“T” in subscript in formulasWhy does Ruthenium only have one electron in its 5s orbital in the neutral...

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“T” in subscript in formulas


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.everyoneloves__top-leaderboard:empty,.everyoneloves__mid-leaderboard:empty,.everyoneloves__bot-mid-leaderboard:empty{ margin-bottom:0;
}







11












$begingroup$


Does a “T” in a formula subscript indicate all possible numbers of atoms? $ce{FeO_T}$ is the specific one I came across (in the "bulk chemistry" table here: https://sciences.ucf.edu/class/simulant_lunarmare), it seems to make sense in context but I've not done chemistry since school (tried googling already) so thought I'd better check.










share|improve this question









New contributor



axx is a new contributor to this site. Take care in asking for clarification, commenting, and answering.
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$endgroup$














  • $begingroup$
    Never saw this one and wouldn't believe it even if I did. Little "x" would do, though.
    $endgroup$
    – Ivan Neretin
    yesterday






  • 1




    $begingroup$
    geokem.com/glossary.html. See the 10th entry.
    $endgroup$
    – William R. Ebenezer
    yesterday












  • $begingroup$
    @IvanNeretin extremely common in geochemistry. For a visible example, see the Earth Wikipedia page, in the chemical composition table.
    $endgroup$
    – Gimelist
    16 hours ago


















11












$begingroup$


Does a “T” in a formula subscript indicate all possible numbers of atoms? $ce{FeO_T}$ is the specific one I came across (in the "bulk chemistry" table here: https://sciences.ucf.edu/class/simulant_lunarmare), it seems to make sense in context but I've not done chemistry since school (tried googling already) so thought I'd better check.










share|improve this question









New contributor



axx is a new contributor to this site. Take care in asking for clarification, commenting, and answering.
Check out our Code of Conduct.






$endgroup$














  • $begingroup$
    Never saw this one and wouldn't believe it even if I did. Little "x" would do, though.
    $endgroup$
    – Ivan Neretin
    yesterday






  • 1




    $begingroup$
    geokem.com/glossary.html. See the 10th entry.
    $endgroup$
    – William R. Ebenezer
    yesterday












  • $begingroup$
    @IvanNeretin extremely common in geochemistry. For a visible example, see the Earth Wikipedia page, in the chemical composition table.
    $endgroup$
    – Gimelist
    16 hours ago














11












11








11





$begingroup$


Does a “T” in a formula subscript indicate all possible numbers of atoms? $ce{FeO_T}$ is the specific one I came across (in the "bulk chemistry" table here: https://sciences.ucf.edu/class/simulant_lunarmare), it seems to make sense in context but I've not done chemistry since school (tried googling already) so thought I'd better check.










share|improve this question









New contributor



axx is a new contributor to this site. Take care in asking for clarification, commenting, and answering.
Check out our Code of Conduct.






$endgroup$




Does a “T” in a formula subscript indicate all possible numbers of atoms? $ce{FeO_T}$ is the specific one I came across (in the "bulk chemistry" table here: https://sciences.ucf.edu/class/simulant_lunarmare), it seems to make sense in context but I've not done chemistry since school (tried googling already) so thought I'd better check.







inorganic-chemistry notation






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New contributor



axx is a new contributor to this site. Take care in asking for clarification, commenting, and answering.
Check out our Code of Conduct.










share|improve this question









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share|improve this question




share|improve this question








edited yesterday









andselisk

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  • $begingroup$
    Never saw this one and wouldn't believe it even if I did. Little "x" would do, though.
    $endgroup$
    – Ivan Neretin
    yesterday






  • 1




    $begingroup$
    geokem.com/glossary.html. See the 10th entry.
    $endgroup$
    – William R. Ebenezer
    yesterday












  • $begingroup$
    @IvanNeretin extremely common in geochemistry. For a visible example, see the Earth Wikipedia page, in the chemical composition table.
    $endgroup$
    – Gimelist
    16 hours ago


















  • $begingroup$
    Never saw this one and wouldn't believe it even if I did. Little "x" would do, though.
    $endgroup$
    – Ivan Neretin
    yesterday






  • 1




    $begingroup$
    geokem.com/glossary.html. See the 10th entry.
    $endgroup$
    – William R. Ebenezer
    yesterday












