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18 Sco: A SOLAR TWIN RICH IN REFRACTORY AND NEUTRON-CAPTURE ELEMENTS. IMPLICATIONS FOR CHEMICAL TAGGING*

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Published 2014 July 21 © 2014. The American Astronomical Society. All rights reserved.
, , Citation Jorge Meléndez et al 2014 ApJ 791 14 DOI 10.1088/0004-637X/791/1/14

0004-637X/791/1/14

ABSTRACT

We study with unprecedented detail the chemical composition and stellar parameters of the solar twin 18 Sco in a strictly differential sense relative to the Sun. Our study is mainly based on high-resolution (R ∼ 110,000), high signal-to-noise ratio (800–1,000) Very Large Telescope UVES spectra, which allow us to achieve a precision of about 0.005 dex in differential abundances. The effective temperature and surface gravity of 18 Sco are Teff = 5823 ± 6 K and log g = 4.45 ± 0.02 dex, i.e., 18 Sco is 46 ± 6 K hotter than the Sun and log g is 0.01 ± 0.02 dex higher. Its metallicity is [Fe/H] = 0.054 ± 0.005 dex, and its microturbulence velocity is +0.02 ± 0.01 km s−1 higher than solar. Our precise stellar parameters and differential isochrone analysis show that 18 Sco has a mass of 1.04 ± 0.02 M and that it is ∼1.6 Gyr younger than the Sun. We use precise High Accuracy Radial velocity Planet Searcher (HARPS) radial velocities to search for planets, but none are detected. The chemical abundance pattern of 18 Sco displays a clear trend with condensation temperature, thus showing higher abundances of refractories in 18 Sco than in the Sun. Intriguingly, there are enhancements in the neutron-capture elements relative to the Sun. Despite the small element-to-element abundance differences among nearby n-capture elements (∼0.02 dex), we successfully reproduce the r-process pattern in the Solar System. This is independent evidence for the universality of the r process. Our results have important implications for chemical tagging in our Galaxy and nucleosynthesis in general.

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1. INTRODUCTION

Solar twins are stars nearly indistinguishable from the Sun (Cayrel de Strobel 1996). The star 18 Sco was first identified as a solar twin by Porto de Mello & da Silva (1997). This star has great importance because it is the brightest (V = 5.51; Ramírez et al. 2012) and closest (13.9 pc) solar twin (Porto de Mello & da Silva 1997; Soubiran & Triaud 2004; Takeda et al. 2007; Datson et al. 2012, 2014; Porto de Mello et al. 2014); thus it can be studied through a variety of techniques. Moreover, 18 Sco has a declination of −8° and hence is observable from both the Northern and Southern Hemispheres.

Besides the many recent high-resolution chemical abundance studies (e.g., Luck & Heiter 2005; Meléndez & Ramírez 2007; Neves et al. 2009; Ramírez et al. 2009a; Takeda & Tajitsu 2009; González Hernández et al. 2010; da Silva et al. 2012; Monroe et al. 2013), 18 Sco has been observed for chromospheric activity (e.g., Hall et al. 2007), magnetic fields (Petit et al. 2008), debris disks (e.g., Trilling et al. 2008), companions through high-resolution imaging (e.g., Tanner et al. 2010), granulation (Ramírez et al. 2009b), seismology (Bazot et al. 2011, 2012), and interferometry (Bazot et al. 2011; Boyajian et al. 2012). In addition, different techniques can be combined to obtain further insights on the fundamental properties of this solar twin (Li et al. 2012).

Most previous abundance studies on 18 Sco report a somewhat enhanced (about 10–15%) iron abundance and a Li content about three to four times higher than solar, but otherwise approximately solar abundance ratios for other elements (e.g., Porto de Mello & da Silva 1997; Meléndez & Ramírez 2007; Takeda & Tajitsu 2009), except for some recent high-precision studies on 18 Sco (e.g., Meléndez et al. 2009; Ramírez et al. 2009a; Monroe et al. 2013), which show a clear trend with condensation temperature. The situation regarding the heavy elements is less clear, with Porto de Mello & da Silva (1997) reporting a slight excess in the elements heavier than Sr, but the recent study by Mishenina et al. (2013a) finds approximately solar ratios for the neutron-capture elements in 18 Sco. Instead, da Silva et al. (2012) found a clear enhancement in Sr, Ba, Nd, and Sm but solar ratios for Y and Ce. To further complicate the situation, González Hernández et al. (2010) found a solar ratio for Nd (an element that was found enhanced by da Silva et al. (2012)), but Eu and Zr showed the largest enrichment. The worst cases are Zr and Nd, with a spread of 0.15 dex and 0.14 dex, respectively, and individual values of [Zr/Fe] = −0.05, +0.06, +0.10, and [Nd/Fe] = −0.01, 0.13, 0.00, according to Mishenina et al. (2013a), da Silva et al. (2012), and González Hernández et al. (2010), respectively.

In order to better understand the likely chemical differences between 18 Sco and the Sun and to clarify the situation regarding the heavy elements (Z > 30), we perform a highly precise abundance analysis of 18 Sco for 38 chemical elements, thus making it the most complete and precise abundance study to date on the chemical composition of 18 Sco. In addition, our precise stellar parameters will be used in a forthcoming paper to better constrain the fundamental properties of 18 Sco in synergy with other techniques such as asteroseismology (M. Bazot et al., in preparation).

Our work is also relevant regarding "chemical tagging" (Freeman & Bland-Hawthorn 2002), which aims to reconstruct the buildup of our Galaxy by identifying stars with a common origin. Although the dynamical information about their origin could have been lost, the chemical information should be preserved. In this context, the disentangling of the complex abundance pattern of 18 Sco can help us to assess which elements should be targeted for chemical tagging.

The analysis is mainly based on UV–optical spectra acquired with the Ultraviolet and Visual Echelle Spectrograph (UVES) at the Very Large Telescope (VLT) and complemented with optical spectra taken with the High-Resolution Echelle Spectrometer (HIRES) at Keck.

