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Inverse beta decay

Inverse beta decay (IBD), also known as antineutrino-proton scattering, is a charged-current process in which an electron antineutrino interacts with a proton to produce a and a , as described by the reaction \bar{\nu}_e + p \to n + e^+. This reaction serves as the primary mechanism for detecting reactor antineutrinos and has a kinematic of approximately 1.806 MeV for the incoming antineutrino, arising from the -proton difference of about 1.293 MeV plus the rest . The cross-section for this process is on the order of $10^{-43} to $10^{-42} cm² at typical reactor antineutrino energies around 1–10 MeV, making it rare but detectable in large target volumes. The process was first experimentally observed in 1956 by Clyde Cowan and at the Savannah River nuclear reactor, confirming the existence of the predicted by in 1930 to conserve energy, momentum, and in . Their experiment utilized a detector consisting of sandwiches around a cadmium-loaded target, identifying IBD events through the prompt annihilation signal (two 511 keV gamma rays) followed by the delayed gamma rays on nuclei, achieving a detection rate of about 3 events per hour. received the in 1995 for this pioneering work, which validated the weak force's role in interactions. Since its , inverse beta decay has become central to physics, enabling precise measurements of fluxes from reactors for studies of , sterile neutrinos, and reactor monitoring. Modern experiments like Daya Bay, Double Chooz, and RENO rely on IBD in organic liquid scintillators doped with for enhanced detection, achieving sub-percent precision in oscillation parameters such as \sin^2 2\theta_{13}. As of 2025, the experiment, which began data taking in 2024, also uses IBD to determine the mass hierarchy. The reaction's simplicity and clean —distinguished by the positron's energy correlating with the antineutrino energy—make it indispensable, though backgrounds from accidental coincidences and other interactions require careful mitigation.

Fundamentals

Definition

Inverse beta decay refers to the that reverses the process of , where a interacts with a to transform it into the opposite type of while producing a corresponding charged . In , a decays into a proton, , and electron antineutrino (or a proton into a , , and ), mediated by the ; inverse beta decay inverts this by absorbing a to effect the change. This process exemplifies charged-current s and is fundamental to understanding physics. The primary and most studied form of inverse beta decay involves an electron antineutrino interacting with a free proton, yielding a and a according to the balanced equation: \bar{\nu}_e + p \rightarrow n + e^+ This , often denoted as IBD, requires the antineutrino to possess sufficient to overcome the mass between the proton and , enabling the transformation. The process is mediated by the charged-current via the exchange of a virtual W^- boson, which couples the left-handed and currents, facilitating the down- to up- transition in the and the electron antineutrino to flavor change. The reaction adheres to key conservation laws, including (preserved as both initial and final states feature one ), (net zero on both sides), and electron (both the antineutrino and contribute -1).

Historical Background

The neutrino hypothesis emerged in the context of beta decay theory when proposed in 1930 that a , later named the , was emitted alongside the electron and antineutrino to conserve and in beta decay processes. This idea was formalized by in his 1934 theory of beta decay, which incorporated the as an essential component of weak interactions, implicitly suggesting the existence of inverse processes where neutrinos could interact with matter to induce beta-like transitions. In 1946, proposed using inverse beta decay as a practical method for detecting s, specifically through the reaction \nu_e + Z \to e^- + (Z+1), where a interacts with a to produce an and a higher isotope, enabling experimental observation of these elusive particles. This suggestion built on the theoretical framework and highlighted the potential for reactor-based experiments to generate sufficient neutrino flux for detection. The first experimental effort to observe inverse beta decay was undertaken by Clyde Cowan and Frederick Reines, who in 1953 deployed a detector at the Hanford nuclear reactor using a 300-liter liquid scintillator target to search for antineutrinos via \bar{\nu}_e + p \to n + e^+, but encountered significant challenges including high cosmic ray backgrounds and inconclusive signals of about 0.4 events per minute. Addressing these issues, they redesigned the apparatus with a larger 1400-liter scintillator and a water-cadmium chloride target for better neutron capture and moved to the higher-flux Savannah River reactor in 1955, achieving clear confirmation in 1956 with a detection rate of 3.0 events per hour, definitively verifying the neutrino's existence through inverse beta decay. Reines received the 1995 Nobel Prize in Physics for this breakthrough, with Cowan recognized posthumously. Subsequent experiments further validated neutrino-induced variants of inverse beta decay, notably the Homestake Mine detector initiated in the 1960s by Raymond Davis Jr., which employed perchloroethylene to capture solar neutrinos via \nu_e + ^{37}\mathrm{Cl} \to ^{37}\mathrm{Ar} + e^-, measuring fluxes that revealed discrepancies with theoretical predictions and advanced solar neutrino physics.

