氮饱和过程中水体中硝酸盐的氧稳定同位素比值及硝酸盐浓度

Y. Tabayashi, M. Yamamuro
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引用次数: 0

摘要

测定了秩父地区水体氮饱和过程中主要无机离子和硝酸盐氮氧稳定同位素比值。研究区硝酸盐浓度呈较高的西-东梯度。硝酸盐中氧的稳定同位素比值与硝酸盐浓度有明显的关系。在较低的硝酸盐浓度范围内,氧的稳定同位素比值随硝酸盐浓度的增加而增加。而在中、高浓度硝态氮中,硝态氮的氧稳定同位素比值几乎没有增加。这一现象可能表明硝酸盐的氧稳定同位素比值反映了森林生态系统中氮饱和的一个阶段。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Oxygen-Stable Isotope Ratios of Nitrate and Nitrate Concentration in Stream Water during the Course of Nitrogen Saturation
We measured major inorganic ions and stable isotope ratios of nitrogen and oxygen of nitrate in the stream water in the Chichibu region during the course of nitrogen saturation. Nitrate concentration showed a high west-east gradient in the study area. Stable isotope ratios of oxygen in nitrate showed clear relationships with nitrate concentration. A direct relationship was apparent in the lower range of nitrate concentrations in that the stable isotope ratio of oxygen increases as the nitrate concentration increases. On the other hand, oxygen stable isotope ratios of nitrate hardly increase in the middle to higher concentrations of nitrate. This phenomenon may suggest that the oxygen stable isotope ratios of nitrate reflect a phase of the nitrogen saturation in the forest ecosystems.
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