Abstract
Measurements of cross sections of inelastic and diffractive processes in proton–proton collisions at LHC energies were carried out with the ALICE detector. The fractions of diffractive processes in inelastic collisions were determined from a study of gaps in charged particle pseudorapidity distributions: for single diffraction (diffractive mass M _{ X }<200 GeV/c ^{2}) \(\sigma_{\mathrm{SD}}/\sigma_{\mathrm {INEL}} = 0.21 \pm 0.03, 0.20^{+0.07}_{0.08}\), and \(0.20^{+0.04}_{0.07}\), respectively at centreofmass energies \(\sqrt{s} = 0.9, 2.76\mbox{, and }7~\mbox{TeV}\); for double diffraction (for a pseudorapidity gap Δη>3) σ _{DD}/σ _{INEL}=0.11±0.03,0.12±0.05, and \(0.12^{+0.05}_{0.04}\), respectively at \(\sqrt{s} = 0.9, 2.76\mbox{, and }7~\mbox{TeV}\). To measure the inelastic cross section, beam properties were determined with van der Meer scans, and, using a simulation of diffraction adjusted to data, the following values were obtained: \(\sigma_{\mathrm{INEL}} = 62.8^{+2.4}_{4.0} (\mathrm{model}) \pm1.2 (\mathrm{lumi})\) mb at \(\sqrt{s} = 2.76\ \mbox{TeV}\) and \(73.2^{+2.0}_{4.6} (\mathrm{model}) \pm2.6 (\mathrm{lumi})~\mbox{mb}\) at \(\sqrt{s} = 7\ \mbox{TeV}\). The single and doublediffractive cross sections were calculated combining relative rates of diffraction with inelastic cross sections. The results are compared to previous measurements at proton–antiproton and proton–proton colliders at lower energies, to measurements by other experiments at the LHC, and to theoretical models.
1 Introduction
The cross sections of inelastic and diffractive processes in proton–proton (pp) collisions are among the basic observables used to characterize the global properties of interactions, and thus are always a subject of interest at a new centreofmass energy. The behaviour of hadronic cross sections at high energies is usually described in the framework of Regge theory [1–3] and its various QCDinspired interpretations [4, 5]. As these collisions are dominated by relatively smallmomentum transfer processes, such measurements contribute to the theoretical understanding of QCD in the nonperturbative regime. Recent developments in the field can be found in Refs. [6–18]. As the LHC explores hadron collisions at centreofmass energies (up to \(\sqrt{s} = 7~\mbox{TeV}\) used in the present analysis), corresponding to laboratory energies between 4×10^{14} and 2.6×10^{16} eV, close to the knee (10^{15}–10^{16} eV) observed in the energy distribution of cosmic rays, these measurements are also relevant in this context.
It is customary to distinguish two contributions to the inelastic cross section: diffractive processes and nondiffractive processes. At a centreofmass energy \(\sqrt{s} = 1.8\ \mbox{TeV}\), at the Tevatron, diffractive processes (single and double diffraction combined) represent about 25 % of inelastic collisions [19, 20]. At LHC energies, it is expected that diffractive processes also account for a large fraction of the inelastic cross section.
When presenting LHC measurements such as particle momentum distributions, cross sections, etc. for NonSingle Diffractive (NSD) or Inelastic (INEL) event classes, the uncertainty on the diffractive processes may dominate the overall systematic error (see, for instance, Ref. [21]). Therefore, it is essential to measure, as precisely as possible, the properties of these processes. In addition, the nucleon–nucleon inelastic cross section is a basic parameter used as an input for model calculations to determine the number of participating nucleons and the number of nucleon–nucleon binary collisions for different centrality classes in heavyion collisions [22], the main focus of the ALICE scientific programme. This publication reports measurements of inelastic pp cross sections with a precision better than 6 %, and emphasizes the importance of diffraction processes in such measurements.