2. OBSERVATIONS

In order to cover a wide spectral range, we observed 18 Sco and the Sun (using solar reflected light from asteroids) in different spectrograph configurations. Both 18 Sco and the reference solar spectrum were acquired in the same observing runs and using identical setups. We obtained visitor mode observations with the UVES spectrograph at the VLT (2009 August 30) and with the HIRES spectrograph at Keck (2005 June 16), covering with both data sets the UV/optical/near-IR spectrum from 306 to 1,020 nm.

The UVES observations were taken in dichroic mode, obtaining thus simultaneous UV (blue arm) plus optical (red arm) coverage with the standard settings 346 nm + 580 nm, and another set of observations with the standard 346 nm setting plus a nonstandard setting centered at 830 nm. With this configuration we achieved a high signal-to-noise ratio (S/N) in the UV, as the 346 nm setting (306–387 nm) was covered in both setups. The 580 nm standard setting covered the optical (480–682 nm) region, and our 830 nm setting included the red region (642–1020 nm). Notice that our nonstandard setting at 830 nm was chosen to overlap the 580 nm setting in the 642–682 nm interval, so a higher S/N was achieved around 670 nm in order to measure lithium with extremely high precision (e.g., Monroe et al. 2013).

The bulk of the analysis is based on the UVES optical spectra obtained in the red arm covering the 480–1,020 nm region. The observations with the red arm were obtained using the 0.3 arcsec slit, achieving a high resolving power (R = 110,000) and a very high S/N (typical S/N ∼ 800 pixel−1, and around the Li feature S/N ∼ 1000). Some elements showing lines in the UV were studied with the UVES blue arm using the 346 nm setup (306–387 nm) with a slit of 0.6 arcsec, resulting in high-resolution (R = 65,000), high S/N (∼600 at 350 nm) spectra. The asteroid Juno was employed to obtain our reference solar spectrum for the UVES observations, and similar S/Ns were achieved both for 18 Sco and Juno.

The spectral regions 387–480 nm and 577–585 nm are missing in our UVES data; thus, for them we employed high-resolution (R = 100,000), high S/N (∼400) spectra obtained with the HIRES spectrograph at Keck, which covers the optical spectra (388–800 nm) using a mosaic of three CCDs. The asteroid Ceres was used to obtain a solar spectrum for our HIRES observations. In Meléndez et al. (2012) we made a detailed comparison of both UVES and HIRES observations of 18 Sco relative to the Sun and concluded that there is an excellent agreement between both data sets, resulting in negligible abundance differences (mean difference of 0.002 ± 0.001 dex and element-to-element scatter σ = 0.005 dex); thus we complement our UVES equivalent-width measurements with HIRES data when needed.

Data reductions of the UVES and HIRES spectra are described in Monroe et al. (2013) and Meléndez et al. (2012), respectively. A comparison of the reduced UVES spectra of 18 Sco and the Sun is shown around 6,085 Å (Figure 1) and 5,320 Å (Figure 2). As can be seen in Figure 1, overall the spectrum of 18 Sco is very similar to the Sun's, as expected for a solar twin, yet, when a closer look is taken for the lines of neutron-capture elements, a clear enhancement is seen in 18 Sco, as shown for example in Figure 2 for the 5,319.8 Å Nd ii line.

Figure 1.

Figure 1. UVES spectra of 18 Sco and the Sun in the 6,078–6,095 Å region. Although both stars show similar spectra, their different chemical compositions can be revealed through careful measurements.

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Figure 2.

Figure 2. UVES spectra of 18 Sco and the Sun around 5,320 Å, showing a clear enhancement in the n-capture element Nd in 18 Sco, relative to the Sun.

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3. ABUNDANCE ANALYSIS

The abundance analysis closely follows our recent high-precision studies on the solar twins HIP 56948 (Meléndez et al. 2012) and HIP 102152 (Monroe et al. 2013). We measured the equivalent widths (EW) automatically with the Automatic Routine for line Equivalent widths in stellar Spectra (ARES; Sousa et al. 2007) for lines with EW larger than 10 mÅ. Weaker lines and species with fewer than five lines available were measured by hand using IRAF. In further iterations the outliers resulting from the automatic EW measurements are carefully measured by hand, making sure that exactly the same criteria are used in the measurements of 18 Sco and the Sun, i.e., for each line we choose the same continuum definition, and the same interval was selected to fit a Gaussian profile. The main difference in relation to Meléndez et al. (2012) and Monroe et al. (2013) is that we have significantly expanded our line list to obtain more precise results and also to include many heavy elements. For example, in Meléndez et al. (2012) only 54 iron (42 Fe i, 12 Fe ii) and 12 chromium (7 Cr i, 5 Cr ii) lines were included, while in the present work 98 iron (86 Fe i, 12 Fe ii) and 21 chromium (14 Cr i, 7 Cr ii) lines are used. In comparison to Monroe et al. (2013), we have 87 additional lines, many of which were included to study the neutron-capture elements.

Because our abundances were estimated from EW, we selected mostly clean lines. For example, the oxygen abundance was estimated using the clean O i triplet at 777 nm rather than the blended forbidden [O i] line at 630 nm. When necessary we used lines somewhat affected by blending, measuring them by using multiple Gaussians with the deblend option of the task splot in IRAF. The list of lines with the differential equivalent-width measurements is presented in Table 1, except for nitrogen and lithium, which were analyzed by spectral synthesis of an NH feature at 340 nm and the Li i feature at 670.7 nm, respectively.

Table 1. Adopted Atomic Data and Equivalent Widths

Wavelength Ion χexc log gf C6 EW EW
(Å) (eV) 18 Sco Sun
5044.211 26.0 2.8512 −2.058 0.271E-30 74.8 74.3
5054.642 26.0 3.640 −1.921 0.468E-31 40.9 40.5
5127.359 26.0 0.915 −3.307 0.184E-31 97.5 96.1
5127.679 26.0 0.052 −6.125 0.12E-31 18.9 19.1
5198.711 26.0 2.223 −2.135 0.461E-31 99.3 98.1
5225.525 26.0 0.1101 −4.789 0.123E-31 72.5 72.1
5242.491 26.0 3.634 −0.967 0.495E-31 88.3 86.9
5247.050 26.0 0.0872 −4.946 0.122E-31 67.4 66.9
5250.208 26.0 0.1212 −4.938 0.123E-31 66.3 65.9
5295.312 26.0 4.415 −1.49 0.654E-30 31.0 30.3

Only a portion of this table is shown here to demonstrate its form and content. A machine-readable version of the full table is available.

