1. Introduction
Long-baseline accelerator neutrino experiments involve the production of neutrinos through the decay in flight of light mesons, such as pions or kaons. These experiments typically utilize powerful proton accelerators that direct high-energy protons at a solid or liquid phase target [
1]. The resulting particles are then focused into a decay tunnel, where they generate muon neutrinos primarily through the two-body decays of
and
or the corresponding decays of negatively charged mesons. This creates an intense beam of muon neutrinos that travels unimpeded in the forward direction after exiting the tunnel. The tunnel axis, which aligns with the neutrino beam axis, points directly at the neutrino detector, while the distance between the tunnel and the detector is referred to as the facility’s
baseline (
L).
Long-baseline experiments can take advantage of facilities with baselines ranging from hundreds to thousands of kilometers, limited only by the size of the Earth itself. This is because neutrinos have a tiny interaction cross-section and can pass through the Earth’s surface with minimal beam losses. However, these experiments do face a significant reduction in flux, as the neutrino flux at the detectors decreases as .
The neutrino beam also includes electron neutrinos that originate from the decays of charged kaons or the decay-in-flight of muons inside the tunnel. Long-baseline beams can be enriched in either or by changing the magnet polarity of the focusing system. For instance, a neutrino beam where focusing is achieved by a magnetic horn can reverse the horn polarity focusing and defocusing . In this case, the neutrino beam will be rich of originating from the and depleted from originating from the . If the neutrino detectors can distinguish the neutrino flavor, they will measure the number of neutrinos after oscillations along the beamline L. For a neutrino-enriched run, the detector will measure the oscillation probability and , together with the survival probability . Similarly, after an antineutrino-enriched run, we can measure the CP conjugate probabilities of the neutrino-enriched run: and , and the CPT conjugate of the neutrino disappearance probability: ). All these measurements, however, rely on a precise knowledge of the neutrino flux and flavor at the end of the decay tunnel, which corresponds to the initial un-oscillated flux. Measurements of these initial conditions are provided by neutrino detectors located just after the decay tunnel and are called near detectors. The baseline of the near detectors is of the order of hundreds of meters and, therefore, standard oscillations are negligible. The size of the detectors located at the long baseline L (far detector) is usually much larger than the size of the near detector because the far detector must compensate for the flux loss. It is customary to employ the same technologies for both the near and far detectors so that detector systematics cancel at leading order.
After the completion of the CNGS program based on OPERA [
2], all current long-baseline experiments are only capable of observing
and
, together with their antiparticles. As a consequence, the observables of long-baseline experiments are the following oscillation probabilities:
As a result, long-baseline facilities have access to a limited set of observables, a restricted range of
L, and a relatively narrow range of neutrino energies
E, as accelerators primarily produce muon neutrinos from 100 MeV to 100 GeV. When neutrino oscillation parameters were still unknown, there was skepticism about the feasibility of utilizing these facilities to explore the neutrino Yukawa sector of the Standard Model. However, the situation changed dramatically between 2002 and 2012, and long-baseline beams are now considered the most effective tool for investigating this sector.
In this review, we will discuss the significance of long-baseline facilities in investigating the neutrino Yukawa sector, particularly focusing on the discovery of
and its implications (
Section 2). The discovery of
sparked an ambitious experimental program that led to the development of HyperKamiokande (HK) and DUNE (
Section 3 and
Section 4, respectively). Furthermore, we will explore the limitations of current long-baseline experiments and explore potential avenues for future progress (
Section 5). We do not discuss other experimental approaches, e.g., based on reactor or atmospheric neutrinos, which can also access some of these oscillation parameters [
3,
4].
