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The impact of new (α, n) reaction rates on the weak s-process in metal-poor massive stars

NUCLEAR PHYSICS AND INTERDISCIPLINARY RESEARCH

The impact of new (α, n) reaction rates on the weak s-process in metal-poor massive stars

Wen-Yu Xin,
Chun-Ming Yip,
Ken’ichi Nomoto,
Xian-Fei Zhang,
Shao-Lan Bi
Nuclear Science and TechniquesVol.37, No.8Article number 146Published in print Aug 2026Available online 20 May 2026
19600

Massive stars are significant sites for the weak s-process (ws-process). In metal-rich stars, 22Ne and 16O are, respectively, the main neutron source and poison for the ws-process. In metal-poor stars, however, the abundance of 22Ne is limited by metallicity, so the contribution of 22Ne(α, n)25Mg reaction on the s-process is smaller. Conversely, the 17O(α, n)20Ne reaction becomes more prominent in these stars because of the most abundant 16O at all metallicities. In this study, we calculated the evolution of four metal-poor stars (Z=10-3) for the Zero-Age Main-Sequence (ZAMS) masses of M (ZAMS) = 15, 20, 25, and 30 M⊙ to investigate the effect of reaction rates on the ws-process. We adopt the new 17O(α, n)20Ne and 17O(α, γ)21Ne reaction rates suggested by Best et al. (2013) and 22Ne(α, n)25Mg and 22Ne(α, γ)26Mg reaction rates from Wiescher et al. (2023). The yields of the s-process isotopes with the updated reaction rates are compared with the results using the default reaction rates from JINA REACLIB. We found that the new 17O+α reaction rates enhance the ws-process in all stages, whereas the new 22Ne+α reaction rates enhance the ws-process only in the C and Ne burning stages. Updating these new reaction rates would increase the production of ws-process isotopes by tens of times. We also note that for more massive stars, the enhancement by the new 17O+α reaction rates becomes more significant.

Massive starsSupernovaes-processNuclear reactionsNucleosynthesis
1

Introduction

Massive stars play crucial roles in galactic chemical evolution by synthesizing elements up to the iron group through charged-particle reactions during thermonuclear burning. The slow neutron capture process (s-process), produces heavy elements in stars by allowing atomic nuclei to capture neutrons at a rate slow enough to allow unstable isotopes to undergo beta decay before capturing additional neutrons.

In massive stars with Zero-Age Main-Sequence (ZAMS) masses greater than ~12 M⊙, the weak s-process (ws-process) is a key mechanism for producing neutron-rich isotopes, particularly those in the atomic mass range of A = 60–90 [1]. Early studies associated the ws-process primarily with core helium (He) burning [2-7]. Later research identified significant production during shell carbon (C) burning, which is characterized by higher temperatures and neutron densities [8-11]. More recent models include explosive nucleosynthesis during core-collapse supernovae (CCSNe), although these events have minimal impact on ws-process yields [12-16]. Limongi and Chieffi [14] and Tur et al. [15] showed that the yields of the ws-process are not strongly modified by supernova explosions.

In contrast to the main s-process in asymptotic giant branch (AGB) stars, which relies on the 13C(α, n)16O reaction, the ws-process in massive stars is driven by the 22Ne(α, n)25Mg reaction [2, 5, 17-19]. 22Ne in core He burning is produced via a sequence of reactions, 14N(α, γ)18F()18O(α, γ)22Ne. The ws-process is activated by the 22Ne(α, n)25Mg reaction once the temperature exceeds 2.0×108 K. During shell C burning, this reaction is re-activated by α produced by the 12C(12C, α)20Ne channel [20].

22Ne is primarily synthesized by α-capture involving 14N, whose amount depends on the initial metallicity of stars. Consequently, one would expect the yields of the ws-process elements to be low in metal-poor stars [6, 21]. However, recent observations found that the ws-process elements in metal-poor stars are not as low as previously predicted [22-24]. To account for this discrepancy, theoretical models have proposed that fast-rotating massive stars may enhance the production of ws-process elements. In these models, rotation can promote the mixing of 14N from the H-rich envelope into the convective core of He burning and increase their production [16, 24, 25].

Moreover, uncertainties in 17O+α reaction rates significantly affect the yields of the ws-process, particularly in metal-poor stars, where 16O acts as a major neutron poison through 16O(n, γ)17O reaction [26-28]. Subsequent competing reactions 17O(α, n)20Ne and 17O(α, γ)21Ne determine whether neutrons are released or captured. Although recent studies have explored these effects in rotating stars [25, 29, 30], few have investigated the combined impact of 17O+α and 22O+α reactions in non-rotating metal-poor stars. Since 16O is extremely abundant across all metallicities, the neutrons released by the 22Ne(α, n)25Mg reaction in metal-poor stars are possibly captured by 16O, instead of attending the ws-process, followed by a large amount of production of 17O. Therefore, the 17O(α, n)20Ne reaction could play a more important role.

