Geology For Dummies. Alecia M. Spooner

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(covalent bonds)

      When two atoms bond together, and neither one donates or gives up an electron, they form a covalent bond. In a covalent bond the atoms share the electrons in their outer orbital shells. The sharing of electrons in covalent bonding creates a very strong bond because each atom participating in the electron share has a full outer shell and a neutral charge.

Schematic illustration of the ionic bond between sodium and chloride to form a molecule of NaCl.

      Migrating electrons (metallic bonds)

Schematic illustration of covalent bonding in a water molecule.

      FIGURE 5-5: Covalent bonding in a water molecule.

Schematic illustration of the metallic bonding between atoms in a sea of electrons.

      FIGURE 5-6: Metallic bonding between atoms in a sea of electrons.

The unique nature of metallic bonds is what gives metals such as gold or silver their unique characteristics. The ability to conduct electrical current is a result of the movement of electrons. The shiny, or metallic appearance is due to the large number of freely floating electrons. And the fact that metals can be bent and molded without breaking is also a result of the movement of electrons between atoms in the metallic bond.

      The bonding of elements to form compounds is fundamental to understanding the formation of rocks and minerals (which I describe in Chapter 6). When scientists discuss the processes of rock formation, as well as other earth processes involving chemical changes (such as weathering, described in Chapter 7), they use a shorthand of chemical formulas.

      The chemical formula of a compound describes the number of different atoms of each element that are combined into a compound. For example, the chemical formula for quartz is as follows:

      SiO2

      This formula indicates that one atom of silicon (Si) and two atoms of oxygen (O) have bonded together, forming the compound.

      

In the case of geology, most chemical formulas describe minerals, which are solid structures built of molecules (see Chapter 6). In mineral compounds, sometimes multiple elements can fill the same spot in the mineral structure. For example, the mineral olivine has this formula:

      (Mg, Fe)2SiO4

      Two atoms of either magnesium (Mg) or iron (Fe) will combine with one atom of silicon (Si) and four atoms of oxygen (O). Either magnesium or iron can create the mineral olivine, so when you write the chemical formula, you put a parenthesis around and a comma separating the possible atoms that can form that particular chemical compound.

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