2. Neutrino Physics with Long-Baseline Beams
The Yukawa sector of the Standard Model (SM) is responsible for generating and mixing fermion masses. This sector is described by complex matrices that represent the coupling between the Higgs field and matter fields through Yukawa couplings [
5]. Unlike vector bosons, the Higgs mechanism does not provide any predictions about the size of the Yukawa couplings. As a result, the masses of elementary fermions and the mixing between mass and gauge eigenstates are not constrained. To express this sector in terms of physical quantities, we introduce three mass eigenstates for neutrinos (
and
), three mixing angles (
,
, and
), and a CP violating phase (
). In the Standard Model, neutrinos are described as Dirac fields, so only one complex phase is needed to describe lepton mixing. However, some extensions of the Standard Model consider neutrinos as Majorana particles, which require the introduction of two additional phases (e.g., see Chapter 6 in [
6]). These phases cannot be measured by oscillation experiments and, hence, the discussion below is still applicable in the presence of Majorana neutrinos.
The minimal extension of the SM that accommodates massive neutrinos is what is now called the Standard Model even if the SM, in its original formulation, employed massless neutral elementary fermions. Such an extension became mandatory after 1998, when oscillation data demonstrated the massive nature of neutrinos [
7]. In the minimally extended SM, massive neutral leptons are treated as (massive) quarks. Their flavor eigenstates are linear combinations of mass eigenstates and the linear operator that mixes the flavor and mass eigenfunctions is a
complex matrix. In the quark sector, this matrix is called the Cabibbo–Kobayashi–Maskawa (CKM) matrix. The corresponding matrix in the neutrino sector is the Pontecorvo–Maki–Nakagawa–Sakata (PMNS) matrix
. The
index runs over the flavor eigenstates (
) and the
i index runs over the mass eigenstates
. The only active neutrino fields in SM are left-handed chirality flavor fields
and
Here, we dropped the dependence of the field on space–time and the subscript
L. It is important to note that in the (minimally extended) SM only fields with left-handed chirality (
) appear in the charged currents (CCs) that describe the coupling of fermions with the
bosons. The minimally extended SM Lagrangian is built by applying the quark formalism to neutrinos and, hence, neutrinos are Dirac particles. As for the CKM, the PMNS matrix is unitary (
) and can be parameterized [
5] by three angles and one complex phase. The parameterization that has been adopted for the PMNS locates the complex phase in the 1–3 sector, i.e., in the rotation matrix between the first and third mass eigenstates:
In Equation (
3), the three rotation angles are labeled
, and
and
. In this parameterization,
and
. Physical observables are independent of parameterization, ensuring that the range of angles and the choice of the complex phase in the 1-3 sector can be made without loss of generality.
All these parameters can be measured by neutrino oscillation experiments except for an overall neutrino mass scale. The neutrino oscillation probability between the two flavor eigenstates
is the probability of observing a flavor
in a neutrino detector located at a distance
L from the source. The source produces neutrinos with flavor
and energy
E. The oscillation probability in Natural Units (NUs) is given by
where
and
L is the distance traveled by the neutrino. For antineutrino oscillations, we need to replace
U by
in Equation (
4), which corresponds to changing the sign of the third term. As a consequence, oscillation experiments can reconstruct all rotation angles and the CP phase. They also can measure the squared mass differences among eigenstates. It should be noted that oscillations are sensitive to (squared) mass differences only. Since there are just two independent squared mass differences and three mass eigenstates, the absolute mass neutrino scale or, equivalently, the absolute value of the lightest mass eigenstate cannot be determined by neutrino oscillations through Equation (
4). CP violation in the leptonic sector can be established by measuring the difference between
and P
if
. Since the leading oscillation term, i.e., the second term of Equation (
4), depends on a squared sine, determining the signs of
is also very challenging. The sign of
was determined at the beginning of the century by solar neutrino experiments [
5,
8] but the sign of
has not been determined yet [
9].