In this study, we investigate the ws-process in non-rotating massive stars, specifically comparing the new reaction rates suggested in recent references with those in JINA REACLIB [31]. We evaluate the implications of these new reaction rates on the ws-process, emphasize how variations in these rates influence the nucleosynthesis. In Sect. 2, we present the parameters of our stellar models and compare the results using the reaction rates from the new references with those from JINA REACLIB. In Sect. 3, we use a model with M(ZAMS) = 25 M⊙ as an example to illustrate the evolution of metal-poor stars. We further compare the effects of the 17O+α and 22Ne+α reactions on nucleosynthesis in Sect. 4. We conclude the study in Sect. 6.

2

Models and Input Physics

We employ the Modules for Experiments in Stellar Astrophysics (MESA, version 12778; Paxton et al. [32-36], Jermyn et al. [37]) to follow various nuclear burnings and the structure evolution in stars from ZAMS until the Fe core collapse, when the infall velocity of the Fe core reaches 103 km s-1. We only focus on nucleosynthesis before the explosion, as the final explosion makes only a slight modification of the ws-process abundance [15].

We calculate the evolution of four metal-poor stellar models of M (ZAMS) = 15, 20, 25, and 30 M⊙ with MESA1. The trajectories of these models are utilized in the WinNet code [38] to investigate the effects of the reaction rates on the ws-process. For the 17O+α reactions, we incorporate both competing reactions, 17O(α, n)20Ne and 17O(α, γ)21Ne, as reported by Best et al. [39]. The reaction rates for 22Ne+α, including both the (α, n) and (α, γ) reactions, are updated according to Wiescher et al. [40]. To assess the impact of these reactions, we compare four reaction recipes for each model, as listed in Table 1. The differences among these reaction rates are discussed in Sect. 2.1. Most physical parameters follow Xin et al. [41, 42] with some changes clarified in Sect. 2.2. Section 2.3 outlines the setup within the WinNet code.

Table 1
The reaction recipes used in this work
Case 17O+α 22Ne+α
1 REACLIB* REACLIB
2 REACLIB Wiescher et al. [40]
3 Best et al. [39] REACLIB
4 Best et al. [39] Wiescher et al. [40]
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* The 22Ne+α reaction rates adopted in JINA REACLIB come from Longland et al. [9], while the 17O(α, n)20Ne and 17Ne(α, γ)21Ne reaction rates used in JINA REACLIB come from NACRE [27] and CF88 [28], respectively.
2.1
Reactions for Weak s-process

The 22Ne(α, n)25Mg reaction is active at T ~ 0.2 GK and 1.0 GK in He and C burning shells, respectively. This reaction competes with 22Ne(α, γ)26Mg, which consumes 22Ne without releasing neutrons. In these shells, 16O is the most abundant isotope and acts as the main neutron poison through 16O(n, γ)17O. Fortunately, the neutrons absorbed by 16O can be released again via 17O(α, n)20Ne. Therefore, the availability of neutrons for the ws-process is determined by the (α, n)/(α, γ) ratio for both 22Ne+α and 17O+α reactions.

In Fig. 1, we show the (α, n)/(α, γ) ratios for the 22Ne+α (top panel) and 17O+α (bottom panel) reactions as a function of the temperature. In the top panel, the (α, n)/(α, γ) ratio for 22Ne+α, as recommended by Wiescher et al. [40], is observed to be 1.2 to 2.0 times higher than the values provided by REACLIB below 1.5 GK, a range typically associated with He and C shell burning. Notably, this enhancement increases dramatically, reaching several tens of times above 1.5 GK.

Fig. 1
(Color online) The (α, n)/(α, γ) ratio as a function of temperature for 22Ne+α (top) and 17O+α (bottom) reactions
pic

In the bottom panel, the (α, n)/(α, γ) ratio for the 17O+α reaction suggested by Best et al. [39] is similar to REACLIB below 0.7 GK, where only He burns, but this ratio rapidly increases to several tens of times in the C, Ne, and O layers. With these updated reaction rates, we anticipate an increase in neutron release from 22Ne while reducing neutron consumption by 16O. Consequently, the yields of the ws-process isotopes were significantly enhanced.

2.2
Input Physics in MESA

To achieve the convergence of the model structures within approximately 10%, a nuclear network comprising at least 127 isotopes should be included [43]. In this study, we utilized a more extensive nuclear network (mesa_161.net) that incorporates additional neutron-rich isotopes. Table 2 lists all the isotopes in mesa_161.net. We adopt a metallicity of and assume solar metallicity ratios based on the work of Anders and Grevesse [44].

Table 2
Nuclides included in the nuclear reaction network of mesa_161.net
Element Amin Amax Element Amin Amax
n 1 1 S 31 35
H 1 2 Cl 35 38
He 3 4 Ar 35 40
Li 7 7 K 39 44
Bea 7 10 Ca 39 46
B 8 8 Sc 43 48
C 12 13 Ti 43 51
N 13 15 V 47 53
O 14 18 Cr 47 57
F 17 19 Mn 51 57
Ne 18 22 Fe 51 61
Na 21 24 Co 55 63
Mg 23 26 Ni 55 64
Al 25 28 Cu 59 64
Si 27 31 Zn 60 64
P 30 33
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a8Be is not included

We enhanced both the temporal and spatial resolutions to ensure numerical convergence. The mass resolution is critical for accurately capturing changes in the stellar structure [43, 45]. The parameter max_dq controls the maximum fractional mass of a cell in the model, and we set max_dq=5d-4, which resulted in over 3,500 cells in the model. We adopted a minimum diffusion coefficient of Dmin = 10-2 cm2 s-1 to ensure that the global mixing timescale () was significantly longer than the lifetimes of the stellar models. This allows us to neglect the effects of global mixing and smooth local composition gradients [45].

