{"title":"大气无机活性氮(Nr)在Nr排放热点城市-工业-农村样带中的湿沉降(印度)","authors":"Moh Naseem, U. C. Kulshrestha","doi":"10.1007/s10874-021-09425-w","DOIUrl":null,"url":null,"abstract":"<div><p>The present study comprehensively reports the simultaneous measurement of wet deposition of total inorganic nitrogen (TIN; which is the sum of the NH<sub>4</sub><sup>+</sup>-N and NO<sub>3</sub><sup>−</sup>-N) at three different sites in Nr emission hotspot of Indo-Gangetic plain (IGP) over a year-long temporal scale from October 2017 to September 2018. At rural Meetli (MTL) site, urban Baraut (BRT) site and industrial Loni (LNI) site, the annual wet deposition of NH<sub>4</sub><sup>+</sup>-N was estimated as 21.87, 19.48 and 7.43 kg N ha<sup>−1</sup> yr<sup>−1</sup>, respectively; the annual wet deposition NO<sub>3</sub><sup>−</sup>-N was estimated as 12.96, 12.17 and 4.44 kg N ha<sup>−1</sup> yr<sup>−1</sup>, respectively; and the annual wet deposition of TIN was estimated as 34.83, 31.64 and 11.87 kg N ha<sup>−1</sup> yr<sup>−1</sup>, respectively. NH<sub>4</sub><sup>+</sup>-N was dominantly contributing species in annual, monsoon and non-monsoon-time wet deposition of TIN at all sites. The spatial gradient (variability) in percent contribution of NH<sub>4</sub><sup>+</sup> to total annual volume-weighted mean (VWM) concentration of all analyte ions was observed as MTL (43.23%) > BRT (37.90%) > LNI (30%). On the other hand, the spatial gradient in percent contribution of NO<sub>3</sub><sup>−</sup> to total annual VWM concentration of all analyte ions was observed as MTL (7.45%) > BRT (6.89%) > LNI (5.32%). The extremely narrow range of NH<sub>4</sub><sup>+</sup>-N/NO<sub>3</sub><sup>−</sup>-N ratios (ranging from 1.60 at BRT site to 1.69 at LNI site) showed the approximately equal relative abundance of oxidized and reduced nitrogen (N) deposition across all sites. Inferences from enrichment factor analysis, principal component analysis and Pearson’s correlation coefficient analysis suggested that across all sites, virtually all NH<sub>4</sub><sup>+</sup>-N and NO<sub>3</sub><sup>−</sup>-N depositions were originated anthropogenically. The annual wet deposition of TIN measured in this study showed ≥ 6865%, ≥ 6228% and ≥ 2274% increment than the natural N deposition rate at MTL, BRT and LNI site, respectively. These empirically measured annual wet depositions of TIN also emanated theoretical transgression of critical N load threshold across all sites therefore signifying probable undermining of long-term elastic stability and resilience of ecosystems against stressor in the study domain.</p></div>","PeriodicalId":611,"journal":{"name":"Journal of Atmospheric Chemistry","volume":"78 4","pages":"271 - 304"},"PeriodicalIF":3.0000,"publicationDate":"2021-10-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://link.springer.com/content/pdf/10.1007/s10874-021-09425-w.pdf","citationCount":"0","resultStr":"{\"title\":\"Wet deposition of atmospheric inorganic reactive nitrogen (Nr) across an urban-industrial-rural transect of Nr emission hotspot (India)\",\"authors\":\"Moh Naseem, U. C. 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NH<sub>4</sub><sup>+</sup>-N was dominantly contributing species in annual, monsoon and non-monsoon-time wet deposition of TIN at all sites. The spatial gradient (variability) in percent contribution of NH<sub>4</sub><sup>+</sup> to total annual volume-weighted mean (VWM) concentration of all analyte ions was observed as MTL (43.23%) > BRT (37.90%) > LNI (30%). On the other hand, the spatial gradient in percent contribution of NO<sub>3</sub><sup>−</sup> to total annual VWM concentration of all analyte ions was observed as MTL (7.45%) > BRT (6.89%) > LNI (5.32%). The extremely narrow range of NH<sub>4</sub><sup>+</sup>-N/NO<sub>3</sub><sup>−</sup>-N ratios (ranging from 1.60 at BRT site to 1.69 at LNI site) showed the approximately equal relative abundance of oxidized and reduced nitrogen (N) deposition across all sites. 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引用次数: 0