Theoretical Framework

Kinematics and Energy Threshold

Inverse beta decay (IBD) is a two-body reaction described by \bar{\nu}_e + p \to e^+ + n, where the incoming electron antineutrino interacts with a target proton at rest in the laboratory frame, producing a positron and a neutron. Due to the extremely small mass of the neutrino (upper limit < 0.45 eV/c² from direct measurements as of 2025, and sum of masses < 0.12 eV from cosmology), relativistic effects are negligible, and the antineutrino propagates essentially as a massless particle with momentum |\vec{p}_{\bar{\nu}_e}| \approx E_{\bar{\nu}_e}/c. Kinematic analysis requires conservation of four-momentum in the reaction, leading to constraints on the minimum energy for the process to occur. The energy threshold arises because the rest mass of the final state (m_n + m_e) exceeds that of the initial state (m_p, with m_{\bar{\nu}_e} \approx 0), necessitating sufficient to enable the transition. In the laboratory frame, with the proton at rest, the threshold antineutrino energy E_{\rm th} is derived by setting the center-of-mass energy \sqrt{s} equal to m_n + m_e, the minimum for producing the final particles at rest in the CM frame. The Mandelstam variable s = (E_{\bar{\nu}_e} + m_p c^2)^2 - (p_{\bar{\nu}_e} c)^2 \approx m_p^2 c^4 + 2 m_p c^2 E_{\bar{\nu}_e} (in units where c=1). Setting s = (m_n + m_e)^2 yields: E_{\rm th} = \frac{(m_n + m_e)^2 - m_p^2}{2 m_p} \approx 1.806 \, \rm MeV, using m_p = 938.272 \, \rm MeV/c^2, m_n = 939.565 \, \rm MeV/c^2, and m_e = 0.511 \, \rm MeV/c^2. This value accounts for the neutron-proton mass difference \Delta = m_n - m_p \approx 1.293 \, \rm MeV and the positron rest mass. Below this threshold, the reaction is kinematically forbidden. In the laboratory frame, the CM frame moves with velocity \beta_{\rm CM} \approx E_{\bar{\nu}_e} / (E_{\bar{\nu}_e} + m_p) relative to the lab, but for typical IBD energies (E_{\bar{\nu}_e} \sim 1{-}10 \, \rm MeV), \beta_{\rm CM} \ll 1, so lab and CM kinematics are nearly coincident, with small recoil effects on the neutron (typically <50 keV). The positron total energy E_{e^+} and the antineutrino energy are related approximately by E_{\bar{\nu}_e} \approx E_{e^+} + \Delta, neglecting higher-order recoil terms of order E_{e^+}^2 / m_p. More precisely, including recoil: E_{\bar{\nu}_e} \simeq (E_{e^+} + \Delta) \left(1 + \frac{E_{e^+}}{m_p}\right) + \frac{\Delta^2 - m_e^2}{m_p}, which simplifies to E_{\bar{\nu}_e} \approx E_{e^+} + \Delta for E_{e^+} \ll m_p. The positron kinetic energy is then T_{e^+} = E_{e^+} - m_e \approx E_{\bar{\nu}_e} - \Delta - m_e. In detectors, the visible prompt energy E_{\rm vis} from the positron includes its kinetic energy plus the energy from annihilation into two 511 keV photons (assuming full containment): E_{\rm vis} = T_{e^+} + 2 m_e c^2 \approx E_{\bar{\nu}_e} - \Delta + m_e \approx E_{\bar{\nu}_e} - 0.782 \, \rm MeV. This relation allows reconstruction of the incident antineutrino energy from the measured prompt signal, with the delayed neutron capture providing coincidence tagging. The threshold implies that IBD is insensitive to antineutrinos below ~1.8 MeV, limiting its use for detecting low-energy sources like solar pp neutrinos (~0.4 MeV) or reactor antineutrinos near the spectrum tail below 2 MeV; detection efficiency rises sharply above the threshold and remains viable up to ~60 MeV, where multi-nucleon effects begin to alter the simple two-body kinematics.

