Acid Rain. RUSSELL R. DICKERSON. Sandstone portal Figure on Herten Castle in Ruhr district of Germany. Sculpted 1702; photographed in 1908. Same sandstone portal figure photographed in 1969. ACID DEPOSITION See Turco, Ch. 9 Finlayson-Pitts & Pitts, Part 6 Seinfeld & Pandis Ch. 20
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RUSSELL R. DICKERSON
See Turco, Ch. 9
Finlayson-Pitts & Pitts, Part 6
Seinfeld & Pandis Ch. 20
The industrial revolution greatly increased the amount of acid in the atmosphere. These acids accelerate the rate of “weathering” of both natural and man-made materials. (Figures of sandstone Madonna). Today we will discuss what acid deposition is, what its effects are, the chemistry and physics of formation and transport, and who is responsible for it.
As early as 1852, R. A. Smith analyzed rain that near the industrial city of Manchester, England and found that urban aerosol particles tend to be composed primarily of sulfuric acid, but as the air is transported away from sources over more rural areas, the acid is neutralized by absorption of ammonia.
urban → suburban → rural
H₂SO₄ + NH₃ → (NH₄)HSO₄ (+NH₃) → (NH₄)₂SO₄
sulfuric acid → ammonium bisulfate → ammonium sulfate
Throughout the early part of the twentieth century, European scientists documented the sources and effects of atmospheric acids. It was not until 1958 that acidity of precipitation in the US was characterized (Junge and Werby, 1958)
Soils (Figure) have colloidal molecules (clay particles) that have a layer of negative charge. They hold positively charged cations such as , Al³⁺, K⁺, Mg²⁺, and Ca²⁺. Some of these cations are essential plant nutrients (K⁺, Mg²⁺, Ca²⁺), while Al³⁺ is toxic. Hydrogen ions from acid deposition replace these cations on the outer layer of colloidal molecules. The metal ions are then dissolved and leached into solution and can be washed away from the soil and into surface or ground water. Soil fertilitiy is reduced and aluminum ions can replace calcium in the fish’s gills. Acidity can also come from oxidation (weathering) of sulfur-rich mine tailings, and from nitrification of ammonium.
Forests can be especially sensitive to nutrient loss. In Europe in 1993 abou ta quarter of the trees have died or are more than 25% defoliated. This “Waldsterben” or “forest death” has been attributed at, least in part, to environmental degradation from a combination of acid deposition, ground-level ozone, and excess nutrification, primarily nitrogen. In the US, loss of forests has been so dramatic, although several species including ash and oak are sensitive to acidification of soils.
The sensitivity surface waters depends critically on their neutralizing or buffering capacity. Alkaline materials such as CaCO₃, and MgCO₃ can neutralize acids.
The surface of the American Midwest is predominantly limestone (CaCO₃), and lakes and streams have high neutralizing capacity. In the East granite dominates; soils and surface waters lacking buffering capacity, are highly sensitive to acidification.
The Ocean is strongly pH buffered, has a high sulfate content naturally, and is relatively insensitive to “acid rain.” Over much of the ocean, however, nitrate is the limiting nutrient for biological activity. Addition of nitrogen from the atmosphere can increase primary productivity, and the consequences reverberate throughout the ecosystem. The Chesapeake Bay is particularly sensitive to excess nutrients. Additional nitrate or ammonium from atmospheric deposition to the Bay or its watershed contributes to the problem of excess eutrophication. Nitrate allows thick beds of aquatic layers of the waters. Loss of higher animals follows.
The Taj Mahal, the friezes on the Parthenon, the Madonna in Herten, Germany, and the Lincoln Memorial are made of marble. Marble, a particular crystalline form of calcite (CaCO₃), and sandstone (grains of sand held together by calcite), are subject to attack by sulfuric acid.
CaSO₄ is gypsum, which is 100 times more soluble than CaCO₃. Many priceless historic structures have been lost to acid deposition.
On a more pragmatic note, the rate of corrosion of galvanized (zinc coated) steel is 0.62 um/yr in the Adirondacks, 1.01 in Washington, DC, and 1.47 in Stubenville, OH.
Covered already in Lectures 1 and 9.
Primarily power generation and ore smelting (pie charts).
For example nickel is mined as nickel sulfide, NiS. In smelting, it is heated in air (Sudbury, Canada).
The molecular weight of nickel is 57 g/mole, so smelting produces more than a ton of SO₂ for each ton of nickel produced.
d) Formation and Composition
Gas Phase production of nitric acid:
OH + NO₂ + M → HNO₃ + M
Aqueous phase production of nitric acid:
NO₂ + O₃ → NO₃ + O₂
NO₃ + NO₂ + M = N₂O₅ + M
N₂O₅ + H₂O(l) → 2HNO₃(aq)
NO₃ + hv → NO₂ + O
Gas Phase production of sulfuric acid:
OH + SO₂ + M → HOSO₂ + M
Aqueous phase production of sulfuric acid:
SO₂ + H₂O₂ → H₂SO₄
Lifetime and Transport
Wet vs dry deposition
SO2: coal-fired power plants
t = 3.9d
t = 1.3d
t = 1.0d
Chin et al. 
1. A dinosaur extinction theory suggests that massive heating of theEarth's atmosphere in the path of a falling asteroid would have led toextremely acid rain, killing the land vegetation and hence thedinosaurs' food supply. What acid would have been involved?
2. Nitrate deposited by acid rain can fertilize the biosphere. Explain why.