The ALICE detector was used to measure the properties of gaps in the pseudorapidity distribution of particles emitted in pp collisions, in order to estimate the relative contributions of diffractive processes. This publication is organized as follows: in Sect. 2 we discuss diffractive processes and explain the definitions of diffraction adopted in this article; Sect. 3 gives a short description of the ALICE detector elements relevant to this study, and describes the data samples used here and datataking conditions; Sect. 4 presents relative rates of diffractive processes as measured from a pseudorapidity gap analysis, used to adjust these rates in the Monte Carlo event generators; Sect. 5 discusses van der Meer beam scans, used to determine the LHC luminosity and the cross section corresponding to the trigger selection; in Sect. 6, the simulation adjusted with our measurement is used to determine the inelastic cross section from the measured trigger cross section, and in turn the cross sections for diffractive processes; finally a comparison is made between the ALICE cross section measurements and data from other experiments. The results are also compared with predictions from a number of models.
2 Diffraction
2.1 Diffractive processes
In Regge theory at high energies, diffraction proceeds via the exchange of Pomerons (see Refs. [1–3]). The Pomeron is a colour singlet object with the quantum numbers of the vacuum, which dominates the elastic scattering amplitude at high energies. The Feynman diagrams corresponding to onePomeron exchange in elastic, single and doublediffraction processes are shown in Fig. 1. Single and doublediffraction processes, p+p→p+X and p+p→X _{1}+X _{2}, where X (X _{1}, X _{2}) represent diffractive system(s), are closely related to smallangle elastic scattering. These processes can be considered as binary collisions in which either or both of the incoming protons may become an excited system, which decays into stable finalstate particles. Single Diffraction (SD) is similar to elastic scattering except that one of the protons breaks up, producing particles in a limited rapidity region. In Double Diffraction (DD), both protons break up.
In SD processes, there is a rapidity gap between the outgoing proton and the other particles produced in the fragmentation of the diffractive system of mass M _{ X } (Fig. 2 middle). For high masses, the average gap width is \(\Delta\eta\simeq\Delta y \simeq\ln(s/M_{X}^{2}) =  \ln \xi \), where \(\xi= M_{X}^{2}/s\). Typically, at \(\sqrt{s} = 7\ \mbox{TeV}\), Δη varies from 13 to 7 for M _{ X } from 10 to 200 GeV/c ^{2}. In DD processes, there is a rapidity gap between the two diffractive systems (Fig. 2 right). The average gap width in this case is \(\Delta\eta\simeq\Delta y \simeq\ln (ss_{0}/M_{X_{1}}^{2}M_{X_{2}}^{2})\), where the energy scale s _{0}=1 GeV^{2}, and \(M_{X_{1}}\), \(M_{X_{2}}\) are the diffractivesystem masses. Typically, at \(\sqrt{s}= 7\ \mbox{TeV}\), one expects Δη≃8.5 for \(M_{X_{1}} = M_{X_{2}} = 10\ \mbox{GeV}/c^{2}\).
Experimentally, there is no possibility to distinguish large rapidity gaps caused by Pomeron exchange from those caused by other colourneutral exchanges (secondary Reggeons), the separation being modeldependent. Therefore, in this study, diffraction is defined using a large rapidity gap as signature, irrespective of the nature of the exchange. SD processes are those having a gap in rapidity from the leading proton limited by the value of the diffractive mass M _{ X }<200 GeV/c ^{2} on the other side (i.e. at \(\sqrt{s} = 7\ \mbox{TeV}\), Δη≳7); other inelastic events are considered as NSD. The choice of the upper M _{ X } limit corresponds approximately to the acceptance of our experiment and was used in previous measurements [23]. DD processes are defined as NSD events with a pseudorapidity gap Δη>3 for charged particles. The same value was used for separation between DD and NonDiffractive (ND) processes in another measurement [24].