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We obtain both stellar parameters and elemental abundances through a differential line-by-line analysis (e.g., Meléndez et al. 2012; Monroe et al. 2013; Ramírez et al. 2011, 2014a), using Kurucz ODFNEW model atmospheres (Castelli & Kurucz 2004) and the 2002 version of MOOG (Sneden 1973). For the Sun we fixed Teff = 5,777 K and log g = 4.44 (Cox 2000), and as an initial guess we used a microturbulence velocity of vt = 0.86 km s−1 (Monroe et al. 2013). Solar abundances were then computed, and the final solar microturbulence was found by imposing no trend between the abundances of Fe i lines and reduced equivalent width (EWr = EW/λ). We found $v_t^\odot$ = 0.88 km s−1 and used this value and the above Teff and log g to compute the reference solar abundances ($A_i^\odot$).

Next, adopting as an initial guess for 18 Sco the solar stellar parameters, we computed abundances for 18 Sco ($A_i^*$) and then differential abundances for each line i,

Equation (1)

The effective temperature is found by imposing the differential excitation equilibrium of δAi for Fe i lines:

Equation (2)

while the differential ionization equilibrium of Fe i and Fe ii lines was used to determine the surface gravity:

Equation (3)

The microturbulence velocity, vt, was obtained when the differential Fe i abundances $\delta A_i^{\rm Fe\,\scriptsize{I}}$ showed no dependence with the logarithm of the reduced equivalent width:

Equation (4)

The spectroscopic solution is reached when the three conditions above (Equations (2)–(4)) are satisfied simultaneously to better than ∼one-third the error bars in the slopes of Equations (2) and (4), and better than ∼one-third of the error bar of the quadratic sum of the error bars of Fe i and Fe ii lines for Equation (3).10 We preferred to adopt these convergence criteria based on the observational error bars rather than using fixed values. Also, the metallicity obtained from the iron lines must be the same as that of the input model atmosphere (within 0.01 dex).

We emphasize that our iron line list was built to minimize potential correlations between the atmospheric parameters, by including lines of different line strengths at a given excitation potential and by having, as much as possible, a homogeneous distribution of lines with excitation potential. In addition, we keep in our line list only iron lines that could be reliably measured at high precision at our spectral resolution.

The differential spectroscopic equilibrium (Figure 3)11 results in the following stellar parameters: Teff = 5,823 ± 6 K (46 ± 6 K hotter than the Sun), log g = 4.45 ± 0.02 dex (+0.01 ± 0.02 dex above the Sun), [Fe/H] = 0.054 ± 0.005 dex, and Δvt = +0.02 ± 0.01 km s−1 higher than solar. The above errors include both the measurement uncertainties (from the errors in the slopes and the errors in the iron abundances) and the degeneracies in the stellar parameters, by estimating how the error in a given stellar parameter affects the uncertainty in the others. For example, besides the uncertainty in log g due to the errors in Fe i and Fe ii, we estimated systematic errors in log g due to changes in Fe ii–Fe i owing to the uncertainties in Teff, vt and [Fe/H].

Figure 3.

Figure 3. Differential iron abundances vs. excitation potential (top panel) and reduced equivalent width (bottom panel) of Fe i (stars) and Fe ii (circles) lines. The dashed lines show fits to the Fe i lines. The solution is achieved when the slopes are equal or smaller than one-third of the error bar in the slopes and when the mean abundance of Fe ii agrees with the mean abundance of Fe i within one-third of the combined error bar.

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In Meléndez et al. (2012) we found that the small differential non-LTE corrections to Fe i lines in the solar twin HIP 56948 do not affect the excitation temperature derived in LTE. Here we also computed NLTE corrections for Fe i as in Bergemann et al. (2012). Again, the differential NLTE corrections are so small that they do not have any impact on our spectroscopic solution. Notice that, within the error bars, the differential ionization equilibrium is satisfied also by Cr, Ti, and Sc, as shown in Figure 4. This good agreement among different species reinforces our results.

Figure 4.

Figure 4. Singly ionized minus neutral differential abundances of Fe, Cr, Ti, and Sc. The surface gravity found by the ionization equilibrium of iron also satisfies, within the error bars, the ionization equilibrium of Sc, Ti, and Cr.

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Our stellar parameters are in excellent agreement with those independently determined by Monroe et al. (2013), who found a Teff only 1 K hotter, exactly the same log g and vt, and [Fe/H] only 0.001 dex higher, and by Takeda & Tajitsu (2009), who determined Teff = 5,826 ± 5 K, log g = 4.45 ± 0.01 dex, and [Fe/H] = 0.06 ± 0.01 dex, using high-resolution (R = 90,000), high S/N (∼1,000 at 600 nm) High-Definition Spectrograph (HDS)/Subaru spectra. Our results are also in firm agreement with stellar parameters recently determined by Ramírez et al. (2014b) using several high-resolution (R = 65,000–83,000), high S/N (= 400) spectra taken with the MIKE spectrograph at the Magellan telescope, Teff = 5816 ± 4 K, log g = 4.45 ± 0.01 dex, and [Fe/H] = 0.053 ± 0.003. Also, there is a good agreement with other results found in the literature, as well as an exceptional accord with their weighted mean value, Teff = 5822 ± 4 K, log g = 4.45 ± 0.01 dex, and [Fe/H] = 0.053 ± 0.004, as shown in Table 2.

