“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
Why does Ruthenium only have one electron in its 5s orbital in the neutral oxidation state?Why does reduced mass help when talking about two body problems?X[Y|Z] formulasPhase subscript for supercritical reagent?Brackets in chemical formulasUse of subscript cc for HCl and H2SO4Different formulas for copper pyrites and bauxiteHow does the energy released during a bond formation typically manifest itself on atomic level?
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$begingroup$
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.
inorganic-chemistry notation
New contributor
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add a comment |
$begingroup$
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.
inorganic-chemistry notation
New contributor
$endgroup$
$begingroup$
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
add a comment |
$begingroup$
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.
inorganic-chemistry notation
New contributor
$endgroup$
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
inorganic-chemistry notation
New contributor
New contributor
edited yesterday
andselisk♦
22.2k8 gold badges77 silver badges149 bronze badges
22.2k8 gold badges77 silver badges149 bronze badges
New contributor
asked yesterday
axxaxx
562 bronze badges
562 bronze badges
New contributor
New contributor
$begingroup$
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
add a comment |
$begingroup$
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
add a comment |
2 Answers
2
active
oldest
votes
$begingroup$
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
- 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.
$endgroup$
add a comment |
$begingroup$
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).
$endgroup$
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
add a comment |
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2 Answers
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2 Answers
2
active
oldest
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active
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$begingroup$
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
- 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.
$endgroup$
add a comment |
$begingroup$
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
- 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.
$endgroup$
add a comment |
$begingroup$
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
- 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.
$endgroup$
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
- 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.
answered yesterday
andselisk♦andselisk
22.2k8 gold badges77 silver badges149 bronze badges
22.2k8 gold badges77 silver badges149 bronze badges
add a comment |
add a comment |
$begingroup$
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).
$endgroup$
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
add a comment |
$begingroup$
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).
$endgroup$
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
add a comment |
$begingroup$
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).
$endgroup$
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).
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
add a comment |
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
add a comment |
axx is a new contributor. Be nice, and check out our Code of Conduct.
axx is a new contributor. Be nice, and check out our Code of Conduct.
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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