  • $begingroup$
    @IvanNeretin extremely common in geochemistry. For a visible example, see the Earth Wikipedia page, in the chemical composition table.
    $endgroup$
    – Gimelist
    16 hours ago
















$begingroup$
Never saw this one and wouldn't believe it even if I did. Little "x" would do, though.
$endgroup$
– Ivan Neretin
yesterday




$begingroup$
Never saw this one and wouldn't believe it even if I did. Little "x" would do, though.
$endgroup$
– Ivan Neretin
yesterday




1




1




$begingroup$
geokem.com/glossary.html. See the 10th entry.
$endgroup$
– William R. Ebenezer
yesterday






$begingroup$
geokem.com/glossary.html. See the 10th entry.
$endgroup$
– William R. Ebenezer
yesterday














$begingroup$
@IvanNeretin extremely common in geochemistry. For a visible example, see the Earth Wikipedia page, in the chemical composition table.
$endgroup$
– Gimelist
16 hours ago




$begingroup$
@IvanNeretin extremely common in geochemistry. For a visible example, see the Earth Wikipedia page, in the chemical composition table.
$endgroup$
– Gimelist
16 hours ago










2 Answers
2






active

oldest

votes


















13













$begingroup$

Interesting question.
It looks like this is a rather common notation in geology and refers to the total iron(II) and iron(III) oxide (e.g. ferrous and ferric) content.
For a chemist this is probably somewhat confusing as “total” is normally denoted via subscripted abbreviation “tot”.
Flipping through numerous sources, it appears there is no standardized notation and alongside with $ce{FeO_T},$ $ce{FeO_t},$ $ce{FeOt}$ and $ce{FeO^mathrm{t}}$ are being used.



An introductory textbook by Shikazono [1, p. 21] explicitly defines $ce{FeO^mathrm{t}}$:




$ce{FeO^mathrm{t}}$: Total iron $(ce{FeO} + ce{Fe2O3})$




Reference




  1. Shikazono, N. Introduction to Earth and Planetary System Science: New View of Earth, Planets and Humans; Springer: Tokyo; New York, 2012. ISBN 978-4-431-54058-8.






share|improve this answer









$endgroup$























    9













    $begingroup$

    I will add to the correct answer by andselisk that the reason for this notation is that in most geochemical analytical methods, oxygen is not measured.
    Instead, all metals are measured and oxygen is calculated by stoichiometry assuming (often very reasonably) that all metals are as oxides.



    As the vast majority of major elements in geological materials have only one oxidation state throughout all geologically reasonable conditions, this works out very well.



    Iron is an exception: it is a major element that commonly exists both as divalent and trivalent. Because the oxidation state is much harder to analyse than the iron contents, iron is commonly reported as either all 2+ as FeO(t) or all 3+ as Fe2O3(t).






    share|improve this answer











    $endgroup$











    • 1




      $begingroup$
      This seems similar to, for example, how a fertiliser can have its phosphorus content measured in "percent weight as $ce{P2O5}$" or "percent weight as $ce{PO_4^{3-}}$. I've always found it confusing and opaque; why perform the completely unnecessary assumption that the element is found as a particular substance, especially in cases which clearly do not reflect reality, such as $ce{P2O5}$? Such easily avoidable problems...
      $endgroup$
      – Nicolau Saker Neto
      23 hours ago










    • $begingroup$
      @NicolauSakerNeto that's mostly a matter of opinion and convention. To me, as a geochemist, using $ce{PO4^3-}$ is misleading, because it adds oxygens that do not "belong" to the phosphorus. It is also not a neutral thermodynamic component, which personally makes me cringe. On the other hand, $ce{P2O5}$, or $ce{PO_{2.5}}$, is perfectly fine as it tells you exactly how much phosphorus (and associated oxygen) there is in the compound, without any assumptions.
      $endgroup$
      – Gimelist
      16 hours ago
















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    2 Answers
    2






    active

    oldest

    votes








    2 Answers
    2






    active

    oldest

    votes









    active

    oldest

    votes






    active

    oldest

    votes









    13













    $begingroup$

    Interesting question.
    It looks like this is a rather common notation in geology and refers to the total iron(II) and iron(III) oxide (e.g. ferrous and ferric) content.
    For a chemist this is probably somewhat confusing as “total” is normally denoted via subscripted abbreviation “tot”.
    Flipping through numerous sources, it appears there is no standardized notation and alongside with $ce{FeO_T},$ $ce{FeO_t},$ $ce{FeOt}$ and $ce{FeO^mathrm{t}}$ are being used.