Table 2. Comparison of Stellar Parameters of 18 Sco

Teff Error log g Error [Fe/H] Error Source
(K) (K) (dex) (dex) (dex) (dex)
5823 6 4.45 0.02 0.054 0.005 This work
5816 4 4.45 0.01 0.053 0.003 Ramírez et al. (2014b)
5824 5 4.45 0.02 0.055 0.010 Monroe et al. (2013)
5810 12 4.46 0.04 0.05 0.01 Tsantaki et al. (2013)
5831 10 4.46 0.02 0.06 0.01 Meléndez et al. (2012)
5817 30 4.45 0.13 0.05 0.05 da Silva et al. (2012)
5826 5 4.45 0.01 0.06 0.01 Takeda & Tajitsu (2009)
5840 20 4.45 0.04 0.07 0.02 Meléndez et al. (2009)
5848 46 4.46 0.06 0.06 0.02 Ramírez et al. (2009a)
5818 13 4.45 0.02 0.04 0.01 Sousa et al. (2008)
5834 36 4.45 0.05 0.04 0.02 Meléndez & Ramírez (2007)
5822 4 4.451 0.006 0.053 0.004 Weighted mean from the literature

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We took hyperfine structure (HFS) into account for 11 elements. The calculation is performed including HFS for each individual line, and then a differential line-by-line analysis is performed. Also, isotopic splitting was taken into account for the heavier elements. For V, Mn, Ag, Ba, La, and Pr the combined HFS+isotopic splitting is a minor differential correction (⩽0.002 dex), but for Co and Cu the differential correction amounts to 0.004 dex, for Y the correction is 0.005 dex, and for Yb it is very large at 0.023 dex. The most dramatic case is for Eu, for which neglecting the corrections would result in an error of 0.155 dex in the differential abundances.

As shown in Meléndez et al. (2012) and Monroe et al. (2013), differential NLTE effects in solar twins relative to the Sun are minor. Here, we consider differential NLTE corrections for elements showing the largest differential corrections in our previous works, Mn (Bergemann & Gehren 2008) and Cr (Bergemann & Cescutti 2010), but the largest differential correction is only 0.003 dex for Mn. As mentioned above, differential NLTE effects on Fe (Bergemann et al. 2012) were also estimated to check for potential systematics in our differential stellar parameters, but there is no impact in our solutions.

Our differential abundances (which are based on EW measured by J. Meléndez) are in excellent agreement with those obtained using an independent set of EW measurements in 18 Sco by Monroe et al. (2013), with an average abundance difference of 0.002 dex (J.M.'s measurements in this paper; Monroe et al. 2013) and an element-to-element scatter of only 0.005 dex. Another independent set of EW measurements obtained by M. Tucci Maia (which were obtained fully by hand, unlike the measurements done by J.M and T.M., which used ARES first and then remeasured the outliers by hand) results in abundances with a difference from our work of 0.002 dex and scatter of only 0.004 dex. These comparisons and our previous testing in Meléndez et al. (2012), for which we obtained an element-to-element scatter of σ =0.005 dex, in the similarity of HIRES and UVES abundances of 18 Sco minus the Sun, suggest that careful differential measurements can achieve a precision of about 0.005 dex in differential abundances.

The measurement errors are adopted as the standard error of the differential abundances, except for elements with just a single line, in which case we adopted as observational error the standard deviation of five differential EW measurements performed with somewhat different criteria. The typical measurement uncertainties in the differential abundances of the lighter elements (Z ⩽ 30) are about 0.004 dex, in good agreement with the measurement errors discussed above. Including the systematic errors due to uncertainties in the stellar parameters, the total error is about 0.007 dex. The differential abundances for each element and their errors are given in Table 3.

Table 3. Differential Abundances of 18 Sco Relative to the Sun and their Errors

Element [X/H] ΔTeff Δlog g Δvt Δ[M/H] Parama Obsb Totalc
+6K +0.02 dex +0.01 km s−1 +0.01 dex
(dex) (dex) (dex) (dex) (dex) (dex) (dex) (dex)
C −0.009 −0.004 0.004 0.000 0.000 0.006 0.007 0.009
N 0.003 0.002 0.004 0.006 0.007 0.010 0.013 0.017
O −0.003 −0.005 0.000 −0.001 0.002 0.005 0.006 0.008
Na 0.025 0.003 0.000 −0.001 0.000 0.003 0.003 0.004
Mg 0.039 0.004 −0.001 −0.002 0.000 0.005 0.008 0.009
Al 0.034 0.002 −0.002 −0.001 0.000 0.003 0.006 0.007
Si 0.047 0.001 0.001 −0.001 0.001 0.002 0.002 0.003
S 0.016 −0.003 0.003 0.000 0.001 0.004 0.007 0.008
K 0.041 0.005 −0.007 −0.002 0.001 0.009 0.005 0.010
Ca 0.057 0.004 −0.003 −0.002 0.000 0.005 0.003 0.006
Scd 0.047 0.000 0.007 −0.002 0.003 0.008 0.004 0.009
Tid 0.051 0.006 0.001 −0.001 −0.001 0.006 0.002 0.007
V 0.041 0.006 0.002 −0.001 −0.001 0.006 0.003 0.007
Crd 0.056e 0.005 −0.001 −0.002 0.000 0.005 0.001 0.006
Mn 0.041e 0.005 −0.002 −0.002 0.001 0.006 0.001 0.006
Fed 0.054 0.004 −0.001 −0.002 0.000 0.005 0.001 0.005
Co 0.027 0.004 0.002 −0.001 0.000 0.005 0.003 0.005
Ni 0.041 0.003 0.000 −0.002 0.001 0.004 0.002 0.004
Cu 0.032 0.003 0.001 −0.002 0.001 0.004 0.004 0.006
Zn 0.017 0.001 0.002 −0.002 0.003 0.004 0.002 0.005
Sr 0.097 0.006 0.000 −0.004 −0.001 0.007 0.011 0.013
Y 0.099 0.001 0.006 −0.005 0.004 0.009 0.007 0.011
Zr 0.102 0.001 0.008 −0.003 0.003 0.009 0.010 0.014
Mo 0.115 0.001 0.002 −0.001 0.000 0.002 0.015 0.015
Ru 0.143 0.001 0.002 −0.002 0.000 0.003 0.028 0.028
Pd 0.125 0.001 0.003 −0.002 0.001 0.004 0.010 0.011
Ag 0.126 0.001 0.002 −0.004 0.001 0.005 0.001 0.005
Ba 0.118 0.002 0.002 −0.004 0.005 0.007 0.006 0.009
La 0.135 0.001 0.009 0.000 0.003 0.010 0.006 0.011
Ce 0.117 0.001 0.009 −0.001 0.003 0.010 0.006 0.011
Pr 0.134 0.001 0.009 0.000 0.003 0.010 0.014 0.017
Nd 0.153 0.002 0.009 −0.001 0.003 0.010 0.009 0.013
Sm 0.165 0.002 0.009 −0.001 0.003 0.010 0.018 0.020
Eu 0.187 0.002 0.007 −0.004 0.004 0.009 0.030 0.031
Gd 0.171 0.002 0.010 −0.001 0.004 0.011 0.003 0.011
Dy 0.178 0.002 0.009 −0.002 0.004 0.010 0.012 0.016
Yb 0.156 0.003 0.003 −0.005 0.005 0.008 0.012 0.015