Equation (
4) cannot be applied to long-baseline experiments without further modifications. Since
L implies a long journey of the neutrinos through the Earth’s upper crust, matter effects perturb the oscillation probabilities. Unlike astrophysical neutrinos, where matter perturbations cause a strong change of the probability, the nearly constant, moderate-size matter density represents a small perturbation for accelerator neutrinos that can be accounted for by considering a perturbative expansion of the full oscillation formula and retaining only first-order perturbations in
The perturbative expansion of the
oscillation probability at the second order in
[
10,
11] is the master formula of long-baseline experiments and deserves careful consideration:
In this formula,
and the terms contributing to the so-called Jarlskog invariant [
5,
12] are split into the small parameter
, the
term
, and the CP term
;
with
representing the Fermi coupling constant and
the electron density in matter. The sign of
depends on the sign of
. A positive (negative) sign of
signifies that the lightest mass eigenstate
is the eigenstate that has the largest mixing with the electron (tau) neutrino [
5,
6]. It is positive (negative) for the normal (inverted) ordering of neutrino masses. This definition stems from the analogy with quarks. The normal ordering reflects the possible similarity between the mass hierarchy of neutrinos and that of quarks. Evidence for the inverted ordering (
) would show that the mass hierarchy of the neutrinos follows the opposite quark pattern. In inverted order, the lightest neutrino mass eigenstates are mainly mixed with the tau neutrino, whose charged counterpart (the tau lepton) is the heaviest among charged elementary leptons.
The relevance of Equation (
6) for experimental neutrino physics was established between 2002 and 2012 and brought long-baseline experiments to the forefront of neutrino physics. Long-baseline experiments can easily achieve
(the oscillation peak if we neglect matter effects) because accelerator neutrinos with a mean energy of 1 GeV have
when
Since
(see
Table 1), the oscillation peak at 1 GeV corresponds to a baseline of 495 km and matter effect does not change this finding by more than 20%. The ideal baselines for those facilities are thus well within the range of terrestrial experiments. Thanks to the measurements of
provided by solar [
8,
13,
14] and reactor [
15] experiments in the 2000s, we became aware that
. This result boosted proposals for long-baseline beams because the size of the subdominant
and
terms in the master formula are not too small compared with the leading term
. Still, the overall size of
driven by
and the key measurement of
only became available in 2012. The value measured by Daya Bay [
16], RENO [
17], Double Chooz [
18], and T2K [
19,
20] turned out to be very large, just below the previous limits from Chooz [
5,
21,
22]. Indeed, the smallest neutrino mixing angle (
) has a size comparable with the Cabibbo angle (
, i.e., the largest quark mixing angle, and brings the leading term of the master formula to
The discovery of
demonstrated that a long-baseline experiment capable of investigating oscillation probabilities at a <1‰ level could reconstruct the neutrino Yukawa sector of the Standard Model, with the exception of determining the size of the lightest mass eigenstate. This realization led to the design and construction of
Superbeams: neutrino beams generated by megawatt-class proton accelerators, directed towards neutrino detectors of unprecedented mass situated hundreds of kilometers from the sources [
23]. These remarkable facilities represent the evolution of long-baseline experiments such as K2K [
24], OPERA [
2], T2K [
25], and NOvA [
26], and are the focus of this paper.
3. The HyperKamiokande Experiment
The T2K experimental facility is anchored by a proton accelerator, the JPARC Proto-Synchrotron, boasting an energy output of 30 GeV and supporting a beamline equipped with three magnetic horns [
27,
28]. Mesons travel to and decay within a 96-meter-long decay volume. While the facility was initially designed to achieve a nominal power of 750 kW, this benchmark was only recently reached. However, the beamline is structured to accommodate upgrades on a Superbeam scale, with the potential for power enhancements up to a maximum of 1.3 MW. Plans for such an upgrade were in place well before the discovery of
[
29], but post-2012, it became apparent that an upgraded T2K would be optimally configured to uncover a CP violation in the leptonic sector and precisely measure
[
30]. This ambitious goal necessitates a 1.3 MW beam, contingent upon the availability of a far detector significantly larger than SuperKamiokande (SK). Presently, T2K is nearing completion of its physics program following upgrades to the near detector and the introduction of gadolinium doping in SK, enhancing its neutron tagging efficiency. The cornerstone of the forthcoming HyperKamiokande facility lies in the deployment of a far detector five times the size of SK, leveraging the T2K beam at its maximum 1.3 MW power capacity [
31]. Approved in January 2020, the HyperKamiokande project is progressing steadily, with data collection slated to commence in 2027.