2.2 Simulation of diffraction
Diffraction processes are described by the distribution of the mass (or masses) of the diffractive system(s), the scattering angle (or the fourmomentum transfer −t), and the diffractivesystem fragmentation. The results depend only weakly on the assumption made for the distribution in t, and in all models, calculating acceptance and efficiency corrections, we integrated over this dependence. The tdistribution and fragmentation of diffractive systems are simulated with the PYTHIA6 (Perugia0, tune 320) [25–27] and PHOJET [28] Monte Carlo generators. Both PYTHIA6 and PHOJET Monte Carlo generators give a reasonable description of UA4 data [29] on charged particle pseudorapidity distribution in SD events.
The main source of uncertainty in the simulation of diffractive collisions comes from the uncertainty on the M _{ X } distribution (see, for example, the discussion in [30]). In Regge theory, in the single Regge pole approximation, the SD cross section (dσ/dM _{ X }) for producing a highmass system, M _{ X }, is dominated by the diagram shown in Fig. 3. In the general case, each of the legs labeled (R _{1} R _{2})R _{3}, can be a Pomeron \(\mathbb{P}\) or a secondary Reggeon \(\mathbb{R}\) (e.g. the ftrajectory) [1–3]. At very high energies, the SD process is dominated by the (\(\mathbb {P}\mathbb{P}\))\(\mathbb{P}\) and (\(\mathbb{P}\mathbb{P}\))\(\mathbb{R}\) terms, which have similar energy dependence, but a different M _{ X } dependence. The \((\mathbb{P}\mathbb{P})\mathbb{P}\) term is proportional to \(1/M_{X}^{1+2\Delta}\) and the \((\mathbb{P}\mathbb{P})\mathbb{R}\) term to \(1/M_{X}^{2+4\Delta }\), where Δ=α _{P}−1, with α _{P} the intercept of the Pomeron trajectory. The \((\mathbb{P}\mathbb{P})\mathbb{R}\) term dominates the process at very low mass, but vanishes at higher masses (\(M_{X}^{2} \gg s_{0}\)), because the corresponding Regge trajectory has intercept smaller than unity.
In both the PYTHIA6 and PHOJET generators, the diffractivemass distribution for the SD processes is close to 1/M _{ X } (Fig. 4), which corresponds to the (\(\mathbb{P}\mathbb{P}\))\(\mathbb{P}\) term with Δ=0. However, experimental data show that at low masses the dependence is steeper than 1/M _{ X }. This is discussed, for example, in publications by the CDF collaboration [19, 20], and supports the values of Δ>0 and also the above theoretical argument for inclusion of terms other than (\(\mathbb {P}\mathbb{P}\))\(\mathbb{P}\). A recent version of PYTHIA having a steeper M _{ X } dependence at low masses, PYTHIA8 [31], uses an approximation with a \(1/M_{X}^{1+2\Delta}\) dependence with Δ=0.085, based on the \((\mathbb{P}\mathbb{P})\mathbb{P}\) term in the Donnachie–Landshoff model [32].
For this study the M _{ X } distributions in PYTHIA6 and PHOJET were modified so as to use the distributions from model [18] (Fig. 4), which includes in the calculation of the SD cross section all eight terms contributing to the diagram of Fig. 3. Their relative contributions are determined from a fit to lowerenergy data. The predictions of this model for the total, elastic, and diffractive cross sections at LHC energies [33] are found to be consistent with measurements [34–36]. The modification of PYTHIA6 and PHOJET consists in reproducing the model M _{ X } distribution, by applying weights to the generated events. Numerical values of the diffractivemass distributions from this model, at the three centreofmass energies relevant to this publication, can be found in [38].
In addition, the fractions of diffractive processes in the models were adjusted according to measurements presented here, by a normalization factor. In what follows, “adjusted” PYTHIA6 or PHOJET means that these event generators are used with the modified diffractivemass distribution, and the modified relative rate of diffractive processes.