After C burning, the core structure becomes more complex because of multi-shell burning, with the central entropy being significantly influenced by shell burning (see Xin et al. [42]). To achieve finer granularity during evolution, we imposed limits on the changes in the logarithm of the central density and temperature. Specifically, we set and . Additionally, we restrict the change in the mass fraction of isotopes with dX_nuc_drop_limit=3 × 10-2 and tightening this limit to dX_nuc_drop_limit_at_high_T=10-2 when log Tc > 9.45.

2.3
Post-processing Calculation with WinNet

The detailed nucleosynthesis in the stellar models was computed in post-processing using an extensive nuclear reaction network code, WinNet [38]. The network consists of approximately 2000 isotopes from neutron and proton to thorium (Z = 90). The reaction rates of , , , (α, n), (α, p), , and their inverse reactions from the JINA REACLIB database [31] were included. Theoretical weak rates from Langanke and Martínez-Pinedo [46], electron chemical potentials from Timmes and Arnett [47], and screening corrections from Kravchuk and Yakovlev [48] were used.

For each stellar model, we mapped the initial composition and time evolution of the temperature and density from the MESA simulation on the trajectories. The nucleosynthesis calculation of these trajectories was performed until the onset of iron core collapse. The region inside the steepest density jump is expected to eventually collapse into a neutron star and does not contribute to the yield of the ws-process nucleosynthesis. The steepest density jump occurs at the most active burning shell and has been defined by Xin et al. [42]. We briefly describe the MESA result in Sect. 3.

3

pre-CCSN Evolution and Explodability

3.1
Evolution of Massive Stars

In Fig. 2, we show the central temperature against the central density for the evolution of stars with M (ZAMS) = 15, 20, 25, and 30 M⊙. The gray dashed lines show the ignition lines of C, Ne, O, and Si burning, where the energy generation rate by nuclear burning equals the energy loss rate by neutrino emissions. In the region to the left of the black line, stars are dynamically unstable owing to electron-positron pair creation (indicated as “pair instability”) (Ohkubo et al. [49]), general relativistic effects (“GR instability”) (see, for example, Osaki [50]), and the photo-disintegration of matter in nuclear statistical equilibrium (NSE) at Ye = 0.5 (“photodisintegration”) (Ohkubo et al. [49]). After core He burning, the mass fraction of 12C in the center is smaller for larger M (ZAMS). Only the star with M (ZAMS) = 15 M⊙ can ignite convective C burning in the center, as it has sufficient fuel with X(12C) ~ 0.2. In contrast, other models with larger M (ZAMS) undergo contraction because the neutrino energy loss rate exceeds the energy production rate of C burning. After Si burning, the star with M (ZAMS) = 15 M⊙ exhibits distinct behavior compared to other models because shell Si burning is energetic. However, the effects of shell Si burning are not the focus of this study and will be discussed in future works.

Fig. 2
(Color online) The central temperature against the central density for the evolution of stars with M (ZAMS) = 15, 20, 25, and 30 M⊙. The gray dashed lines show the ignition lines of C, Ne, O, and Si burning, where the energy generation rate by nuclear burning equals the energy loss rate by neutrino emissions. In the region to the left of the black line, stars are dynamically unstable owing to electron-positron pair creation (indicated as “pair instability”) (Ohkubo et al. [49]), general relativistic effects (“GR instability”) (see, for example, Osaki [50]), and the photo-disintegration of matter in nuclear statistical equilibrium (NSE) at Ye = 0.5 (“photo-disintegration”) (Ohkubo et al. [49])
pic

More massive stars eject more materials but explode less frequently [51]. Considering the combined effects of ejected masses and event frequencies, stars with M (ZAMS) = 25 M⊙ are regarded as the most significant contributors to the chemical enrichment of galaxies [21, 52]. Therefore, we select the model of M (ZAMS) = 25 M⊙ as a typical example for discussing stellar nucleosynthesis.

In Fig. 3, we present the Kippenhahn diagram for the star with M(ZAMS) = 25 M⊙, tracking its evolution from H burning to Fe core collapse. The central temperature reaches approximately 0.2 GK at τ = tfinal-t = 105.6 yr. Here, t is the time from the ZAMS and tfinal denotes the time at the final stage of evolution, which is defined as the moment when the infall speed of the Fe core reaches 1000 km s-1. The orange line indicates the isotherm at T = 0.2 GK.

