Table 4
Slopes and zero-points of the abundance gradients for various elements.
Element | Range | Slope | Zero-point | rms | N | Slope (previous studies) | rms |
kpc | dex/kpc | dex | dex/kpc | ||||
|
|||||||
[Na/H] | [4−15] | –0.066 ± 0.015 | 0.843 ± 0.146 | 0.177 | 42 | –0.047 ± 0.003 | 0.131 |
[7−15] | –0.049 ± 0.016 | 0.673 ± 0.161 | 0.154 | 39 | |||
[Mg/H] | [4−15] | –0.050 ± 0.013 | 0.594 ± 0.133 | 0.185 | 54 | –0.048 ± 0.004 | 0.160 |
[7−15] | –0.030 ± 0.015 | 0.381 ± 0.150 | 0.174 | 51 | |||
[Al/H] | [4−15] | –0.046 ± 0.013 | 0.508 ± 0.122 | 0.170 | 55 | –0.049 ± 0.003 | 0.130 |
[7−15] | –0.030 ± 0.014 | 0.343 ± 0.142 | 0.164 | 52 | |||
[Si/H] | [4−15] | –0.068 ± 0.009 | 0.690 ± 0.089 | 0.139 | 62 | –0.048 ± 0.002 | 0.088 |
[7−15] | –0.057 ± 0.011 | 0.575 ± 0.110 | 0.140 | 58 | |||
[S/H] | [4−15] | –0.095 ± 0.015 | 1.031 ± 0.152 | 0.206 | 52 | –0.076 ± 0.005 | 0.159 |
[7−15] | –0.079 ± 0.017 | 0.857 ± 0.173 | 0.202 | 50 | |||
[Ca/H] | [4−15] | –0.044 ± 0.012 | 0.409 ± 0.119 | 0.173 | 61 | –0.041 ± 0.003 | 0.114 |
[7−15] | –0.033 ± 0.014 | 0.302 ± 0.138 | 0.173 | 58 | |||
[Y/H] | [4−15] | –0.062 ± 0.012 | 0.569 ± 0.114 | 0.166 | 61 | –0.061 ± 0.003 | 0.116 |
[Zr/H] | [4−15] | –0.078 ± 0.016 | 0.814 ± 0.158 | 0.162 | 41 | –0.047 ± 0.005 | 0.127 |
[La/H] | [4−15] | –0.045 ± 0.012 | 0.541 ± 0.111 | 0.168 | 60 | –0.031 ± 0.004 | 0.144 |
[Ce/H] | [4−15] | –0.043 ± 0.012 | 0.597 ± 0.113 | 0.158 | 55 | –0.034 ± 0.003 | 0.133 |
[Nd/H] | [4−15] | –0.046 ± 0.013 | 0.593 ± 0.131 | 0.165 | 55 | –0.037 ± 0.003 | 0.114 |
[Eu/H] | [4−15] | –0.066 ± 0.013 | 0.778 ± 0.122 | 0.184 | 59 | –0.042 ± 0.005 | 0.171 |
[7−15] | –0.056 ± 0.015 | 0.671 ± 0.153 | 0.184 | 55 |
Notes. We also indicate the root mean square (rms) of the residuals and the number of data points for the fit. For some elements, we also computed the gradient over a different distance range. The gradient values and rms obtained by Luck & Lambert (2011) are tabulated for comparison (Luck et al. (2011) for S and Zr).
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