Many chemical reactions do not involve any change in oxidation state. For example, when we reacted aqueous solutions of copper(II) sulfate and sodium hydroxide to form a precipitate of copper(II) hydroxide and a solution of sodium sulfate, no changes in oxidation state occurred:
CuSO4(aq) + 2 NaOH(aq) → Cu(OH)2(s) + Na2SO4(aq)
or, showing the oxidation states:
Cu2+(aq) + SO42–(aq) + 2 Na+(aq) + 2 OH–(aq) → [Cu2+(OH–)2](s) + 2 Na+(aq) + SO42–(aq)
On both sides of the equation, copper is in the +2 oxidation state, sulfate –2, sodium +1, and hydroxide –1.
Oxidation state 0 is the neutral form of any element, such as (at standard conditions) aluminum in its metallic form or chlorine in its gaseous form. An element in oxidation state 0 possesses the same number of negatively charged electrons in its shell as the number of positively charged protons in its nucleus, leaving a net charge of 0.
If a chlorine atom at oxidation state 0 gains an electron, that chlorine atom becomes a chlorine ion with a charge of –1, and an oxidation state of –1. Conversely, if a chlorine atom at oxidation state 0 loses an electron, that chlorine atom becomes a chlorine ion with a charge of +1, and an oxidation state of +1. With the exception of the noble gases—helium, neon, argon, krypton, xenon, and radon, all in column 18 of the periodic table—all elements are commonly found in at least one oxidation state other than 0. Some elements have only one or two known nonzero oxidation states. Other elements are commonly found in many oxidation states. For example, in its natural form and in its many compounds, carbon can be found in oxidation states –4, –3, –2, –1, 0, +1, +2, +3, and +4.
Oxidation and reduction also apply to atoms that are in oxidation states other than 0. For example, iron is found in three oxidation states. Metallic iron is in oxidation state 0. Metallic iron can be oxidized to the Fe2+ ion, also called the ferrous ion or the iron(II) ion. The Fe2+ ion can be further oxidized to the Fe3+ ion—also called the ferric ion or the iron(III) ion—or it can be reduced to metallic iron. The Fe3+ ion can be reduced to the Fe2+ ion by gaining one electron, or all the way to Fe0 (iron metal) by gaining three electrons.
Ions of a particular element in different oxidation states can have very different chemical and physical properties. For example, solutions that contain vanadium ions in different oxidation states show a rainbow of colors. Solutions of V5+ ions are yellow; those of V4+ are blue; V3+, green; and V2+, violet. Solutions of ions in different oxidations states of chromium, manganese, and other elements show similar color differences.
It’s important to understand that in a redox reaction oxidation and reduction are two sides of the same coin. If one atom is oxidized during the reaction, another must be reduced, and vice versa. Furthermore, the total number of electrons lost by the atom or atoms being oxidized must equal the total number of electrons gained by the atom or atoms that are being reduced. Charge must be conserved. For example, when aluminum reacts with the H+ ions from hydrochloric acid to form Al3+ ions, the three electrons lost when one aluminum atom is oxidized reduce three H+ ions to H0 atoms.
The laboratory sessions in this chapter explore various aspects of redox reactions.
It may surprise you to learn that at least one redox reaction was discovered and used thousands of years ago. Like many discoveries in chemistry, this one was purely accidental. We can speculate about what happened. One evening long ago, some of our remote ancestors gathered around a fire built in a circle of stones. Those stones happened to be chunks of a copper-bearing ore, probably copper carbonate.
All of the required elements were present. The copper ore provided the copper ions. The charred wood provided the carbon in the form of charcoal. The fire provided the heat needed to initiate and sustain the reaction. Here’s what happened:
2 CuCO3(s) + C(s) → 2 Cu(s) + 3 CO2(g)
or, showing the oxidation states:
2 [Cu2+[C4+(O2–3)]2–](s) + C0(s) → 2 Cu0(s) + 3 [C4+(O2–2)](g)
As the fire burned during the night, some of the copper ore and charcoal disappeared and, as if by magic, were replaced by a shiny puddle of metallic copper. Chances are that this had happened many times before and no one thought much about it, if they even noticed. But this time someone did notice and started wondering. What was this shiny new substance? Could it be used for anything? Can we get more of it just by heating rocks?
At the time, metallic copper was known, but the only source was small, rare deposits of natural metallic copper. The discovery that copper metal could be obtained by heating copper ore in conjunction with charcoal, a process called smelting, marked the end of the Stone Age.
In this lab, we’ll recreate that first accidental smelting of copper ore to copper metal.
This experiment uses the hot flame provided by a gas burner. Be careful with the flame, have a fire extinguisher readily available, and use care in handling hot objects (a hot crucible looks exactly like a cold crucible). Wear splash goggles, gloves, and protective clothing.
