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  2. Soil acidification - Wikipedia

    en.wikipedia.org/wiki/Soil_acidification

    This compound causes rainfall pH to be around 5.0–5.5. When rainfall has a lower pH than natural levels, it can cause rapid acidification of soil. Sulfur dioxide and nitrogen oxides are precursors of stronger acids that can lead to acid rain production when they react with water in the atmosphere

  3. Acid rain - Wikipedia

    en.wikipedia.org/wiki/Acid_rain

    The amount of sulfur dioxide that can be emitted into the atmosphere is capped by the EPA. This reduces the quantity of sulfur dioxide in the air that turns into sulfur trioxide and sulfuric acid. [14] Sulfuric acid concentrations in workroom air are restricted by OSHA to 1 mg/m 3. Moreover, NIOSH advises a time-weighted average limit of 1 mg/m ...

  4. Soil pH - Wikipedia

    en.wikipedia.org/wiki/Soil_pH

    The prevailing view in the 1940s and 1950s was that P availability was maximized near neutrality (soil pH 6.5–7.5), and decreased at higher and lower pH. [ 29 ] [ 30 ] Interactions of phosphorus with pH in the moderately to slightly acidic range (pH 5.5–6.5) are, however, far more complex than is suggested by this view.

  5. Acid Rain Program - Wikipedia

    en.wikipedia.org/wiki/Acid_Rain_Program

    Title IV of the Clean Air Act Amendments of 1990 established the allowance market system known today as the Acid Rain Program. Initially targeting only sulfur dioxide, Title IV set a decreasing cap on total SO 2 emissions for each of the following several years, aiming to reduce overall emissions to 50% of 1980 levels.

  6. Freshwater acidification - Wikipedia

    en.wikipedia.org/wiki/Freshwater_acidification

    Volcanic activity can release sulfur dioxide (SO₂) and other acidic oxides into the atmosphere. [8] In air, sulfur dioxide converts to sulfuric acid: [9] This sulfuric acid dissociates into sulfate ions (SO₄²⁻) and hydrogen ions (H⁺), increasing the acidic condition. SO 2 + ½ O 2 + H 2 O → H 2 SO 4; H 2 SO 4 → 2H⁺ + SO 4 2 ⁻

  7. Soil management - Wikipedia

    en.wikipedia.org/wiki/Soil_management

    [5] the usage of artificial fertilizer in the agricultural field it leads to nutrition imbalance in the soil. Soils can sequester carbon dioxide (CO 2) from the atmosphere, primarily by storing carbon as soil organic carbon (SOC) through the process of photosynthesis. CO 2 can also be stored as inorganic carbon but this is less common ...

  8. Bjerrum plot - Wikipedia

    en.wikipedia.org/wiki/Bjerrum_plot

    Example Bjerrum plot: Change in carbonate system of seawater from ocean acidification.. A Bjerrum plot (named after Niels Bjerrum), sometimes also known as a Sillén diagram (after Lars Gunnar Sillén), or a Hägg diagram (after Gunnar Hägg) [1] is a graph of the concentrations of the different species of a polyprotic acid in a solution, as a function of pH, [2] when the solution is at ...

  9. Soil fertility - Wikipedia

    en.wikipedia.org/wiki/Soil_fertility

    While typically limited by nitrogen, phosphorus and potassium, low levels of carbon dioxide can also act as a limiting factor on plant growth. Peer-reviewed and published scientific studies have shown that increasing CO 2 is highly effective at promoting plant growth up to levels over 300 ppm.