Notes. aErrors due to stellar parameters. bObservational errors. cQuadric sum of errors due to observational and stellar parameter uncertainties. dFor Sc, Ti, Cr, and Fe, the systematic errors due to stellar parameters refer to Sc ii, Ti i, Cr i, and Fe i, respectively. eNLTE abundances are reported for these elements. LTE abundances are [Cr/H] = 0.058, [Mn/H] = 0.044.

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4. MASS, AGE, ROTATION, AND LITHIUM

We determine the mass and age of 18 Sco using our precise stellar parameters (Teff = 5823 ± 6 K, log g = 4.45 ± 0.02 dex, [Fe/H] = 0.054 ± 0.005 dex) and Yonsei–Yale isochrones (Yi et al. 2001; Kim et al. 2002; Demarque et al. 2004). The method, which uses the stellar parameters, their error bars, and probability distribution functions, is described in detail in Meléndez et al. (2012) and Chanamé & Ramírez (2012). The method was calibrated to reproduce the solar values, as described in Meléndez et al. (2012).

We obtain an age of 2.9$_{-1.0}^{+1.1}$ Gyr for 18 Sco, i.e., 1.6 Gyr younger than the Sun, for which we derived an age of 4.5 Gyr using the same set of isochrones (Meléndez et al. 2012). Stellar ages can be well-constrained from isochrones, provided that stellar parameters are known with extreme precision, as shown in Figure 5(a), where we compare our stellar parameters and error bars to the Yonsei–Yale isochrones. We show in Figure 5(b) that Padova isochrones12 (Bressan et al. 2012) are compatible with the relative ages between the Sun and 18 Sco obtained from Yonsei–Yale isochrones. Our age agrees well with the value found by do Nascimento et al. (2009), 2.89$_{-0.81}^{+1.09}$ Gyr, using lithium abundances and stellar parameters. Within the error bars, our age also agrees with that determined by Li et al. (2012), 3.66$_{-0.50}^{+0.44}$ Gyr, using different constraints (stellar parameters, lithium abundance, rotation, and average large-frequency separation). Notice, however, that the adopted stellar parameters by Li et al. (2012) are not as precise as those reported in this work. We are currently modeling our High Accuracy Radial velocity Planet Searcher (HARPS) seismic observations of 18 Sco to obtain even better constraints on its age.

Figure 5.

Figure 5. Location of the Sun and 18 Sco on the HR diagram. (a) Yonsei–Yale isochrones of [Fe/H] = +0.05 (the metallicity of 18 Sco) and age = 1.5, 2.9, and 4.5 Gyr are shown (dashed lines) along with a solar metallicity isochrone of solar age (dotted line). The high precision of our derived stellar parameters for 18 Sco allows us to infer a reasonable estimate of its age from the theoretical isochrones, even though they are densely packed in this main-sequence region. (b) As above for Padova isochrones, showing consistent results for the relative ages between 18 Sco and the Sun.

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Following Meléndez et al. (2012), we obtain v sin i18Sco/v sin i = 1.069 ± 0.029. Adopting v sin i = 1.90 km s−1 for the Sun (Bruning 1984; Saar & Osten 1997), this implies v sin i18Sco = 2.03 ± 0.05 km s−1. The higher rotation rate in 18 Sco is compatible with its younger age. Fortunately, the rotation period has been determined for this star, P = 22.7 ± 0.5 days (Petit et al. 2008), resulting in a rotational age of 3.36 ± 0.52 Gyr using the rotation–age relationship given in Barnes (2007). This value is in good agreement with our derived isochronal age (2.9$_{-1.0}^{+1.1}$ Gyr).

The mass derived here is 1.04 ± 0.02 M, which agrees well with the detailed study of Li et al. (2012), who reported 1.045 M using isochrones, 1.030 M adding also lithium, and 1.030, including stellar parameters, lithium, and the mean large-frequency separation. The mass derived by do Nascimento et al. (2009), 1.01 ± 0.01 M, is also in agreement with our results within the error bars and with the mass derived using asteroseismology, 1.02 ± 0.03 M (Bazot et al. 2011) and 1.01 ± 0.03 M (Bazot et al. 2012). We are performing a more detailed seismic analysis of 18 Sco, including also new HARPS observations (M. Bazot et al., in preparation).

The Li abundance ($A_{\rm Li}^{\rm NLTE}$ = 1.62 ± 0.02 dex) was derived using the line list presented in Meléndez et al. (2012) and NLTE corrections by Lind et al. (2009), and it is identical to that obtained by Monroe et al. (2013), as the stellar parameters are essentially the same, except for a 1 K difference in the effective temperature. We refer the reader to Monroe et al. (2013) for further details, but we stress here that our Li abundance fits well the trend of Li depletion with age of several nonstandard solar models (e.g., Charbonnel & Talon 2005; do Nascimento et al. 2009; Xiong & Deng 2009; Denissenkov 2010).

5. COMPANIONS AROUND 18 Sco

The 18 Sco is included in our HARPS Large Program to search for planets around solar twins; hence we can evaluate whether planets or a binary component are present.