In order to estimate the systematic errors coming from the uncertainty in the functional shape of the M _{ X } dependence, the following modifications were used: the model distribution was multiplied by a linear function aM _{ X }+b, which is equal to unity at the upper diffractivemass value M _{ X }=200 GeV/c ^{2} and is equal to 0.5 or 1.5 at the diffractivemass threshold, i.e. M _{ X }≈1.08 GeV/c ^{2} (sum of proton and pion masses). A linear function was chosen because it is the simplest way to vary the relative fractions of lowmass (or non detected) and highmass (or detected) single diffractive events. The resulting variation is illustrated in Fig. 4, where the diffractivemass distributions are normalized to have the integral between threshold and M _{ X }=200 GeV/c ^{2} equal to unity. The influence of the change of the M _{ X } dependence on the SD rate is given roughly by the variation of the yield in the highM _{ X } region (above ≃10 GeV/c ^{2}, where the events are measured) relative to that in the lowM _{ X } region (where an extrapolation has to be used). The distribution from the Donnachie–Landshoff model [32] was also used in the evaluation of the systematic uncertainties due to the extrapolation to lowM _{ X } region. The ATLAS collaboration, in their measurement of the inelastic cross section [34], used unmodified PYTHIA6 and PHOJET event generators, with an approximate 1/M _{ X } dependence, the (\(\mathbb{P}\mathbb{P}\))\(\mathbb{P}\) term of the Donnachie–Landshoff model (as parameterized in PYTHIA8), around which they varied the mass distribution (see Fig. 4), and also the calculations with model [6–8]. Thanks to the collaboration of the authors of Refs. [6–9, 13–17] we were able to check that the singlediffraction mass dependencies of the corresponding models, when normalized at the M _{ X }=200 GeV/c ^{2}, are well within the limits assumed in this analysis.
Concerning the simulation of DD processes in PYTHIA6 and PHOJET event generators, only their overall fraction was adjusted according to our data, otherwise it was left unmodified. However, all NSD events with pseudorapidity gap Δη>3, including those flagged by a generator as ND, are considered to be DD. This way, processes with secondary Reggeon legs are also taken into account, albeit in a very modeldependent way. Therefore, the results for DD fractions and cross sections are subject to larger uncertainties than those for SD.
3 Experiment description
3.1 The ALICE detector
The ALICE detector is described in Ref. [39]. The analysis presented here is mainly based on data from the VZERO detector, the Silicon Pixel Detector (SPD) and the Forward Multiplicity Detector (FMD). The SPD and the VZERO hodoscopes provide trigger information for the selection of minimumbias events and for van der Meer [40] protonbeam scans. The TimeProjection Chamber (TPC) [41] and the whole Inner Tracking System (ITS) [42], both situated in the ALICE central barrel, are used in this study only to provide the interaction vertex position, from reconstructed tracks.
Throughout this publication, the detector side at negative (positive) pseudorapidity is referred to as left or “Lside” (right or “Rside”). The asymmetric arrangement of the detectors comes about because of the space constraints imposed by the ALICE muon arm on the Lside.
The two VZERO hodoscopes, with 32 scintillator tiles each, are placed on each side of the interaction region at z≃3.3 m (V0R) and z≃−0.9 m (V0L), covering the pseudorapidity ranges 2.8<η<5.1 and −3.7<η<−1.7, respectively (z is the coordinate along the beam line, with its origin at the centre of the ALICE barrel detectors, oriented in the direction opposite to the muon arm [39]). Each hodoscope is segmented into eight equal azimuthal angle (φ) sectors and four equal pseudorapidity η rings. This implies that the pseudorapidity resolution is similar to that required for the binning (δη=0.5) used for the analysis. The time resolution of each hodoscope is better than 0.5 ns.