    An introductory textbook by Shikazono [1, p. 21] explicitly defines $ce{FeO^mathrm{t}}$:




    $ce{FeO^mathrm{t}}$: Total iron $(ce{FeO} + ce{Fe2O3})$




    Reference




    1. Shikazono, N. Introduction to Earth and Planetary System Science: New View of Earth, Planets and Humans; Springer: Tokyo; New York, 2012. ISBN 978-4-431-54058-8.






    share|improve this answer









    $endgroup$




















      13













      $begingroup$

      Interesting question.
      It looks like this is a rather common notation in geology and refers to the total iron(II) and iron(III) oxide (e.g. ferrous and ferric) content.
      For a chemist this is probably somewhat confusing as “total” is normally denoted via subscripted abbreviation “tot”.
      Flipping through numerous sources, it appears there is no standardized notation and alongside with $ce{FeO_T},$ $ce{FeO_t},$ $ce{FeOt}$ and $ce{FeO^mathrm{t}}$ are being used.



      An introductory textbook by Shikazono [1, p. 21] explicitly defines $ce{FeO^mathrm{t}}$:




      $ce{FeO^mathrm{t}}$: Total iron $(ce{FeO} + ce{Fe2O3})$




      Reference




      1. Shikazono, N. Introduction to Earth and Planetary System Science: New View of Earth, Planets and Humans; Springer: Tokyo; New York, 2012. ISBN 978-4-431-54058-8.






      share|improve this answer









      $endgroup$


















        13














        13










        13







        $begingroup$

        Interesting question.
        It looks like this is a rather common notation in geology and refers to the total iron(II) and iron(III) oxide (e.g. ferrous and ferric) content.
        For a chemist this is probably somewhat confusing as “total” is normally denoted via subscripted abbreviation “tot”.
        Flipping through numerous sources, it appears there is no standardized notation and alongside with $ce{FeO_T},$ $ce{FeO_t},$ $ce{FeOt}$ and $ce{FeO^mathrm{t}}$ are being used.



        An introductory textbook by Shikazono [1, p. 21] explicitly defines $ce{FeO^mathrm{t}}$:




        $ce{FeO^mathrm{t}}$: Total iron $(ce{FeO} + ce{Fe2O3})$




        Reference




        1. Shikazono, N. Introduction to Earth and Planetary System Science: New View of Earth, Planets and Humans; Springer: Tokyo; New York, 2012. ISBN 978-4-431-54058-8.






        share|improve this answer









        $endgroup$



        Interesting question.
        It looks like this is a rather common notation in geology and refers to the total iron(II) and iron(III) oxide (e.g. ferrous and ferric) content.
        For a chemist this is probably somewhat confusing as “total” is normally denoted via subscripted abbreviation “tot”.
        Flipping through numerous sources, it appears there is no standardized notation and alongside with $ce{FeO_T},$ $ce{FeO_t},$ $ce{FeOt}$ and $ce{FeO^mathrm{t}}$ are being used.



        An introductory textbook by Shikazono [1, p. 21] explicitly defines $ce{FeO^mathrm{t}}$:




        $ce{FeO^mathrm{t}}$: Total iron $(ce{FeO} + ce{Fe2O3})$




        Reference




        1. Shikazono, N. Introduction to Earth and Planetary System Science: New View of Earth, Planets and Humans; Springer: Tokyo; New York, 2012. ISBN 978-4-431-54058-8.







        share|improve this answer












        share|improve this answer



        share|improve this answer










        answered yesterday









        andseliskandselisk

        22.2k8 gold badges77 silver badges149 bronze badges




        22.2k8 gold badges77 silver badges149 bronze badges




























            9













            $begingroup$

            I will add to the correct answer by andselisk that the reason for this notation is that in most geochemical analytical methods, oxygen is not measured.
            Instead, all metals are measured and oxygen is calculated by stoichiometry assuming (often very reasonably) that all metals are as oxides.



            As the vast majority of major elements in geological materials have only one oxidation state throughout all geologically reasonable conditions, this works out very well.



