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生物炭对土壤有机碳矿化的激发效应及其机理研究进展
引用本文:陈颖,刘玉学,陈重军,吕豪豪,汪玉瑛,何莉莉,杨生茂.生物炭对土壤有机碳矿化的激发效应及其机理研究进展[J].应用生态学报,2018,29(1):314-320.
作者姓名:陈颖  刘玉学  陈重军  吕豪豪  汪玉瑛  何莉莉  杨生茂
作者单位:1.浙江师范大学化学与生命科学学院, 浙江金华 321004;2.浙江省农业科学院环境资源与土壤肥料研究所, 杭州 310021;3.浙江省生物炭工程技术研究中心, 杭州 310021;4.苏州科技大学环境科学与工程学院, 江苏苏州 215009
基金项目:本文由国家自然科学基金项目(41701334)、浙江省自然科学基金项目(LY14D010005,LY16D010004)、浙江省重点研发计划项目(2015C03020)、国家公益性行业(农业)科研专项(201303095)和苏州市科技计划项目(SYN201411)资助
摘    要:近年来由于生物炭具有碳素稳定性强和孔隙结构发达等特性,其在土壤固碳减排方面的作用研究受到广泛关注.然而当生物炭进入土壤环境后最终是增加土壤碳的储存还是促进土壤碳的排放?目前学术界对该问题仍存在争议.生物炭对土壤有机碳的激发效应及其机理研究有待进一步深入开展.本文在分析生物炭自身碳素组分和稳定性、孔隙结构及表面形态特征的基础上,综述了添加生物炭对土壤本底有机碳矿化产生激发效应的研究进展,分别阐述了产生正激发和负激发效应(即促进和抑制矿化)的机制机理,认为正激发效应主要是基于生物炭促进土壤微生物活性增强、生物炭中易分解组分的优先矿化以及由此引发的土壤微生物的共代谢作用,而负激发效应主要是基于生物炭内部孔隙结构和外表面对土壤有机质的包封作用和吸附保护作用、生物炭促进土壤有机-无机复合体形成的稳定化作用、生物炭对土壤微生物及其酶活性的抑制作用.最后对今后相关研究方向进行了展望,以期为生物炭在土壤固碳减排方面的应用提供理论依据.

关 键 词:生物炭  土壤有机碳  激发效应  矿化作用  固碳
收稿时间:2017-02-22

Priming effect of biochar on the minerialization of native soil organic carbon and the mechanisms: A review.
CHEN Ying,LIU Yu-xue,CHEN Chong-jun,LYU Hao-hao,WANG Yu-ying,HE Li-li,YANG Sheng-mao.Priming effect of biochar on the minerialization of native soil organic carbon and the mechanisms: A review.[J].Chinese Journal of Applied Ecology,2018,29(1):314-320.
Authors:CHEN Ying  LIU Yu-xue  CHEN Chong-jun  LYU Hao-hao  WANG Yu-ying  HE Li-li  YANG Sheng-mao
Institution:;1.College of Chemistry and Life Sciences, Zhejiang Normal University, Jinhua 321004, Zhejiang, China;2.Institute of Environment, Resource, Soil and Fertilizer, Zhejiang Academy of Agricultural Sciences, Hangzhou 310021, China;3.Engineering Research Center of Biochar of Zhejiang Province, Hangzhou 310021, China;4.School of Environmental Science and Engineering, Suzhou University of Science and Technology, Suzhou 215009, Jiangsu, China
Abstract:In recent years, studies on carbon sequestration of biochar in soil has been in spotlight owing to the specific characteristics of biochar such as strong carbon stability and well developed pore structure. However, whether biochar will ultimately increase soil carbon storage or promote soil carbon emissions when applied into the soil? This question remains controversial in current academic circles. Further research is required on priming effect of biochar on mineralization of native soil organic carbon and its mechanisms. Based on the analysis of biochar characteristics, such as its carbon composition and stability, pore structure and surface morphology, research progress on the priming effect of biochar on the decomposition of native soil organic carbon was reviewed in this paper. Furthermore, possible mechanisms of both positive and negative priming effect, that is promoting and suppressing the mineralization, were put forward. Positive priming effect is mainly due to the promotion of soil microbial activity caused by biochar, the preferential mineralization of easily decomposed components in biochar, and the co-metabolism of soil microbes. While negative priming effect is mainly based on the encapsulation and adsorption protection of soil organic matter due to the internal pore structure and the external surface of biochar. Other potential reasons for negative priming effect can be the stabilization resulted from the formation of organic-inorganic complex promoted by biochar in the soil, and the inhibition of activity of soil microbes and its enzymes by biochar. Finally, future research directions were proposed in order to provide theoretical basis for the application of biochar in soil carbon sequestration.
Keywords:biochar  soil organic carbon  priming effect  mineralization  carbon sequestration
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