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应用生态学报 ›› 2025, Vol. 36 ›› Issue (4): 1071-1080.doi: 10.13287/j.1001-9332.202504.014

• 研究论文 • 上一篇    下一篇

林火对小兴安岭阔叶红松林土壤理化性质、酶活性和微生物群落的长期影响

车佳聪, 杨佳, 吴政鸿, 谷会岩*   

  1. 东北林业大学林学院/黑龙江凉水森林生态系统国家定位观测研究站, 哈尔滨 150040
  • 收稿日期:2024-09-18 接受日期:2025-02-17 出版日期:2025-04-18 发布日期:2025-10-18
  • 通讯作者: *E-mail: ghuiyan@nefu.edu.cn
  • 作者简介:车佳聪, 女, 2000年生, 硕士研究生。主要从事森林植物资源调查及土壤微生物研究。E-mail: 2801571163@qq.com
  • 基金资助:
    科技基础调查专项(2021FY100702)

Long-term effects of forest fires on soil physicochemical properties, enzyme activities, and microbial communities in the broad-leaved Korean pine forest of the Xiaoxing'an Mountains, Northeast China

CHE Jiacong, YANG Jia, WU Zhenghong, GU Huiyan*   

  1. College of Forestry, Northeast Forestry University/Liangshui National Field Observation and Research Station for Forest Ecosystem, Harbin 150040, China
  • Received:2024-09-18 Accepted:2025-02-17 Online:2025-04-18 Published:2025-10-18

摘要: 小兴安岭阔叶红松林是温带针阔混交林的典型代表,为探究阔叶红松林火烧迹地自然恢复28年后土壤理化性质、酶活性及土壤微生物特征,选取阔叶红松林火烧迹地及其相邻未受火烧影响的区域(对照)为研究对象,测定了土壤理化性质、酶活性及微生物群落特征,并分析了影响土壤酶活性和微生物群落的主要土壤因子。结果表明: 1)与对照样地相比,火烧迹地土壤总氮、碱解氮和含水量显著降低,降幅分别为28.0%、39.3%和4.5%;而过氧化氢酶、限制性核酸内切酶、脲酶、硝酸还原酶和土壤脱氢酶活性显著增加。2)火烧28年后,火烧迹地森林土壤细菌、真菌群落的α和β多样性与对照样地无显著差异,但群落组成在门和属水平上存在差异物种。3)冗余分析和结构方程模型分析表明,土壤pH值是影响酶活性和微生物群落的主要因子。4)火烧28年后,火烧迹地森林土壤细菌网络的稳定性和复杂性增强,真菌网络则呈相反趋势。综上,林火对森林土壤生态系统的影响是长期的,火烧后土壤理化性质、酶活性及微生物群落呈现出不同的恢复模式。

关键词: 火烧迹地, 土壤理化性质, 酶活性, 土壤微生物群落, 长期影响

Abstract: The broad-leaved Korean pine forest in the Xiaoxing'an Mountains is representative of temperate mixed coniferous and broad-leaved forests. In this study, we selected burned area of broad-leaved Korean pine forest and the adjacent unburned area (control) to investigate soil physicochemical properties, enzyme activities, and microbial characteristics after 28 years natural recovery. We further analyzed the main soil factors influencing enzyme activities and microbial communities. The results showed that: 1) soil total nitrogen, alkali-hydrolyzable nitrogen, and water content in the burned area were significantly lower than the control by 28.0%, 39.3% and 4.5%, respectively. However, the activities of catalase, restriction endonuclease, urease, nitrate reductase, and soil dehydrogenase were significantly increased. 2) The α- and β-diversity of soil bacterial and fungal communities in the burned area was not different from those of the control after 28 years recovery, but marked differences were observed in community composition at phylum and genus levels. 3) Redundancy analysis and structural equation modeling revealed that soil pH was the primary factor influencing enzyme activities and microbial communities. 4) After 28 years, the stability and complexity of soil bacterial network in the burned area increased, while the fungal network showed an opposite trend. These results suggested that forest fires have long-term effects on soils, with soil physicochemical properties, enzyme activities, and microbial communities exhibiting distinct post-fire recovery patterns.

Key words: burned area, soil physicochemical properties, enzyme activity, soil microbial community, long-term effects