Cross-Section and Interaction Details

The cross-section for inverse beta decay, a charged-current quasielastic process \bar{\nu}_e + p \to e^+ + n, is derived using , which relates the transition rate to the squared matrix element and the phase-space density of final states. The matrix element incorporates the V-A structure of the weak current, with the effective low-energy approximation yielding a total cross-section of \sigma \approx \frac{G_F^2 \cos^2 \theta_C}{\pi} (g_V^2 + 3 g_A^2) E_e p_e, where G_F = 1.166 \times 10^{-5} GeV^{-2} is the Fermi constant, \theta_C is the Cabibbo angle (\cos \theta_C \approx 0.975), g_V \approx 1 is the vector coupling constant (from the conserved vector current hypothesis), and g_A \approx 1.27 is the axial-vector coupling constant (determined from neutron beta decay). This form assumes point-like nucleons and neglects higher-order terms, with the numerical prefactor incorporating natural units conversion to yield \sigma \approx 9.5 \times 10^{-44} (E_e p_e / \mathrm{MeV}^2) cm^2, where E_e and p_e are the positron total energy and momentum, respectively. The dependence arises primarily from the phase-space factors E_e p_e, with E_e = E_{\bar{\nu}_e} - (m_n - m_p + m_e) + \mathrm{[recoil](/page/Recoil)} and p_e = \sqrt{E_e^2 - m_e^2}, leading to \sigma \propto E_{\bar{\nu}_e}^2 for E_{\bar{\nu}_e} \gg 1.8 MeV (the kinematic ). At reactor antineutrino energies (\sim 1-10 MeV), this quadratic scaling dominates detection rates, though a \sigma \approx 9.2 \times 10^{-43} (E_{\bar{\nu}_e} / \mathrm{MeV}) cm^2 is sometimes used for rough flux estimates due to the near-relativistic . More precise calculations include nucleon form factors to account for the finite size of the proton and neutron. The vector form factors f_1(t) and weak magnetism f_2(t) follow dipole parametrizations with a vector mass scale M_V \approx 0.85 GeV, while the axial-vector form factor g_1(t) uses an axial mass M_A \approx 1.0 GeV, and the induced pseudoscalar g_3(t) (or g_P) contributes negligibly at low momentum transfer |t| \lesssim (10 \mathrm{MeV})^2 due to partial conservation of the axial current. Induced tensor terms g_2(t) and second-class currents are suppressed by O(10^{-3}). Radiative corrections, including inner (weak) and outer (QED) contributions, modify the cross-section by \sim 2\% at low energies, with the leading QED term \alpha/\pi \ln(m_p/E_e). These effects are incorporated in updated evaluations, reducing theoretical uncertainties to \sim 0.5\% at E_{\bar{\nu}_e} \sim 10 MeV. Recent calculations as of 2025 further refine these uncertainties to below 0.5% at reactor energies. In comparison to neutral-current processes, such as \bar{\nu}_e + p \to \bar{\nu}_e + p, the charged-current cross-section for inverse beta decay dominates by a factor of \sim 1/\sin^2 \theta_W \approx 4 at low energies, as the neutral-current amplitude is suppressed by the weak mixing angle (\sin^2 \theta_W \approx 0.23) and involves smaller effective couplings (g_V^p \approx 0.04, g_A^p \approx -0.5). This makes charged-current events the primary signal in antineutrino detectors, with neutral-current backgrounds comprising only \sim 10-20\% of the total rate.