            Iron is an exception: it is a major element that commonly exists both as divalent and trivalent. Because the oxidation state is much harder to analyse than the iron contents, iron is commonly reported as either all 2+ as FeO(t) or all 3+ as Fe2O3(t).






            share|improve this answer











            $endgroup$











            • 1




              $begingroup$
              This seems similar to, for example, how a fertiliser can have its phosphorus content measured in "percent weight as $ce{P2O5}$" or "percent weight as $ce{PO_4^{3-}}$. I've always found it confusing and opaque; why perform the completely unnecessary assumption that the element is found as a particular substance, especially in cases which clearly do not reflect reality, such as $ce{P2O5}$? Such easily avoidable problems...
              $endgroup$
              – Nicolau Saker Neto
              23 hours ago










            • $begingroup$
              @NicolauSakerNeto that's mostly a matter of opinion and convention. To me, as a geochemist, using $ce{PO4^3-}$ is misleading, because it adds oxygens that do not "belong" to the phosphorus. It is also not a neutral thermodynamic component, which personally makes me cringe. On the other hand, $ce{P2O5}$, or $ce{PO_{2.5}}$, is perfectly fine as it tells you exactly how much phosphorus (and associated oxygen) there is in the compound, without any assumptions.
              $endgroup$
              – Gimelist
              16 hours ago


















            9













            $begingroup$

            I will add to the correct answer by andselisk that the reason for this notation is that in most geochemical analytical methods, oxygen is not measured.
            Instead, all metals are measured and oxygen is calculated by stoichiometry assuming (often very reasonably) that all metals are as oxides.



            As the vast majority of major elements in geological materials have only one oxidation state throughout all geologically reasonable conditions, this works out very well.



            Iron is an exception: it is a major element that commonly exists both as divalent and trivalent. Because the oxidation state is much harder to analyse than the iron contents, iron is commonly reported as either all 2+ as FeO(t) or all 3+ as Fe2O3(t).






            share|improve this answer











            $endgroup$











            • 1




              $begingroup$
              This seems similar to, for example, how a fertiliser can have its phosphorus content measured in "percent weight as $ce{P2O5}$" or "percent weight as $ce{PO_4^{3-}}$. I've always found it confusing and opaque; why perform the completely unnecessary assumption that the element is found as a particular substance, especially in cases which clearly do not reflect reality, such as $ce{P2O5}$? Such easily avoidable problems...
              $endgroup$
              – Nicolau Saker Neto
              23 hours ago










            • $begingroup$
              @NicolauSakerNeto that's mostly a matter of opinion and convention. To me, as a geochemist, using $ce{PO4^3-}$ is misleading, because it adds oxygens that do not "belong" to the phosphorus. It is also not a neutral thermodynamic component, which personally makes me cringe. On the other hand, $ce{P2O5}$, or $ce{PO_{2.5}}$, is perfectly fine as it tells you exactly how much phosphorus (and associated oxygen) there is in the compound, without any assumptions.
              $endgroup$
              – Gimelist
              16 hours ago
















            9














            9










            9







            $begingroup$

            I will add to the correct answer by andselisk that the reason for this notation is that in most geochemical analytical methods, oxygen is not measured.
            Instead, all metals are measured and oxygen is calculated by stoichiometry assuming (often very reasonably) that all metals are as oxides.



            As the vast majority of major elements in geological materials have only one oxidation state throughout all geologically reasonable conditions, this works out very well.



            Iron is an exception: it is a major element that commonly exists both as divalent and trivalent. Because the oxidation state is much harder to analyse than the iron contents, iron is commonly reported as either all 2+ as FeO(t) or all 3+ as Fe2O3(t).






            share|improve this answer











            $endgroup$



            I will add to the correct answer by andselisk that the reason for this notation is that in most geochemical analytical methods, oxygen is not measured.
            Instead, all metals are measured and oxygen is calculated by stoichiometry assuming (often very reasonably) that all metals are as oxides.



            As the vast majority of major elements in geological materials have only one oxidation state throughout all geologically reasonable conditions, this works out very well.