Fig. 3
(Color online) The Kippenhahn diagram of the star with M(ZAMS) = 25 M⊙. The inner part of Mr = 0 - 14 M⊙ is shown. Blue, gray, and pink represent the convection, overshoot, and semiconvection regions, respectively. The orange line is the isotherm line of 0.2 GK, and the red line shows the location of Mr=1.84 M⊙. Between these two lines, the hatched region indicates where the ws-process is considered
pic

The ws-process is assumed to occur interior to this isotherm. After core He burning, this region extends to Mr ~ 6.0 M⊙, and the He and CO core masses are 7.8 and 4.96 M⊙, respectively. C burning ignites off-center at yr, nearly three years before the collapse. After τ=10-3 yr (10 h before collapse), shell C burning merges with shell O burning at Mr = 1.84 M⊙, marking the location of the highest energy generation rate, as indicated by the red line. The inner part of this region is predicted to form a proto-neutron star (PNS), whereas the outer layers are ejected. Therefore, this study considers only the ws-process isotopes produced in the hatched region.

Figure 4 illustrates the mass distributions of the main isotopes at . The ws-process region extends from the Si/O interface to the bottom of the He burning shell, primarily composed of 16O, 28Si, 20Ne, 12C, and 4He. The mass fraction of the iron-group elements ranges from 10-4 to 10-5. Additionally, the neutron excess, expressed as , of the ws-process region was observed to be 10-3–10-4, as shown in Fig. 5. In the interior to Mr=1.84 M⊙, the neutron excess increases rapidly toward the center, reaching η ~ 0.2 at the center. This jump is primarily attributed to the reactions during O burning, including 16O(16O, n)31S and the weak interactions such as 30P(e+, ν)30S, 33S(e-, ν)33P, 35Cl(e-, ν)35S, and 37Ar(e-, ν)37Cl [53].

Fig. 4
(Color online) The mass distribution of the main isotopes at t=tfinal from MESA. The two grey regions indicate where M⊙ and GK, respectively
pic
Fig. 5
(Color online) The mass distribution of the Ye (red) and logρ (blue) at t=tfinal. The two black lines indicate where Mr = 1.84 M⊙ and T = 0.2 GK, respectively
pic
3.2
The Mass Cut

In Fig. 5, prominent jumps in both the density and Ye are observed near the mass coordinate Mr = 1.84 M⊙. This layer corresponds to the base of shell O burning, which is the layer of peak energy generation. To measure the strength of shell burning, we usepic(1)where U and V are defined in earlier studies [54-57].

As explained in detail by Xin et al. [42], U is related to the degree of the density jump, and V/U is the pressure gradient against Mr. The mass coordinate at which V/U reaches its maximum is represented as M(V/Umax). The relationship between V/U and the strength of shell burning is straightforward. When shell O burning is more energetic, it produces higher energy to prevent the contraction and even to cause the expansion of outer layers, which makes the gradients of entropy and pressure against Mr (i.e., V/U) larger.

Figure 6 shows the distribution of log V/U against Mr at for each model. We note that M(V/Umax) coincides with M4, that is, Mr at a specific entropy of s=4 erg g-1K-1, which was previously used for the mass cut that would divide the inner proto-neutron star (PNS) and the outer ejecta in the explosion [58-61]. In the present study, we adopt M(V/Umax) as the mass cut, because it is the location of the steepest gradients of pressure and density [42]. The core masses and M(V/Umax) values for our models are listed in Table 3.

Fig. 6
(Color online) The mass distribution of log V/U at t=tfinal. The black diamonds represent the location of M4, which is defined at the mass coordinate of specific entropy s=4 erg g-1K-1)
pic
Table 3
The final mass, He core mass, CO core mass, and M(V/Umax) for each model. The M(He) and M(CO) are defined at the layers where X(H) and X(He) lower than 10-4
M(ZAMS)M⊙ M(final)M⊙ M(He)M⊙ M(CO)M⊙ M(V/Umax)M⊙
15 14.88 4.66 2.39 1.41
20 19.79 6.25 3.85 1.85
25 24.73 7.80 4.96 1.84
30 29.50 9.86 6.76 2.07
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4

Nucleosynthesis and the effect of reaction rates

4.1
The Nucleosynthesis in the 25 M⊙ model

In this section, we present the results of post-process nucleosynthesis and discuss the effects of the updated reaction rates.

We selected a zone at Mr = 2.3 M⊙ as a representative example to reveal the change in the mass fraction X(i) of isotope i occurring during each burning stage after updating the (α, n) reaction rates. X(Ga-Zr) and X(Nb-Th) are the cumulative mass fractions of isotopes from Ga to Zr (Z = 31 - 40) and Nb to Th (Z>41-90), respectively. The reaction rate recipes used in Fig. 7(a–d) correspond to cases 1–4 listed in Table 1. The chemical evolution of the main isotopes is depicted in the top panel of Fig. 7. The changes in X(n) and 4He for the default rates are displayed in the bottom panel of Fig. 7(a), while in Fig. 7(b)–(d), the value is normalized by Xdef(i) in Fig. 7(a) to emphasize the effect of these reaction rates. Table 4 lists the total mass fraction of the “Ga-Zr” elements in the initial abundance (Xini), after He burning (XHe-b), C burning (XC-b), and Ne burning (XNe-b). The data are visualized in Fig. 8 by the ratios of ΔX to Xini, where ΔX is the change in the mass fraction in each burning stage.

