Imagine two wheat fields: one rooted in dark brown, rich soils teeming with life and another in gray, compacted ground depleted by decades of intensive tillage and fertilizer use. Both may produce grain, but the health of the soil beneath them tells very different stories about the past – and the future – of our food systems.
Wheat research field (left) and contrasting tillage practices (right) at the CSU Agricultural Experimental station.
These soil differences matter more than ever. Making crop production more resource efficient and environmentally sustainable hinges on transformative advances in precision agriculture and a deeper understanding of the biogeochemical processes that support soil health. Central to this effort is the management of carbon – the currency of energy in nature that cycles between the atmosphere, the soil, and all living organisms. We now face a soil carbon (C) dilemma in agriculture. On one hand, we aim to sequester atmospheric C and stabilize it as soil organic matter (SOM) below-ground to reduce greenhouse gas emissions; on the other, we rely on the breakdown of this same SOM to sustain crop growth. Tackling this dilemma requires a quantitative understanding of soil C dynamics and reliable tools to track them, enabling the development towards a climate-smart food system that nourishes and protects the planet.
As a FFAR Fellow at Colorado State University (CSU), my area of research focuses on soil health and investigating the driving factors of SOM dynamics below ground. Much like a banking system, SOM exists in both fast-cycling “checking” accounts – composed of partially decomposed plant and animal residues – and long-term “savings” accounts, where organic matter binds to minerals and persists over extended timescales. In this analogy, soil microbes act as the bank tellers, processing organic inputs through their enzymatic activity to convert nutrients into plant-available forms and driving the transformation of SOM. Despite decades of research, our understanding of how soil microbes influence SOM cycling remain limited. Gaining deeper mechanistic insight into how microbial activity and soil minerals interact to process organic C input will unlock new strategies to enhance SOM formation, and strengthen the quantitative models used to monitor and predict soil C dynamics – knowledge vital for sustainable and precision agriculture.