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林业科学 ›› 2022, Vol. 58 ›› Issue (9): 25-35.doi: 10.11707/j.1001-7488.20220903

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中度火灾一年后马尾松林土壤碳库特征

罗斯生1,2,罗碧珍1,*,魏书精2,胡海清1,李小川2,王振师2,周宇飞2,宋兆2,钟映霞2   

  1. 1. 东北林业大学林学院 哈尔滨 150040
    2. 广东省森林培育与保护利用重点实验室 广东省林业科学研究院 广州 510520
  • 收稿日期:2020-08-17 出版日期:2022-09-25 发布日期:2023-01-18
  • 通讯作者: 罗碧珍
  • 基金资助:
    广东省自然科学基金项目(2021A1515010946);国家重点研发计划项目(2018YFE0207800);广西自然科学基金项目(2014GXNSFBA118108)

Characteristics of Soil Carbon Pool in Pinus massoniana Forest One Year after Moderate Forest Fires

Sisheng Luo1,2,Bizhen Luo1,*,Shujing Wei2,Haiqing Hu1,Xiaochuan Li2,Zhenshi Wang2,Yufei Zhou2,Zhao Song2,Yingxia Zhong2   

  1. 1. College of Forestry, Northeast Forestry University Harbin 150040
    2. Guangdong Provincial Key Laboratory of Silviculture, Protection and Utilization Guangdong Academy of Forestry Guangzhou 510520
  • Received:2020-08-17 Online:2022-09-25 Published:2023-01-18
  • Contact: Bizhen Luo

摘要:

目的: 分析不同林龄马尾松次生林在森林火灾前后土壤理化性质、土壤活性有机碳组分(LOC)的动态特征及变化趋势,定量评价中度林火强度对土壤碳库稳定性的影响,可为定量研究中度林火对土壤碳平衡与碳循环的影响提供参考。方法: 选择成熟林、中龄林和幼龄林的马尾松次生林,采集火烧迹地及相邻未烧林分0~60 cm土壤,测定其土壤理化性质、细根生物量和土壤LOC组分含量,通过计算土壤碳库管理指数(CPMI)分析土壤碳库变化特征,采用通径分析探讨土壤CPMI的直接影响和间接影响因素。结果: 与对照样地相比,森林火灾后各林龄0~60 cm土层的土壤密度提高3.80%~4.85%、土壤pH值提高4.21%~5.78%、土壤全磷含量提高7.97%~12.44%,土壤含水率降低3.41%~3.97%、土壤全氮含量降低15.09%~17.45%、土壤有机碳含量降低10.07%~14.31%,幼龄林、中龄林和成熟林的土壤活性有机碳(LOC)分别降低22.70%、19.48%和17.48%。不同林龄马尾松次生林土壤CPMI对森林火灾的响应有差异,幼龄林、中龄林和成熟林的土壤CPMI分别为26.15、30.57和32.09,呈随林龄的增长而增加的趋势。马尾松次生林土壤CPMI与土壤LOC各组分呈极显著相关关系(P<0.01),与土壤理化性质和土壤细根生物量亦呈极显著相关关系(P<0.01)。通径分析表明,土壤全氮含量对土壤CPMI的直接影响最大,通径系数达1.786,土壤全磷含量、土壤细根生物量对其影响次之,通径系数分别为-1.021和0.981。结论: 中度林火对马尾松次生林土壤有机碳库稳定性产生重要影响,森林火灾后3种林龄之间的土壤活性有机质矿化释放的土壤养分产生差异,是马尾松次生林土壤碳库稳定性变化不一致的主要原因。土壤有机碳库稳定性随着林龄的增加和土壤深度增加而增强。因此,在制定火烧迹地生态修复策略时,应加强成熟林地的保护,同时加强对中幼龄林地的人工抚育,促进火后马尾松次生林的自然更新和恢复。

关键词: 森林火灾, 马尾松次生林, 林龄, 土壤碳库, 碳库管理指数

Abstract:

Objective: The soil physicochemical properties, dynamic characteristics and changing trends of soil labile organic carbon (LOC) before and after forest fires in the secondary forests of Pinus massoniana were analyzed, and the impact of moderate forest fire intensity on the stability of the soil carbon pools was quantitatively evaluated, which can provide a reference for quantitative research on the effects of moderate forest fire intensity on soil carbon balance and carbon cycle. Method: The secondary forests of P. massoniana in mature forests, middle-aged forests and young forests were selected, and the soil samples from 0-60 cm layers in the burned area and adjacent unburned forests were collected. The soil physicochemical properties, fine root biomass and the soil LOC component content were measured and analyzed, and the soil carbon pool management index (CPMI) was calculated to explore the soil carbon pool change characteristics. The path analysis was used to explore the direct and indirect effects of soil CPMI. Result: Compared with the control plots, the soil bulk density increased by 3.80%-4.85%, soil pH increased by 4.21%-5.78%, and total soil phosphorus increased by 7.97%-12.44% in the 0-60 cm soil layers of each forest age after the forest fire. The soil moisture content decreased by 3.41%-3.97%, soil total nitrogen decreased by 15.09%-17.45%, and soil organic carbon decreased by 10.07%-14.31%. The soil labile organic carbon (LOC) in the young-aged, middle-aged and mature forests decreased by 22.70%, 19.48% and 17.48%, respectively. The soil CPMI of the secondary forest of P. massoniana with different forest ages was different in response to forest fire. The soil CPMI of young forest, middle-aged forest and mature forest was 26.15, 30.57 and 32.09, respectively, showing a increasing trend with the increase of forest age. Soil CPMI of P. massoniana secondary forest had a very significant correlation with each component of soil LOC (P < 0.01), and also had a very significant correlation with soil physicochemical properties and soil fine root biomass (P < 0.01). Path analysis showed that soil TN had the greatest direct effect on soil CPMI, with a path coefficient of 1.786, followed by soil TP and soil fine root biomass, with the path coefficients of -1.021 and 0.981, respectively. Conclusion: Moderate forest fire intensity has an important impact on the stability of soil organic carbon pool in the secondary forest of P. massoniana. The difference in soil nutrients released by mineralization of soil active organic matter among the three forest ages after forest fire is the key to the stability of soil carbon pool in the secondary forest of P. massoniana. The stability of soil organic carbon pool increases with the increase of stand age and soil depth. Therefore, when formulating the ecological restoration strategy in the burned area, the protection of mature forest land should be strengthened, and the artificial tending of young and middle-aged forest land should be strengthened to promote the natural regeneration and restoration of the secondary forest of P. massoniana after the fire.

Key words: forest fires, secondary forest of Pinus massoniana, different forest ages, soil organic carbon pools, carbon pool management index

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