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Clerical:
Reminder: Quizzes 1-4 are due by the end of September.
Quizzes 5-10 are also now posted. They are due by 5:00pm on the date of Exam #2, 10/12/09.
Themes of the Day:
- Ions & Chemical Bonding
- Size of Atoms and Ions
Ions
- Ions - charged atoms with # of electrons not equal to # of protons - important for bonding
- Anions - negative charge - # of Electrons > # of Protons - ex. Chlorine (Cl-), Oxygen (O2-)
- Cations - positive charge - # of Electrons < # of Protons - ex. Sodium (Na+), Magnesium (Mg2+)
- Ionic charge = valence = oxidation state
- Periodic Table - helps predict ionic charges
- Electronegativity - Linus Pauling (1960) - propensity to gain or lose electrons - the difference in electronegativity between cation and anion can be related to the percent ionic character of the bond (more below)
- Ions with similar charges and sizes may substitute for each other in some minerals
- Abundance of elements in the Earth's crust:
| Element |
Chemical Symbol and Common Ion(s) |
Percent (by weight) |
| Oxygen |
O2- |
46 |
| Silicon |
Si4+ |
28 |
| Aluminum |
Al3+ |
8 |
| Iron |
Fe2+ or Fe3+ |
6 |
| Magnesium |
Mg2+ |
4 |
| Calcium |
Ca2+ |
2.4 |
| Potassium |
K1+ |
2.3 |
| Sodium |
Na1+ |
2.1 |
| All others |
|
<1 |
Chemical Bonding
- Bonding is what happens when ions share electrons.
- Valence Related Bonding
- Ionic bonds - electron(s) substantially transferred - e.g., Halite (NaCl) - tend to be brittle bonds
- Covalent bonds - electron(s) more evenly shared - e.g., Diamond (C) - strong bonds (diamond is strongest)
- Metallic bonds - transition metal nuclei swimming in a sea of shared electrons - e.g., Gold (Au) - malleable
- Range of Bond Character
- Percent Ionic Character
- Bonds Not Involving Valence Electrons - generally weak (often feels greasy)
- Hydrogen bonds - e.g., ice (H2O) - Mohs Hardness = 3
- van der Waals bonds - e.g., graphite (C) or talc (Mg3AlSi3O10(OH)2)
- Silicate minerals, containing covalently bonded SiO4 tetrahedra are most common in Earth's crust and mantle
Size of Atoms and Ions
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