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

生物炭 土壤水分 木炭 固碳 环境科学 农学 营养物 斜线和字符 土壤碳 根际 土壤肥力 化学 环境化学 热解 生物 土壤科学 二氧化碳 有机化学 遗传学 细菌
作者
Stephen Joseph,Annette Cowie,Lukas Van Zwieten,Nanthi Bolan,Alice Budai,Wolfram Buss,María Luz Cayuela,Ellen R. Gräber,James A. Ippolito,Yakov Kuzyakov,Yu Luo,Yong Sik Ok,Kumuduni Niroshika Palansooriya,Jessica G. Shepherd,Scott L. Stephens,Zhe Weng,Johannes Lehmann
出处
期刊:Gcb Bioenergy [Wiley]
卷期号:13 (11): 1731-1764 被引量:810
标识
DOI:10.1111/gcbb.12885
摘要

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.
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