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Latitude Effect on Carbon, Nitrogen and Oxygen Stable Isotope Ratios

机译:纬度对碳,氮和氧稳定同位素比率的影响

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摘要

Cosmic rays in the upper troposphere (30000 feet to 50000 feet; 9000 meters to 15000 meters) initiate the nuclear chemical reaction: ~1n + ~(14)N =>~(14)C + ~1H. Previous research has shown a strong effect of latitude on the abundance of neutrons from cosmic rays. However, to date, there has been little exploration of the relationship between the latitude effect for cosmic-ray neutrons and latitudinal variations of stable isotope ratios in aerosols and foliage. In this study, aerosol samples (PM 4.5) and foliage samples were collected in Singapore in November 2009, February 2010 and July 2010 and in Fairbanks, Alaska, U.S.A. in January 2010, April 2010 and September 2010. Ion chromatography, gas chromatography-mass spectrometry, and element mass spectrometry were used to measure anion concentrations and nitrogen and oxygen stable isotope ratios in nitrogen oxide ions of the aerosol samples, as well as to measure carbon and nitrogen stable isotope ratios in the foliage samples. The average value of δ~(15/14) in foliage in Fairbanks was -1.84 [per mil], whereas the average value in Singapore was -1.3 [per mil]. These results show a clear latitude effect on δ~(15/14)N in foliage. Furthermore, the average value of δ~(15/14)N in the nitric-oxide substances in the aerosol samples in Fairbanks was -2.70 [per mil], whereas the average value in Singapore was +7.61 [per mil], demonstrating that δ~(15/14)N in nitric-oxide substances from aerosol samples also experiences a latitude effect. However, no clear latitudinal pattern was observed for δ~(13/12)C in foliage or for δ~(18/16)O in nitric-oxide substances from aerosols. In both Singapore and Fairbanks, it was observed that values of δ~(13/14)N in nitric-oxide substances from aerosols were correlated with declination. The value of δ~(15/14) N in nitric-oxide substances from aerosols in Fairbanks increased with increasing declination due to more active conversions from 14N to ~(14)C by neutron bombardment.
机译:对流层上方的宇宙射线(30000英尺至50000英尺; 9000米至15000米)引发核化学反应:〜1n +〜(14)N =>〜(14)C +〜1H。先前的研究表明,纬度对宇宙射线中子的丰度有很大的影响。但是,迄今为止,关于宇宙射线中子的纬度效应与气溶胶和树叶中稳定同位素比率的纬度变化之间的关系的探索很少。在这项研究中,分别于2009年11月,2010年2月和2010年7月以及在美国阿拉斯加的费尔班克斯于2010年1月,2010年4月和2010年9月收集了气溶胶样品(PM 4.5)和树叶样品。离子色谱,气相色谱-质谱质谱法和元素质谱法分别用于测量气溶胶样品中氮离子的阴离子浓度和氮,氧稳定同位素比,以及测量树叶样品中的碳,氮稳定同位素比。费尔班克斯的树叶中δ〜(15/14)的平均值为-1.84 [每密耳],而新加坡的平均值为-1.3 [每密耳]。这些结果表明纬度对叶片中的δ〜(15/14)N有明显的影响。此外,费尔班克斯气溶胶样品中一氧化氮物质中δ〜(15/14)N的平均值为-2.70 [每mil],而新加坡的平均值为+7.61 [每mil],这表明气溶胶样品中一氧化氮物质中的δ〜(15/14)N也受到纬度影响。然而,对于气溶胶中的δ〜(13/12)C或一氧化氮物质中的δ〜(18/16)O,没有观察到清晰的纬向分布。在新加坡和费尔班克斯,都观察到气溶胶中的一氧化氮物质中的δ〜(13/14)N值与磁偏角相关。由于中子轰击将更多的活性从14N转化为〜(14)C,费尔班克斯气溶胶中的一氧化氮物质中的δ〜(15/14)N值随磁偏角的增加而增加。

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