Summary

Agronomy encompasses the science and practice of crop production and soil management, integrating biological, chemical and physical principles to sustain and enhance agricultural productivity. It addresses the interactions between plants, soils, climate and management practices to optimise yields, maintain soil health and support ecosystem services. Core disciplines include soil fertility and nutrient cycling, water management through irrigation and conservation tillage, crop physiology under abiotic and biotic stresses, and mechanisation and precision technologies for seeding, fertilisation and pest control. Agronomists develop and evaluate practices that preserve soil structure and organic matter, regulate pH and nutrient availability, mitigate erosion and greenhouse-gas emissions, and adapt cropping systems to climate variability and resource constraints. The ultimate aim is to produce sufficient food, fibre and bioenergy while maintaining the natural resource base and reducing environmental impacts.

Research from Nature Portfolio

In a 30-year field study on a temperate Mollisol, perennial grassland and rotationally grazed pasture systems maintained or enhanced full-profile soil organic carbon stocks, whereas continuous row-crop and alfalfa systems lost carbon at rates up to 0.8 Mg C ha⁻¹ yr⁻¹. Density-corrected, deep-sampling methods revealed that traditional surface-only assessments can overestimate carbon gains under annual cropping. Another study quantified greenhouse-gas emissions from maize grown on drained peat soils for biomethane production, finding soil CO₂ fluxes up to three times greater than those from natural gas combustion. These findings highlight the necessity of including soil-borne emissions and whole-profile carbon changes in assessments of cropping system sustainability and bioenergy life cycles.

Agronomy publication trend

The graph below shows the total number of articles in agronomy across all publications each year (not limited to Nature Index journals).

Technical terms

Soil pH: A measure of hydrogen-ion activity in soil, indicating its acidity or alkalinity on a scale of 0 (strongly acidic) to 14 (strongly alkaline).

Cation exchange capacity (CEC): The total capacity of soil to hold and exchange positively charged ions (cations), reflecting its nutrient-retention and buffering abilities.

Buffering capacity: The ability of soil to resist changes in pH when acids or bases are added, determined by organic matter, clay minerals and carbonate content.

Exchangeable aluminium: Aluminium ions adsorbed on soil particle surfaces that become soluble under low pH and are toxic to plant roots.

Nitrification: Microbial oxidation of ammonium (NH₄⁺) to nitrate (NO₃⁻), releasing protons (H⁺) that contribute to soil acidification.

References

  1. Soil carbon maintained by perennial grasslands over 30 years but lost in field crop systems in a temperate Mollisol. Communications Earth & Environment (2024).
  2. Impact of long-term fertilization in no-till on the stratification of soil acidity and related parameters. Soil and Tillage Research (2023).
  3. Soil Nutrient Retention and pH Buffering Capacity Are Enhanced by Calciprill and Sodium Silicate. Agronomy (2022).

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