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Deposition and light absorption characteristics of precipitation dissolved organic carbon (DOC) at three remote stations in the Himalayas and Tibetan Plateau, China

机译:喜马拉雅山和青藏高原三个偏远站的降水溶解有机碳(DOC)的沉积和光吸收特性

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摘要

The concentrations, depositions and optical properties of precipitation DOC at three remote stations (Nam Co, Lulang and Everest) were investigated in the Himalayas and Tibetan Plateau (HTP). The results showed that their volume-weighted mean DOC concentrations were 1.05 ± 1.01 mg C L~(-1) 0.83 ± 0.85 mg C L~(-1) and 0.86 ± 0.91 mg C L~(-1), respectively, close to those of other remote areas in the world and lower than those of typical polluted urban cities. Combined with precipitation amounts, the DOC depositions at these three stations were calculated to be 034 ± 032 g Cm~(-2) yr~(-1), 0.84 ± 0.86 g C m~(-2) yr~(-1) and 0.16 ± 0.17 g Cm~(-2) yr~(-1), respectively. The annual DOC deposition in the HTP was approximately 0.94 ± 0.87 Tg C, the highest and lowest values appeared in the southeastern and northwestern plateau, respectively. The sources of DOC in the precipitation at these three stations were remarkably different indicating large spatial heterogeneity in the sources of precipitation DOC over the HTP. Nam Co presented combustion sources from South Asia and local residents, Lulang showed biomass combustion source from South Asia, and Everest was mainly influenced by local mineral dust The values of the MAC_(DOC) at 365 nm were 0.48 ± 0.47 m~2 g~(-1), 0.25 ± 0.15 m~2 g~(-1), and 0.64 ± 0.49 m~2 g~(-1), respectively, for the precipitation at the three stations. All of these values were significantly lower than those of corresponding near-surface aerosol samples because precipitation DOC contains more secondary organic aerosol with low light absorption abilities. Additionally, this phenomenon was also observed in seriously polluted urban areas, implying it is universal in the atmosphere. Because precipitation DOC contains information for both particle-bound and gaseous components from the near surface up to the altitude of clouds where precipitation occurs, the MAC_(DOC) of precipitation is more representative than that of near-surface aerosols for a given region.
机译:在喜马拉雅山和青藏高原(HTP)对三个偏远站点(南姆公司,鹿朗和珠穆朗玛峰)降水DOC的浓度,沉积和光学性质进行了研究。结果表明,它们的体积加权平均DOC浓度分别为1.05±1.01 mg CL〜(-1)0.83±0.85 mg CL〜(-1)和0.86±0.91 mg CL〜(-1),接近于世界其他偏远地区,低于典型的污染城市。结合降水量,计算出这三个站的DOC沉积量分别为:034±032 g Cm〜(-2)yr〜(-1),0.84±0.86 g Cm〜(-2)yr〜(-1)。和0.16±0.17 g Cm〜(-2)yr〜(-1)。 HTP的年DOC沉积量约为0.94±0.87 Tg C,最高和最低值分别出现在东南高原和西北高原。这三个站的降水中的DOC来源明显不同,这表明HTP上降水DOC的来源存在很大的空间异质性。 Nam Co展示了来自南亚和当地居民的燃烧源,Lulang展示了来自南亚的生物质燃烧源,而珠穆朗玛峰则主要受到当地矿物粉尘的影响。365 nm处的MAC_(DOC)值为0.48±0.47 m〜2 g〜三个站的降水分别为(-1),0.25±0.15 m〜2 g〜(-1)和0.64±0.49 m〜2 g〜(-1)。所有这些值均明显低于相应的近地表面气溶胶样品的值,因为降水量DOC包含更多的具有较低光吸收能力的次级有机气溶胶。此外,在严重污染的城市地区也观察到了这种现象,这意味着它在大气中是普遍存在的。因为降水DOC包含从近地表到发生降水的云层高度的颗粒结合和气态成分的信息,所以对于给定区域,降水的MAC_(DOC)比近地气溶胶更具代表性。

著录项

  • 来源
    《The Science of the Total Environment》 |2017年第15期|1039-1046|共8页
  • 作者单位

    Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China,Laboratory of Green Chemistry, Lappeenranta University of Technology, Sammonkatu 12, Mikkeli 50130, Finland,CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing 100101, China;

    Laboratory of Green Chemistry, Lappeenranta University of Technology, Sammonkatu 12, Mikkeli 50130, Finland;

    State Key Laboratory of Cryospheric Sciences, Northwest Institute of Em-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China,CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing 100101, China,University of Chinese Academy of Sciences, Beijing 100049, China;

    State Key Laboratory of Cryospheric Sciences, Northwest Institute of Em-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China;

    State Key Laboratory of Cryospheric Sciences, Northwest Institute of Em-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China,University of Chinese Academy of Sciences, Beijing 100049, China;

    Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China,University of Chinese Academy of Sciences, Beijing 100049, China;

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

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

    Laboratory of Green Chemistry, Lappeenranta University of Technology, Sammonkatu 12, Mikkeli 50130, Finland;

    Laboratory of Green Chemistry, Lappeenranta University of Technology, Sammonkatu 12, Mikkeli 50130, Finland,Department of Civil and Environmental Engineering, Florida International University, Miami, FL 33174, USA;

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

    Dissolved organic carbon; The Third Pole; Deposition; Light absorption;

    机译:溶解的有机碳;第三极;沉积光吸收;

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