Reaction Variants

Antineutrino-Induced Reaction

The antineutrino-induced inverse beta decay is the standard process for detecting electron antineutrinos from nuclear reactors, governed by the reaction \bar{\nu}_e + p \to e^+ + n. This charged-current interaction converts a proton into a neutron and produces a positron, serving as the primary detection channel for antineutrinos with energies above the reaction threshold. The reaction is endothermic, with a Q-value of Q = (m_p + m_{\bar{\nu}_e} - m_n - m_{e^+})c^2 \approx -1.804 MeV, derived from the neutron-proton mass difference of m_n - m_p \approx 1.293 MeV and the positron rest mass of $0.511 MeV (neglecting the near-zero antineutrino mass).[](https://physics.nist.gov/cgi-bin/cuu/Value?mnmmpc2mev) This negative Q-value necessitates a minimum antineutrino kinetic energy of approximately &#36;1.806 MeV for the reaction to occur on a stationary proton. The interaction yields a distinctive experimental signature: a prompt signal from the positron, which promptly annihilates with an to produce two back-to-back 511 keV s, and a delayed signal from the recoiling . The thermalizes via scattering in the medium before capture, typically on a proton via n + p \to d + \gamma, emitting a 2.223 MeV after a mean delay of about 200 \mus in liquid or water-based detectors. This temporal separation between the prompt positron event and the delayed enables robust rejection of uncorrelated backgrounds through coincidence gating. For antineutrinos from reactors, which have a extending from roughly 2 MeV to 8 MeV with an average near 2 MeV, the cross-section is small but features helicity suppression at low energies due to the right-handed of the antineutrino conflicting with the left-handed V-A weak current. In this regime, the axial-vector component dominates the cross-section, contributing a factor of approximately three times more than the vector part in the effective low-energy approximation \sigma \propto g_V^2 + 3 g_A^2, where g_V \approx 1 and g_A \approx 1.27.

Neutrino-Induced Reaction

The neutrino-induced variant of inverse beta decay involves the charged-current in which an is absorbed by a , resulting in the production of a proton and an : \nu_e + n \to p + e^- This process is exothermic, with a Q-value of approximately 0.782 MeV arising from the neutron-proton mass difference (m_n - m_p ≈ 1.293 MeV, minus the of 0.511 MeV), allowing it to occur for arbitrarily low neutrino energies without a strict kinematic , unlike the endothermic antineutrino counterpart. In practice, the cross section vanishes at zero energy and rises as σ ≈ 9.5 × 10^{-46} (E_ν / MeV)^2 cm² for free s at low energies (E_ν ≲ 30 MeV), governed by the V-A structure of the . When occurring on bound neutrons within nuclei, the effective energy threshold increases due to nuclear binding energies, Coulomb barriers, and possible excitation of the daughter nucleus, often shifting it to several MeV or higher. The prompt signal consists of the energetic electron, detectable via ionization or , without the characteristic positron gamma rays seen in antineutrino-induced reactions; the proton is typically low-energy (≲ 10 MeV) and may escape detection in dense targets. The total cross section remains of similar magnitude to the antineutrino case (∼10^{-45} to 10^{-44} cm² at MeV scales). This reaction is particularly valuable for detecting low- to moderate-energy electron neutrinos, such as those from fusion, where it provides flavor-specific charged-current sensitivity. A seminal example is the , which utilized the nuclear variant ν_e + ^{37}Cl → ^{37}Ar + e^- (threshold 0.814 MeV) in a 615-ton target to measure fluxes via radiochemical extraction of the unstable ^{37}Ar product, yielding 2.56 ± 0.23 SNU over 25 years of operation. In water Cherenkov detectors like , charged-current reactions on bound neutrons in oxygen (e.g., ν_e + ^{16}O → ^{16}F + e^-, threshold ∼15.4 MeV) contribute to event samples for higher-energy neutrinos (primarily ^8B), supplementing the dominant channel and aiding in flavor composition studies, though their rate is suppressed by the elevated threshold.