HyperKamiokande employs the same detection strategy as T2K. HK will be a water Cherenkov detector with a water mass of 258 kton (fiducial mass: 187 kton). It consists of a cylindrical tank of 68 m diameter and 71 m height. Like SK, the tank volume will be divided into the Inner Detector and the Outer Detector by an inactive cylindrical structure. The structure optically separates the two detector volumes and holds the PMTs looking both inwards to the Inner Detector and outwards to the Outer Detector. The Outer Detector consists of 8 cm PMTs and wavelength shifting plates. It is used to reject cosmic ray muons to constrain the external background.In the Inner Detector, there will be 20,000 50 cm (20 inches) diameter PMTs by Hamamatsu Photonics and approximately 800 multi-PMT modules (mPMTs). The HyperKamiokande PMTs perfect a technique that has been developed in the course of the upgrades from Kamiokande [
32] to SuperKamiokande [
33] to HyperKamiokande. The HK PMTs have the same size (20” diameter) as the “Venetian blinds” PMTs used in the Super-Kamiokande detector, but a higher quantum efficiency and different dynode structure. The transit time spread (2.7 ns) is smaller leading to better time resolution at one photo-electron equivalent pulse height. The dark noise is about 4 kHz and each PMT covers about 2000 cm
2. The light yield of 20,000 installed PMTs is about 6 photoelectrons/MeV. Leveraging the studies performed by non-accelerator experiments (JUNO [
34] and KM3NeT [
35]), HK will also employ about 800 multi-PMTs made of 3” devices. The 3” PMTs are not arranged facing parallel directions, but point in slightly different directions. The better granularity and directional sensitivity of these smaller PMTs will thus improve the detector systematics and energy calibration.
The excavation of the HK cavern is unprecedented in neutrino physics. The main cavern consists of a rooftop portion, which is called a “dome section,” and a cylindrical “barrel section” under the dome section. The main cavern is approximately 94 m high (the dome section is 21 m high, and the barrel section is 73 m high) with a diameter of 69 m. The total excavation volume of the main cavern is approximately 330,000 m
3 [
36]. At the time of writing, most of the access tunnels are available and the excavation of the main cavern is close to completion.
The core upgrade of the T2K beamline in preparation for HK resides in the operating conditions of the PS Main Ring. Since the beam power is inversely proportional to the repetition cycle, and is proportional to the number of protons per pulse, both parameters will be enhanced. At present, the repetition cycle is 2.48 s (
protons/cycle) and will be upgraded to 1.16 s (
protons/cycle). This implies the replacement of the power supplies for the main magnets and the RF cavities. The HK baseline is very similar to T2K. The detector will be hosted in the Tochibora mine, about 295 km away from the J-PARC proton accelerator research complex in Tokai, Japan. It will lie under the peak of Nijuugo-yama, with an overburden of 650 m of rock or a 1750 m water equivalent. It will be offset with respect to the beam axis by about 2.5°, as in T2K. The off-axis configuration allows for a narrower energy spread of the incoming neutrinos, whose mean energy will be 0.6 GeV. For such a baseline, matter effects are negligible and
in Equation (
6). As a consequence, the master formula does not depend on the sign of
, and CP-violating effects are easier to establish, even when using a beam with a small momentum spread.
The strength of the HK program is twofold. HK offers a clear environment to establish CP violation in the leptonic sector comparing the
oscillation probability with the corresponding
probability measured in
-enriched runs. In addition, HK showcases impressive physics capabilities with natural neutrino sources given its size and underground location. The observation of atmospheric neutrinos using the same technique employed by SK is particularly rewarding. Since all oscillation parameters are fixed by long-baseline data, HK will employ a large sample of atmospheric
and
interactions to measure matter effects and establish the sign of
using an independent neutrino source. This method partially overcomes the lack of matter effects in beam events and can establish the neutrino ordering using the same technique as SuperKamiokande [
37] but with enhanced statistical power.