The SPD makes up the two innermost layers of the ALICE Inner Tracking System (ITS) and it covers the pseudorapidity ranges η<2 and η<1.4, for the inner and outer layers respectively. The SPD has in total about 10^{7} sensitive pixels on 120 silicon ladders which were aligned using pp collision data to a precision of 8 μm. The SPD can also be used to provide the position of the interaction vertex by correlating hits in the two siliconpixel layers to obtain track elements called tracklets. The resolution achieved on the position of the vertex from the SPD is slightly worse than that for the vertex from tracks reconstructed with the TPC and the whole ITS. It depends on the track multiplicity and is approximately 0.1–0.3 mm in the longitudinal direction and 0.2–0.5 mm in the direction transverse to the beam line. If the vertex from reconstructed tracks is not available, the vertex from the SPD is used.
The FMD consists of Sistrip sensors with a total of above 5×10^{4} active detection elements, arranged in five rings perpendicular to the beam direction, covering the pseudorapidity ranges −3.4<η<−1.7 (FMD3) and 1.7<η<5.1 (FMD1 and FMD2). Combining VZERO, SPD and FMD, ALICE has a continuous acceptance over a pseudorapidity interval of 8.8 units.
3.2 Event samples and datataking conditions
ALICE data were collected at three centreofmass energies (\(\sqrt{s} = 0.9, 2.76\mbox{, and }7\ \mbox{TeV}\)), at low beam current and low luminosity, hence corrections for beam backgrounds and event pileup in a given bunch crossing are small. The maximum average number of collisions per bunch crossing was 0.1 at \(\sqrt{s} = 7\ \mbox{TeV}\).
The minimumbias data used for the diffractive study were collected using the trigger condition MB_{OR}, which requires at least one hit in the SPD or in either of the VZERO arrays. This condition is satisfied by the passage of a charged particle anywhere in the 8 units of pseudorapidity covered by these detectors.
For the van der Meer scan measurements, the trigger requirement was a time coincidence between hits in the two VZERO scintillator arrays, V0L and V0R, MB_{AND}.
Control triggers taken for various combinations of filled and empty bunch buckets were used to measure beaminduced background and accidental triggers due to electronic noise or cosmic showers. Beam backgrounds were removed offline using two conditions. First, VZERO counter timing signals, if present, had to be compatible with particles produced in collisions. Second, the ratio of the number of SPD clusters to the number of SPD tracklets is much higher in background events than in beam–beam collisions, thus a cut on this ratio was applied. The latter condition was adjusted using beambackground events selected with VZERO detector. The remaining background fraction in the sample was estimated from the number of controltrigger events that passed the event selection. It was found to be negligible for the three centreofmass energies, except in the case of the van der Meer scan at \(\sqrt{s} = 2.76\ \mbox{TeV}\) at large displacements of the beams, as discussed in Sect. 5.
At each centreofmass energy, several datataking runs were used, with different event pileup rates, in order to correct for pileup, as described below. For the measurement of the inelastic cross sections, runs were chosen to be as close in time as possible to the runs used for the van der Meer scans in order to ensure that the detector configuration had not changed.
At \(\sqrt{s} = 0.9\ \mbox{TeV}\), 7×10^{6} events collected in May 2010 were used for diffractive studies. No van der Meer scan was performed at this energy, hence the inelastic cross section was not measured by ALICE.
At \(\sqrt{s} = 7~\mbox{TeV}\), 75×10^{6} events were used for diffractive studies, and van der Meer scans were performed five months apart during the pp datataking period (scan I in May 2010, scan II in October 2010).
The data at \(\sqrt{s} = 2.76~\mbox{TeV}\) were recorded in March 2011, at an energy chosen to match the nucleon–nucleon centreofmass energy in Pb–Pb collisions collected in December 2010. For diffraction studies, 23×10^{6} events were used. One van der Meer scan was performed (scan III in March 2011). Because of a technical problem the FMD was not used in diffraction measurement at this energy, resulting in a larger systematic uncertainty in diffractive crosssection measurements at this energy.