            Iron is an exception: it is a major element that commonly exists both as divalent and trivalent. Because the oxidation state is much harder to analyse than the iron contents, iron is commonly reported as either all 2+ as FeO(t) or all 3+ as Fe2O3(t).







            share|improve this answer














            share|improve this answer



            share|improve this answer








            edited 16 hours ago

























            answered yesterday









            GimelistGimelist

            4,11716 silver badges46 bronze badges




            4,11716 silver badges46 bronze badges











            • 1




              $begingroup$
              This seems similar to, for example, how a fertiliser can have its phosphorus content measured in "percent weight as $ce{P2O5}$" or "percent weight as $ce{PO_4^{3-}}$. I've always found it confusing and opaque; why perform the completely unnecessary assumption that the element is found as a particular substance, especially in cases which clearly do not reflect reality, such as $ce{P2O5}$? Such easily avoidable problems...
              $endgroup$
              – Nicolau Saker Neto
              23 hours ago










            • $begingroup$
              @NicolauSakerNeto that's mostly a matter of opinion and convention. To me, as a geochemist, using $ce{PO4^3-}$ is misleading, because it adds oxygens that do not "belong" to the phosphorus. It is also not a neutral thermodynamic component, which personally makes me cringe. On the other hand, $ce{P2O5}$, or $ce{PO_{2.5}}$, is perfectly fine as it tells you exactly how much phosphorus (and associated oxygen) there is in the compound, without any assumptions.
              $endgroup$
              – Gimelist
              16 hours ago
















            • 1




              $begingroup$
              This seems similar to, for example, how a fertiliser can have its phosphorus content measured in "percent weight as $ce{P2O5}$" or "percent weight as $ce{PO_4^{3-}}$. I've always found it confusing and opaque; why perform the completely unnecessary assumption that the element is found as a particular substance, especially in cases which clearly do not reflect reality, such as $ce{P2O5}$? Such easily avoidable problems...
              $endgroup$
              – Nicolau Saker Neto
              23 hours ago










            • $begingroup$
              @NicolauSakerNeto that's mostly a matter of opinion and convention. To me, as a geochemist, using $ce{PO4^3-}$ is misleading, because it adds oxygens that do not "belong" to the phosphorus. It is also not a neutral thermodynamic component, which personally makes me cringe. On the other hand, $ce{P2O5}$, or $ce{PO_{2.5}}$, is perfectly fine as it tells you exactly how much phosphorus (and associated oxygen) there is in the compound, without any assumptions.
              $endgroup$
              – Gimelist
              16 hours ago










            1




            1




            $begingroup$
            This seems similar to, for example, how a fertiliser can have its phosphorus content measured in "percent weight as $ce{P2O5}$" or "percent weight as $ce{PO_4^{3-}}$. I've always found it confusing and opaque; why perform the completely unnecessary assumption that the element is found as a particular substance, especially in cases which clearly do not reflect reality, such as $ce{P2O5}$? Such easily avoidable problems...
            $endgroup$
            – Nicolau Saker Neto
            23 hours ago




            $begingroup$
            This seems similar to, for example, how a fertiliser can have its phosphorus content measured in "percent weight as $ce{P2O5}$" or "percent weight as $ce{PO_4^{3-}}$. I've always found it confusing and opaque; why perform the completely unnecessary assumption that the element is found as a particular substance, especially in cases which clearly do not reflect reality, such as $ce{P2O5}$? Such easily avoidable problems...
            $endgroup$
            – Nicolau Saker Neto
            23 hours ago












            $begingroup$
            @NicolauSakerNeto that's mostly a matter of opinion and convention. To me, as a geochemist, using $ce{PO4^3-}$ is misleading, because it adds oxygens that do not "belong" to the phosphorus. It is also not a neutral thermodynamic component, which personally makes me cringe. On the other hand, $ce{P2O5}$, or $ce{PO_{2.5}}$, is perfectly fine as it tells you exactly how much phosphorus (and associated oxygen) there is in the compound, without any assumptions.
            $endgroup$
            – Gimelist
            16 hours ago






            $begingroup$
            @NicolauSakerNeto that's mostly a matter of opinion and convention. To me, as a geochemist, using $ce{PO4^3-}$ is misleading, because it adds oxygens that do not "belong" to the phosphorus. It is also not a neutral thermodynamic component, which personally makes me cringe. On the other hand, $ce{P2O5}$, or $ce{PO_{2.5}}$, is perfectly fine as it tells you exactly how much phosphorus (and associated oxygen) there is in the compound, without any assumptions.
            $endgroup$
            – Gimelist
            16 hours ago












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