关于地球-大气系统中活性氮的来源和转化的同位素追踪研究进展。

Q3 Environmental Science
Wei Song, Xue-Yan Liu
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引用次数: 0

摘要

自工业革命以来,人类活动导致活性氮产生量持续快速增加,造成地球表面氮富集,引发了许多生态和环境问题。稳定同位素是追踪环境过程来源和机制的有效工具。地表环境中的氮同位素值综合了不同氮源的同位素特征和转化过程的同位素分馏效应。因此,氮同位素的组成可用于追踪地表氮的来源和循环,帮助制定减少活性氮排放的策略,并评估氮富集对生态的影响。我们回顾了氮同位素在大气系统活性氮源、植物氮利用和森林生态系统氮过程追踪方面的研究进展。我们进一步讨论了如何更系统、更准确地了解地表环境各领域内部和之间的氮循环。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Research progress on isotope tracing on the sources and transformations of reactive nitrogen in the earth-atmosphere system.

Since the Industrial Revolution, human activities have led to a rapid and sustained increase in reactive nitrogen production, resulting in nitrogen enrichment at the Earth's surface and triggering many ecological and environmental issues. Stable isotopes are effective tools for tracing the sources and mechanisms of environmental processes. The nitrogen isotope values in surface environments integrate the isotope signatures of different nitrogen sources and the isotope fractionation effects of transformation processes. The composition of nitrogen isotopes can thus be utilized to trace the sources and cycling of nitrogen at the surface, aiding the development of strategies to reduce reactive nitrogen emissions, and assess the ecological effects of nitrogen enrichment. We reviewed the research progress on nitrogen isotope in the sources of reactive nitrogen in atmospheric systems, plant nitrogen utilization, and tracking of nitrogen processes in forest ecosystems. We further discussed how to gain a more systematic and accurate understanding of nitrogen cycle within and between the various spheres of the surface environment.

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应用生态学报
应用生态学报 Environmental Science-Ecology
CiteScore
2.50
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11393
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