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应用生态学报 ›› 2022, Vol. 33 ›› Issue (8): 2161-2170.doi: 10.13287/j.1001-9332.202208.016

• 研究论文 • 上一篇    下一篇

草甸草原土壤与植物系统自然丰度氮稳定同位素的年际变化及其指示作用

王斌1,3, 王汝振1*, 张英1, 顾柏滔1, 李甜1,2, 张玉革2, 姜勇1,4   

  1. 1中国科学院沈阳应用生态研究所, 沈阳 110016;
    2沈阳大学环境学院, 沈阳 110044;
    3中国科学院大学, 北京 100049;
    4河北大学生命科学学院, 河北保定 071002
  • 收稿日期:2022-01-04 接受日期:2022-04-16 出版日期:2022-08-15 发布日期:2023-02-15
  • 通讯作者: * E-mail: ruzhenwang@iae.ac.cn
  • 作者简介:王 斌, 男, 1996年生, 硕士研究生。主要从事土壤化学和草地生态学研究。E-mail: wangbin19@mails.ucas.ac.cn
  • 基金资助:
    国家自然科学基金项目(32071563)资助。

Interannual variations in natural abundance of nitrogen stable isotopes in soil and plant and their implications in a meadow steppe

WANG Bin1,3, WANG Ru-zhen1*, ZHANG Ying1, GU Bai-tao1, LI Tian1,2, ZHANG Yu-ge2, JIANG Yong1,4   

  1. 1Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China;
    2College of Environment, Shenyang University, Shenyang 110044, China;
    3University of Chinese Academy of Sciences, Beijing 100049, China;
    4College of Life Sciences, Hebei University, Baoding 071002, Hebei, China
  • Received:2022-01-04 Accepted:2022-04-16 Online:2022-08-15 Published:2023-02-15

摘要: 氮是陆地生态系统生产力的首要限制性养分,利用自然丰度δ15N(15N/14N)可以有效指示生态系统氮循环过程。本试验研究了内蒙古草甸草原土壤与植物系统自然丰度δ15N、土壤净氮矿化潜势的年际变化。结果表明: 2017—2020年,土壤NO3--N含量(9.83~14.79 mg·kg-1)均显著高于NH4+-N含量(3.92~5.00 mg·kg-1);土壤NH4+的δ15N值(13.3‰~18.3‰)显著高于NO3-的δ15N值(3.76‰~6.14‰),土壤NO3-的δ15N值与土壤NO3-含量呈显著负相关;干旱年NH4+的δ15N值相对较高,降水较高或较低年NO3-的δ15N值显著降低。干旱年土壤净氮矿化速率、净氨化速率显著高于湿润年,而土壤硝化速率与年降水量无显著相关性。植物δ15N值与土壤δ15N值无显著相关性,但与植物N含量呈显著负相关;豆科植物与非豆科植物δ15N值、N含量均呈显著正相关,在一定程度上表明豆科植物对非豆科植物的N吸收具有促进作用。研究结果可为草原土壤-植物系统氮循环过程及其对降水变化的响应提供数据支撑。

关键词: 氮稳定同位素, 氮循环, 氮矿化, 草原生态系统, 降水变化

Abstract: Nitrogen is the most limiting nutrient for ecosystems. The natural abundance of δ15N (15N/14N) can efficiently indicate ecosystem nitrogen cycling processes. We investigated the interannual variations in natural abundance of δ15N in soil-plant system and soil net nitrogen mineralization in a meadow steppe of Inner Mongolia. Results across the four sampling years (2017-2020) showed that the content of soil NO3--N (9.83-14.79 mg·kg-1) was significantly higher than that of NH4+-N (3.92-5.00 mg·kg-1) and that δ15N value of soil NH4+ (13.3‰-18.3‰) was significantly higher than that of NO3-(3.76‰-6.14‰). The δ15N value of soil NO3- was negatively correlated with soil NO3- content. The δ15N value of soil NH4+ was relatively higher in the dry years, while the δ15N value of soil NO3- significantly decreased in the wetter and drier years. Soil net mineralization and ammonification rates were significantly higher in the dry years than that of the wet years, while soil nitrification rates showed no correlation with annual precipitation. The δ15N values of plants were not related to that of soils, but nega-tively correlated with plant nitrogen content. Both δ15N values and nitrogen contents were significantly and positively correlated between the leguminous and non-leguminous plants, suggesting that legume could facilitate nitrogen uptake of non-leguminous plants. These results could provide supporting data for nitrogen cycling and their responses to changes in precipitation in grassland soil-plant systems.

Key words: nitrogen stable isotope, nitrogen cycling, nitrogen mineralization, grassland ecosystem, precipitation change