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应用生态学报 ›› 2026, Vol. 37 ›› Issue (8): 2537-2546.doi: 10.13287/j.1001-9332.202608.006

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长期氮沉降对亚热带天然林土壤微生物呼吸及代谢熵的影响

胡晓蝶1,2, 王小红1,2*, 高红1,2, 张伟1,2, 黄冰彬1,2, 姚晓东1,2, 陈光水1,2   

  1. 1福建师范大学地理科学学院/湿润亚热带山地生态国家重点实验室培育基地, 福州 350007;
    2福建三明森林生态系统国家野外科学观测研究站, 福建三明 365002
  • 收稿日期:2026-04-03 修回日期:2026-06-07 出版日期:2026-08-18 发布日期:2027-02-18
  • 通讯作者: *E-mail: wangxh@fjnu.edu.cn
  • 作者简介:胡晓蝶, 女, 2001年生, 硕士研究生。主要从事森林生态系统碳氮循环研究。E-mail: 1104203675@qq.com
  • 基金资助:
    国家重点研发计划项目(2021YFD2200403)和国家自然科学青年基金项目(32301560)

Effects of long-term nitrogen deposition on soil microbial respiration and metabolic quotient in subtropical natural forests

HU Xiaodie1,2, WANG Xiaohong1,2*, GAO Hong1,2, ZHANG Wei1,2, HUANG Bingbin1,2, YAO Xiaodong1,2, CHEN Guangshui1,2   

  1. 1School of Geographical Sciences, Fujian Normal University/Breed Base of State Key Laboratory of Humid Subtropical Mountain Ecology, Fuzhou 350007, China;
    2Fujian Sanming Forest Ecosystem National Observation and Research Station, Sanming 365002, Fujian, China
  • Received:2026-04-03 Revised:2026-06-07 Online:2026-08-18 Published:2027-02-18

摘要: 本研究依托福建三明森林生态系统国家野外科学观测研究站连续施氮9年的亚热带常绿阔叶林模拟氮沉降实验平台,设置对照(0 kg N·hm-2·a-1)、低氮(40 kg N·hm-2·a-1)和高氮(80 kg N·hm-2·a-1)3个处理,分析表层(0~10 cm)土壤的理化性质、微生物生物量及土壤胞外酶碳(C)、氮(N)、磷(P)化学计量特征,并通过室内培养试验测定了土壤微生物呼吸,以探究长期氮沉降对亚热带森林土壤微生物呼吸及代谢熵(qCO2)的影响。结果表明:与对照相比,高氮处理使土壤C/N显著降低18.8%,土壤N/P显著提高52.9%,低氮和高氮处理分别使可溶性有机C/N显著降低31.8%和34.6%,使微生物N/P失衡提高了72.8%和29.8%。低氮处理的微生物呼吸显著高于高氮处理,二者均与对照无显著差异;低氮和高氮处理的qCO2分别较对照显著提高36.8%和21.1%,且低氮处理显著高于高氮处理。逐步回归分析表明,土壤C/N和微生物N/P失衡分别是微生物呼吸和qCO2变异的主要影响因子,解释度分别为56.2%和58.4%。综上,长期氮沉降对亚热带森林土壤微生物呼吸及代谢熵的影响呈剂量依赖性,即高氮沉降通过降低土壤C/N抑制微生物呼吸,而低氮沉降通过加剧微生物N/P失衡提高微生物代谢熵。

关键词: 代谢熵, 氮沉降, 化学计量特征, 酶活性, 微生物群落结构, 异养呼吸

Abstract: Based on a 9-year nitrogen (N) addition experiment in a subtropical evergreen broad-leaved forest at the Fujian Sanming Forest Ecosystem National Field Observation and Research Station, we examined the effects of long-term N addition on soil microbial respiration and metabolic quotient (qCO2). We collected surface soils (0-10 cm) from control (CK, 0 kg N·hm-2·a-1), low nitrogen (LN, 40 kg N·hm-2·a-1), and high nitrogen (HN, 80 kg N·hm-2·a-1) treatments, analyzed soil physicochemical properties, microbial biomass, and the stoichiometric characteristics of extracellular enzymes related to carbon (C), N, and phosphorus (P), and measured the soil microbial respiration through laboratory incubation experiments. The results showed that the HN treatment significantly decreased the soil C/N by 18.8% and increased the soil N/P by 52.9%. The LN and HN treatments significantly decreased the dissolved organic C/N by 31.8% and 34.6%, and increased the microbial N/P by 72.8% and 29.8%, respectively. Microbial respiration in the LN treatment was significantly higher than that in the HN treatment, with no differences observed between either treatment and CK. The qCO2 in the LN and HN treatments was significantly increased by 36.8% and 21.1%, respectively, and the qCO2 in the LN treatment was significantly higher than that in the HN treatment. Stepwise regression analysis indicated that soil C/N and microbial N/P were the primary factors influencing the microbial respiration and qCO2, accounting for 56.2% and 58.4% of the variance, respectively. In conclusion, the effects of long-term N deposition on soil microbial respiration and metabolic quotient in subtropical forests were dose-dependent. High N deposition suppressed microbial respiration by reducing soil C/N, whereas low N deposition increased microbial metabolic quotient by exacerbating microbial N/P imbalance.

Key words: metabolic quotient, nitrogen deposition, stoichiometric characteristics, enzyme activity, microbial community structure, heterotrophic respiration