Fig. 7
(Color online) Chemical evolution in the OSi shell (Mr=2.3 M⊙). In the top panels of (a)–(d), changes in the mass fractions X(i) of 4He, 12C, 16O, and 20Ne show the burning stages. X(Ga - Zr) and X(Nb - Th) are the cumulative mass fractions of the s-process isotopes from Ga to Zr (Z = 31 - 40) and Nb to Th (Z=41-90), respectively. In the bottom panel, the changes in Xdef(i) of neutrons and 4He for the default rates are shown in (a). In (b)–(d) shown are the changes in the ratios X(i)/Xdef(i) between the “new” and default rates for n and 4He
pic
Table 4
The total mass fractions of the ws-process isotopes of Z=31-40 in the initial abundance, after He burning, C burning and Ne burning stages, respectively, in Fig. 7
Figure Xini XHe-b XC-b
7a 7.87×10-8 3.42×10-7 5.55×10-7 5.95×10-7
7b 7.87×10-8 2.87×10-7 1.38×10-6 1.95×10-6
7c 7.87×10-8 1.21×10-6 2.39×10-6 2.56×10-6
7d 7.87×10-8 9.34×10-7 7.34×10-6 9.02×10-6
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Fig. 8
(Color online) The total mass fraction of the ws-process isotopes from A=31-40 after He, C, and Ne burning. All values are normalized by the initial abundance, Xini=7.87 × 10-8. The total value is written above each pillar, and the fractional contribution of each burning stage is written in the center of the box
pic

Overall, these new reaction rates significantly alter the production of the “Ga-Zr” elements rather than the “Nb-Th” elements. Thus, we focus on the “Ga-Zr” elements in this section. The initial value of X(Ga-Zr) was . Enhancements in X(Ga-Zr) are observed four times at the end of He burning, the beginning of C burning, the end of C burning and Ne burning. These coincide with the neutron peaks and 4He production in Fig. 7.

After Ne burning, the total enhancement of X(Ga-Zr) is estimated by the ratio of ()/Xini, where and Xini are listed in Table 4. Compared with Xini, X(Ga-Zr) increases by a factor of 6.56, 23.77, 31.58, and 113.62 for (a)–(b), respectively. The forthcoming O burning will not enhance but rather reduce their abundance because of the increased destruction at high temperatures [15].

When the default rates are used as in Fig. 7(a), the “Ga-Zr” elements are mainly synthesized during the He (51%) and C (41%) burning stages (see Fig. 8). Only 8% of them are synthesized during the Ne burning stage because the main neutron source isotope 22Ne is almost exhausted during this stage.

With the new 17O+α reaction rates in Fig. 7(c), more than 93% of the “Ga-Zr” elements are synthesized during the He and C burning stages, which is similar to (a). The final X (Ga-Zr) is enhanced by a factor of 4.81 compared to the default rates. Because both new 17O(α, n)20Ne and 17O(α, γ)21Ne reaction rates are lower than the default ones at temperatures below 0.7 GK (see Sect. 5.1), X(17O) reaches a higher level at the end of He burning with the new rates. When the temperature exceeds 0.7 GK, the ratio of (α, n)/(α, γ) increases significantly. Therefore, the new 17O+α reaction rates significantly enhanced the production of the “Ga-Zr” elements at all stages, although only slightly alter their contribution percentages.

Comparing Fig. 7(a) and (b), the production of the “Ga-Zr” elements is enhanced by a factor of 23.8 using the new 22Ne+α reaction rates. This is smaller than the increase in using the new 17O+α reaction rates. Because the new 22Ne+α rates are smaller than those in REACLIB (see Fig. 14), 22Ne is not exhausted until the core collapse. The (α, n)/(α, γ) ratio of the new rates is 10 times higher than that of the default rates when the temperature exceeds 1.5 GK. A significant increase in neutron levels was observed six months before the explosion. As a result, almost 89% of the “Ga - Zr” elements are synthesized during C and Ne burning.

In Fig. 7(d), both the new 17O+α and new 22Ne+α reaction rates are updated. The production of the “Ga-Zr” elements was enhanced by more than one order of magnitude. However, the contributions of He and Ne burning are only 10% and 18%, respectively, and most of the “Ga-Zr” elements are synthesized during the C burning stage, which should alter the isotope composition of the “Ga-Zr" elements. By comparing (a, c) with (b, d), we can also determine whether Ne burning contributes significantly to the ws-process, depending on the 22Ne(α, γ)25Mg reaction rate.

Figure 9 shows the abundance distributions of the s-process elements. We observe two distinct bumps in the abundance of both “Ga-Zr” and “Nb-Th” in the region of Mr = 2.2–5.9 M⊙. The first bump, located at Mr = 2.0–3.6 M⊙, corresponds to the C, Ne, and O burning shells, while the second bump, found at Mr = 5.0–5.9 M⊙, is associated with shell He burning. Between these two bumps, X (Ga-Zr) decreases owing to low α production in the unburned regions.