摘要
本研究全面报道了湿沉降法测定总无机氮(TIN;为2017年10月至2018年9月印度恒河平原(IGP)三个不同地点的NH4+-N和NO3−-N在1年时间尺度上的总和。在农村Meetli (MTL)、城市Baraut (BRT)和工业Loni (LNI)样地,NH4+-N的年湿沉降量分别为21.87、19.48和7.43 kg N ha−1 yr−1;年湿沉降NO3−-N分别为12.96、12.17和4.44 kg N ha−1 yr−1;TIN的年湿沉降量分别为34.83、31.64和11.87 kg N ha−1 yr−1。NH4+-N是各站点年、季风和非季风期TIN湿沉降的主要贡献种。NH4+对所有分析离子年总体积加权平均(VWM)浓度的百分比贡献的空间梯度(变异)为MTL (43.23%) > BRT (37.90%) > LNI(30%)。另一方面,NO3−对所有分析离子年总VWM浓度的百分比贡献的空间梯度为MTL (7.45%) > BRT (6.89%) > LNI(5.32%)。NH4+-N/NO3−-N比值范围极窄(BRT站点为1.60,LNI站点为1.69),表明所有站点的氧化氮和还原氮沉积相对丰度大致相等。富集因子分析、主成分分析和Pearson相关系数分析表明,在所有研究点上,几乎所有NH4+-N和NO3−-N沉积都是人为造成的。研究中测得的TIN年湿沉降量分别比MTL、BRT和LNI站点的自然N沉降量增加≥6865%、≥6228%和≥2274%。这些经验测量的TIN的年湿沉积也在所有地点产生了临界N负荷阈值的理论突破,因此表明可能破坏研究领域生态系统对应力源的长期弹性稳定性和恢复力。
Wet deposition of atmospheric inorganic reactive nitrogen (Nr) across an urban-industrial-rural transect of Nr emission hotspot (India)
The present study comprehensively reports the simultaneous measurement of wet deposition of total inorganic nitrogen (TIN; which is the sum of the NH4+-N and NO3−-N) at three different sites in Nr emission hotspot of Indo-Gangetic plain (IGP) over a year-long temporal scale from October 2017 to September 2018. At rural Meetli (MTL) site, urban Baraut (BRT) site and industrial Loni (LNI) site, the annual wet deposition of NH4+-N was estimated as 21.87, 19.48 and 7.43 kg N ha−1 yr−1, respectively; the annual wet deposition NO3−-N was estimated as 12.96, 12.17 and 4.44 kg N ha−1 yr−1, respectively; and the annual wet deposition of TIN was estimated as 34.83, 31.64 and 11.87 kg N ha−1 yr−1, respectively. NH4+-N was dominantly contributing species in annual, monsoon and non-monsoon-time wet deposition of TIN at all sites. The spatial gradient (variability) in percent contribution of NH4+ to total annual volume-weighted mean (VWM) concentration of all analyte ions was observed as MTL (43.23%) > BRT (37.90%) > LNI (30%). On the other hand, the spatial gradient in percent contribution of NO3− to total annual VWM concentration of all analyte ions was observed as MTL (7.45%) > BRT (6.89%) > LNI (5.32%). The extremely narrow range of NH4+-N/NO3−-N ratios (ranging from 1.60 at BRT site to 1.69 at LNI site) showed the approximately equal relative abundance of oxidized and reduced nitrogen (N) deposition across all sites. Inferences from enrichment factor analysis, principal component analysis and Pearson’s correlation coefficient analysis suggested that across all sites, virtually all NH4+-N and NO3−-N depositions were originated anthropogenically. The annual wet deposition of TIN measured in this study showed ≥ 6865%, ≥ 6228% and ≥ 2274% increment than the natural N deposition rate at MTL, BRT and LNI site, respectively. These empirically measured annual wet depositions of TIN also emanated theoretical transgression of critical N load threshold across all sites therefore signifying probable undermining of long-term elastic stability and resilience of ecosystems against stressor in the study domain.
期刊介绍:
The Journal of Atmospheric Chemistry is devoted to the study of the chemistry of the Earth''s atmosphere, the emphasis being laid on the region below about 100 km. The strongly interdisciplinary nature of atmospheric chemistry means that it embraces a great variety of sciences, but the journal concentrates on the following topics:
Observational, interpretative and modelling studies of the composition of air and precipitation and the physiochemical processes in the Earth''s atmosphere, excluding air pollution problems of local importance only.
The role of the atmosphere in biogeochemical cycles; the chemical interaction of the oceans, land surface and biosphere with the atmosphere.
Laboratory studies of the mechanics in homogeneous and heterogeneous transformation processes in the atmosphere.
Descriptions of major advances in instrumentation developed for the measurement of atmospheric composition and chemical properties.