4 Measurement of relative rates of diffractive processes
4.1 Pseudorapidity gap study
For this study the events were selected by the hardware trigger MB_{OR} followed by the ALICE offline event selection described in Sect. 3. The pseudorapidity distribution of particles emitted in the collision is studied by associating the event vertex with a “pseudotrack” made from a hit in a cell of the SPD, of the VZERO or of the FMD detector. In the case of VZERO, the cells are quite large (δη about 0.5), so for this detector hits were distributed randomly within the cell pseudorapidity coverage.
Note that the effective transversemomentum threshold for the pseudotrack detection is very low (about 20 MeV/c). It is practically pseudorapidity independent and determined by the energy loss in the material. This implies that our detector misses only a very small fraction of particles.
The vertex is reconstructed using information from the ITS and TPC, if possible. If it is not possible to form a vertex in this way, a position is calculated using the SPD alone. If this is also not possible (as it occurs in 10 % of cases), then a vertex is generated randomly using the measured vertex distribution. Such cases occur mainly where there is no track in the SPD and hit information is in the VZERO or FMD detectors only.
In the analysis described below, we separate the events into three categories, called “1armL”, “1armR” and “2arm”. The purpose of the classification is to increase the sensitivity to diffractive processes. As will be described below, the categories 1armL and 1armR have an enriched singlediffraction component, while a subset of the 2arm category can be linked to double diffraction.
We distinguish between “onetrack” events and those having more than one track, i.e. “multipletrack” events. Let η _{L}, η _{R} be the pseudorapidities of the leftmost (lowestpseudorapidity) and rightmost (highestpseudorapidity) pseudotracks in the distribution, respectively. If an event has just one pseudotrack, then η _{L}=η _{R}. We classify as onetrack events all events satisfying the condition \(\eta_{\rm R}\eta _{\mathrm{L}}<0.5\) and having all pseudotracks within 45^{∘} in φ. For such events, we determine the centre of the pseudorapidity distribution as \(\eta_{\mathrm{C}} = \frac{1}{2}(\eta _{\mathrm{L}}+\eta_{\mathrm{R}})\), and

(i)
if η _{C}<0 the event is classified as 1armL;

(ii)
if η _{C}>0 the event is classified as 1armR.
The multitrack events are classified in a different way. For these events, we use the distance d _{L} from the track with pseudorapidity η _{L} to the lower edge of the acceptance, the distance d _{R} from the track with pseudorapidity η _{R} to the upper edge of the acceptance, and the largest gap Δη between adjacent tracks (see Fig. 5). Then,

(i)
if the largest gap Δη between adjacent tracks is larger than both d _{L} and d _{R}, the event is classified as 2arm;

(ii)
if both of the edges η _{L}, η _{R} of the pseudorapidity distribution are in the interval −1≤η≤1, the event is classified as 2arm;

(iii)
otherwise, if η _{R}<1 the event is classified as 1armL, or if η _{L}>−1 the event is classified as 1armR;

(iv)
any remaining events are classified as 2arm.
The ALICE Monte Carlo simulation consists of four main stages: (a) event generation; (b) transport through material; (c) detector simulation, and (d) event reconstruction. In Figs. 6 and 7, we compare gap properties between data and Monte Carlo simulation after event reconstruction (stage d).
In Fig. 6 left, the gap width distribution for 2arm events is compared to simulations with and without DD, to illustrate the sensitivity to the DD fraction. The gap width distribution at large Δη cannot be described by simulations without DD. However, the default DD fraction in PYTHIA6 significantly overestimates the distribution of large pseudorapidity gaps, while the default DD distribution in PHOJET significantly underestimates it. Adjustments to these fractions can bring the predictions of the two generators into better agreement with the data, and lead to a method to estimate the DD fraction. A similar approach was employed by the CDF collaboration [24]. The DD fractions in PYTHIA6 and PHOJET were varied in steps so as to approach the measured distribution.