Fig. 9
(Color online) The abundance distributions of the ws-process elements at Mr = 1.84 - 7.3 M⊙ in the He core of the M(ZAMS)=25 M⊙ star. The solid lines symbolize the “Ga-Zr" elements, while the dashed lines symbolize the heavier elements
pic

In Fig. 10, the distribution of 21Ne is similar to the “Ga-Zr” elements, while 22Ne displays an opposite trend. Compared to the unburned shells, more 4He is produced in the burning shells, which can consume 22Ne and release more neutrons. The new 22Ne+α reaction rates enhanced X (Ga-Zr) only in the first bump, whereas the new 17O+α reaction rates positively affected X (Ga-Zr) across all the ws-process regions. Additionally, the new 17O+α reaction rates increase X (Nb–Th) by 50%, unlike the 22Ne+α reaction rates, because these elements are produced during the He burning stage. Notably, the sharp peak observed at Mr = 1.84–2.0 M⊙ remains unaffected by both the 22Ne+α and 17O+α reaction rates, as these “Ga - Zr” elements are generated through the NSE process.

Fig. 10
(Color online) The distribution of the mass fractions of the main isotopes at obtained from the post-processing calculation. Note that mixing is not considered in the post-processing calculation because WinNet is a one-zone code. A comparison between Fig. 10 and Fig. 4 is presented in Sect. 5.2
pic

In this section, we follow the variation of the ws-process isotopes throughout the stellar evolution history and their mass distribution at the final stage for various reaction networks. We found that both the new 22Ne+α and 17O+α reaction rates increased the production of ws-process isotopes.

(1) The new 17O+α reaction rates only increase neutron density by ~3 times during He and C burning stages. In contrast, the new 22Ne+α reaction rates increase the neutron density by several tens of times during the C and Ne burning.

(2) The new 17O+α reaction rates doesn’t vary the contribution in each burning stage. In contrast, the new 22Ne+α reaction rates significantly increase the contribution in the C and Ne burning stages, but decrease that in the He burning stage.

(3) Before the explosion, the ws-process isotopes are primarily concentrated in the burning shells, with their abundances decreasing in the outer layers of the CO core. This is because there is no C burning in the outer layers of the CO core, and thus, little 4He is released.

4.2
The Integrated Yields

As indicated in Fig. 7, the ws-process isotopes produced between the mass cut and the top of the He burning shell may contribute to the overall enhancement. We integrated all isotopes in this region rather than the entire star. We assumed that the modifications of the ws-process yields in explosive nucleosynthesis can be ignored and that all radioactive isotopes decay into stable ones after the explosion. Such approximations are reasonable for investigating the sensitivity of the reaction rates.

In Fig. 11 and 12, we show the ratios between the yields with the new reaction rates (Yieldnew) and those with the default reaction rates (Yielddef) for M(ZAMS) = 15, 20, 25, and 30 M⊙, respectively.

Fig. 11
(Color online) The ratios of isotopic yields (from C to Zr) between new rates and default rates for M(ZAMS) = 15, 20, 25 and 30 M⊙, respectively
pic
Fig. 12
(Color online) Same as Fig. 11, but for elements from Mo to Bi
pic

(1) From C to Zn: With the new 22Ne+α reaction rates, we observe the increase in the yields of several neutron-rich isotopes of Ne, Mg, Si, S, Ar, and Ca, particularly those in 25Mg, 29, 30Si, 36S, 40Ar, and 46Ca. The significant decrease in the 22Ne(α, γ)26Mg reaction rate at GK (during Ne burning) reduces the yield of 26Mg. As a result, a greater amount of 22Ne was converted to 25Mg (see Sect. 5.1), leading to a significant increase in neutron production during Ne burning. Consequently, the yields of 21, 22Ne increase owing to neutron capture on 20Ne. Similarly, some 29, 30Si and most of the rare isotopes 36S, 40Ar, and 46Ca are also produced in the Ne burning shell [21]. In contrast, the new 17O+α reaction rates do not increase the number of neutrons in the Ne shell, thus leaving the yields of those isotopes unchanged. The iron peak isotopes remain unaffected by both the new 17O+α and 22Ne+α reaction rates, as they are primarily produced by the NSE process at M⊙, which is affected by Ye. However, Ye is only altered by weak interactions.

(2) From Ga to Zr: The isotopes in this range are most significantly affected by the new reaction rates. The effect of the new 17O+α rates differs significantly from that of the new 22Ne+α reaction rates. For the same element, the increases owing to the new 17O+α reaction rates in the isotopic yields are similar. However, for the new 22Ne+α reaction rates, the yields of some isotopes with fewer neutrons were reduced. With enriched neutrons, the isotopic yields increase rapidly. As M(ZAMS) increases, the enhancement due to the new 17O+α reaction rates also increases, whereas the enhancement due to the new 17O+α reaction rates is not significantly affected by M(ZAMS).

(3) From Mo to Bi The isotopes in this range were not significantly altered by the new reaction rates. The new 22Ne+α reaction rates increase the yields of only a few isotopes for M(ZAMS) = 15 M⊙ models. The number of such isotopes increases only slightly for more massive models.

In principle, the abundance of elements in the solar system arises from the cumulative contributions of numerous generations of stars with varying metallicities. Typically, stars in the range contribute more than 90% to the solar abundance [14]. It is general to use the production factors (PFs) to see which element is contributed significantly by a generation of stars. The PF of element i is defined aspic(2)where denotes the solar mass fraction of element i. runs over all elements and represents the yield of element i averaged by the initial mass function (IMF) from Salpeter [62] with γ=-2.35.