Electron-Induced Reaction

The electron-induced inverse beta decay process involves a proton capturing an to form a and an , represented as p + e^- \to n + \nu_e. This reaction is equivalent to on protons but is conceptualized as the inverse of beta-minus decay in the context of weak interactions. This process predominantly occurs in extreme astrophysical environments, such as the cores of neutron stars or the dense plasmas within progenitors, where the degenerate electron gas achieves Fermi energies surpassing the reaction's energy threshold of approximately 0.78 MeV—corresponding to the effective Q-value accounting for the neutron-proton mass difference minus the . Unlike antineutrino- or -induced variants, it requires no incident neutrino and instead produces one, thereby serving as a neutrino emission mechanism rather than a detection channel. Kinematically, the reaction is endothermic, demanding incident electrons with relativistic energies to supply the necessary ~1.293 MeV for neutron production, which limits its feasibility to highly degenerate conditions. The associated cross-section remains low, constrained by factors that restrict the available final-state momentum configurations for the outgoing and , resulting in suppressed reaction rates even in dense media. Astrophysically, electron-induced inverse beta decay drives neutronization in the collapsing cores of massive during supernovae, progressively converting protons to neutrons and lowering the electron fraction Y_e to promote neutron-rich compositions essential for core collapse dynamics. In white dwarfs approaching the and in envelopes, repeated cycles involving this process and subsequent beta decays enable efficient cooling, releasing thermal energy and regulating .

Detection and Applications

Experimental Detection Methods

The detection of inverse beta decay (IBD) primarily relies on the distinctive prompt-delayed coincidence signature produced by the reaction \bar{\nu}_e + p \to [e^+](/page/E!) + [n](/page/N+), where the annihilation yields a prompt signal, and the subsequent emits a delayed . This temporal separation, typically on the order of microseconds to milliseconds, allows for effective identification of IBD events amid backgrounds. In liquid scintillator detectors, such as those employed in the Daya Bay and KamLAND experiments, the prompt signal arises from the positron's kinetic energy and subsequent annihilation gammas, producing visible light with energies above approximately 1.8 MeV, while the delayed signal comes from , often enhanced by doping to yield a characteristic 8 MeV gamma cascade within about 30 microseconds. -doped liquid scintillator, as used in Daya Bay with 0.1% Gd concentration, accelerates compared to undoped cases, improving time correlation and efficiency. In contrast, water Cherenkov detectors like detect the prompt Cherenkov light from the positron and a weaker delayed signal from on oxygen, which emits 2.2 MeV gammas after a longer mean time of around 200 microseconds, though with lower tagging efficiency. As of 2025, has been upgraded with doping (SK-Gd), enabling efficient neutron tagging in water Cherenkov detection for IBD events. Background rejection in IBD detection exploits the coincidence's spatial and temporal properties, requiring the prompt and delayed events to occur within a few meters and specific time windows (e.g., 1-200 microseconds in KamLAND), alongside pulse-shape discrimination to distinguish signals from -induced fast neutrons or accidental coincidences. veto systems, such as surrounding water shields in Double Chooz and Daya Bay, further suppress cosmogenic backgrounds by tagging high-energy muons that produce neutrons. Segmented detector designs, like the near-far configuration in Double Chooz, enable comparative analysis to isolate reactor signals from uncorrelated noise. Detection efficiency for IBD events depends on factors including the target proton density in the medium (e.g., higher in liquid scintillator than water), neutron capture cross-sections (favoring over for faster, more visible signals), and energy thresholds set above the 1.8 MeV kinematic limit to reduce noise. In gadolinium-doped systems, neutron capture efficiency reaches over 90%, compared to about 25% on alone, though overall IBD efficiency incorporates selection cuts and geometric factors, achieving values around 80-90% in experiments like Daya Bay. Contemporary advancements integrate IBD detection with coherent neutrino-nucleus scattering (CEvNS) in ton-scale detectors, leveraging CEvNS's lower energy threshold to probe reactor antineutrino fluxes below the IBD limit and cross-calibrate backgrounds, as explored in designs like those for surface-level ton-scale systems.