Radial velocities were obtained with the HARPS instrument and binned to yield one radial velocity (RV) value per night for a total of 59 nights spanning 2004 May to 2014 February. The observations include 20 nights of high-cadence asteroseismic observations without simultaneous reference in addition to 39 nights of observations with simultaneous ThAr reference for instrumental drift correction. The asteroseismic data have a scatter of 1 m s−1 throughout the course of a single night. When a moving average is applied to smooth out random noise, a coherent and repeated nightly pattern with an amplitude on the order of 2 m s−1 emerges. We conclude that this coherent noise may be instrumental in origin, and we minimize its effect on the data by using only a single data point from each night, obtained by a weighted average of points from the four hours with lowest air mass. In addition, the radial velocities show drifts throughout the course of the two asteroseismic observing runs, which may be instrumental or, in the case of the 2012 May observations, may be a signal from star spots. We make no attempt to remove these drifts due to the uncertainty of their origin.

Activity indices were also calculated for each HARPS spectrum from the Ca ii H & K lines. The activity cycle of 18 Sco is present in the data, with radial velocities increasing at times of high activity as photospheric convection is suppressed. This variation occurs on a timescale of 7.6 yr in the data, consistent with the previously measured period of seven years from photometry and chromospheric activity (Hall et al. 2007). We remove the effect of the activity cycle on the RVs by fitting and subtracting a linear correlation between radial velocity and continuum-normalized Ca ii H & K flux (SHK).

The resulting radial velocity measurements were searched for planet signals with no significant detections. We quantify our upper limits on potential planets as follows. We make a flat-line fit to the data and subtract the offset. We then fold all jitter in the radial velocities into the uncertainties on the residuals by scaling them with the reduced chi-squared of the fit. The residuals are resampled randomly with replacement, and a Keplerian signal of fixed planet period and mass is added. If the resulting simulated RVs are inconsistent with a flat-line fit by three or more sigma for 99% of randomized trials at a given planet period and mass, we consider the planet to be excluded by the data. The resulting exclusion limits rule out sub-Neptune-mass objects out to a period of seven days and Jupiter-mass objects out to approximately 13 yr (Figure 6). As with all ground-based radial velocity observations, these data show aliases on timescales around one day (due to observing nightly) and at approximately 30 and 365 days due to the effects of the lunar cycle and seasonal observability on sampling.

Figure 6.

Figure 6. Detection limits based on our HARPS data are shown for different eccentricities (e) as a function of orbital period. Planets above the curves are ruled out.

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Our HARPS RV measurements also exclude the presence of a binary component, which is consistent with no detection of companions around 18 Sco by high-contrast adaptive optics (AO) imaging (Tanner et al. 2010).

6. THE COMPLEX ABUNDANCE PATTERN OF 18 Sco

As can be seen in Figure 7, 18 Sco presents a complex abundance pattern. On top of the typical trend with condensation temperature seen in other solar twins (Meléndez et al. 2009; Ramírez et al. 2009a, 2010), corresponding in Figure 7 to the group of elements with enhancements [X/H] ⩽ 0.06 dex (filled circles), there is a group of elements with much larger enhancements (0.09 < [X/H] < 0.19 dex; filled triangles). All elements in the latter group are neutron-capture elements.

Figure 7.

Figure 7. Differential abundances of 18 Sco relative to the Sun. Elements with [X/H] ⩽ 0.06 (filled circles) have Z ⩽ 30, i.e., zinc and lighter elements, while the elements with [X/H] > 0.09 (filled triangles) have Z > 30.

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In order to understand the large enhancement of the n-capture elements in 18 Sco, we first need to subtract the trend with condensation temperature, as it is probably related to the deficiency of refractory elements in the Sun (Meléndez et al. 2009); besides, the yields of asymptotic giant branch (AGB) stars and supernova (SN) do not produce such a trend (Meléndez et al. 2012). We fit [X/H] versus condensation temperature (Lodders 2003) for the lighter elements with Z ⩽ 30 because they only seem affected by the condensation temperature. The fit (Figure 8) results in

Equation (5)

with an element-to-element scatter of only 0.008 dex, which is similar to the mean total error (0.007 dex) of our differential abundances for elements with Z ⩽ 30 (Table 3), showing thus that our small error bars are realistic. The significance of the slope is 9σ.

Figure 8.

Figure 8. Fit of the trend with condensation temperature for elements with Z ⩽ 30. The slope has a significance of 9σ, and the element-to-element scatter from the fit is only 0.008 dex.

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Next, we subtract the above trend from the [X/H] abundances:

Equation (6)

The [X/H]T ratios are given in Table 4 and are shown by filled circles in Figure 9.

Figure 9.

Figure 9. Filled circles are the [X/H] ratios in 18 Sco after they have been subtracted from the condensation temperature trend shown in Figure 8. Elements with Z ⩽ 30 now have abundance ratios close to zero, but the neutron-capture elements remain enhanced. The open triangles represent the effect of pollution by an AGB star (see the text for details). Although a good match can be seen for the s-process elements Sr, Y, Zr, and Ba, there is a disagreement for other elements.

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Table 4. Neutron-capture Enhancement in 18 Sco

Z Element [X/H]T [X/H]AGB sSima sBisb
(dex) (dex)
38 Sr 0.051 0.043 0.890 0.67
39 Y 0.046 0.046 0.719 0.70
40 Zr 0.046 0.056 0.809 0.64
42 Mo 0.064 0.030 0.677 0.577
44 Ru 0.094 0.023 0.39 0.373
46 Pd 0.084 0.032 0.445 0.531
47 Ag 0.096 0.013 0.212 0.221
56 Ba 0.072 0.064 0.853 0.83
57 La 0.085 0.055 0.754 0.711
58 Ce 0.070 0.054 0.814 0.81
59 Pr 0.084 0.032 0.492 0.49
60 Nd 0.102 0.037 0.579 0.56
62 Sm 0.115 0.018 0.331 0.31
63 Eu 0.145 0.003 0.027 0.06
64 Gd 0.118 0.008 0.181 0.135
66 Dy 0.125 0.010 0.121 0.148
70 Yb 0.109 0.024 0.318 0.399

Notes. as-process solar system fractions by Simmerer et al. (2004). bs-process solar system fractions by Bisterzo et al. (2011, 2013).

