
应用生态学报 ›› 2024, Vol. 35 ›› Issue (9): 2362-2371.doi: 10.13287/j.1001-9332.202409.031
宋韦, 刘学炎*
收稿日期:2024-05-29
接受日期:2024-07-04
出版日期:2024-09-18
发布日期:2025-03-18
通讯作者:
* E-mail: liuxueyan@tju.edu.cn
作者简介:宋韦, 男, 1985年生,副教授。主要从事氮同位素地球化学研究. E-mail: songwei2015@tju.edu.cn
基金资助:SONG Wei, LIU Xueyan*
Received:2024-05-29
Accepted:2024-07-04
Online:2024-09-18
Published:2025-03-18
摘要: 工业革命以来,人为活动导致活性氮的产生快速持续增加,造成了地表氮富集,诱发了一系列生态环境问题。稳定同位素是示踪物质来源和环境过程机制的有效手段之一。地表环境中活性氮化合物的氮同位素值整合了不同来源氮的同位素值和转化过程中的同位素分馏效应。因此,氮同位素组成可用于示踪地表氮素来源和循环过程,进而服务于地表活性氮减排策略的制定和地表氮富集的生态环境效应的评估。本文总结了氮同位素在大气系统活性氮来源、植物氮利用以及森林生态系统氮过程示踪中的研究进展,并对如何更加系统和准确地理解地表各圈层内以及圈层间的氮循环进行了展望。
宋韦, 刘学炎. 地-气系统活性氮来源与转化的同位素示踪研究进展[J]. 应用生态学报, 2024, 35(9): 2362-2371.
SONG Wei, LIU Xueyan. Research progress on isotope tracing on the sources and transformations of reactive nitrogen in the earth-atmosphere system[J]. Chinese Journal of Applied Ecology, 2024, 35(9): 2362-2371.
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