If you have not already done so, put on your splash goggles, gloves, and protective clothing.
Weigh a clean, dry crucible and lid and record the mass to 0.01 g on line A of Table 10-1.
Weigh about 5.0 g of copper carbonate and record the mass to 0.01 g on line B of Table 10-1.
Weigh about 3.0 g of activated charcoal and record the mass to 0.01 g on line C of Table 10-1.
Mix the copper carbonate and activated charcoal thoroughly, and transfer them to the crucible.
Weigh the crucible and contents and record the mass to 0.01 g on line D of Table 10-1.
Set up your tripod stand or ring stand with the clay triangle, put the covered crucible in place, and place the gas burner to direct the hottest part of its flame at the bottom of the crucible.
Heat the crucible strongly for at least 15 minutes.
Allow the crucible to cool to room temperature. You can check the temperature of the crucible by placing your hand near, but not touching, its surface to check for radiated heat.
Reweigh the crucible and contents and record the mass to 0.01 g on line E of Table 10-1.
Calculate the mass loss (line D minus line E) and enter the value to 0.01 g on line F of Table 10-1.
The waste material from this lab can be ground to powder and flushed down the drain with plenty of water.
Item | Data |
A. Mass of crucible + lid | ______.______ g |
B. Mass of copper carbonate | ______.______ g |
C. Mass of carbon (charcoal) | ______.______ g |
D. Mass of crucible, lid, and reactants (A + B + C) | ______.______ g |
E. Mass of crucible, lid, and products | ______.______ g |
F. Mass loss (D – E) | ______.______ g |
Many elements can exist in several oxidation states, which may differ noticeably in color. In the introduction, we mentioned vanadium as one such element. Manganese is another element whose various oxidation states have different colors, including MnO4– (+7, violet), MnO42– (+6, green), MnO2 (+4, orange), Mn2O3 (+3, violet), and Mn2+(+2, pale pink).
In this laboratory, we’ll begin with a solution of potassium permanganate, in which manganese is in the +7 oxidation state, and reduce the oxidation state to observe the color changes associated with various oxidation states of manganese. To achieve these changes in oxidation state, we’ll react potassium permanganate with sodium bisulfite in neutral, basic (sodium hydroxide), and acid (sulfuric acid) solutions, which are represented by the equations shown in Table 10-2.
Solutions of sodium hydroxide and sulfuric acid are corrosive. Wear splash goggles, gloves, and protective clothing.
Solution | Oxidation state | Ion | Color | Equation |
Neutral | +4 | MnO2 | orange | 2 MnO4–(aq) + 3 HSO3–+ OH–Đ 2 MnO2(s) + 3 SO42–(aq) + 2 H2O(l) |
Basic (sodium hydroxide) | +6 | MnO42– | green | 2 MnO4–(aq) + HSO3–+ 3 OH–Đ 2 MnO42–(aq) + SO42–(aq) + 2 H2O(l) |
Acid (sulfuric acid) | +2 | Mn2+ | pink | 2 MnO4–(aq) + 5 HSO3–+ H+Đ 2 Mn2+(aq) + 5 SO42–(aq) + 3 H2O(l) |
If you have not already done so, put on your splash goggles, gloves, and protective clothing.
Label four test tubes A through D, place them in the test tube rack, and transfer about 10 mL of 0.01 M potassium permanganate solution to each of the tubes.
Test tube A will contain only the potassium permanganate solution, and will serve as the control and example of manganese in oxidation state +7. Record the color of this solution on line A of Table 10-3.
With stirring, slowly add 0.01 M sodium bisulfite solution to test tube B until no further color change occurs. Record the color and the presence or absence of any precipitate on line B of Table 10-3.
Add 8 mL of 1.0 M sodium hydroxide solution to test tube C.
With stirring, slowly add 0.01 M sodium bisulfite solution to test tube C until no further color change occurs. Record the color and the presence or absence of any precipitate on line C of Table 10-3.
Add 6 mL of 1.0 M sulfuric acid solution to test tube D.
With stirring, slowly add 0.01 M sodium bisulfite solution to test tube D until no further color change occurs. Record the color and the presence or absence of any precipitate on line D of Table 10-3.
Comparing the appearances of the contents of the four test tubes, decide which oxidation state of manganese is represented by the contents of each test tube and enter that value on the appropriate line of Table 10-3.
Test tube | Color | Precipitate? | Oxidation state |
A. Potassium permanganate only | |||
B. Potassium permanganate + sodium bisulfite | |||
C. Potassium permanganate + sodium hydroxide + sodium bisulfite | |||
D. Potassium permanganate + sulfuric acid + sodium bisulfite |