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Detailed File Information |
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File Name |
m00024.dat.547.core.composition.1.pdf |
Data Type |
spreadsheet |
Computer Program |
Microsoft Excel 2000 |
File Size |
39.00 KB - 2 files [ pdf,xls ] |
Expert Level |
High School (Grade 9-12) |
Contributor |
ERESE Database Team |
Source |
McDonough 1998
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Resource Matrix |
The Earth's Mantle |
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Description
The attached data table provides detailed element composition of the core compared to the bulk earth and silicate earth. Comparing the composition data for each area, it can be seen where a large percentage of the bulk earth's material lies within the earth. For example, the percentage of iron (Fe) within the core is believed to be 85%, while the silicate earth is about 6%. Based on the thickness of the different layers, it has been determined that the bulk earth is then comprised of about 32% iron. Similar analysis can be made with other elements in determining where they are most abundant within the Earth (i.e. silica (Si) and nickel (Ni)). The presence of lighter elements in the core is due to their affinity for iron (siderophile elements). Similarly, the sulfer (S) in the core may also have attracted elements like potassium (K), which have an affinity for sulfer (chalcophilic elements). |
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Keywords ERESE, core, element, bulk earth, silicate earth |
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Copyright Owner Enduring Resources for Earth Science Education (ERESE) |
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