Earth Materials. John O'Brien

−1 Gain one electron to achieve stable configuration Cl⁻¹, F⁻¹, Br⁻¹, I⁻¹ 18 (VIIIA) 0 Stable electron configuration; neither gain nor lose electrons He, Ne, Ar, Kr

      Metallic elements have relatively low first ionization energies (<900 kJ/mol) and tend to give up one or more weakly held electrons rather easily. Column 1 and 2 (group IA and group IIA) elements, the alkali metals and alkali earths, respectively, tend to display the most metallic behaviors. Most of the elements in columns 3–12 (groups IIIB through IIB), called the transition metals, also display metallic tendencies.

Nonmetallic elements have high first ionization energies (>900 kJ/mol) and tend not to release their tightly bound electrons. With the exception of the stable, nonreactive, very nonmetallic Noble elements in column 18 (group VIIIA), nonmetallic elements tend to be electronegative and possess high electron affinities. Column 16–17 (group VIA and group VIIA) elements, with their especially high electron affinities, display a strong tendency to capture additional electrons to fill their highest principle quantum levels. They provide the best examples of highly electronegative, nonmetallic elements. A brief summary of the characteristics of the columns and elemental groups is presented below and in Table 2.4.

       Column 1 (IA) metals are the only elements with a single s‐electron in their highest quantum levels. Elements in column 1 (IA) achieve the stable configuration of the next lowest quantum level when they lose their single s‐electron from the highest principal quantum level. For example, if sodium (Na) with the electron configuration (1s2, 2s2, 2p6, 3s1) loses its single 3s electron (Na+1), its electron configuration becomes that of the stable noble element neon (1s2, 2s2, 2p6) with the “stable octet” in the highest principle quantum level. Similar behavior is true for Li+1, K+1, and the other univalent (+1) cations in column 1 (IA).

       Column 2 (IIA) metals are the only elements with only two electrons in their highest quantum levels in their electrically neutral states. Column 2 (IIA) elements achieve stability by the removal of two s‐electrons from the outer electron shell to become divalent (+2) cations.

       Columns 3–12 (IIIB through IIB) transition elements are situated in the middle of the periodic table. Column 3 (IIIB) elements tend to occur as trivalent (+3) cations by giving up three of their electrons (s2, d1) to achieve a stable electron configuration. The other groups of transition elements, from column 4 (IVB) through column 12 (IIB) are cations that occur in a variety of ionization states. Depending on the chemical reaction in which they are involved, these elements can give up as few as one s‐electron as in Cu+1, Ag+1, and Au+1 or as many as six or seven electrons, two s‐electrons, and four or five d‐electrons as in Cr+6, W+6, and Mn+7. An excellent example of the variable ionization of a transition metal is iron (Fe). In environments where oxygen is relatively scarce, iron commonly gives up two electrons to become Fe+2 or ferrous iron. In other environments, especially those where oxygen is abundant, iron gives up three electrons to become smaller Fe+3 or ferric iron.

       Column 13 (IIIA) elements such as Al+3 commonly exist as trivalent (+3) cations by losing three electrons (s2, p1).

       Column 14 (IVA) elements such as Si+4 commonly exist as tetravalent (+4) cations by losing four electrons. The behavior of the heavier elements in this group is somewhat more variable than in those groups discussed previously. It depends on the chemical reaction in which the elements are involved. Tin (Sn) and lead (Pb) behave in a similar manner to silicon and germanium in some chemical reactions, but in other reactions they only lose the two s‐electrons in the highest principal quantum level to become divalent cations.

       Column 15 (VA) elements commonly have a wide range of ionization states from tetravalent (+5) cations through trivalent (−3) anions. These elements are not particularly electropositive, nor are they especially electronegative. Their behavior depends on the other elements in the chemical reaction in which they are involved. For example, in some chemical reactions, with electropositive elements, nitrogen attracts three additional electrons to become the trivalent anion N−3. In other chemical reactions, with electronegative elements, nitrogen releases as many as five electrons in the second principal quantum level to become the pentavalent cation N+5. In still other situations, nitrogen gives up or attracts smaller numbers of electrons to form a cation or anion of smaller charge. All the other elements in group VA exhibit analogous situational ionization behaviors. Phosphorous, arsenic, antimony and bismuth all have ionic states that range from +5 to −3.

       Column 16 (VIA) nonmetallic elements commonly exist as divalent (−2) anions. These elements attract two additional electrons into their highest principal quantum levels to achieve a stable electron configuration. For example, oxygen adds two electrons to become the divalent anion O−2. With the exception of oxygen, however, the column 16 elements display other ionization states as well, especially when they react chemically with oxygen, as will be discussed later in this chapter. Sulfur and the other VIA elements are also quite electronegative, with strong electron affinities, so that they tend to attract two electrons to achieve a stable configuration and become divalent anions such as S−2. However, in the presence of highly electronegative oxygen these elements may lose electrons and become cations such as S+6.

       Column 17 (VIIA) nonmetallic elements such as Cl− and F−1 commonly exist as monovalent (−1) anions. Because electrons are very difficult to remove from their electron clouds, these elements tend to attract one additional electron into their highest principal quantum level to achieve a stable electron configuration.

       Column 18 (VIIIA) noble gas elements such as He, Ar, and Ne contain complete outer electron shells (s2, p6) and do not commonly combine with other elements to form minerals. Instead, they tend to exist as monatomic (composed of single atoms) gases.

      The periodic table is a highly visual and logical way in which to illustrate patterns in the electron configurations of the elements. Elements are grouped in rows or classes according to the highest principal quantum level in which electrons occur in the ground state. Elements are grouped into columns or groups based on similarities in the electron configurations in the higher principal quantum levels; those that are farthest from the nucleus and involved in most chemical reactions. More thorough explanations of the periodic table and the properties of elements are available in many standard texts in chemistry and physics.

      From the discussion above, it should be clear that during the chemical reactions that produce Earth materials, elements display behaviors that are related to their electron configurations. Group 18 (VIIIA) elements in the far right column of the periodic table have stable electron configurations and tend to exist as uncharged atoms. Metallic elements toward the left side of the periodic table are strongly electropositive and tend to give up one or more electrons to become positively charged particles called cations. Nonmetallic elements toward the right side of the periodic table, especially in groups 16 (VIA) and 17 (VIIA), are strongly electronegative and tend to attract electrons to become negatively charged particles called anions. Elements toward the middle of the periodic table are somewhat electropositive and tend to lose various numbers of electrons to become cations with various amounts of positive charge. These tendencies are summarized in Table 2.4.

Figure 2.6 Trends in variation of atomic radii (in angstroms; 1 Å = 10⁻¹⁰ m) with their position on the periodic table, illustrated by rows 3 and 4. With few exceptions, radii tend to decrease from left to right and from bottom to top.