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We first verify if the observed enhancement in the n-capture elements is due to pollution by AGB stars. We used a model of a 3 M AGB star of Z = 0.01 (Karakas 2010)13 and diluted the yields of a small fraction of AGB ejecta (⩽1% of material injected) into a 1 M protocloud of solar composition (Asplund et al. 2009). Then, we computed the enhancement in the abundance ratios relative to the initial composition of the protocloud, [X/H]AGB. A dilution of 0.23% mass of AGB material matched the observed enhancement in the light s-process element14 yttrium. The [X/H]AGB ratios are given in Table 4 and are shown by open triangles in Figure 9. As can be seen, a good match cannot be achieved for all of the n-capture elements, showing that there is an additional source for the abundance enhancement. Nevertheless, other s-process elements besides Y, such as Sr, Zr, and Ba, are well fitted; thus, the observed enhancement could be due at least partly to AGB stars. In order to find out if the residual enhancement is due to the r process, we estimate its enrichment in 18 Sco by subtracting the AGB contribution

Equation (7)

and compare these results with the predicted enhancement based on the r-process fractions in the solar system, rSS = 1 − sSS, using the s fractions (sSS) by Simmerer et al. (2004) and Bisterzo et al. (2011, updated for a few elements by Bisterzo et al. 2013). Then, we can estimate the r-process contribution [X/H]$_r^{SS}$ from

Equation (8)

where we define ΔT as the average of the three most enhanced s-process and r-process elements, corresponding to ΔT = 0.093 dex for the observed [X/H]T enrichment in 18 Sco (Table 4).

Therefore, the predicted r-process contribution based on the solar system r fractions, [X/H]$_r^{SS}$, is

Equation (9)

In Figure 10, we compare the "observed" r-process enhancement [X/H]r (Equation (7)) with the predicted one based on the solar system r-process fractions, [X/H]$_r^{SS}$ (Equation (9)). There is an astonishing agreement, strongly suggesting that the remaining enhancement is indeed due to the r process. The impressive agreement, even at the scale of the small fluctuations (∼0.02 dex) among nearby n-capture elements (Figure 10), also suggests that even for heavy elements we succeeded in achieving abundances with errors of about 0.01 dex.

Figure 10.

Figure 10. Filled circles represent the [X/H] ratios in 18 Sco after they have been subtracted from the condensation temperature trend (Figure 8) and from the AGB contribution (Figure 9). The residual enhancement, [X/H]r (filled circles), is in extraordinary agreement with the predicted r-process enhancement based on the solar system r-process fractions by Simmerer et al. (2004) and Bisterzo et al. (2011, 2013), represented by dashed and solid lines, respectively.

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Another way to show that the residual enhancement (after subtracting the AGB contribution) is due to the r process is by comparing the r fractions of the [X/H]T ratios with the r fractions in the solar system. Since the Bisterzo et al. (2011, 2013) sSS fractions fit somewhat better our [X/H]r ratios (Figure 10), we will use their values in the comparison. The "observed" r fractions in the [X/H]T ratios in 18 Sco are estimated by

Equation (10)

The "observed" r fractions and the solar system rSS fractions (Bisterzo et al. 2011, 2013) are compared in Figure 11. Again, the agreement is remarkable (slope of 0.90 and element-to-element scatter of only 0.04), showing that after both the Tcond trend and the AGB contribution are subtracted, the remaining material can be explained by the r process. Our high-precision abundances provide independent evidence of the universality of the r process, i.e., of the remarkable similarity of the relative abundance pattern among different r-process elements. Our finding is similar to what is found in metal-poor stars, where the scaled solar r-process pattern matches the abundances of most neutron-capture elements (e.g., Cowan et al. 2002; Hill et al. 2002; Frebel et al. 2007; Sneden et al. 2008; Siqueira Mello et al. 2013).

Figure 11.

Figure 11. r-process fractions in the [X/H]T abundance ratios in 18 Sco vs. the r fractions in the solar system (Bisterzo et al. 2011, 2013). The line shows a linear fit with slope of 0.90 and element-to-element scatter of only 0.04.

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The complex abundance pattern of 18 Sco can be thus explained by the condensation temperature trend, the s process, and the r process. The excess of refractory elements relative to the Sun seems to be typical of solar-like stars (Meléndez et al. 2009; Ramírez et al. 2009a, 2010; Schuler et al. 2011; Liu et al. 2014; Mack et al. 2014), so 18 Sco looks normal in this regard. As we will see below, the additional enhancement in the n-capture elements may be explained by the younger age of 18 Sco (Section 4).

A deficiency in the abundances of the s-process elements have been reported in our analysis of the pair of almost solar twins 16 Cyg (Ramírez et al. 2011) and the solar twin HIP 102152 (Monroe et al. 2013), which are both older than the Sun by 2.5 and 3.7 Gyr, respectively. In contrast, the s-process elements seem enhanced in the young solar twin 18 Sco. Thus, the increasing enhancement of the s-process elements with decreasing age is probably due to the pollution of successive generations of AGB stars, which can be tracked using solar twins spanning ages from 2.9 Gyr (18 Sco) up to 8.2 Gyr (HIP 102152). Similar enhancements of the s-process elements have been found in open clusters (e.g., D'Orazi et al. 2009; Maiorca et al. 2011; Yong et al. 2012; Jacobson & Friel 2013; Mishenina et al. 2013b), with Ba showing the clearest trend of increasing abundance for younger ages. A similar trend was observed in field stars (Edvardsson et al. 1993; Bensby et al. 2007; da Silva et al. 2012), but Mishenina et al. (2013a) found no dependence of [Ba/Fe] and [La/Fe] with age. Although there is no consensus yet, most evidence points to enhanced s-process abundance with decreasing age.

