Correct option is B
Introduction
- Biogeochemical cycles describe the movement of chemical elements through biotic (living) and abiotic (non-living) components of the Earth.
- These cycles are traditionally classified into two types:
- Gaseous cycles: Major reservoir is the atmosphere (e.g., nitrogen, carbon)
- Sedimentary cycles: Major reservoir is Earth's crust (e.g., phosphorus, sulfur)
- However, some cycles exhibit characteristics of both types, making them hybrid cycles.
Information Booster:
- Sulfur Cycle Processes:
- Atmospheric oxidation: H₂S → SO₂ → SO₄²⁻ (acid rain formation)
- Biological reduction: Sulfate-reducing bacteria convert SO₄²⁻ to H₂S
- Weathering: Releases sulfates from rocks into soil and water
- Volcanic activity: Major natural source of atmospheric sulfur
- Environmental Significance:
- Acid rain: SO₂ + H₂O → H₂SO₄
- Climate regulation: DMS affects cloud formation
- Industrial impact: Fossil fuel combustion releases stored sulfur
- Major long-term reservoir is Earth's crust
- Gaseous Phase Components:
- Hydrogen sulfide (H₂S) - released from volcanic activity, decomposition
- Sedimentary Phase Components:
- Sulfate minerals in rocks and soil (gypsum, pyrite)
- Organic sulfur in fossil fuels (coal, petroleum)
- Sulfate ions (SO₄²⁻) in ocean sediment
Additional knowledge:
- Carbon Cycle - Primarily gaseous
- While sedimentary rocks contain carbonates, the active cycling is predominantly atmospheric
- Nitrogen Cycle - Primarily gaseous
- 78% of atmosphere is N₂
- Gaseous exchange through N₂, N₂O, NH₃ is primary
- Phosphorus Cycle - Purely sedimentary
- NO gaseous phase at all (no stable gaseous compounds)
- Reservoir is entirely in rocks, soil, and sediments
