF) achieves better results when fitting particles such as electrons, likely to undergo bremsstrahlung, and is deployed in e.g. the ATLAS tracking chain.

### Kalman formalism and Kalman track fitter

Tip

See Kalman Filter (KF) [wip] for a description of the implementation of the Kalman Filter in the core library.

The basis of the Kalman formalism is a state vector, that can be identified with the set of track parameters \(\vec x\). Note that the concrete parametrization plays a subordinate role in this context. Rather than building an estimate of the state of a system in real time, a Kalman track fit can be understood as estimating the parameters iteratively in steps. In the track fitting application, each step is defined by a measurement to be included. The evolution of the state vector is described by

where the linear function \(\mathbf F_{k-1}\) transports the state vector at step \(k-1\) to step \(k\). \(\vec w_{k-1}\) is additional so-called process noise that affects the transport additively. Each step has an associated measurement, with the fixed relationship between the measurement and the state vector

Here, \(\mathbf H_k\) is the *measurement mapping function*, which
transforms the state vector into the measurement space. In the ideal case,
this purpose can be achieved by a simple projection matrix, which extracts a
subspace of the state vector. Additionally, \(\epsilon_k\) represents the
measurement uncertainty.

The Kalman fit process is divided into different phases:

**Prediction**of the state vector at the next step \(k+1\) based on the information at the current step \(k\).**Filtering**of the prediction by incorporating the measurement associated to the step**Smoothing**of the state vector by walking back the steps and using information for the subsequent step \(k+1\) to improve the estimate at the current step \(k\).

An illustration of these concepts is found in Fig. 15. Here, a series of three sensors is shown with measurements on them. The KF then predicts the track parameters at an intersection, shown in blue. Subsequently, a filtered set of parameters is calculated as a mixture between the measurement and the prediction. Not shown in this picture is the smoothing step.

In many cases, the first two phases run in tandem, with prediction and filtering happening alternatingly at each step. The smoothing phase is launched once the last measurement has been encountered. Starting from a state \(k\), first, a prediction of the state vector at the next measurement location is obtained via

with the linear transport function from above. \(\vec x_k^{k-1}\) is the prediction of the state vector at step \(k\) based on step \(k-1\). The next stage is the filtering. Here, the state vector is refined by taking into account the measurement at the current step. Following one of two variants of filtering from 2, the gain matrix formalism, the state vector is updated like

with the *Kalman gain matrix*

Note that \(\vec x_k\) is the filtered state vector at step \(k\), based on information from previous steps and step \(k\) itself. This is in contrast to \(\vec x_k^{k-1}\), which is the prediction of the state vector at step \(k\) based on \(k-1\), and is used to calculate the filtered state vector. One input to these equations is the covariance matrix prediction \(\mathbf C_k^{k-1}\) at step \(k\) based on step \(k-1\), which can be written as

in the linear version from 2, with the covariance \(\mathbf C_{k-1}\) at step \(k-1\), and the covariance \(\mathbf Q_{k-1}\) associated with \(\vec w_{k-1}\) from above. Also needed is \(\mathbf V_k\), which is the covariance associated with \(\epsilon_k\), effectively representing the measurement uncertainty.

Similar to the state vector itself, the corresponding covariance matrix is also filtered using

In the smoothing phase, the state vector at step \(k\) is improved using the information from the subsequent step \(k+1\) using

Here, \(\vec x_{k+1}^n\) is the smoothed state vector and \(\vec
x_{k+1}^k\) the predicted state vector at the subsequent step \(k+1\). Also
needed is the *smoother gain matrix*

with the predicted covariance at step \(k+1\), \(\mathbf C_k^{k+1}\). Finally, the covariance at the current step \(k\) can also be smoothed with

After smoothing, the parameter estimate at the first step contains information from all other measurement states. As mentioned above, in case the uncertainties entering the Kalman fit are Gaussian distributions without biases, the KF can be shown to be the optimal solution minimizing mean square estimation error. However, certain caveats exist. The KF assumes that a linear transport function \(\mathbf F\) exists that can propagate the state vector. In the presence of inhomogeneous magnetic fields this is not the case. Instead of explicitly applying \(\mathbf F\) to the state vector for the prediction, the ACTS KF turns to the numerical integration, discussed in Numerical integration. With it, the prediction from this equation is simply the intersection of the extrapolated trajectory with the next sensitive surface. Aside from this, \(\mathbf F\) is also used to transport the covariance between steps (see here). Here, the semi-analytical method for covariance transport in the numerical integration can be used. \(\mathbf F\) can then be identified with the transport Jacobian accumulated between surfaces.

For smoothing, two possibilities exist to obtain the needed covariances from subsequent measurement steps. Either, the inverse transport Jacobian is used and applied, in a way similar to this equation, or the numerical integration is executed again in an inverse fashion, propagating from the subsequent step to the current one.

### Combinatorial Kalman Filter

Tip

See Combinatorial Kalman Filter for information on the CKF implementation found in the core library.

