Nitrogen input alleviates the priming effects of biochar addition on soil organic carbon decomposition

IF 9.8 1区 农林科学 Q1 SOIL SCIENCE Soil Biology & Biochemistry Pub Date : 2024-12-09 DOI:10.1016/j.soilbio.2024.109689
Xuhui Zhou , Zhiqiang Feng , Yixian Yao , Ruiqiang Liu , Junjiong Shao , Shuxian Jia , Yining Gao , Kui Xue , Hongyang Chen , Yuling Fu , Yanghui He
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Abstract

The combination of biochar and nitrogen (N) addition has been proposed as a potential strategy to sustain crop productivity and mitigate climate change by increasing soil fertility, sequestering carbon (C), and reducing soil greenhouse gas emissions. However, our current knowledge about how biochar and N additions interactively alter mineralization of native soil organic C (SOC), which is referred to priming effects (PEs), is largely limited. To address this uncertainty, C3 biochar (pyrolyzing rice straw at 300, 550, and 800 °C) and its combination with N fertilizer (urea) were incubated in a C4-derived soils at 25 °C. All these 3 types of biochar with different addition rates caused positive priming of native soil organic matter decomposition (up to +58.4%). The maximum negative priming effects (up to −25.4%) occurred in soil treated with 1% of N-bound biochar pyrolyzed at 300 °C. In addition, a negative correlation was found between the priming intensity and soil inorganic N content across all treatments. The decrease in biochar-induced PEs was related with a shift in microbial community composition and reduction in microbial biomass determined by chloroform-fumigation. Such a reduction, however, was not confirmed by PLFA analysis. These findings advance our understanding on the microbial mechanisms mediating net soil C balance with the adequate biochar use for blending traditional mineral fertilizers.
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氮输入缓解了生物炭添加对土壤有机碳分解的启动效应
生物炭和氮(N)添加的组合被认为是一种潜在的策略,可以通过提高土壤肥力、固碳(C)和减少土壤温室气体排放来维持作物生产力和减缓气候变化。然而,我们目前关于生物炭和N添加如何相互作用改变原生土壤有机碳(SOC)矿化的知识,被称为启动效应(PEs),在很大程度上是有限的。为了解决这一不确定性,C3生物炭(在300、550和800°C下热解稻草)及其与氮肥(尿素)的组合在25°C的c4衍生土壤中孵育。3种添加量不同的生物炭对土壤有机质分解均有正向促进作用(+58.4%)。在300°C下,用1%的n结合生物炭处理土壤,最大的负启动效应为- 25.4%。各处理土壤无机氮含量与灌浆强度呈显著负相关。生物炭诱导PEs的减少与微生物群落组成的变化和氯仿熏蒸测定的微生物生物量的减少有关。然而,PLFA分析并未证实这种减少。这些发现促进了我们对微生物机制调节土壤净碳平衡的理解,并充分利用生物炭与传统矿物肥料混合。
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来源期刊
Soil Biology & Biochemistry
Soil Biology & Biochemistry 农林科学-土壤科学
CiteScore
16.90
自引率
9.30%
发文量
312
审稿时长
49 days
期刊介绍: Soil Biology & Biochemistry publishes original research articles of international significance focusing on biological processes in soil and their applications to soil and environmental quality. Major topics include the ecology and biochemical processes of soil organisms, their effects on the environment, and interactions with plants. The journal also welcomes state-of-the-art reviews and discussions on contemporary research in soil biology and biochemistry.
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