Figure 1 shows the sensitivity of HK to CP violation as a function of the true value of
assuming the mass ordering to be measured with HK atmospheric neutrinos or other experiments (JUNO, ORCA, NO
A, and DUNE). The beam from J-PARC is expected to provide
protons-on-target (pots) per year [
38]. The sensitivity to
mainly comes from
’s appearance, while the sensitivity to
and
is mostly due to disappearance data (
). Since the flux and cross-section of antineutrinos at 0.6 GeV is about three times smaller than neutrinos, the HK collaboration is planning to increase the duration of
-enriched runs at a ratio of 3:1 compared with the
-enriched runs. HK is very sensitive to CP violation and can get higher than eight
significance for excluding CP conservation, assuming the mass ordering is known. After 10 years of data collection, CP conservation will be excluded for 61% of true values of
assuming normal ordering.
HK is not expected to improve oscillation parameters such as
and
compared to dedicated reactor experiments like JUNO [
39]. This is because the dependence of the master formula on these parameters is weak, and the observation of oscillations at the ’solar peak’ by reactor or solar neutrino experiments is more effective. This oscillation maximum corresponds to
and long-baseline accelerator neutrino experiments usually operate far from this peak. In the master formula, the large distance from the solar peak of accelerator neutrinos corresponds to the
suppressions of the terms representing three-family interference (
and
), as well as the
term
, which is due to the oscillations driven by
. Conversely, HK and DUNE will play a key role in understanding whether the mixing induced by
is maximal (
) or deviates from maximality. The determination of the
octant of
, which is of relevance for flavor models, can be established by HK. The wrong octant can be excluded at 3
for true
and true
.
The physics capabilities of HK hinge on a comprehensive systematic reduction program, as both HK and DUNE stand to gain from the unparalleled statistics generated by the beam intensity and detector size. Systematic uncertainties are primarily tackled by the near detector, which tightly constrains the flux prior to oscillations. This detector plays a pivotal role in mitigating other sources of systematic uncertainty, such as cross-section uncertainties and detector inefficiencies. Additionally, the reduction program incorporates ancillary measurements, such as hadroproduction experiments utilizing an HK replica target, or novel assessments of neutrino cross-sections derived from specialized experiments [
40]. This underscores why the near detector complexes of HK and DUNE are the most advanced facilities proposed to date.
In addition to the T2K near detector upgrade [
41], the HK collaboration is planning an intermediate water Cherenkov detector [
31]. The detector utilizes an innovative design pioneered by the PRISM collaboration [
42] for HK and also adopted by DUNE. The intermediate water Cherenkov detector (IWCD) of HK will consist of a tall vertical shaft outfitted with multiple PMTs, situated roughly 1 km from the beam source. The IWCD is movable along the shaft in the vertical direction, allowing for off-axis angles ranging from one to four degrees. This flexibility enables the monitoring of the beam at various energies, including the off-axis angle relevant to HK, facilitating a data-driven modeling approach for extrapolating the flux from the near to the far detector. The IWCD will also detect events using the same water Cherenkov technology as the far detector, as the event rate at 1 km is manageable and the overlap of Cherenkov rings from different events is negligible. Employing a water Cherenkov detector at the near location (250 m) is not feasible due to the unprecedented beam intensity. Instead, the near detector of T2K/HK relies on alternative techniques, which may introduce efficiency biases in the extrapolation from the near to the far detector.
4. The DUNE Experiment
The design approach of DUNE differs significantly from that of HK [
43]. While water Cherenkov detectors provide scalability advantages due to the low cost of the target material (water), they come with limitations in resolution. Reconstruction of neutrino interactions is hindered by final state particles below the Cherenkov threshold and by events with large multiplicities, leading to overlapping Cherenkov rings. In contrast, DUNE utilizes detectors much smaller than HK but focuses on achieving precise neutrino reconstruction through the use of liquid argon time projection chambers (LArTPC).
