生态环境学报 ›› 2022, Vol. 31 ›› Issue (6): 1160-1168.DOI: 10.16258/j.cnki.1674-5906.2022.06.011

• 研究论文 • 上一篇    下一篇

不同林龄顶坛花椒林地土壤微生物浓度与生物量化学计量特征

喻阳华1,*(), 吴银菇2, 宋燕平1, 李一彤1   

  1. 1.贵州师范大学喀斯特研究院/国家喀斯特石漠化防治工程技术研究中心,贵州 贵阳 550001
    2.贵州师范大学地理与环境科学学院,贵州 贵阳 550025
  • 收稿日期:2022-04-06 出版日期:2022-06-18 发布日期:2022-07-29
  • 通讯作者: *
  • 作者简介:喻阳华(1984年生),男,副教授,博士,研究方向为喀斯特环境保护与治理。E-mail: yuyanghua2003@163.com
  • 基金资助:
    贵州省科技支撑计划项目(黔科合支撑[2022]一般103);2021年特色林业科技推广项目(贵[2021]TSLY01号)

Stoichiometric Characteristics of Soil Microbial Concentration and Biomass in Zanthoxylum planispinum var. Dintanensis Plantations of Different Ages

YU Yanghua1,*(), WU Yingu2, SONG Yanping1, LI Yitong1   

  1. 1. School of karst Science/State Engineering Technology Institute for Karst Decertification Control, Guizhou Normal University, Guiyang 550001, P. R. China
    2. School of Geography and Environment Science, Guizhou Normal University, Guiyang 550025, P. R. China
  • Received:2022-04-06 Online:2022-06-18 Published:2022-07-29

摘要:

阐明顶坛花椒人工林土壤微生物化学计量随林龄的变化特征,以及对土壤化学特性的响应规律,可揭示喀斯特区土壤养分与质量状况,有助于制订林分管理措施。以贵州喀斯特区4个林龄级(5—7、10—12、20—22、28—32 a)的顶坛花椒人工林土壤为对象,通过测定微生物浓度、生物量,阐明不同林龄土壤微生物化学计量特征及其互作关系,探讨土壤理化性质的变化。结果表明,(1)土壤细菌、真菌、放线菌浓度依次为3.3×105—7.9×105、2.10×103—4.15×103、2.20×105—3.95×105 CFU∙g-1,表现为细菌>放线菌>真菌,随林龄增加优势菌群未发生改变。(2)随顶坛花椒生长年限增加,土壤微生物生物量碳(MBC)差异不显著,微生物生物量氮(MBN)先升高后降低,微生物生物量磷(MBP)以28—32 a的林分最低;土壤MBC/MBP和MBN/MBP以28—32 a林分最高,MBC/MBN在4个龄级之间差异显著。(3)土壤微生物浓度、生物量之间的相关性较其计量比相对偏低。(4)冗余分析表明,土壤微生物生物量对土壤养分的依赖程度强于其计量比,其中土壤pH值、全钾和速效钾等是土壤微生物化学计量变化的主要影响因子,土壤微生物化学计量与部分化学因子具有趋同效应。综上表明,喀斯特区土壤微生物化学计量对林龄的响应存在差异,顶坛花椒人工林经营管理过程中应适当施加K肥与调控pH值。

关键词: 林龄, 顶坛花椒人工林, 土壤微生物浓度, 微生物生物量, 化学计量, 喀斯特

Abstract:

The change laws of soil microbial stoichiometry with forest age and soil chemical characteristics in Zanthoxylum planispinum var. dintanensis plantations, were studied to reveal soil nutrients and quality in a karst area, as well as to formulate stand management measures. Taking Zanthoxylum planispinum var. dintanensis plantation soils of 4 age classes (5-7, 10-12, 20-22, 28-32 years) in Guizhou karst area as the objects, characterization and interactions of soil microbial stoichiometry at different forest ages, and the change of soil physical and chemical properties was clarified by testing the soil microbial concentration and biomass. The results showed that: (1) The concentration of soil bacteria, fungi and actinomycetes were 3.3×105-7.9×105, 2.10×103-4.15×103 and 2.20×105-3.95×105 CFU∙g-1, showing that bacteria>actinomycetes>fungi, and the dominant flora remained unchanged with the increase of the plantation age. (2) With the increase of growth years of Zanthoxylum planispinum var. dintanensis, there was no significant differences in soil microbial biomass carbon (MBC). Microbial biomass nitrogen (MBN) increased first and then decreased, and MBP was the lowest in the stand of 28-32 years; MBC:MBP and MBN:MBP were the highest in the stand of 28-32 years, and MBC:MBN showed significant differences among the 4 age classes. (3) The correlation between soil microbial concentration and biomass was relatively lower than its stoichiometric ratio. (4) Redundancy analysis showed that the dependence of SMB on soil nutrients was stronger than its stoichiometric ratio. Soil pH, total potassium, and available potassium were the main driving factors of soil microbial stoichiometry. Soil microbial stoichiometry had a convergence effect with some chemical factors. In summary, responses of soil microbial stoichiometry to plantation ages in karst area were partially different; potash fertilizer should be properly used; and pH should be adjusted in the management of Zanthoxylum planispinum var. dintanensis plantation.

Key words: age, Zanthoxylum planispinum var. dintanensis plantation, soil microbial concentration, microbial biomass, stoichiometry, karst

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