Earth Materials. John O'Brien
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Letters 28: 391–417.
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Chapter 2 Atoms, elements, bonds, and coordination polyhedra
4 2.4 Pauling's rules and coordination polyhedra
5 2.5 The chemical classification of minerals
If we zoom in on any portion of Earth, we will see that it is composed of progressively smaller entities. At very high magnification, we will be able to discern very small particles called atoms. Almost all Earth materials are composed of atoms which, in turn, strongly influence their material properties. Understanding the ways in which these basic chemical constituents combine to produce larger scale Earth materials is essential to understanding our planet.
In this chapter we will consider the fundamental chemical constituents that bond together to produce Earth materials such as minerals and rocks. We will discuss the nuclear and electron configurations of atoms and then discuss the role these play in determining both atomic and mineral properties and the conditions under which minerals form. This information will provide a basis for understanding how and why minerals, rocks and other Earth materials have the following characteristics:
1 They possess specific properties that characterize and distinguish them.
2 They provide benefits and hazards through their production, refinement and use.
3 They form in response to particular sets of environmental conditions and processes.
4 They record information about the conditions and processes that produce them.
5 They permit us to infer significant events in Earth's history.
2.1 ATOMS
Earth materials are composed of smaller entities. At very small scales, such as viewed through a tunneling electron microscope, we are able to discern particles called atoms whose effective diameters are a few angstroms (1 Å = 10−10 m, about a million times smaller than the width of a human hair). These tiny atoms, in turn, consist of three main particles – electrons, protons, and neutrons – which were discovered between 1895 and 1902. The major properties of electrons, protons, and neutrons are summarized in Table 2.1.
Protons (p+) and neutrons (n0) each have a mass of ~1 atomic mass unit (amu) and are clustered together in a small, positively charged, central region of the atom called the nucleus (Figure 2.1). Protons possess a positive electric charge and neutrons are electrically neutral. The nucleus is surrounded by a vastly larger, mostly “empty”, region called the electron cloud. The electron cloud represents the area in which the electrons (e−) in the atom move about the nucleus in patterns called orbitals (Figure 2.1). Electrons have a negative electric charge and an almost negligible mass of 0.000 005 amu. Knowledge of these three fundamental particles in atoms is essential to understanding how minerals and other materials form, how they can be used as resources and how we can deal with their hazardous effects that can be seen occasionally.
Table 2.1 Major properties of electrons, protons, and neutrons.
| Particle type | Electric charge | Atomic mass (amu)a |
|---|---|---|
| Proton (p+) | +1 | 1.00 728 |
| Neutron (n0) | 0 | 1.00 867 |
| Electron (e−) | −1 | 0.0 000 054 |
a amu = atomic mass unit = 1/12 mass of an average carbon atom.