生物炭调理酸化土壤的作用机制

Mechanism of biochar conditioning acidified soil

  • 摘要: 生物炭(biochar)是有机物质在无氧或缺氧条件下热解炭化而成的一种固态、稳定、高度芳香化的富炭材料,具有碳量高、化学性质稳定、比表面积大及孔隙结构丰富等特点,且生物炭中的含氧官能团、有机阴离子和无机碱等成分能够有效的调理酸化土壤,因而常用作土壤改良剂。本文简述了土壤酸化的原因及其相关影响,介绍了生物炭的种类、特征和组成部分,重点关注了近年来生物炭施用对提高土壤pH、缓解铝毒、增强土壤微生物活性及改变化肥使用量方面的影响,并探讨了其作用机制。最后对生物炭在酸化土壤调理应用中尚存在的问题进行了展望,以期为生物炭在调理酸化土壤的理论研究和实际应用方面提供参考。

     

    Abstract: Biochar is a solid, stable and highly aromatic carbon-rich substance produced by pyrolysis of organic substances under anaerobic or anoxic conditions, which exhibits high carbon content, stable chemical properties, large specific surface area and abundant pore structure. Due to its abundant oxygen-containing functional groups, organic anions and inorganic alkali, biochar is commonly used as a soil amendment. This paper briefly described the causes of soil acidification and its related effects, and introduced the types, characteristics and components of biochar. The effects of biochar application in acidizing soil conditioning in recent years were highlighted particularly in increasing soil pH, alleviating Al toxicity, enhancing soil microbial activity and changing the amount of chemical fertilizer. The mechanism involved was discussed. The unsolved problems of biochar in acidifying soil conditioning was finally prospected so as to provide reference for the theory and practice of biochar application in acidified soil.

     

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