Applications in Neutrino Physics

Inverse beta decay (IBD) serves as a primary detection channel for electron antineutrinos in reactor-based experiments, enabling precise studies of neutrino oscillations. The KamLAND experiment, utilizing IBD signals from distant reactors, provided the first long-baseline confirmation of neutrino oscillations by observing a distortion in the antineutrino energy spectrum, yielding measurements of the solar mixing angle \sin^2 \theta_{12} = 0.304 \pm 0.022 and mass-squared difference \Delta m^2_{21} = (7.54 \pm 0.56) \times 10^{-5} eV². Similarly, the Daya Bay experiment measured reactor antineutrino disappearance over kilometer-scale baselines through IBD event rates and spectral analysis, determining \sin^2 2\theta_{13} = 0.0851 \pm 0.0024 and \Delta m^2_{32} = (2.466 \pm 0.060) \times 10^{-3} eV² for normal mass ordering with a dataset of over 5.55 million IBD candidates. These results, derived from the characteristic prompt-delayed coincidence signature of IBD, have established the three-flavor neutrino oscillation framework and constrained matter effects in solar neutrino propagation. IBD facilitates antineutrino flux monitoring for applications in nuclear non-proliferation and geophysics. In non-proliferation efforts, compact IBD detectors placed near reactor cores can remotely monitor fissile material burnup and detect diversions, as antineutrino emission correlates directly with reactor power; a typical 1 GW thermal reactor emits approximately $1.9 \times 10^{20} antineutrinos per second, allowing detection of an 8 kg plutonium diversion with over 90% confidence in 90 days using a 5-ton detector at 25 m distance. For geoneutrinos, the Borexino experiment observed IBD events from uranium and thorium decays in Earth's interior, reporting a rate of $3.9^{+1.6}_{-1.3} events per 100 ton-year and excluding a georeactor powering more than 3 TW at 95% confidence level, thereby informing models of Earth's radiogenic heat budget contributing about 50% to surface heat flux. Prospective detection of supernova neutrino bursts relies on the high cross-section of IBD for antineutrinos above 1.8 MeV. The detector, enhanced with for neutron tagging in IBD events, is expected to observe around 10,000 events from a galactic core-collapse at 10 kpc distance, enabling real-time alerts and multi-messenger astronomy; for the historical SN1987A at 50 kpc, similar signals would yield hundreds of events, constraining temperatures and burst dynamics. Searches for sterile neutrinos exploit IBD rate deficits in short-baseline experiments to probe anomalies like those suggested by LSND. The NEOS experiment, analyzing IBD events near a 2.8 GW , set limits on active-sterile mixing |\sin^2 2\theta_{ee}| < 0.013 for \Delta m^2 \sim 1 eV², consistent with no evidence for eV-scale sterile neutrinos and challenging interpretations of the antineutrino anomaly as new physics. Precision measurements using IBD highlight challenges in properties. Limits on the magnetic moment from experiments using on electrons, such as GEMMA, reach \mu_\nu < 2.9 \times 10^{-11} \mu_B at 90% confidence, though such processes can also appear as backgrounds in IBD detection. Absolute flux normalization remains uncertain due to discrepancies between predicted and measured IBD rates, with the antineutrino anomaly showing a 6% and an unexplained 5 MeV spectral bump, arising from incomplete nuclear beta-decay data and up to 15% uncertainties in isotope yields.