植物生态学报

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杉木不同器官不同碳氮比对土壤激发效应的影响及其机理

黄智军1,甘子莹2,祝嘉新1,丘清燕2,胡亚林2   

  1. 1. 福建农林大学林学院
    2. 福建农林大学
  • 收稿日期:2024-08-12 修回日期:2025-01-23 发布日期:2025-03-12

Impacts and mechanisms of carbon to nitrogen ratios of different organs of Cunninghamia lanceolata on soil priming effect

  • Received:2024-08-12 Revised:2025-01-23

摘要: 凋落物质量是影响土壤激发效应强度与方向的一个重要因素。然而, 当前对于不同器官或者是同一器官不同碳氮比(C:N)凋落物输入是否对土壤激发效应产生差异化影响及其作用机理仍不清楚。为此, 该研究旨在探究杉木(Cunninghamia lanceolata)叶、茎、根的同一器官不同C:N对土壤激发效应的影响及其机理。以13C标记杉木幼苗为研究对象, 通过设置施肥与不施肥处理获取具有低C:N与高C:N的杉木叶、茎、根, 以此研究低C:N和高C:N杉木叶、茎、根输入对土壤激发效应的影响, 并通过测定土壤微生物生物量、酶活性以及土壤有效氮含量等指标阐明其作用机理。结果表明: 杉木叶输入的初始阶段诱导正激发效应, 但是从整个培养期间(180天)来看, 其对原有土壤有机碳(SOC)的矿化影响不明显; 低C:N杉木根的输入使SOC的矿化量降低10.1%, 诱导负激发效应; 而高C:N杉木根以及杉木茎的输入均对SOC的矿化影响不明显。杉木同一器官不同C:N对土壤激发效应的影响不明显, 可能是因为不同C:N杉木凋落物添加对土壤微生物碳量含量及碳代谢相关酶活性的影响不显著。杉木叶输入初期诱导正激发效应与其输入土壤显著降低土壤有效氮含量有关, 当土壤有效氮含量降低时微生物为满足自身对氮的需求, 从而加速对原有SOC的分解。低C:N杉木根添加诱导负激发效应主要在于其输入显著提高了微生物对这些外源添加物的利用, 而外源添加物释放的氮能够满足微生物对氮的需求, 从而减少了对原有SOC的矿化, 因而“底物优先利用”是低C:N杉木根输入诱导土壤负激发效应的主要原因。

关键词: 激发效应, 凋落物质量, 碳氮比, 土壤有机碳矿化, 杉木

Abstract: Abstract Aims Litter quality plays an important role in regulating the magnitude and direction of soil priming effect. However, it remains unclear how the inputs of litter with different carbon to nitrogen ratios (C:N) affect soil priming effect. Methods Cunninghamia lanceolata seedlings were 13C-labeled. To obtain low and high C:N of C. lanceolata leaves, stems, and roots, one half of the C. lanceolata seedlings were fertilized and another half were unfertilized. The priming effect is quantified by the difference in CO2 emissions from native soil organic carbon (SOC) between soil amended with and without litter. Moreover, this research investigated the impacts of the input of low C:N and high C:N C. lanceolata leaves, stems, and roots on the soil priming effect and to clarify the mechanism via measuring soil microbial biomass, enzyme activities, and soil available nitrogen content. Important findings After 180 days of incubation, the input of C. lanceolata leaves induced a positive priming effect at the early stage of incubation. However, over the entire incubation period (180 days), it had no significant effect on SOC mineralization. The input of low C:N of C. lanceolata roots decreased SOC mineralization by 10.1% and induced a negative priming effect. However, the addition of C. lanceolata roots high C:N of as well as the C. lanceolata stems had no significant effect on SOC mineralization. Different C:N (high vs. low) of the same organ of C. lanceolata had no significant effect on soil priming effect. The additions of litter with different C:N did not significantly affect soil microbial biomass carbon and related C metabolic enzyme activities. The structural equation model showed that priming effect was mainly affected by 13C-microbial biomass carbon (MBC), soil available nitrogen, microbial biomass nitrogen (MBN) and β-glucosidase. These factors could explain 30%of the variation of priming effect. Moreover all factors (except for 13C-MBC) were negatively correlated with soil priming effect.

Key words: priming effect, litter quality, carbon to nitrogen ratio, soil organic carbon mineralization, Cunninghamia lanceolata