Step 1: Organic matter composition dictates decomposition rates. Sugars decompose most rapidly, followed by chitin, with lignin decomposing slowest. Elevated nitrogen content also boosts microbial activity, accelerating decomposition.
Step 2: Soil A contains 40% lignin (slow decomposition), 0% sugar (rapid decomposition), 45% chitin, and 5% nitrogen. The high lignin percentage and low nitrogen content suggest a slower decomposition rate.
Step 3: Soil B comprises 5% lignin, 35% sugar (rapid decomposition), 15% chitin, and 45% nitrogen. The substantial sugar and nitrogen levels indicate a faster decomposition rate.
Step 4: In comparison, Soil A, possessing higher lignin and lower sugar/nitrogen levels, will exhibit a slower decomposition rate than Soil B, which benefits from increased sugar and nitrogen to support enhanced microbial activity.
Consequently, Soil A demonstrates a slower decomposition rate than Soil B.