植物生态学报 ›› 2020, Vol. 44 ›› Issue (12): 1285-1295.DOI: 10.17521/cjpe.2020.0225

• 研究论文 • 上一篇    下一篇

亚热带人工林乔灌草根际土壤氮矿化特征

扈明媛1,2, 袁野3, 戴晓琴1,2,*(), 付晓莉1,2, 寇亮1,2, 王辉民1,2   

  1. 1中国科学院地理科学与资源研究所生态系统网络观测与模拟重点实验室千烟洲试验站, 北京 100101
    2中国科学院大学资源与环境学院, 北京 100190
    3安徽师范大学生命科学学院安徽省重要生物资源保护与利用研究重点实验室, 安徽芜湖 241000
  • 收稿日期:2020-07-06 接受日期:2020-09-27 出版日期:2020-12-20 发布日期:2021-04-01
  • 通讯作者: 戴晓琴
  • 作者简介:* (daixq@igsnrr.ac.cn)
  • 基金资助:
    国家自然科学基金(41830860);国家自然科学基金(31971634)

Characteristics of soil nitrogen mineralization in the rhizosphere of trees, shrubs, and herbs in subtropical forest plantations

HU Ming-Yuan1,2, YUAN Ye3, DAI Xiao-Qin1,2,*(), FU Xiao-Li1,2, KOU Liang1,2, WANG Hui-Min1,2   

  1. 1Qianyanzhou Ecological Research Station, Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Science and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
    2College of Resource and Environment, University of Chinese Academy of Sciences, Beijing 100190, China
    3Anhui Provincial Key Laboratory of the Conservation and Exploitation of Biological Resources, College of Life Science, Anhui Normal University, Wuhu, Anhui 241000, China
  • Received:2020-07-06 Accepted:2020-09-27 Online:2020-12-20 Published:2021-04-01
  • Contact: DAI Xiao-Qin
  • Supported by:
    National Natural Science Foundation of China(41830860);National Natural Science Foundation of China(31971634)

摘要:

为了探讨人工林内优势乔木和林下灌草根际土壤氮矿化特征, 明确乔灌草根际土壤氮转化差异, 该研究以江西泰和千烟洲站区典型人工杉木(Cunninghamia lanceolata)、马尾松(Pinus massoniana)和湿地松(Pinus elliottii)林为对象, 在植被生长季初期(4月)和旺盛期(7月)分析3种人工林内乔木、优势灌木(檵木(Loropetalum chinense)、杨桐(Adinandra millettii)、格药柃(Eurya muricata))和草本(狗脊蕨(Woodwardia japonica)、暗鳞鳞毛蕨(Dryopteris atrata))根际土壤的净氮矿化速率、土壤化学性质及土壤微生物特征。结果发现: 1)物种、林型和取样季节显著影响了根际土壤净氮矿化速率(Nmin)、净铵化速率(Namm)和净硝化速率(Nnit)。马尾松和湿地松林内林下灌草根际土壤净氮矿化的季节敏感性高于乔木: 4月乔木根际土壤NminNamm显著高于大多数林下灌草, 而7月林下灌草根际土壤NminNamm显著提高, 与乔木不再具有显著差异, 与主成分综合得分方差分析的结果一致。一般情况下, 杉木林NminNnit显著高于马尾松林和湿地松林。7月净氮矿化显著高于4月。2)土壤铵态氮、硝态氮、全氮及土壤微生物量氮含量是影响根际土壤净氮矿化的主要因素。土壤化学性质对人工林根际土壤净氮矿化变异的贡献率为29.2%, 显著高于土壤微生物的解释率。充分考虑不同季节林下植被根际土壤的净氮矿化及其关键影响因素可为准确评估人工林生态系统养分循环状况提供重要支撑。

关键词: 根际土壤氮矿化, 林下植被, 乔木, 人工林, 红壤

Abstract:

Aims The objective was to explore the characteristics of soil nitrogen mineralization in the rhizosphere soils of trees, shrubs, and herbs in plantations and their variations among different species, forest types, and seasons.
Methods The rhizosphere soils of trees, shrubs (Loropetalum chinense, Adinandra millettii, and Eurya muricate), and herbs (Woodwardia japonica and Dryopteris atrata) were sampled in the early growth season (April) and the vigorous growth season (July) in Cunninghamia lanceolata, Pinus massoniana, and Pinus elliottii plantations at Qianyanzhou Ecological Research Station, Taihe, Jiangxi. Net mineralization rate (Nmin), net ammonification rate (Namm), net nitrification rate (Nnit), soil chemical properties, and microbial properties were measured.
Important findings The results found that, 1) Species, forest types, and sampling seasons significantly affected Nmin, Namm, and Nnit. Understory plants showed a higher seasonal sensitivity of rhizosphere soil Nnit than trees did in P. massoniana plantations and P. elliottii plantations. It means that rhizosphere soil Nmin and Namm of trees were significantly higher than those of most of the understory plants in April, but rhizosphere soil Nmin and Namm of the understory plants significantly increased and showed no difference with those of trees in July. This finding was consistent with the variance analysis of comprehensive scores by principal component analysis. Generally, rhizosphere soil Nmin and Nnit in C. lanceolata plantation were higher than those in P. massoniana and P. elliottii plantations. Rhizosphere soil nitrogen mineralization in July was higher than those in April. 2) Soil ammonium nitrogen, nitrate nitrogen, soil total nitrogen concentration, and soil microbial nitrogen concentration were the main factors affecting net nitrogen mineralization of rhizosphere soil. Soil chemical properties contributed to 29.2% of the variation of rhizosphere soil nitrogen mineralization, which was significantly higher than soil microbial properties. Consideration of the seasonal variations of soil nitrogen mineralization in the rhizosphere of understory plants and their influencing factors will provide an important foundation for accurately evaluating nutrient cycling in the plantation ecosystem.

Key words: rhizosphere soil nitrogen mineralization, understory vegetation, overstory tree, plantation, red soil