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林业科学 ›› 2021, Vol. 57 ›› Issue (7): 20-31.doi: 10.11707/j.1001-7488.20210703

• 论文与研究报告 • 上一篇    下一篇

湿地松人工林土壤呼吸及其组分对模拟酸雨的响应

房焕英1,2,肖胜生2,3,余小芳4,熊永5,欧阳勋志1,*,秦晓蕾2   

  1. 1. 江西农业大学林学院 南昌 330045
    2. 江西省水土保持科学研究院 南昌 330029
    3. 江西省土壤侵蚀与防治重点实验室 南昌 330029
    4. 江西师范大学 南昌 330022
    5. 江西省水利规划设计研究院 南昌 330029
  • 收稿日期:2020-04-10 出版日期:2021-07-25 发布日期:2021-09-02
  • 通讯作者: 欧阳勋志
  • 基金资助:
    国家自然科学基金项目(41303064);国家自然科学基金项目(41761063);江西省水利科技重大研究项目(KT201716)

Responses of Soil Respiration and Its Components to Simulated Acid Rain in Pinus elliottii Plantation

Huanying Fang1,2,Shengsheng Xiao2,3,Xiaofang Yu4,Yong Xiong5,Xunzhi Ouyang1,*,Xiaolei Qin2   

  1. 1. College of Forestry, Jiangxi Agricultural University Nanchang 330045
    2. Jiangxi Institute of Soil and Water Conservation Nanchang 330029
    3. Jiangxi Provincial Key Laboratory of Soil Erosion and Prevention Nanchang 330029
    4. Jiangxi Normal University Nanchang 330022
    5. Jiangxi Provincial Water Conservancy Planning Design and Research Institute Nanchang 330029
  • Received:2020-04-10 Online:2021-07-25 Published:2021-09-02
  • Contact: Xunzhi Ouyang

摘要:

目的: 分析不同强度酸雨对湿地松人工林土壤总呼吸速率(Rs)及其组分(微生物异养呼吸速率Rh和根系自养呼吸速率Ra)的影响规律,进一步了解森林土壤呼吸过程,为酸沉降胁迫下的森林管理提供科学依据。方法: 以亚热带湿地松人工林为对象,采用壕沟法分离土壤呼吸组分,设置3种酸沉降水平(CK:pH 6.5、低酸LA:pH 4.5,强酸HA:pH 2.5),参照研究区降雨比例分次喷洒,运用LI-8100A土壤碳通量自动测量系统原位测定土壤呼吸速率,同时测定土壤温湿度和土壤生化性质等指标。结果: 不同酸处理下,RsRaRh均呈夏季高、冬季低的单峰模式,土壤温度是导致土壤呼吸季节变化的主要驱动因素;酸雨可显著降低RsP<0.05),LA和HA处理后分别降低25.83%和30.95%,其中,Rh分别降低29.60%和35.20%,Ra分别降低19.15%和23.40%,但这种抑制效应仅体现在生长季,非生长季LA可显著促进RaP<0.05);CK样地RhRs中占比63.94%,LA和HA处理后该比例显著降低(P<0.05),同时Ra响应强度随酸雨增强而增加;RsRhRa与土壤温度均呈极显著指数关系(P<0.01),酸处理后其温度敏感系数(Q10)均降低;土壤湿度与RsRhRa在HA处理下极显著相关(P<0.01),土壤温湿度的协同作用极显著影响土壤呼吸速率(P<0.01);Rh变异主要与土壤脲酶、蔗糖酶、表层土壤总有机碳(TOC)含量和土壤pH有关,而Ra变异则主要与土壤脲酶、土壤温度和TOC有关,以上因素可共同解释Rs变异的83.9%。结论: 土壤总呼吸速率及各组分呼吸速率的季节变化特征相似,主要受土壤温度控制;酸雨造成土壤酸化,引发土壤酶、土壤有机碳含量显著变化或呈一定变化趋势,其共同作用导致RhRa被抑制,进而显著降低Rs,土壤水热因子促使这种抑制效应在生长季更显著;RhRs中的占比随酸雨强度增加而逐渐降低,但短期内Rh仍是Rs的主导组分。

关键词: 土壤呼吸, 模拟酸雨, 影响机制, 呼吸组分, 湿地松人工林

Abstract:

Objective: The study was aimed to investigate the patterns of impacts of acid rain at different intensities on total soil respiration rate(Rs) and its components of soil heterotrophic respiration rate(Rh) and soil autotrophic respiration rate(Ra) in Pinus elliottii plantation, in order to improve our understandings of the process of soil respiration and further to provide a scientific basis for forest management under environmental stresses such as acid deposition. Method: We conducted a one-way factorial acid rain addition(CK: pH 6.5; low acid addition level(LA): pH 4.5; high acid addition(HA): pH 2.5, with 3 replicates) field experiment in a subtropical P. elliottii plantation in China. The trenching method was used to separate the heterotrophic and autotrophic soil respiration. From January to December of 2015, the Rs, Ra, Rh effluxes were measured twice a month using a LI-8100A automated soil CO2 flux system. Soil temperatures and soil volumetric water content and soil biochemical properties adjacent to each soil respiration points were simultaneously detected. Result: Rs, Ra, Rh showed clear seasonal dynamics with similar single peak curves in all treatments, and were mainly driven by the surface soil temperature. Compared to the Rs under CK, the Rs under LA and HA were significantly reduced by 25.83% and 30.95%(P < 0.05). Also, LA and HA treatments inhibited the Rh effluxes by 29.60% and 35.20%(P < 0.05), reduced the Ra effluxes by 19.15% and 23.40%(P < 0.05). The inhibitory effect of simulated acid addition on soil respiration rates only showed in the growing season. Ra even being promoted in non-growth season(P < 0.05). In the CK plots, Rh accounted for 63.94% in Rs, and the proportion was significantly reduced(P < 0.05) in the LA and HA treatments. The intensity of Ra increased with the enhancement of acid rain. There were significant exponential correlations between Rs, Rh, Ra and soil temperature(P < 0.01), and both addition levels of the simulated acid rain could reduce the temperature sensitivity coefficient of soil respiration. Surface soil moisture was significantly related to the total soil respiration rates and the two main components under HA treatments(P < 0.01). The combined action of soil temperature and soil moisture also had a significant impact on soi respiration(P < 0.01). The variation of Rh was mainly controlled by the activity of soil urease and soil sucrase, topsoil organic carbon(TOC) and soil pH, while the Ra rates were mainly influenced by the soil urease activity, soil temperature and TOC, and the these factors jointly contributed 83.9% to the variation of Rs. Conclusion: The seasonal characteristics of soil respiration and its main components were similar and mainly controlled by surface soil temperature. Simulated acid rain exacerbated soil acidification, and significantly changed soil enzymes and soil organic carbon, which caused the inhibitory effects of Rs mainly due to Rh and Ra, and the changes of soil hydrothermal status induced the inhibition effects more obvious in the growing season. The proportion of Rh in the total soil respiration decreased with the increase of simulated acid rain intensities, but in the short term, the Rs variation was mainly controlled by the change of Rh.

Key words: soil respiration, simulated acid rain, influence mechanism, components of soil respiration, Pinus elliottii plantation

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