Summary
This chapter synthesises the rationale for using soil nitrogen mineralization potential as an index of nitrogen availability to plants in terrestrial ecosystems. The authors argue that mineralization potentials—measuring the net production of inorganic nitrogen under standardised conditions—are superior to static measurements of soil inorganic nitrogen concentrations because nutrient supply rates are more ecologically meaningful than instantaneous pool sizes. The review contextualises mineralization assays within broader soil nitrogen dynamics, noting that standard methods typically exclude plant uptake, leaching, immobilisation, and denitrification to isolate the soil's capacity to generate available nitrogen.
Regional applicability
This is a methodological and conceptual contribution grounded in North American soil science, but the principles of nitrogen mineralization as a fertility indicator are widely applicable. The approach has been adopted internationally and remains relevant to UK soil assessment and fertility management practices, though specific mineralization rates will vary by soil type, climate, and management history.
Key measures
Nitrogen mineralization potential (net inorganic nitrogen production under standard conditions), inorganic soil nitrogen concentrations, labile soil organic matter pool size, nitrification rates, soil respiration potentials
Outcomes reported
The paper evaluates nitrogen mineralization potential—the net production of inorganic nitrogen under standard conditions—as a superior indicator of soil nitrogen fertility compared to instantaneous inorganic nitrogen pool size. It examines how mineralization potentials reflect both the labile soil organic matter pool and microbial oxidation activity.
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