Skip to content
Reaction atlas · CNO cycles

Radiative capture · CNO-III

17O(p,γ)18F

: oxygen‑17 + proton → fluorine‑18 + gamma rayHow to read the notation

ImprovingMeasured at LUNA
On this page

Oxygen-17 captures a proton and becomes radioactive fluorine-18. It opens the third CNO cycle.

In nova explosions this reaction makes fluorine-18. When fluorine-18 decays it emits positrons, and their annihilation produces γ-rays that space telescopes could detect in the first hours after the explosion. The rate also sets, together with 17O(p,α)14N, how much oxygen-17 and oxygen-18 a nova ejects, which is compared with the isotope ratios of presolar grains thought to come from novae.

Facts

How well known
Well measured at the temperatures of nova explosions; at the lower temperatures of ordinary stars it depends on a very weak resonance measured directly only once.
Live evaluation
No live evaluation yet · Evaluations
Reaction rates
Explore the rates →
Q-value · energy released
5.607 MeV
Gamow window
  • 65 ± 19 keVAGB star, 50 MK (CNO-III)
  • 165 ± 61 keVclassical nova, 0.2 GK (CNO-III)
Product 18F
radioactive, t½ = 1.83 h
Kind
Radiative capture

How it was measured

8 measurements, 2005–2024, 3 at LUNAShow the list
  1. 2005

    LENA, TUNLTriangle Universities Nuclear Laboratory

    Direct measurement at the surface · 140–540 keV (proton energy)

    Proton beams of up to 100 µA on tantalum backings anodised in 17O-enriched water; new thermonuclear rate including the 183 keV resonance. [1]

  2. 2005

    CSNSM, OrsayCentre de Sciences Nucléaires et de Sciences de la Matière (CNRS/IN2P3 and Université Paris-Sud), since 2020 part of IJCLab

    Activation · around Ep = 194 keV

    The (p,γ) channel of the 183 keV resonance measured by 18F activation, together with the (p,α) channel. [2]

  3. 2012

    DRAGON, TRIUMFTRIUMF

    Inverse kinematics and recoil separators · 250–500 keV

    S-factor measured in inverse kinematics with the DRAGON recoil separator, which detects the 18F recoils directly. [3]

  4. 2012

    Nuclear Science Laboratory, Notre DameUniversity of Notre Dame

    Direct measurement at the surface

    The primary γ-ray transitions were used in an R-matrix analysis to estimate the direct-capture contribution; the new rate combines these data with earlier S-factor determinations. [4]

  5. 2012

    LUNA 400 kVLaboratori Nazionali del Gran Sasso (INFN)

    Direct measurement underground · 200–370 keV

    First direct measurement in the Gamow window of classical novae; ωγ(183 keV) = 1.67 ± 0.12 µeV, the most precise value then, and a rate uncertainty reduced by a factor of 4. [5]

  6. 2014

    LUNA 400 kVLaboratori Nazionali del Gran Sasso (INFN)

    Direct measurement underground · nova Gamow window

    Full analysis of the LUNA campaign with prompt γ-ray detection and activation; recommended rate with which the oxygen and fluorine isotopes ejected by novae are predicted to about 10%. [6]

  7. 2015

    LENA, TUNLTriangle Universities Nuclear Laboratory

    Direct measurement at the surface · 170–530 keV (proton energy)

    Beam currents up to 2 mA; ωγ = (1.86 ± 0.13) µeV for the resonance at Ep = 193 keV and (13.70 ± 0.96) meV at 518 keV, and a direct-capture S(0) = 4.82 ± 0.41 keV b. [7]

  8. 2024

    LUNA 400 kVLaboratori Nazionali del Gran Sasso (INFN)

    Direct measurement underground · 64.5 keV resonance

    First direct measurement of the 64.5 keV resonance, the lowest strength ever measured directly: ωγ = 30 ± 6 (stat) ± 2 (syst) peV. The proton width, 34 ± 7 ± 3 neV, agrees with the LUNA result from the (p,α) channel. [8]

Measurements (EXFOR)

Every dataset EXFOR holds for this reaction, drawn by the energies it covers, against the energies a star uses.

33 datasets in 11 EXFOR entries, 1973–2017 · 4 without an energy range, not drawn

Temperature
Lowest energy in EXFOR
160 keV
Buckner et al., 2015 · S · C2155.002 Not yet in EXFOR: LUNA 400 kV (2024), 64.5 keV resonance.
Distance from the Gamow peak
2.5 Gamow widths above
E₀ = 65.1 keV, window 45.8–84.5 keV
Rate from energies not in EXFOR
> 99.99%
at T₉ = 0.05, smooth estimate · > 99.99% of it lies below the lowest energy in EXFOR
100 eV1 keV10 keV100 keV1 MeV10 MeVCentre-of-mass energy (keV)E₀ = 65.1 keVσSσ→Eₓdσ/dΩωγlowest in EXFOR 160 keV
  • Gamow window, hatched where no measurement reaches
  • Outlined bars are shown but not counted (the rule is under “How these numbers are made”).
  • A diamond is a dataset at a single energy. Bars running off the right edge continue to higher energies.
The datasets of the gap map, by quantity
The datasets of the gap map, by quantity
QuantityDatasetsE_cm range (keV)
σcross section3257 keV – 1.7 MeV
SS-factor710 keV – 1.78 MeV
σ→Eₓpartial5167 keV – 1.53 MeV
dσ/dΩangular distribution6283 keV – 1.81 MeV
ωγresonance strength8557 eV – 1.04 MeV
How these numbers are made

