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Lead isotopic composition of insoluble particles from widespread mountain glaciers in western China: Natural vs. anthropogenic sources

机译:来自中国西部山区冰川的不溶性颗粒的铅同位素组成:自然与人为来源

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摘要

Stable lead (Pb) isotopic fingerprints provide opportunities to trace natural and anthropogenic Pb sources in the environment. In order to evaluate Pb deposition from different sources over mountainous areas of western China, Pb isotopic compositions were characterized from modern aeolian dust in 15 snowpit samples collected from 13 typical mountain glaciers between 2008 and 2010. Most of the snowpits sampled cover more than a whole year of accumulation and overlap with each other on deposition date. Pb isotopic variability among all the samples is small, varying in the range of 18.1399-18.9199 for ~(206)Pb/~(204)Pb, 15.5979-15.8743 for ~(207)Pb/~(204)Pb, 38.2272-39.9453 for ~(208)Pb/~(204)Pb, 1.1605-1.2009 for ~(206)Pb/~(207)Pb and 2.4433-2.5182 for ~(208)Pb/~(207)Pb. Three isotopic plots of the different Pb isotope ratios(~(207)Pb/~(204)Pb vs. ~(206)Pb/~(204)Pb ~(208)Pb/~(204)Pb vs. ~(206)Pb/~(204)Pb, and ~(208)Pb/~(207)Pb vs. ~(206)Pb/~(207)Pb) in all the sam- ples show identical geographic trends, with more radiogenic in the south and less in the north. This trend is consistent with the distribution of natural dust sources and supports the interpretation of a regional/ local source for insoluble particles (IP) to snow/glaciers in this region. Comparison with the Pb isotope results from potential dust sources, however, it shows that the Pb isotopic compositions of IP samples in snow samples are relatively less radiogenic. Parts of these less-radiogenic Pb isotopes are comparable with the ice core results during recent decades, which are shown to be influenced by anthropogenic sources. At sites located along the periphery of western China, the Pb isotopic compositions are much closer to anthropogenic results. Natural and anthropogenic Pb sources are roughly assessed using a simple binary model. The sites with a high anthropogenic fraction are at lower elevations and are relatively close to population centers.
机译:稳定的铅(Pb)同位素指纹提供了追踪环境中自然和人为铅源的机会。为了评估中国西部山区不同来源的Pb沉积量,从2008年至2010年从13个典型的高山冰川收集的15个雪坑样本中,通过现代风尘对Pb同位素组成进行了表征。大部分采样点覆盖了整个雪堆沉积的年份和彼此重叠的年份。所有样品中的铅同位素变异性很小,〜(206)Pb /〜(204)Pb在18.1399-18.9199之间变化,〜(207)Pb /〜(204)Pb在15.5979-15.8743之间变化,38.2272-39.9453对于((208)Pb /〜(204)Pb),1.1605-1.2009(对于〜(206)Pb /〜(207)Pb)和2.4433-2.5182对于((208)Pb /〜(207)Pb)。不同铅同位素比率的三个同位素图(〜(207)Pb /〜(204)Pb vs.〜(206)Pb /〜(204)Pb〜(208)Pb /〜(204)Pb vs.〜(206) )Pb /〜(204)Pb和〜(208)Pb /〜(207)Pb与〜(206)Pb /〜(207)Pb)相比,在所有样品中均显示出相同的地理趋势,其中南部,北部更少。这种趋势与自然粉尘源的分布相一致,并支持对该地区的雪/冰川的不溶性颗粒物(IP)的区域/局部来源的解释。与Pb同位素的比较来自潜在的粉尘源,但是,它表明雪样品中IP样品的Pb同位素组成的放射成因相对较低。这些放射性较低的铅同位素的某些部分可与近几十年来的冰芯结果相媲美,事实表明,这些结果受人为来源的影响。在中国西部的外围地区,铅的同位素组成更接近于人为的结果。使用简单的二元模型可以粗略评估天然和人为铅的来源。人为比例高的地点海拔较低,并且相对靠近人口中心。

著录项

  • 来源
    《Atmospheric environment》 |2013年第8期|224-232|共9页
  • 作者单位

    State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences,No 360 Donggang West Road, Lanzhou 730000, PR China;

    State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences,No 360 Donggang West Road, Lanzhou 730000, PR China;

    State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences,No 360 Donggang West Road, Lanzhou 730000, PR China;

    Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences,Beijing 100101, PR China;

    Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences,Beijing 100101, PR China;

    State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences,No 360 Donggang West Road, Lanzhou 730000, PR China;

    State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences,No 360 Donggang West Road, Lanzhou 730000, PR China;

    State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences,No 360 Donggang West Road, Lanzhou 730000, PR China;

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  • 正文语种 eng
  • 中图分类
  • 关键词

    Stable lead isotopes; Insoluble particles; Snowpit; Qinghai-Xizang (Tibet) Plateau; Western China;

    机译:稳定的铅同位素;不溶性颗粒;雪坑;青藏高原中国西部;

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