The DUNE project encompasses two primary facilities aimed at supporting the US particle and astroparticle physics program in the coming years. The first facility is a new Superbeam that utilizes the same proton accelerator as NOvA but with enhanced performance [
44]. Neutrinos are produced after the protons hit a solid target and produce mesons, which are subsequently focused by three magnetic horns into a 194 m long helium-filled decay pipe where they decay into muons and neutrinos. Protons (120 GeV) are provided by the Fermilab Main Injector, which is expected to deliver 1.2 MW for the DUNE/LBNF program, with the PIP-II upgrade, corresponding to
protons on target per year. This setup will serve Phase I of DUNE, where a wide-band neutrino beam with a mean energy of approximately 2.5 GeV will reach two LArTPCs located 1300 km from the source. Each TPC will contain 17 kton of liquid argon, corresponding to a fiducial mass of about 10 kton per TPC. DUNE will undergo further upgrades in Phase II, during which the beam intensity will progressively increase to over 2.1 MW, and the beam will serve up to four LArTPCs, resulting in a total fiducial mass of about 40 kton.
The second facility is a large underground laboratory currently under construction in Lead, South Dakota. Known as the Sanford Underground Research Facility (SURF), it will host the DUNE TPCs and is situated within the former Homestake Gold Mine. SURF already serves as the host laboratory for dark matter experiments (such as LZ [
45]) and neutrinoless double beta decay experiments (such as the Majorana Demonstrator). Excavation of the underground halls and ancillary facilities for DUNE was completed in February 2024, and preparations are underway for the installation of the DUNE cryostats.
A notable characteristic of the DUNE neutrino beam (LBNF) is the momentum range of the produced neutrinos. Unlike HK, DUNE is situated along the axis of a wide-band beam. Consequently, DUNE captures oscillations from the first (2.5 GeV) to the second (0.6 GeV) oscillation peak. Observing the entire sinusoidal pattern of oscillations in a single detector enhances the potential to disentangle the effects of the operators in the master formula. This capability is exclusive to high-resolution detectors like the LArTPCs and is pivotal in unraveling the correlation among the oscillation parameters. Specifically, DUNE can concurrently measure the magnitude of , the sign of (mass ordering), and the octant of without the need for external information.
The first DUNE LArTPC [
46] builds upon the knowledge acquired from ICARUS [
47] and MicroBOONE [
48], with an emphasis on scalability given the substantially larger TPC mass compared to ICARUS (600 t). The TPC drift length is 3.5 m and the cathode is operated at -180 kV. To accommodate the relatively short drift length, each TPC features two cathodes and three anodes, as illustrated in
Figure 2. The anode wires are arranged within modules called Anode Plane Assemblies (APAs), measuring
m
2. These APAs are assembled on-site. They both simplify construction and remove the necessity for wires of much greater length compared to those used in ICARUS. The TPC components are thus designed to be modular, allowing for on-site assembly in the underground laboratory, and the cryogenic system has been significantly streamlined. In 2016, ProtoDUNE-SP demonstrated the feasibility of achieving an electron lifetime comparable to that of ICARUS using a cryostat based on cost-effective technology originally developed for industrial applications [
49]. A “membrane cryostat” consists of a corrugated membrane that contains both liquid and gaseous argon, along with a passive insulation system to minimize heat leakage. The structure also includes a reinforced concrete framework to support the pressure exerted by the contents. Additionally, a secondary barrier system integrated into the insulation protects against potential spills of liquid argon, while a vapor barrier applied over the concrete safeguards the insulation from moisture. This system, traditionally employed in the transportation of liquefied natural gases, has been adapted and refined for use with high-purity argon during the research and development phase of DUNE. The use of membrane cryostats remarkably simplified the design of DUNE and this technology will be employed for all DUNE TPCs.
Unlike ICARUS, the charge readout electronics are positioned within the cold volume to minimize noise. This approach enhances noise reduction and decreases the requirement for cryostat penetrations to read the signals from the anodes. Similar to any LArTPC, DUNE also captures the 128 nm scintillation light generated in liquid argon by charged particles. However, significant changes have been made to the light detection system compared to previous detectors. The DUNE system employs a compact device (X-ARAPUCA [
50,
51]) that shifts the photon wavelength toward values that are more amenable to detection by SiPMs and traps those photons inside a finite volume, whose walls are covered by SiPMs. The compact nature of the system enables it to be positioned inside the APA, right before the (semi-transparent) wires of the TPC.