Lowest measured energy, everywhere in the data explorer: the lowest centre-of-mass energy at which a dataset in EXFOR measures the reaction itself (cross section, S-factor, angular distribution, yield or resonance strength), judged point by point. A point counts when it is a value, not an upper or lower limit, when it lies at least one standard deviation above zero, and when its energy is physical: at least 1 keV for charged particles, and not below the threshold of an endothermic reaction. Not counted: extrapolated, calculated, evaluated or derived values; superseded, deleted or preliminary data; ratios; a single S-factor value, which in EXFOR is a fit result; and indirect methods (Trojan horse, Coulomb dissociation, ANC, surrogate reactions), recognized from EXFOR's method and analysis codes, their text and the title. Frame and unit errors of EXFOR are corrected first, and values the literature shows to be upper limits are read as limits, from a list that gives the evidence for each. Datasets that reach the same energy within 0.5% are all credited, earliest first. Rate from energies not in EXFOR: the share of the rate integrand at that temperature outside the energy ranges the counted datasets cover (from their lowest measured point to their highest), with a constant S-factor (σ ∝ S(E₀)/E · e^−2πη, so the integrand is e^(−E/kT − 2πη)); for a neutron capture, σ ∝ 1/v. Resonances make the real integrand lumpy, so read it as a smooth baseline.

Details

How well known, in detail: The nova-relevant resonance is measured directly to about 7%; at lower temperatures the 64.5 keV resonance, measured directly only once, and the direct-capture component dominate the uncertainty.

At nova temperatures the rate is dominated by the resonance at E = 183 keV together with the non-resonant direct-capture contribution; at lower temperatures the narrow resonance at 64.5 keV also contributes. The 183 keV resonance strength and the direct-capture S-factor have been measured with prompt-γ, activation and recoil-separator techniques; the γ-ray decay of the resonance proceeds through many cascades, which makes efficiency and angular corrections important. The LUNA measurements at Gran Sasso gave ωγ(183 keV) = 1.67 ± 0.12 µeV and reduced the rate uncertainty at nova temperatures by a factor of 4; the lower background revealed γ-ray transitions missed at the surface. In 2024 LUNA also measured the 64.5 keV resonance directly, ωγ = 30 ± 6 (stat) ± 2 (syst) peV, about twice the value adopted from indirect data.

Peak energy E0 ± half the 1/e width, centre of mass, from the AME2020 masses.

Evaluations

Compilations that combine the data into a recommended rate.

  • —B. Acharya et al., Rev. Mod. Phys. 97, 035002 (2025) [9]

Open questions

  • The direct-capture S-factor between the low-energy resonances.
  • The strength of the 64.5 keV resonance, where the direct result is about twice the value from indirect data.

Related reactions

References

  1. 1.

    C. Fox, C. Iliadis, A. E. Champagne, R. P. Fitzgerald, R. Longland, J. Newton, J. Pollanen and R. Runkle

    Thermonuclear reaction rate of 17O(p,γ)18F

    Phys. Rev. C 71, 055801 (2005) · 10.1103/PhysRevC.71.055801

  2. 2.

    A. Chafa, V. Tatischeff et al.

    Hydrogen burning of 17O in classical novae

    Phys. Rev. Lett. 95, 031101 (2005) · 10.1103/PhysRevLett.95.031101 · arXiv:astro-ph/0506500

  3. 3.
  4. 4.

    A. Kontos, J. Görres, A. Best, M. Couder, R. deBoer, G. Imbriani, Q. Li, D. Robertson, D. Schürmann, E. Stech, E. Uberseder and M. Wiescher

    Proton capture on 17O and its astrophysical implications

    Phys. Rev. C 86, 055801 (2012); erratum Phys. Rev. C 88, 029905 (2013) · 10.1103/PhysRevC.86.055801 · arXiv:1210.7866

  5. 5.
  6. 6.

    A. Di Leva et al. (LUNA Collaboration)

    Underground study of the 17O(p,γ)18F reaction relevant for explosive hydrogen burning

    Phys. Rev. C 89, 015803 (2014) · 10.1103/PhysRevC.89.015803LUNA

  7. 7.

    M. Q. Buckner, C. Iliadis, K. J. Kelly, L. N. Downen, A. E. Champagne, J. M. Cesaratto, C. Howard and R. Longland

    High-intensity-beam study of 17O(p,γ)18F and thermonuclear reaction rates for 17O + p

    Phys. Rev. C 91, 015812 (2015) · 10.1103/PhysRevC.91.015812

  8. 8.
  9. 9.

How to cite this page

J. Skowronski, 17O(p,γ)18F, in Reaction atlas, 2026-10-12, https://jskowron.eu/atlas/17O-pg-18F.

Cite the date you used; it is the last change to this page.

Something wrong or missing? Report an error (opens a new issue on GitHub) · Suggest a reaction (opens a new issue on GitHub)