Isotopes are fully supported by SPECTRUM in the ``isotope mode'', which can be invoked with the ``i'' switch (see § ). It must be understood that SPECTRUM does not automatically calculate isotope shifts; the isotopic components of a given spectral line must be included in the spectral linelist as individual entries. The format of an isotopic spectral linelist is different from the format for the standard linelist; it must include an additional column indicating the mass number or ``isotope code'' of the isotope in question. As an example, consider the following entries used for the computation of the Li I 6708Å resonance line:
6703.568 26.0 0 22249 37163 -3.15 1.000 01 NIST 6704.476 26.0 0 34017 48928 -2.659 1.000 10 NIST 6705.106 26.0 0 37186 52090 -1.17 1.000 99 AGL 6707.44 26.0 0 37186 52090 -2.40 1.000 99 AGL 6707.752 21.0 0 32659 47563 -2.672 1.000 99 K23 6707.754 3.0 7 0 14904 -0.431 1.000 01 AGL 6707.766 3.0 7 0 14904 -0.209 1.000 01 AGL 6707.771 20.0 0 46748 61652 -4.015 1.000 99 K23 6707.824 26.1 0 93488 108392 -3.094 1.000 99 K23 6707.904 3.0 7 0 14904 -0.733 1.000 01 AGL 6707.917 3.0 7 0 14904 -0.510 1.000 01 AGL 6707.921 3.0 6 0 14904 -0.005 1.000 01 AGL 6708.053 26.1 0 93485 108388 -3.614 1.000 99 K23 6708.072 3.0 6 0 14904 -0.306 1.000 01 AGL 6708.094 23.0 0 9825 24728 -3.113 1.000 99 KFE 6708.167 26.1 0 89727 104630 -3.979 1.000 99 K23 6710.316 26.0 0 11976 26875 -4.874 1.000 21 NIST 6712.44 26.0 0 40231 55125 -2.149 1.000 99 NIST 6713.77 26.0 0 38678 53569 -1.602 1.000 12 NIST
Compare the format of this linelist with that illustrated in § . The third column contains the mass number of the isotope involved; for instance, the entry for the spectral line with a wavelength of 6707.754Å in the above list is for the isotope Li, and the one for 6707.921Å is for Li. Note that many of the spectral lines in the above example have isotope codes of ``0''. The ``0'' code corresponds to the case in which the isotope shifts are considered to be zero, and thus these entries represent all possible isotopes for that species taken together. So, for instance, since iron (26) has isotopes with mass numbers 54, 56, 57, and 58, the single entry
6703.568 26.0 0 22249 37163 -3.15 1.000 01 NISTis equivalent to the entries
6703.568 26.0 54 22249 37163 -3.15 1.000 01 NIST 6703.568 26.0 56 22249 37163 -3.15 1.000 01 NIST 6703.568 26.0 57 22249 37163 -3.15 1.000 01 NIST 6703.568 26.0 58 22249 37163 -3.15 1.000 01 NIST
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Isotopes with odd nucleon numbers can exhibit hyperfine structure; elements with odd atomic numbers are especially subject to this phenomenon. Thus, lines of vanadium (23), manganese (25), cobalt (27) and copper (29) in the solar spectrum commonly show unusually broad profiles formed from the superposition of a number of hyperfine components (see Figure ). It is quite a frequent occurrence for a single line to show both isotope shifts and hyperfine structure; the Ba II 4554Å resonance line is a case in point, and so is the important Eu II 4129.7Å resonance line, the components of which are listed below:
4129.628 -63.1 151 1 24208 -1.512 1.000 01 LWDS 4129.631 -63.1 151 1 24208 -1.035 1.000 01 LWDS 4129.645 -63.1 151 1 24208 -1.316 1.000 01 LWDS 4129.649 -63.1 151 1 24208 -0.977 1.000 01 LWDS 4129.653 -63.1 151 1 24208 -1.512 1.000 01 LWDS 4129.670 -63.1 151 0 24208 -1.257 1.000 01 LWDS 4129.675 -63.1 151 0 24208 -0.847 1.000 01 LWDS 4129.680 -63.1 151 0 24208 -1.316 1.000 01 LWDS 4129.703 -63.1 151 0 24208 -1.294 1.000 01 LWDS 4129.708 -63.1 153 0 24208 -1.512 1.000 01 LWDS 4129.709 -63.1 151 0 24208 -0.696 1.000 01 LWDS 4129.711 -63.1 153 0 24208 -1.035 1.000 01 LWDS 4129.715 -63.1 151 0 24208 -1.257 1.000 01 LWDS 4129.715 -63.1 153 0 24208 -1.316 1.000 01 LWDS 4129.718 -63.1 153 0 24208 -0.977 1.000 01 LWDS 4129.721 -63.1 153 0 24208 -1.512 1.000 01 LWDS 4129.725 -63.1 153 0 24208 -1.257 1.000 01 LWDS 4129.728 -63.1 153 0 24208 -0.847 1.000 01 LWDS 4129.732 -63.1 153 0 24208 -1.316 1.000 01 LWDS 4129.740 -63.1 153 0 24208 -1.294 1.000 01 LWDS 4129.743 -63.1 153 0 24208 -0.696 1.000 01 LWDS 4129.744 -63.1 151 0 24208 -1.480 1.000 01 LWDS 4129.746 -63.1 153 0 24208 -1.257 1.000 01 LWDS 4129.751 -63.1 151 0 24208 -0.545 1.000 01 LWDS 4129.757 -63.1 151 0 24208 -1.294 1.000 01 LWDS 4129.760 -63.1 153 0 24208 -1.480 1.000 01 LWDS 4129.761 -63.1 153 0 24208 -0.545 1.000 01 LWDS 4129.764 -63.1 153 0 24208 -1.294 1.000 01 LWDS 4129.786 -63.1 153 0 24208 -0.401 1.000 01 LWDS 4129.787 -63.1 153 0 24208 -1.480 1.000 01 LWDS 4129.801 -63.1 151 1 24208 -0.401 1.000 01 LWDS 4129.808 -63.1 151 1 24208 -1.480 1.000 01 LWDS
Obviously, in this example, SPECTRUM must be used in the isotope mode, as the Eu II 4129.7Å line involves not only hyperfine components but also isotopic components (indicated by the isotope numbers 151 and 153). Note in this example that the species code (63.1 for Eu II) is entered as a negative number. This prompts SPECTRUM to increase the computation radius for such spectral lines by a factor of three. This is done because each hyperfine component taken on its own may be a very weak spectral line (and thus would have a small computation radius assigned to it), but since it overlaps with other closely spaced hyperfine components, if its computation radius were not increased the far wings of the combined spectral line could be truncated. Indeed, this trick can be used if you observe SPECTRUM truncating the far wings of any line; enter the species code for that line as a negative number, and the normal computation radius for that line will be tripled, up to a maximum of 20Å (10Å in the optical). A handful of lines, such as the Ca II K and H lines, obviously need a larger computational radius than this, and such lines are actually hard-coded into SPECTRUM. See § for more details.