The second DUNE TPC [
52], known as the “Vertical Drift,” capitalizes on the advancements in LArTPC technology made over the past decade. Building on the exceptional performance of the membrane cryostats and the purification system demonstrated in ProtoDUNE-SP, the Vertical Drift TPC features a 6.5 m drift length, with the electric field generated by a cathode positioned in the center of the TPC at -300 kV. Consequently, the ionization electrons drift vertically towards two anodes situated at the bottom and top of the TPC. Additionally, the anode wires are replaced with strips on PCBs, presenting an innovative design that further streamlines detector construction and reduces costs compared to the APA solution used in the first TPC (“Horizontal Drift”). While the photon detection system still relies on the X-ARAPUCA technology, these devices cannot be installed in the anode due to the opacity of the charge readout strips to light. Instead, in the DUNE Vertical Drift, photon detectors are positioned in the lateral walls of the cryostat just outside the (semi-transparent) field cage and in the cathode. However, since the cathode operates at a -300 kV voltage reference, these devices cannot be read and powered by standard copper cables due to discharge risks. Consequently, the signal is converted into light pulses using commercial optocouplers operated at the temperature of liquid argon (87 K) and transmitted via optical fibers (Signal-over-Fiber). The same technique is used with high-power lasers (Power-over-Fiber) to provide power to the cold electronics and SiPMs used for photon detection.
The DUNE near detector serves multiple purposes, including monitoring the neutrino flux and flavor at the source, obtaining detailed information on beam composition, detecting spectrum biases in near-to-far extrapolation, and mitigating cross-section uncertainties [
53]. A crucial component of the DUNE ND is an LArTPC built using ArgonCube technology, known as ND-LAr. This detector shares the same target nucleus and fundamental detection principles as the far detector but is specifically designed to handle the high event rate near the source. However, ND-LAr begins to lose muon acceptance above 0.7 GeV/c due to lack of containment, necessitating the use of a muon spectrometer as a complement. Both detectors can be horizontally moved perpendicular to the beam axis, employing the same PRISM technique as the HK intermediate Water Cherenkov detector.
The SAND [
53,
54] detector, located on the beam axis, serves as the final component of the DUNE near detector suite. This magnetized beam monitor is crucial for monitoring the neutrino flux heading to the far detector from an on-axis position, where it exhibits higher sensitivity to variations in the neutrino beam. SAND utilizes the KLOE magnet and calorimeter, originally employed for kaon physics studies at the DA
NE collider since the 1990s [
55], now repurposed for DUNE by the Italian Institute for Nuclear Research (INFN). SAND comprises an inner tracker surrounded by the KLOE electromagnetic calorimeter within a large solenoidal magnet. The tracker is composed of straw-tubes, while the magnet features a superconducting coil generating a 0.6 T magnetic field. The calorimeter is a high-resolution, high-granularity lead-scintillator sampling e.m. calorimeter.
DUNE will achieve unparalleled sensitivity in determining mass ordering due to its long baseline and utilization of a wide-band beam. It is projected to determine the sign of
within approximately 2 years of Phase I of data collection, scheduled to commence in 2030. The ultimate sensitivity regarding the CP phase and the
octant is anticipated during Phase II.
Figure 3 and
Figure 4 show, in particular, the precision that can be achieved in the measurement of
and
after 10 years of data taking.
DUNE’s underground location at SURF, with an overburden of about 4300 m water equivalent (1490 m of rock), enables a diverse physics program involving natural sources. It thus complements the HyperKamiokande program. Thanks to the larger mass, HK provides unique sensitivity to proton decay in the mode while DUNE is competitive in the mode because the kaon is below the Cherenkov threshold. Similarly, HK offers unparalleled statistics in the event of a galactic supernova explosion, while DUNE can exploit the larger CC cross-section in argon compared with the elastic scattering typically used in water Cherenkov detectors.