Atmospheric nitrogen deposition to forest and estuary environments in the Pearl River Delta region, southern China

Due to its significant ecological and climate consequences, atmospheric nitrogen (N) deposition is a growing global concern, especially in the severely N-polluted regions such as the Pearl River Delta (PRD) region of southern China. One-year measurements of reactive N species, including ammonium nit...

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Published in:Tellus: Series B, Chemical and Physical Meteorology
Main Authors: Xuemei Wang, Zhiyong Wu, Min Shao, Yunting Fang, Leiming Zhang, Fei Chen, Pak-wai Chan, Qi Fan, Qian Wang, Shengjie Zhu, Ruoyu Bao
Format: Article
Language:English
Published: Stockholm University Press 2013-09-01
Subjects:
Online Access:http://www.tellusb.net/index.php/tellusb/article/download/20480/pdf_1
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author Xuemei Wang
Zhiyong Wu
Min Shao
Yunting Fang
Leiming Zhang
Fei Chen
Pak-wai Chan
Qi Fan
Qian Wang
Shengjie Zhu
Ruoyu Bao
author_facet Xuemei Wang
Zhiyong Wu
Min Shao
Yunting Fang
Leiming Zhang
Fei Chen
Pak-wai Chan
Qi Fan
Qian Wang
Shengjie Zhu
Ruoyu Bao
author_sort Xuemei Wang
collection DOAJ
container_title Tellus: Series B, Chemical and Physical Meteorology
description Due to its significant ecological and climate consequences, atmospheric nitrogen (N) deposition is a growing global concern, especially in the severely N-polluted regions such as the Pearl River Delta (PRD) region of southern China. One-year measurements of reactive N species, including ammonium nitrogen ( -N), nitrate nitrogen (-N) and total organic nitrogen (ON) in dry and wet deposition, were conducted using an automated wet–dry sampler incorporated with a DDAS (dry deposition on aqueous surface) sampling device at Dinghushan (DHS), a natural forest site in the northwest of PRD and at Hengmen (HM), an estuary site in the south of PRD during 2006–2007. Total deposition fluxes of N at DHS and HM were up to 48.2 and 37.8 kg ha−1 yr−1, respectively, with most of the deposition occurring in the rainy season. Wet deposition was the dominant form, contributing 65–70% to the total deposition. -N was the largest contributor to the total N deposition at DHS (47%) due to significant influence of agriculture emissions. ON was the most important N component at HM (41%), which is probably attributed to the marine sources. However, -N deposition is increasing rapidly recently and is expected to be more important in the near future. The current N deposition level in PRD is much higher than those in Europe and North America. Great challenges exist in reducing reactive N emission in this region. Thus, a scenario of rising N deposition in PRD in the near future cannot be ruled out. The environmental consequences due to elevated N deposition should therefore be paid more attention in the future.
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spelling doaj-art-ceb98cec81914f84beeac4e837e2970d2025-08-19T21:43:25ZengStockholm University PressTellus: Series B, Chemical and Physical Meteorology1600-08892013-09-0165011310.3402/tellusb.v65i0.20480Atmospheric nitrogen deposition to forest and estuary environments in the Pearl River Delta region, southern ChinaXuemei WangZhiyong WuMin ShaoYunting FangLeiming ZhangFei ChenPak-wai ChanQi FanQian WangShengjie ZhuRuoyu BaoDue to its significant ecological and climate consequences, atmospheric nitrogen (N) deposition is a growing global concern, especially in the severely N-polluted regions such as the Pearl River Delta (PRD) region of southern China. One-year measurements of reactive N species, including ammonium nitrogen ( -N), nitrate nitrogen (-N) and total organic nitrogen (ON) in dry and wet deposition, were conducted using an automated wet–dry sampler incorporated with a DDAS (dry deposition on aqueous surface) sampling device at Dinghushan (DHS), a natural forest site in the northwest of PRD and at Hengmen (HM), an estuary site in the south of PRD during 2006–2007. Total deposition fluxes of N at DHS and HM were up to 48.2 and 37.8 kg ha−1 yr−1, respectively, with most of the deposition occurring in the rainy season. Wet deposition was the dominant form, contributing 65–70% to the total deposition. -N was the largest contributor to the total N deposition at DHS (47%) due to significant influence of agriculture emissions. ON was the most important N component at HM (41%), which is probably attributed to the marine sources. However, -N deposition is increasing rapidly recently and is expected to be more important in the near future. The current N deposition level in PRD is much higher than those in Europe and North America. Great challenges exist in reducing reactive N emission in this region. Thus, a scenario of rising N deposition in PRD in the near future cannot be ruled out. The environmental consequences due to elevated N deposition should therefore be paid more attention in the future.www.tellusb.net/index.php/tellusb/article/download/20480/pdf_1wet depositiondry depositionaqueous surfaceorganic nitrogenammoniumnitrate
spellingShingle Xuemei Wang
Zhiyong Wu
Min Shao
Yunting Fang
Leiming Zhang
Fei Chen
Pak-wai Chan
Qi Fan
Qian Wang
Shengjie Zhu
Ruoyu Bao
Atmospheric nitrogen deposition to forest and estuary environments in the Pearl River Delta region, southern China
wet deposition
dry deposition
aqueous surface
organic nitrogen
ammonium
nitrate
title Atmospheric nitrogen deposition to forest and estuary environments in the Pearl River Delta region, southern China
title_full Atmospheric nitrogen deposition to forest and estuary environments in the Pearl River Delta region, southern China
title_fullStr Atmospheric nitrogen deposition to forest and estuary environments in the Pearl River Delta region, southern China
title_full_unstemmed Atmospheric nitrogen deposition to forest and estuary environments in the Pearl River Delta region, southern China
title_short Atmospheric nitrogen deposition to forest and estuary environments in the Pearl River Delta region, southern China
title_sort atmospheric nitrogen deposition to forest and estuary environments in the pearl river delta region southern china
topic wet deposition
dry deposition
aqueous surface
organic nitrogen
ammonium
nitrate
url http://www.tellusb.net/index.php/tellusb/article/download/20480/pdf_1
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