How biochar works, and when it doesn't: A review of mechanisms controlling soil and plant responses to biochar
Stephen Joseph,
Annette L. Cowie,
Lukas Van Zwieten,
Nanthi Bolan,
Alice Budai,
Wolfram Buss,
Maria Luz Cayuela,
Ellen R. Graber,
James A. Ippolito,
Yakov Kuzyakov,
Yu Luo,
Yong Sik Ok,
Kumuduni N. Palansooriya,
Jessica Shepherd,
Scott Stephens,
Zhe (Han) Weng,
Johannes Lehmann
Affiliations
Stephen Joseph
School of Materials Science and Engineering University of NSW Kensington New South Wales Australia
Annette L. Cowie
School of Environmental and Rural Science University of New England Armidale New South Wales Australia
Lukas Van Zwieten
New South Wales Department of Primary Industries Wollongbar New South Wales Australia
Nanthi Bolan
Cooperative Research Centre for High Performance Soil (Soil CRC) Callaghan New South Wales Australia
Alice Budai
Norwegian Institute of Bioeconomy Research Division of Environmental and Natural Resources Ås Norway
Wolfram Buss
Research School of Biology Australian National University Canberra Australian Capital Territory Australia
Maria Luz Cayuela
Department of Soil and Water Conservation and Waste Management CEBAS‐CSIC Murcia Spain
Ellen R. Graber
Institute of Soil, Water and Environmental Sciences The Volcani CenterAgricultural Research Organization Rishon LeTzion Israel
James A. Ippolito
Department of Soil and Crop Sciences Colorado State University Fort Collins Colorado USA
Yakov Kuzyakov
Department of Soil Science of Temperate Ecosystems Dept. of Agricultural Soil Science University of Göttingen Göttingen Germany
Yu Luo
Institute of Soil and Water Resources and Environmental Science Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment Zhejiang University Hangzhou China
Yong Sik Ok
Korea Biochar Research Center APRU Sustainable Waste Management Program & Division of Environmental Science and Ecological EngineeringKorea University Seoul South Korea
Kumuduni N. Palansooriya
Korea Biochar Research Center APRU Sustainable Waste Management Program & Division of Environmental Science and Ecological EngineeringKorea University Seoul South Korea
Jessica Shepherd
University of Edinburgh School of Geosciences Edinburgh UK
Scott Stephens
New South Wales Department of Primary Industries Parramatta New South Wales Australia
Zhe (Han) Weng
School of Agriculture and Food Sciences The University of Queensland St. Lucia Queensland Australia
Johannes Lehmann
Soil and Crop Sciences School of Integrative Plant Science Cornell University Ithaca New York USA
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‐CO2 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.