Figure 13 shows the production factors of elements from Cu to Zr. Using the default and new 22Ne+α reaction rates, most elements are underproduced (green lines). However, when the new 17O+α reaction rates are included, the PFs from Zn to Rb increase by more than 0.5 dex. The contribution of stars with 0.1 to the solar abundance should be limited, as approximately 50% of the solar abundance is produced by stars with . Nevertheless, accounting for both the new reaction rates leads to the overproduction of Ga, Ge, As, and Se. Therefore, it is worth calculating the models with 0.5 and and verifying whether the predictions concerning these elements align with observational data. Given the considerable uncertainties involved, it is essential to enhance the measurement accuracy of the (α,n) reaction rate, particularly for the 17O+α reactions.

Fig. 13
(Color online) The production factors of the elements from Cu to Zr. Each element was integrated from 15 to 30 M⊙ with the Salpeter IMF with γ=-2.35
pic
5

Discussion

The primary purpose of this study is to evaluate the effects of the new 22Ne+α from Wiescher et al. [40] (hereafter, W23) and 17O+α reaction rates from Best et al. [39] (hereafter, B13). In fact, some other recent reaction rates were reported by Adsley et al. [63] (hereafter A21) and Hammache et al. [64] (hereafter H24), which were not adopted in our evaluations. In Sect. 5.1, we briefly discuss the effects of differences in these reaction rates on our M(ZAMS) = 25 M⊙ model. In addition, the size of the nuclear network used in MESA is limited to ~300 isotopes, which makes it challenging to cover all the s-process isotopes. Therefore, the evolution and trajectories are based on the MESA calculation, but the detailed nucleosynthesis is based on WinNet. In this section, we discuss some uncertainties related to our calculations.

5.1
Comparisons with Results from Other Reaction Rates

In Fig. 14(a), we compare the 22Ne+α and 17O+α reaction rates used in JINA REACLIB with those reported in different references. As mentioned in Sect. 2.1, the (α, n)/(α, γ) ratio of W23 increases quickly above 1.5 GK because the 22Ne(α, γ)26Mg reaction rate decreases significantly. Compared with the default rates, the rates in W23 enhance the contribution of Ne burning in the ws-process (see Fig. 8). Related enhancement is also observed in the abundance of “Ga-Zr” elements in the region of Mr = 2.2–3.5 M⊙ in Fig. 15.

Fig. 14
(Color online) Top: 22Ne(α, γ)26Mg and 22Ne(α, n)25Mg reaction rates from different references. The gray dashed line shows the default rates in JINA REACLIB from Longland et al. [19]. The red and blue lines represent the reaction rates reported by Adsley et al. [63] and Wiescher et al. [40]. Bottom: 17O(α, γ)21Ne and 17O(α, n)20Ne reaction rates from different references. The gray dashed lines show the default rates in JINA REACLIB, which are from CF88 and NACRE. The red and green lines represent the reaction rates reported by Best et al. [39] and Hammache et al. [64]. To show the difference, all the rates shown here are normalized by the default rate in JINA REACLIB
pic
Fig. 15
(Color online) Same as Fig. 9, but only for the abundances of “Ga-Zr”’ elements. The effects of 22Ne+α reaction rates in different references are compared in the left panel, while the effects of 17O+α reaction rates in different references are compared in the right panel
pic

Because A21 only provides reaction rates below 1.25 GK, in this trial, we switched to the rate from Longland et al. [19] at T > 1.25 GK. In Fig. 14(b), A21 suggests a lower 22Ne(α, n)25Mg reaction rate at GK. Consequently, the production of the “Ga-Zr” elements is reduced in both core and shell He burning, as shown in Fig. 15.

In Fig. 14(c) and (d), H24 suggests a similar 17O(α, γ)21Ne reaction rate with the rate in B13 and a higher 17Ne(α, n)20Ne reaction rate at T < 0.7 GK. At T > 1.0 GK, we also switch to the rate in B13. As a result, the production of the “Ga-Zr” elements during core He burning was enhanced compared with the model with the B13 rate in Fig. 15.

In conclusion, the 22Ne+α reaction rates reported in different studies lead to variations in the yields of the ws-process elements by a factor of approximately 3–5. In contrast, the 17O+α reaction rates published in the literature produce order-of-magnitude differences in the ws-process elemental yields.

5.2
The Effect of Mixing

Nucleosynthesis in each zone was calculated separately because WinNet is a one-zone code. Thus, the effect of convective mixing was not considered. Mixing affects our results in two main aspects. As seen in Fig. 10, 22Ne and 17O are exhausted only in the burning shells in the CO core because the abundance of α particles is quite small in the unburned shells. In Fig. 4 in the region of Mr = 2.5–5.1 M⊙, mixing can transport 22Ne and 17O from unburned shells to the burning shells. Consequently, more neutrons should be released in the MESA calculation. Similarly, the mass fraction of 17O in Fig. 4 is quite low.

