AMineralisation
BCatabolism
CLeaching
DHumification
Answer:
C. Leaching
Read Explanation:
Leaching is the specific biogeochemical process described, where water-soluble inorganic nutrients are washed away from the soil or detritus by percolating water.
This process occurs primarily due to rainfall or irrigation, which carries dissolved substances downward through the soil profile into deeper layers or groundwater.
Once these nutrients reach the deeper layers, they often precipitate as unavailable salts, making them inaccessible to the root systems of most plants.
Leaching is a critical step in the decomposition process, which includes five major stages: Fragmentation, Leaching, Catabolism, Humification, and Mineralization.
Fragmentation: The breakdown of detritus into smaller particles by detritivores like earthworms.
Catabolism: The degradation of detritus by bacterial and fungal enzymes.
Humification: The formation of dark, amorphous substances known as humus, which is highly resistant to microbial action and acts as a reservoir of nutrients.
Mineralization: The final stage where microbes release inorganic nutrients (such as nitrogen, phosphorus, and potassium) back into the soil, completing the nutrient cycle.
The rate of decomposition is significantly influenced by climatic factors (temperature and moisture) and the chemical composition of the detritus (e.g., lignin and chitin content slows down the process).
