author_facet Chatterjee, Nilanjan
Chatterjee, Nilanjan
author Chatterjee, Nilanjan
spellingShingle Chatterjee, Nilanjan
Microscopy Today
Fe 2+/ Fe2+ Calculation In Spinels From Oxygen Deficiency Sum
Pharmacology
author_sort chatterjee, nilanjan
spelling Chatterjee, Nilanjan 2150-3583 1551-9295 Oxford University Press (OUP) Pharmacology http://dx.doi.org/10.1017/s1551929500067201 <jats:title>Abstract</jats:title> <jats:p>A typical electron microprobe printout of an oxide analysis shows weight percent concentrations of different elements in terms of their oxides, Fe is usually expressed as FeO. For minerals, it also shows calculated number of cations on the basis of an assumed (theoretical) number of oxygen atoms. For examplejn olivines, (Mg,Fe)2SiO4, the theoretical number of oxygen atoms is four and the sum of cations should add up to three if the analysis is good. However, in case of spinels such as magnetite, Fe3O4, which contain significant amounts of Fe2O3, the analysis total falls below 100 and the cation sum (based on four oxygens) exceeds the theoretical cation sum. in other words, the formula calculation shows an oxygen deficiency. Geologists use this information to calculate the amount of Fe2O3 in the spinel assuming the other cations have only one oxidation state.</jats:p> <i>Fe</i> 2+/ <i>Fe</i>2+ Calculation In Spinels From Oxygen Deficiency Sum Microscopy Today
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title Fe 2+/ Fe2+ Calculation In Spinels From Oxygen Deficiency Sum
title_unstemmed Fe 2+/ Fe2+ Calculation In Spinels From Oxygen Deficiency Sum
title_full Fe 2+/ Fe2+ Calculation In Spinels From Oxygen Deficiency Sum
title_fullStr Fe 2+/ Fe2+ Calculation In Spinels From Oxygen Deficiency Sum
title_full_unstemmed Fe 2+/ Fe2+ Calculation In Spinels From Oxygen Deficiency Sum
title_short Fe 2+/ Fe2+ Calculation In Spinels From Oxygen Deficiency Sum
title_sort <i>fe</i> 2+/ <i>fe</i>2+ calculation in spinels from oxygen deficiency sum
topic Pharmacology
url http://dx.doi.org/10.1017/s1551929500067201
publishDate 1998
physical 10-11
description <jats:title>Abstract</jats:title> <jats:p>A typical electron microprobe printout of an oxide analysis shows weight percent concentrations of different elements in terms of their oxides, Fe is usually expressed as FeO. For minerals, it also shows calculated number of cations on the basis of an assumed (theoretical) number of oxygen atoms. For examplejn olivines, (Mg,Fe)2SiO4, the theoretical number of oxygen atoms is four and the sum of cations should add up to three if the analysis is good. However, in case of spinels such as magnetite, Fe3O4, which contain significant amounts of Fe2O3, the analysis total falls below 100 and the cation sum (based on four oxygens) exceeds the theoretical cation sum. in other words, the formula calculation shows an oxygen deficiency. Geologists use this information to calculate the amount of Fe2O3 in the spinel assuming the other cations have only one oxidation state.</jats:p>
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author Chatterjee, Nilanjan
author_facet Chatterjee, Nilanjan, Chatterjee, Nilanjan
author_sort chatterjee, nilanjan
container_issue 4
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container_title Microscopy Today
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description <jats:title>Abstract</jats:title> <jats:p>A typical electron microprobe printout of an oxide analysis shows weight percent concentrations of different elements in terms of their oxides, Fe is usually expressed as FeO. For minerals, it also shows calculated number of cations on the basis of an assumed (theoretical) number of oxygen atoms. For examplejn olivines, (Mg,Fe)2SiO4, the theoretical number of oxygen atoms is four and the sum of cations should add up to three if the analysis is good. However, in case of spinels such as magnetite, Fe3O4, which contain significant amounts of Fe2O3, the analysis total falls below 100 and the cation sum (based on four oxygens) exceeds the theoretical cation sum. in other words, the formula calculation shows an oxygen deficiency. Geologists use this information to calculate the amount of Fe2O3 in the spinel assuming the other cations have only one oxidation state.</jats:p>
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spelling Chatterjee, Nilanjan 2150-3583 1551-9295 Oxford University Press (OUP) Pharmacology http://dx.doi.org/10.1017/s1551929500067201 <jats:title>Abstract</jats:title> <jats:p>A typical electron microprobe printout of an oxide analysis shows weight percent concentrations of different elements in terms of their oxides, Fe is usually expressed as FeO. For minerals, it also shows calculated number of cations on the basis of an assumed (theoretical) number of oxygen atoms. For examplejn olivines, (Mg,Fe)2SiO4, the theoretical number of oxygen atoms is four and the sum of cations should add up to three if the analysis is good. However, in case of spinels such as magnetite, Fe3O4, which contain significant amounts of Fe2O3, the analysis total falls below 100 and the cation sum (based on four oxygens) exceeds the theoretical cation sum. in other words, the formula calculation shows an oxygen deficiency. Geologists use this information to calculate the amount of Fe2O3 in the spinel assuming the other cations have only one oxidation state.</jats:p> <i>Fe</i> 2+/ <i>Fe</i>2+ Calculation In Spinels From Oxygen Deficiency Sum Microscopy Today
spellingShingle Chatterjee, Nilanjan, Microscopy Today, Fe 2+/ Fe2+ Calculation In Spinels From Oxygen Deficiency Sum, Pharmacology
title Fe 2+/ Fe2+ Calculation In Spinels From Oxygen Deficiency Sum
title_full Fe 2+/ Fe2+ Calculation In Spinels From Oxygen Deficiency Sum
title_fullStr Fe 2+/ Fe2+ Calculation In Spinels From Oxygen Deficiency Sum
title_full_unstemmed Fe 2+/ Fe2+ Calculation In Spinels From Oxygen Deficiency Sum
title_short Fe 2+/ Fe2+ Calculation In Spinels From Oxygen Deficiency Sum
title_sort <i>fe</i> 2+/ <i>fe</i>2+ calculation in spinels from oxygen deficiency sum
title_unstemmed Fe 2+/ Fe2+ Calculation In Spinels From Oxygen Deficiency Sum
topic Pharmacology
url http://dx.doi.org/10.1017/s1551929500067201