As mentioned above, the Kalman formalism can be used for track finding. In this case, the smoothing step can be dropped, as the resulting track candidates are likely to be refit regardless, therefore saving some time. The CKF explores the event starting from an initial track seed. It does this by considering not only a single sequence of measurements, but allowing the branching of the fit at each sensitive surface that is encountered. To this end, all or a subset of measurements that are found on each surface are considered. Measurements are selected based on their compatibility with the current state estimate, by using their residuals. A predicted residual

and a filtered residual

can be defined, depending on which state estimate is compared with the measurement \(\vec m_k\). Using the filtered residual, an effective \(\chi^2\) increment

can be calculated. The global \(\chi^2\) of the track candidate can be calculated as the sum of all \(\chi^2_+\) across the steps. Measurements with a large \(\chi^2_+\) are considered as outliers, which have low compatibility with the trajectory. By branching out for measurements below a certain \(\chi^2_+\), and following the branches, a tree-like structure of compatible track candidates originating from a track seed is assembled. This feature is shown in Fig. 16, which displays a circular trajectory, and a set of iteratively assembled track candidates. Basic quality criteria can be applied at this stage, to remove bad candidates. A dedicated Ambiguity resolution. selects the candidates most likely to belong to real particle tracks.

## Ambiguity resolution

Due to the combinatorial nature of track finding, and to achieve high
efficiencies, this set of candidates is often large, and contains a
non-negligible fraction of *fake* candidates. These fake candidates are either
completely combinatorial, or arise from real particle measurements with
combinatorial additions. Track candidates coming from a single seed necessarily
share a common stem of measurements. Measurements can potentially also be
shared between candidates from different seeds.

One possibility to resolve this (as is done in e.g. ATLAS tracking) is an ambiguity resolution algorithm, that attempts to filter out as many undesirable tracks as possible. This is implemented by means of a scoring function, that combines properties of the track parameters. Higher scores are correlated with a larger probability to be a desirable track candidate. A larger number of hits results in an increase in the score, as longer compatible hit chains are less likely to be random combinations. On the other hand, missing hits in sensors where a hit was expected negatively impact the score. Experiment specific scoring of hits from different subsystems is also implemented. The overall \(\chi^2\) value computed for the track candidate also plays a role. Candidates that share hits with other candidates are penalized. Another quantity is the measured particle \(p_\mathrm{Y}\), which enters the score, to give preference to tracks with large momenta. For tracks containing measurements with a substantial local \(\chi^2_+\) at the start or end of the trajectory, the ambiguity resolution step can also attempt to remove these hits, and determine whether a refit without them yields a more favorable global \(\chi^2\).

Finally, the output of the ambiguity resolution step is a set of track candidates that contain an enhanced fraction of tracks from actual particles, while fake tracks are suppressed. They are passed into the final precision fit outlined in Track finding and track fitting, to extract the parameter estimate, and used for further aspects of reconstruction.

## Vertex reconstruction

Tip

See Vertexing for a dedicated description of the vertexing as implemented in ACTS.

One very immediate use case for tracks is the reconstruction of interaction
vertices in the event. These are needed for many aspects of higher-level
reconstruction algorithms. Vertices are used in different ways. As shown in
Fig. 17, a single event can have a primary vertex, usually
associated with the hard-scatter event, as well as a number of secondary
vertices. Typically, the primary vertex will be located in the luminous
region. The reconstruction of secondary vertices can help with the
identification of particles, for instance in the form of *\(b\)-tagging*
jets originating from \(b\)-quarks. Here, a characteristic displaced vertex
located inside a jet is a sign for a \(b\)-hadron decay. Additionally, pile-up
interactions can produce vertices that are not associated with the
interaction of interest. Signatures from pile-up interactions can be
rejected, if they can be associated to a pile-up vertex.

Vertex reconstruction can be divided into two stages: vertex finding and vertex fitting, in close analogy to the reconstruction of tracks themselves. Reconstruction begins with a seeding stage. Vertex seeding can be performed in a number of ways. Algorithms differ for primary and secondary vertex reconstruction. For primary vertex seeding, one option is an algorithm, which uses a histogram approach to cluster tracks in the \(z\)-axis. This is based on the assumption that primary vertices will align with the beam spot. Other approaches include the use of a Gaussian track density to identify regions with high track multiplicity as vertex seeds. For secondary vertexing, seeds are formed from pairs of reconstructed tracks, as the constraint to the beam spot does not apply.

With a set of vertex seeds determined, tracks compatible with the vertex are selected. Using a linearized approximation of the helical trajectories in the vicinity of the vertex, a fitting procedure based on the Kalman formalism can estimate the vertex parameters.

One issue with an approach like this is the fact that the assignment of tracks to vertices is not unambiguous. Improvements exist, where tracks that turn out to be a bad fit with the vertex in question are weighted down, avoiding degradation in the obtained result. On the other hand, multi-vertex fit methods can reassign such outlier tracks to a more compatible vertex, yielding improved results for both vertices.

- 1
Gessinger-Befurt, Paul, 30.04.2021. Development and improvement of track reconstruction software and search for disappearing tracks with the ATLAS experiment. 10.25358/openscience-5901

- 2(1,2)
F. Frühwirth, 1987, Application of Kalman filtering to track and vertex fitting, , 11.1016/0168-9002(87)90887-4