Five Years of Biochar Steers Nitrogen Toward Retention Deep in Alkaline Rice Soils

Nitrogen fertilizer is one of the pillars of modern rice production, yet a large fraction of the nitrogen applied to paddy fields never reaches the crop. Once nitrate enters the soil, an invisible microbial contest begins. Different groups of microorganisms compete for the same nitrate molecules, and the winner of that competition determines whether nitrogen stays locked in the soil as plant-available ammonium or escapes into the atmosphere as gases or leaches toward groundwater. A new study published in the journal Biochar suggests that a simple, widely promoted soil amendment—biochar made from rice straw—can tip this contest in favor of nitrogen conservation, and that the effect grows stronger the deeper one looks below the surface.

The research, led by corresponding author Lili Wang and colleagues including Qiannan Yang, Guilong Zhang, Jie Li, Hu Li, and Lukas Van Zwieten, examined an alkaline paddy field in Tianjin, China, where rice-straw biochar had been applied annually for more than five years. Rather than sampling only the familiar topsoil layer where most agronomic studies stop, the team collected soil from four depths extending from the surface down to 80 centimeters below ground. This vertical perspective proved essential, because the study’s central finding is that biochar’s influence on nitrogen cycling changes dramatically with depth.

Using a nitrogen-15 tracer technique, the researchers simultaneously quantified three major nitrate reduction processes that operate in waterlogged paddy soils. The first is denitrification, in which microbes convert nitrate step by step into nitrogen gases that escape to the atmosphere. The second is anaerobic ammonium oxidation, or anammox, a process in which ammonium and nitrate react to produce dinitrogen gas, again removing reactive nitrogen from the system. The third is dissimilatory nitrate reduction to ammonium, known as DNRA, a fermentation-like pathway that reduces nitrate all the way back to ammonium. From a farmer’s standpoint, these pathways could hardly matter more: DNRA keeps nitrogen in the soil where roots can potentially access it, while denitrification and anammox effectively bleed nitrogen out of the field.

The study revealed a striking depth-dependent pattern in how these three pathways partition the nitrate supply. Across the soil profile, the contribution of DNRA increased from 25.7 percent in the surface layer to as high as 91.1 percent at depth, while the contribution of denitrification fell from 67.9 percent to just 7.2 percent. In other words, the deeper the soil, the more nitrate reduction shifted from a nitrogen-losing process to a nitrogen-retaining one. Biochar amplified this trend. Under the biochar treatment, DNRA became increasingly favored below the surface, and in the deepest layer sampled, 60 to 80 centimeters below ground, biochar increased the DNRA contribution by 37.0 percent while reducing the contribution of denitrification by 27.8 percent.

Corresponding author Lili Wang emphasized that this depth sensitivity is the study’s key message. As she put it, the effect of biochar on nitrogen cycling cannot be understood by looking only at the surface soil. As soil depth increased, biochar shifted nitrate reduction toward the pathway that retains nitrogen as ammonium, while suppressing the pathways associated with nitrogen loss. For years, biochar research has concentrated overwhelmingly on the top 20 or 30 centimeters of soil, where most sampling protocols end. The new results suggest that this focus may have missed some of the most consequential chemistry happening far below the plow layer.

Why would biochar favor one microbial pathway over another, and why would that preference change with depth? To answer this, the researchers examined the environmental conditions and microbial communities at each depth. Statistical modeling identified several important controls on the pathway balance: soil pH, the ratio of soil organic carbon to nitrate, dissolved organic carbon, and ferrous iron. These factors are known to shape the competitive hierarchy among nitrate-reducing microbes. Organisms capable of DNRA tend to thrive when carbon is abundant relative to nitrate, while denitrifiers often dominate under different carbon and oxygen regimes. Iron chemistry adds another layer of complexity, because ferrous iron can participate in chemically coupling nitrate reduction to iron oxidation in flooded soils.

Biochar altered these environmental conditions differently at different depths, and those alterations cascaded through the nitrogen-transforming microbial communities and the functional genes they carry. In the surface soil, biochar stimulated several nitrate reduction processes at once, apparently by improving carbon availability and modifying pH in the zone where the amendment was concentrated. Deeper in the profile, however, the picture changed. The soil became more alkaline and carbon availability declined with depth. These conditions increasingly suppressed denitrification and anammox while allowing DNRA to account for a larger and larger share of nitrate transformation. The result is a vertical gradient in nitrogen fate that no surface-only study could have detected.

The practical implications extend well beyond the paddy fields of Tianjin. Nitrogen transformations below the plow layer can determine whether nitrate remains in the soil, moves downward toward groundwater, or is converted into gaseous products that contribute to greenhouse gas emissions and the loss of fertilizer value. In alkaline rice-growing regions, where high pH already shapes microbial activity in distinctive ways, the finding that long-term biochar application may help conserve nitrogen in deeper horizons offers a potential strategy for improving nitrogen use efficiency. More ammonium retained in the profile means less fertilizer needed, fewer nitrate pulses into aquifers, and potentially reduced emissions of nitrous oxide, a potent greenhouse gas produced during denitrification.

The authors are careful to note that biochar’s effects are not universal. They caution that the outcomes depend strongly on soil depth, initial soil pH, the aging of the biochar over successive seasons, and changes in available carbon. Biochar is not chemically static; over years in a flooded field it weathers, its labile carbon fraction diminishes, and its surface chemistry evolves. The Tianjin experiment captured the consequences of more than five years of annual application, but the researchers stress that future studies should compare fresh and naturally aged biochar directly, and should measure nitrogen leaching and gaseous nitrogen losses explicitly rather than inferring them from pathway partitioning alone. Such measurements would close the loop between microbial process rates and actual field-scale nitrogen balances.

What the study delivers now is mechanistic evidence for a principle that soil scientists have increasingly advocated: biochar-based nitrogen management should consider the entire soil profile rather than focusing only on topsoil. The nitrogen-15 tracer approach allowed the team to watch three competing pathways respond in real time to five years of amendment, and the answer that emerged is unusually clear. In deep alkaline paddy soil, biochar nudged the microbial economy toward conservation—toward ammonium that stays put rather than gases that drift away. For a crop grown on roughly 160 million hectares worldwide, much of it in alkaline or calcareous soils, that shift could translate into meaningful gains in fertilizer efficiency and meaningful reductions in nitrogen pollution. The deeper soil, long treated as a black box beneath the sampling auger, turns out to be where some of biochar’s most valuable work is done.

Subject of Research: Long-term biochar effects on nitrate reduction pathways and nitrogen retention in deep alkaline paddy soils

Article Title: Long-term biochar use may help conserve nitrogen deep in alkaline paddy soils

Article References: Long-term biochar use may help conserve nitrogen deep in alkaline paddy soils. (n.d.). Original publication

Image Credits: AI Generated

DOI: Not provided

Keywords: biochar, nitrogen cycling, paddy soil, DNRA, denitrification, anammox, nitrogen-15 tracer, alkaline soil, soil depth, nitrogen retention, rice straw, soil microbiology