Regarding the r-process elements, da Silva et al. (2012) found a decrease of [Sm/Fe] with decreasing age in stars younger than the Sun. Using both Eu abundances (4,129 Å line) and stellar ages determined by Bensby et al. (2005) in thin disk stars, we found that for ages lower than 9 Gyr there is a flat [Eu/Fe] ratio, i.e., no dependence with stellar age. Unfortunately, neither del Peloso et al. (2005) nor Mishenina et al. (2013a) studied the dependence of their [Eu/Fe] ratios with age in thin disk stars. Our analysis of two old solar twins (Ramírez et al. 2011; Monroe et al. 2013) found normal r-process abundances for 16 Cyg B and HIP 102152. Based on the limited evidence, r-process elements seem to have a flat behavior with age.

Since 18 Sco is considerably younger than the Sun, the enhancement in the s-process elements could be due just to normal Galactic chemical evolution. However, the enhancement of the r-process elements in 18 Sco is more difficult to understand because, based on our discussion above, those elements are not expected to be enriched.

The unexpected enhancement of the r-process elements in 18 Sco could be attributed to a somewhat higher contribution of r-process ejecta to the natal cloud of 18 Sco than around other solar-like stars.

Our precise abundances show that whatever sources produced the enrichment in the n-capture elements did not produce substantial quantities of elements lighter than Z = 30. The amount of mass with Z > 30 that would be needed to produce the observed enhancements is very small, only 2.7 × 10−8 M and 2.4 × 10−7 M for the s and r process, respectively.

7. IMPLICATIONS FOR CHEMICAL TAGGING

Studying the detailed abundance pattern of solar-type stars, we may be able to reconstruct the buildup of the Galaxy using chemical tagging (Freeman & Bland-Hawthorn 2002). One of the main problems when tagging individual stars to a given natal cloud may be radial migration (Sellwood & Binney 2002), yet the chemical abundances may be preserved, so by using chemical tagging stellar groups or clusters could be reconstructed.

Based on our precise abundances in 18 Sco, it is clear that different elements should be targeted for chemical tagging. First, as many as possible of the highly volatile (C, N, O) and highly refractory elements (Al, Ti, Sc, Ca, V, Fe) should be analyzed to determine if there is any trend with condensation temperature. If possible it would be important to cover also some semivolatiles (e.g., S, Zn, Na, Cu, K, Mn, P) and some medium refractories (e.g., Si, Mg, Cr, Ni, Co, V), to verify if there is a break in the trend with condensation temperature (Meléndez et al. 2009). Also, it should be important not to discard stars from a given group due to small discrepant abundances because those anomalies could be due to either the formation of terrestrial (Meléndez et al. 2009) or giant (Tucci Maia et al. 2014; Ramírez et al. 2011) planets.

Some of the above elements are of course relevant to different nucleosynthetic processes such as production of α elements (O, S, Ca, Si, Ti) by SNe II or signatures of proton-burning (Na, Mg, Al, O). Lithium is important as a potential chronometer (Baumann et al. 2010; Monroe et al. 2013; Melendez et al. 2014) and in the study of the transport mechanisms inside stars (e.g., Charbonnel & Talon 2005; do Nascimento et al. 2009). The study of 18 Sco also shows the importance of including the heavy elements for chemical tagging. Ideally, at least some elements among Sr, Zr, Y, or Ba should be included to verify the s process, and some elements among Ru, Pd, Ag, Sm, Gd, Eu, or Dy could be explored for the r process.

8. CONCLUSIONS

We have performed the most precise and complete abundance analysis of 18 Sco. Being the brightest of the solar twins, very high S/N, high-resolution spectra were gathered for 18 Sco and the Sun, and a strictly differential line-by-line analysis was performed, allowing us to achieve a precision of about 0.005 dex in differential abundances. In addition, highly precise stellar parameters were obtained, which would be important for further modeling of this solar twin using different techniques. Precise radial velocities were gathered with HARPS, but no planet has been detected yet.

The complex abundance pattern of 18 Sco shows enhancements (relative to the Sun) in the refractory, s-process, and r-process elements. After subtracting the trend with condensation temperature and the contribution from AGB stars, the remaining enhancement shows the same pattern as the r process in the solar system. This shows the universality of the r process. The different contributions to the abundance enrichment in 18 Sco could be disentangled thanks to the exquisite precision achieved in our work.

The 18 Sco serves as a test bed for studies of chemical tagging in large samples of stars of upcoming surveys, such as HERMES,15 which plans to survey about a million stars at high spectral resolution.

J.M. and T.R.M. acknowledge support from FAPESP (2012/24392-2 and 2010/19810-4). M.B. and J.B. acknowledge support for this work from the NSF (grant No. AST-1313119)

Facilities: VLT (UVES) - , Keck (HIRES) - , ESO:3.6m (HARPS) - European Southern Observatory's 3.6 meter Telescope

Footnotes

  • Based on observations obtained at the European Southern Observatory (ESO) Very Large Telescope (VLT) at Paranal Observatory; the 3.6 m telescope at La Silla Observatory, Chile (observing programs 083.D-0871 and 188.C-0265); and at the W.M. Keck Observatory, which is operated jointly by Caltech, the University of California, and NASA.

  • 10 

    When it was difficult to achieve convergence using the criteria of one-third of the error bars, we relaxed our criteria to solutions better than one-half of the error bars.

  • 11 

    Notice that the strongest iron lines do not have a significant impact on our final stellar parameters. If we remove the lines with log (EW/λ) >−4.8, the spectroscopic equilibrium would be preserved for Teff and log g, but only at the 1σ level for the microturbulence. The spectroscopic equilibrium would be fully recovered by changing vt by only −0.01 km s−1, without any impact on both Teff and log g. The resulting [Fe/H] would be only 0.002 dex higher.

  • 12 
  • 13 

    Similar models are considered to derive the s-process contribution in the solar system (e.g., Arlandini et al. 1999).

  • 14 

    As common in the literature, we use the terms s-process and r-process elements, but rigorously speaking that is incorrect because the s and r neutron-capture processes are responsible for the synthesis of isotopes. The s-process and r-process elements are deduced from decomposition of solar system material.

  • 15 
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10.1088/0004-637X/791/1/14