Convective mixing can also affect the locations of the C, Ne, O, and Si burning shells. With mixing, more fresh fuel was transported from the outer layers to the bottom of the burning shells. This would make the life of the burning shells longer. Thus, the bottom of shell O burning located at Mr = 1.84 M⊙ in Fig. 4, would move to Mr = 2.10 M⊙ in Fig. 10. Similarly, the bases of the C and Ne shells are at Mr = 2.0 M⊙ would shift to Mr = 2.6 and 2.7 M⊙, respectively without mixing in WinNet.

5.3
The Effect of Explosion

As mentioned in Sect. 3.2, we assume that the mass cut is located at M(V/Umax) and that the region of contributes to the chemical enrichment. We also assume that the ws-process isotopes produced in explosive nucleosynthesis are destroyed by the shock during the explosion. Thus, we did not calculate the explosive nucleosynthesis. The results from Tur et al. [15] show that explosive burning would reduce the ws-process isotopes by less than 15%. Limongi and Chieffi [14] mentioned that for the isotopes of 70Zn, 76Ge, 74, 77, 82Se, 78Kr, 87Rb, and 84Sr, more than 50% of the yields are produced during explosive burning. These isotopes should be significantly changed by the shock wave. Because the exact explosion mechanism of core-collapse supernovae is not well understood, the explosion energy and choice of mass cut would also affect the final yields of these isotopes.

5.4
Other Effects

The ws-process occurs mainly during the He, C, and Ne burning phases. The physical processes that affect these burning phases may also affect the ws-process yields, such as reaction rates, convection, rotation, and magnetic fields [65]. Tur et al. [15] showed that a 15% change in the 3 α and 12C(α, γ)16O reaction rates may change the yields of the ws-process isotopes by more than a factor of 2. Limongi and Chieffi [16] presented many rotating massive star models, including ws-process nucleosynthesis. Their models involved M(ZAMS) = 13–120 M⊙ and metallicity of . They found the interplay between the He core and the H burning shell, which is triggered by rotation-induced instabilities, enhances the products of CNO (especially for 14N) and produces more neutrons. Consequently, the ws-process should be significantly enhanced in rotating models.

6

Conclusion

In this study, we investigate the impact of the new 17O+α reaction rates from Best et al. [39] and new 22Ne+α reaction rates from Wiescher et al. [40] in comparison with the default reaction rates in JINA REACLIB. We calculate the nucleosynthesis of approximately 2000 isotopes, ranging from neutron and proton to thorium (Z=90), using the one-zone code WinNet and the stellar models are calculated with MESA for an initial metallicity of Z=0.1 Z⊙ and M(ZAMS) = 15, 20, 25, and 30 M⊙. All models are evolved from ZAMS to the Fe core collapse, where the infall speed of the Fe core reached 103 km/s. We assume that the corrections by explosive nucleosynthesis to the yields are minor and that the isotopes lying in the outer layer of the mass cut () would contribute to the chemical enrichment of the Galaxy. The results are summarized as follows:

(1) The new 22Ne+α reaction rates slightly suppress the ws-process during He burning, whereas the new 17O+α reaction rates have the opposite effect. Both enhance the ws-process significantly during C and Ne burning. Using the reaction recipes listed in Table 1, X (Ga-Zr) increases by a factor of 6.56, 23.77, 31.58, and 113.62, respectively, after Ne burning (see Fig. 8).

(2) Without considering the effect of mixing, the mass distribution of the ws-process isotopes provided by WinNet shows a two-bump shape (see Fig. 9). This is because unburned layers release fewer neutrons than burning shells. This results in an underestimation of the yields of the ws-process isotopes. If the nucleosynthesis of the ws-process is calculated by coupling with evolution instead of post-processing, the enhancement of the ws-process should be more significant.

(3) The new 17O+α reaction rates can increase the yields of all isotopes from Cu and Zr, with the enhancement being more pronounced in more massive stars. Conversely, the new reaction rates for 22Ne+α significantly enhance only the yields of the most neutron-rich isotopes (see Fig. 11).

(4) We averaged these four initial masses with Salpeter’s IMF and showed the production factors (PFs) of the elements from Cu to Zr. The new 17O+α reaction rates enhanced the PFs more significantly than the new 22Ne+α reaction rates, particularly for Ga, Ge, As, and Se. Considering such a significant impact that the reaction rates from Best et al. [39] and JINA REACLIB have on the PFs of these elements, it is crucial to improve the accuracy and reliability of the measurement of the 17O+α reaction rates. Additionally, further investigations are necessary to ascertain which reaction rates can explain astronomical observations.

(5) We compared the results from the 22Ne+α and 17O+α reaction rates used in JINA REACLIB with those reported in different references. We conclude that the 22Ne+α reaction rates reported in different studies lead to variations in the yields of the ws-process elements by a factor of approximately 3–5. In contrast, the 17O+α reaction rates published in the literature produce order-of-magnitude differences in the ws-process elemental yields. Because both the 22Ne+α and 17O+α reaction rates have important contributions to the ws-process after core He burning, we suggest that researchers conducting experimental or theoretical studies of nuclear reaction rates provide reaction rates spanning the temperature range of 0.1–10 GK.

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Footnote
1

All these models are available on Zenodo at 10.5281/zenodo.17021896

The authors declare that they have no competing interests.