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首页> 外文期刊>The Science of the Total Environment >Spatial and temporal variability of snow chemical composition and accumulation rate at Talos Dome site (East Antarctica)
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Spatial and temporal variability of snow chemical composition and accumulation rate at Talos Dome site (East Antarctica)

机译:塔洛斯巨蛋场(南极东部)雪化学成分和累积速率的时空变化

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摘要

Five snow pits and five firn cores were sampled during the 2003-2004 Italian Antarctic Campaign at Talos Dome (East Antarctica), where a deep ice core (TALDICE, TALos Dome Ice CorE, 1650 m depth) was drilled in 2005-2008 and analyzed for ionic content Particular attention is spent in applying decontamination procedures to the firn cores, as core sections were stored for approximately 10 years before analysis. By considering the snow pit samples to be unperturbed, the comparison with firn core samples from the same location shows that ammonium, nitrate and MSA are affected by storage post-depositional losses. All the other measured ions are confirmed to be irreversibly deposited in the snow layer. The removal of the most external layers (few centimeters) from the firn core sections is proved to be an effective decontamination procedure. High-resolution profiles of seasonal markers (nitrate, sulfate and MSA) allow a reliable stratigraphic dating and a seasonal characterization of the samples. The calculated mean accumulation-rate values range from 70 to 85 mm w.e. year~(-1) in the period 2003-1973 with small differences between two sectors: 70-74 mm w.e. year~(-1) in the NNE sector (spanning 2003-1996 years) and 81-92 mm w.e. year~(-1) in the SSW sector (spanning 2003-1980 years). This evidence is interpreted as a coupled effect of wind-driven redistribution processes in accumulation/ablation areas. Statistical treatment applied to the concentration values of the snow pits and firn cores samples collected in different points reveals a larger temporal variability than spatial one both in terms of concentration of chemical markers and annual accumulation. The low spatial variability of the accumulation rate and chemical composition measured in the five sites demonstrates that the TALDICE ice core paleo-environmental and paleo-climatic stratigraphies can be considered as reliably representative for the Talos Dome area.
机译:在2003-2004年意大利塔洛斯巨蛋(南极东部)的南极运动期间,采样了五个雪坑和五个火芯,在2005-2008年对深冰芯(TALDICE,TALos Dome Ice CorE,深度为1650 m)进行了钻探并进行了分析。离子含量的特别注意是在对烙铁芯应用去污程序时,因为芯体切片在分析前已存储了大约10年。通过考虑雪坑样本不受干扰,与来自同一位置的烧结岩心样本的比较表明,铵,硝酸盐和MSA受沉积后沉积损失的影响。确认所有其他测量离子不可逆地沉积在雪层中。事实证明,从烧结芯部分去除最外层(几厘米)是一种有效的去污程序。季节性标记(硝酸盐,硫酸盐和MSA)的高分辨率剖面图可提供可靠的地层测年和样品的季节性特征。计算的平均累积速率值范围为70至85 mm w.e.年(-1)在2003-1973年期间,两个扇区之间的差异很小:70-74毫米w.e. NNE部门的年(-1)(跨度2003-1996年)和81-92 mm w.e. SSW部门的年份〜(-1)(跨度2003-1980年)。该证据被解释为累积/消融区域中的风能再分配过程的耦合效应。对在不同点收集的雪坑和冷杉核样品的浓度值进行的统计处理显示,就化学标记物的浓度和年度累积而言,其时空变异性都比空间变异性大。在这五个地点测得的累积速率和化学成分的空间变异性很低,这表明TALDICE冰芯的古环境和古气候地层可以被认为是Talos Dome地区的可靠代表。

著录项

  • 来源
    《The Science of the Total Environment》 |2016年第15期|418-430|共13页
  • 作者单位

    Department of Chemistry 'Ugo Schiff', Via della Lastruccia 3,I-50019, Sesto F.no (Florence), Italy;

    Department of Chemistry 'Ugo Schiff', Via della Lastruccia 3,I-50019, Sesto F.no (Florence), Italy;

    Department of Chemistry 'Ugo Schiff', Via della Lastruccia 3,I-50019, Sesto F.no (Florence), Italy;

    Department of Chemistry 'Ugo Schiff', Via della Lastruccia 3,I-50019, Sesto F.no (Florence), Italy;

    Department of Chemistry 'Ugo Schiff', Via della Lastruccia 3,I-50019, Sesto F.no (Florence), Italy;

    Department of Chemistry 'Ugo Schiff', Via della Lastruccia 3,I-50019, Sesto F.no (Florence), Italy;

    Department of Chemistry 'Ugo Schiff', Via della Lastruccia 3,I-50019, Sesto F.no (Florence), Italy;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Ion species; Snow layer; Talos Dome; Spatial variability; Accumulation rate;

    机译:离子种类;雪层Talos Dome;空间变异性;累积率;

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