How biochar works, and when it doesn't: A review of mechanisms controlling soil and plant responses to biochar

Как действует биоуголь и когда он не работает: обзор механизмов, определяющих реакцию почвы и растений на внесение биоугля
Yakov Kuzyakov, Nanthi Bolan, Yong Sik Ok, Johannes Lehmann, Lukas Van Zwieten, Scott L. Stephens, Yu Luo, Stephen Joseph, Annette Cowie, Kumuduni Niroshika Palansooriya, James A. Ippolito, María Luz Cayuela, Ellen R. Gräber, Zhe Weng, Alice Budai, Wolfram Buss, Jessica G. Shepherd
2021-07-27

biocharpyrolysis conditionsrhizosphere processessoil and plant responsessoil carbon stabilization
Abstract We synthesized 20 years of research to explain the interrelated processes that determine soil and plant responses to biochar. The properties of biochar and its effects within agricultural ecosystems largely depend on feedstock and pyrolysis conditions. We describe three stages of reactions of biochar in soil: dissolution (1–3 weeks); reactive surface development (1–6 months); and aging (beyond 6 months). As biochar ages, it is incorporated into soil aggregates, protecting the biochar carbon and promoting the stabilization of rhizodeposits and microbial products. Biochar carbon persists in soil for hundreds to thousands of years. By increasing pH, porosity, and water availability, biochars can create favorable conditions for root development and microbial functions. Biochars can catalyze biotic and abiotic reactions, particularly in the rhizosphere, that increase nutrient supply and uptake by plants, reduce phytotoxins, stimulate plant development, and increase resilience to disease and environmental stressors. Meta‐analyses found that, on average, biochars increase P availability by a factor of 4.6; decrease plant tissue concentration of heavy metals by 17%–39%; build soil organic carbon through negative priming by 3.8% (range −21% to +20%); and reduce non‐CO 2 greenhouse gas emissions from soil by 12%–50%. Meta‐analyses show average crop yield increases of 10%–42% with biochar addition, with greatest increases in low‐nutrient P‐sorbing acidic soils (common in the tropics), and in sandy soils in drylands due to increase in nutrient retention and water holding capacity. Studies report a wide range of plant responses to biochars due to the diversity of biochars and contexts in which biochars have been applied. Crop yields increase strongly if site‐specific soil constraints and nutrient and water limitations are mitigated by appropriate biochar formulations. Biochars can be tailored to address site constraints through feedstock selection, by modifying pyrolysis conditions, through pre‐ or post‐production treatments, or co‐application with organic or mineral fertilizers. We demonstrate how, when used wisely, biochar mitigates climate change and supports food security and the circular economy.
1
Aging incorporates biochar into soil aggregates, protecting biochar carbon and promoting stabilization of rhizodeposits and microbial products.
2
Average crop yields increased 10%–42%, with the largest gains in low-nutrient, acidic P-sorbing soils and dryland sandy soils when biochar formulations addressed local nutrient and water limitations.
3
Biochar can improve pH, porosity, and water availability, while catalyzing rhizosphere reactions that enhance nutrient uptake, reduce phytotoxins, and increase plant stress resilience.
4
Biochar properties and ecosystem effects depend strongly on feedstock and pyrolysis conditions, producing highly context-dependent soil and plant responses.
5
Biochar undergoes dissolution over 1–3 weeks, reactive surface development over 1–6 months, and aging thereafter, with carbon persisting for hundreds to thousands of years.
6
Meta-analyses reported 4.6-fold higher phosphorus availability, 17%–39% lower plant heavy-metal concentrations, 3.8% greater soil organic carbon from negative priming, and 12%–50% lower non-CO2 soil greenhouse-gas emissions.

biochar in agricultural soils and associated plant–soil systems

the mechanisms and context-dependent effects governing soil and plant responses to biochar, including changes in nutrient availability, carbon stabilization, microbial functions, greenhouse-gas emissions, stress resilience, and crop yield

Publication Details
Publication Date
2021-07-27
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Authors
Yakov Kuzyakov
Nanthi Bolan
Yong Sik Ok
Johannes Lehmann
Lukas Van Zwieten
Scott L. Stephens
Yu Luo
Stephen Joseph
Annette Cowie
Kumuduni Niroshika Palansooriya
James A. Ippolito
María Luz Cayuela
Ellen R. Gräber
Zhe Weng
Alice Budai
Wolfram Buss
Jessica G. Shepherd
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