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Use of isotopic compositions of nitrate in TSP to identify sources and chemistry in South China Sea

机译:利用TSP中硝酸盐的同位素组成识别南海的来源和化学

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摘要

NO3- concentration, nitrogen and oxygen isotopic compositions (delta N-15 and delta O-18) of NO3- were measured in total suspended particulates (TSP) at Yongxing Island in the South China Sea (SCS) between Feb. 2013 and Jan. 2014, as well as on two cruises in the northern South China Sea (NSCS). Measurements aimed to identify NO3- sources, and possible chemical formation processes of NO3-. The delta N-15 and delta O-18 of NO3- in TSP at Yongxing Island ranged from -2.5 to +4.9 parts per thousand, and +48.1 to +99.0 parts per thousand, with annual weighted averages of +1.5 parts per thousand and +83.2 parts per thousand, respectively. Both delta N-15 and delta O-18 had higher values in cool months, indicating that NOx sources and oxidants were different between seasons. In cool months, NOx was mainly from anthropogenic sources, particularly from coal combustion in South China, resulting in high nitrogen deposition that was oxidized by 03 to NO3-. In warm months, natural emissions were an important source of NOx. TSP samples in the NSCS had higher NO3- concentrations, higher delta N-15 and lower delta O-18 values than samples from Yongxing Island over the same period. This suggests that atmospheric processes caused a decrease in NO3- concentrations and delta N-15 but increase in delta O-18 from coast to remote marine. Assuming to oxygen atoms were derived from O-3 during transport in cool months, the mean ratio of NO3- formed by NOx to total NO3- was calculated to be 47.9%. This suggests the mean loss ratio of NOx was 89% while the loss ratio of NO3- was 87% during transport between Chinese coastal areas and Yongxing Island in Nov., 2013. (C)) 2015 Elsevier Ltd. All rights reserved.
机译:在2013年2月至1月之间,对南海永兴岛(SCS)的总悬浮颗粒(TSP)中的NO3-浓度,氮和氧同位素组成(δN-15和δO-18)进行了测量。 2014年,以及两次在南海北部航行(NSCS)。旨在识别NO3-来源以及NO3-可能的化学形成过程的测量。永兴岛TSP中NO3-的N-15增量N-15和O-18增量为-2.5至+4.9千分之和,+ 48.1至+99.0千分之,年加权平均值为+1.5千分之和分别为+83.2千分之一。在凉爽的月份,δN-15和δO-18均具有较高的值,这表明不同季节之间的NOx来源和氧化剂不同。在凉爽的月份,NOx主要来自人为来源,尤其是华南地区的煤炭燃烧,导致高氮沉积,并被03氧化为NO3-。在温暖的月份,自然排放物是NOx的重要来源。与同期永兴岛的样本相比,NSCS中的TSP样本具有更高的NO3-浓度,更高的N-15增量值和更低的O-18值。这表明大气过程导致了NO3浓度和N-15三角洲的减少,但从海岸到偏远海洋的O-18三角洲的增加。假设在凉爽月份的运输过程中O-3衍生了氧原子,则NOx形成的NO3-与总NO3-的平均比例经计算为47.9%。这表明2013年11月在中国沿海地区和永兴岛之间的运输过程中,NOx的平均损失率为89%,而NO3-的损失率为87%。(C))2015 Elsevier Ltd.保留所有权利。

著录项

  • 来源
    《Atmospheric environment》 |2015年第5期|70-78|共9页
  • 作者单位

    Chinese Acad Sci, South China Sea Inst Oceanol, State Key Lab Trop Oceanog, Guangzhou 510301, Guangdong, Peoples R China;

    Chinese Acad Sci, Guangzhou Inst Geochem, Key Lab Marginal Sea Geol, Guangzhou 510640, Guangdong, Peoples R China;

    Chinese Acad Sci, South China Sea Inst Oceanol, State Key Lab Trop Oceanog, Guangzhou 510301, Guangdong, Peoples R China;

    Chinese Acad Sci, Guangzhou Inst Geochem, Key Lab Marginal Sea Geol, Guangzhou 510640, Guangdong, Peoples R China;

    Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Atmospher Boundary Layer Phys & Atm, Beijing 100029, Peoples R China;

    Chinese Acad Sci, South China Sea Inst Oceanol, Xisha Deep Sea Marine Environm Observat & Res Stn, Sansha 157009, Peoples R China;

    Chinese Acad Sci, South China Sea Inst Oceanol, Xisha Deep Sea Marine Environm Observat & Res Stn, Sansha 157009, Peoples R China;

    Chinese Acad Sci, South China Sea Inst Oceanol, Xisha Deep Sea Marine Environm Observat & Res Stn, Sansha 157009, Peoples R China;

    Chinese Acad Sci, Inst Geochem, State Key Lab Environm Geochem, Guiyang 550002, Peoples R China;

    Chinese Acad Sci, Inst Geochem, State Key Lab Environm Geochem, Guiyang 550002, Peoples R China;

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  • 正文语种 eng
  • 中图分类
  • 关键词

    Nitrogen isotope; Oxygen isotope; South China Sea; Nitrate; Atmospheric chemical process; Isotopic fractionation;

    机译:氮同位素氧同位素南海硝酸盐大气化学过程同位素分馏;

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