The aim of the adjustment is to bracket the data. At the end of the adjustment the PYTHIA6 data still overestimate the data, and the PHOJET data underestimate it, but the agreement between data and Monte Carlo is brought to 10 % for the bin in closest agreement above Δη=3 (see Fig. 6 right). Further adjustment leads to a deterioration in the shape of the Δη distribution. The mean value between the PYTHIA6 and PHOJET estimates is taken as the best estimate for the DD fraction, and the spread between the two contributions, integrated over Δη>3, is taken as a a measure of the model error.
Once the value for the DD fraction has been chosen, and its associated error estimated as described above, the measured 1armL(R) to 2arm ratios, which have negligible statistical errors, can be used to compute the SD fractions and their corresponding errors. For this purpose the efficiencies for the SD and NSD events to be detected as 1armL(R) or 2arm classes have to be known. The determination of these efficiencies is described later in this section. A similar method was used by the UA5 collaboration in their measurement of diffraction [23]. In practice, we handle the Lside and Rside independently and the SD fractions are determined separately for Lside and Rside single diffraction.
In summary, three constraints from our measurements, the two 1armL(R) to 2arm ratios and the additional constraint obtained from the gap width distribution (Fig. 6 right), are used to compute the three fractions for DD events, Lside SD, and Rside SD events. The sum of the two latter values is then used to estimate the SD fraction of the overall inelastic crosssection. This way the Monte Carlo event generators PYTHIA6 and PHOJET are adjusted using the experimental data, and this procedure is repeated for different assumptions about the diffractivemass distribution for SD processes, as discussed in Sect. 2.
For the \(\sqrt{s} = 2.76\ \mbox{TeV}\) run, the FMD was not used in the analysis, resulting in a gap in the detector acceptance, so the fraction of DD events in the Monte Carlo generators was not adjusted using the gap distribution for this energy. The resulting DD fraction of the inelastic cross section, however, was modified due to the adjustment of the SD fraction and the experimental definition of DD events. This results in a larger systematic error on the measured DD cross section at this energy.
In Fig. 7 we compare other pseudorapidity distribution properties after event generator adjustment. In addition to the quantities defined above, we use in this comparison the centre position η _{gC} of the Δη pseudorapidity gap. The observed basic features of the edges of pseudorapidity distributions and gaps are reasonably well reproduced by the adjusted simulations for η≥1.5, and more accurately for η≤1.5. Figure 7 shows the \(\sqrt{s} = 7~\mbox{TeV}\) case for illustration. The agreement between data and simulation is similar at \(\sqrt{s} = 0.9\) and 2.76 TeV.
We note that there is less material in the Rside of the ALICE detector. With the adjusted MonteCarlo generators we have obtained a good description for the 1armR event class. On the Lside, there is more material between V0L and the interaction point and the distribution of material is not as precisely known as on the other side. For this reason we have used a larger error margin in our study of the corresponding systematic uncertainty.
Several tests were made to ensure that the material budget and the properties of the detectors do not modify the correlations between observables and rates of diffractive processes to be measured. The material budget was varied in the simulation by ±10 % everywhere, and by +50 % in the forward region only (η>1). In both cases this did not modify the gap characteristics significantly. The maximum effect is for the largest Δη bins in 2arm events, and is still less than 10 %. The effect was found to be negligible for triggering and event classification efficiencies. In the region η≤1 the material budget is known to better than 5 %. In order to assess the sensitivity of the results to details of the detectorresponse simulation, the properties of the pseudorapidity distribution and gaps were also studied with the simulation output after stage b (particle transport without detector response, using ideal hit positions). Only negligible differences between ideal and real detectors were found.
The MB_{OR} trigger covers the pseudorapidity range between −3.7 and 5.1 except for a gap of 0.8 units for 2.0<η<2.8, which results in a small event loss. The proportion of events lost was estimated by counting the number of events having tracks only in the corresponding interval on the opposite pseudorapidity side; the fraction loss of MB_{OR} triggers was found to be below 10^{−3}.
4.2 Relative rate of single diffraction
The detection efficiencies for SD processes corresponding to the different event classes, obtained with PYTHIA6 at \(\sqrt{s} = 0.9\mbox{ and }7\ \mbox{TeV}\), are illustrated in Fig. 8. For small diffractive masses, the produced particles have pseudorapidities close to that of the diffracted proton, therefore, such events are not detected. Increasing the mass of the diffractive system broadens the distribution of emitted particles, and the triggered events are classified mostly as 1armL or 1armR class. Increasing the diffractive mass still further results in a substantial probability of producing a particle in the hemisphere of the recoiling proton, and indeed for masses above ∼200 GeV/c ^{2} such events end up mainly in the 2arm class. Because of multiplicity fluctuations and detection efficiencies, it is also possible for a SD event to be classified in the opposite side 1armR(L) class, albeit with a small probability (see Fig. 8). Masses above ∼200 GeV/c ^{2} end up mainly in the 2arm class, at all three energies. For this study, we have chosen M _{ X }=200 GeV/c ^{2} as the boundary between SD and NSD events. Changing the upper diffractivemass limit in the definition of SD from M _{ X }=200 GeV/c ^{2} to M _{ X }=50 GeV/c ^{2} or 100 GeV/c ^{2} at both \(\sqrt{s} = 0.9\mbox{ and }7~\mbox{TeV}\) does not make a difference to the final results for the inelastic cross section, provided the data are corrected using the same model as that used to parameterize the diffractive mass distribution. For example, at \(\sqrt{s} = 0.9~\mbox{TeV}\), if SD is defined for masses M _{ X }<50 GeV/c ^{2} (M _{ X }<100 GeV/c ^{2}), the measured SD cross section decreases by 20 % (10 %), which agrees with the predictions of the model [18] used for corrections.
The efficiencies, obtained as the average between the adjusted PYTHIA6 and PHOJET values for three processes (Lside SD, Rside SD, and NSD events) and for each event class are listed in Table 1 for the three energies under study. As these efficiencies depend on the adjustment of the event generators are in turn used for the adjustment, one iteration was needed to reach the final values, as well as the final adjustment. The systematic errors in Table 1 include an estimate of the uncertainty from the diffractivemass distribution, and take into account the difference of efficiencies between the two Monte Carlo generators and the uncertainty in the simulation of the detector response. The uncertainty in the material budget is found to give a negligible contribution. In order to estimate the systematic error due to the uncertainty on the diffractivemass distribution, the dependence of the cross section on diffractive mass from the model [18] was varied as described in Sect. 2, and, in addition, the diffractivemass distribution from the DonnachieLandshoff model [32] was used.
The raw numbers of events in the different classes were corrected for collision pileup by carrying out measurements for various runs with different average number of collisions per trigger. The relative rates of SD events (crosssection ratios), Table 2, are calculated from the measured ratios of 1armL(R) to 2arm class events for a given DD fraction, which was adjusted as described above in this section. Even though the two sides of the detector are highly asymmetric and have significantly different acceptances, they give SD cross section values that are consistent, Table 2, which serves as a useful crosscheck for the various corrections.
The SD fraction obtained at \(\sqrt{s} = 0.9~\mbox{TeV}\) is found to be consistent with the UA5 measurement for \(\mathrm{p}\overline{\mathrm{p}}\) collisions [23]. The agreement with the UA5 result is much better if a 1/M _{ X } diffractivemass dependence is used for our correction procedure, as was done for the UA5 measurements.
The MB_{AND} and MB_{OR} trigger efficiencies (Table 3) were obtained from the ALICE simulation, using the adjusted PYTHIA6 and PHOJET event generators. In practice, for each assumption on the diffractivemass distribution and for each fragmentation model, we determined together the diffractive fractions and the MB_{AND} and MB_{OR} trigger efficiencies for detecting inelastic events.