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Stable carbon and nitrogen isotopic composition of PM10 over Indo-Gangetic Plains (IGP), adjoining regions and Indo-Himalayan Range (IHR) during a winter 2014 campaign

机译:在2014年冬季活动期间,在印度难潮平原(IGP),相邻的地区和Indo-Himalayan范围(IHR)稳定的PM10稳定的碳和氮同位素组成

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摘要

For source identification, a field campaign involving simultaneous sampling of particulate matter ( PM10) was conducted at eight sampling sites in the Indian mainland during winter 2014. The sampling sites include Delhi ( upper IGP), Lucknow ( middle IGP), and Kolkata ( lower IGP) in the Indo-Gangetic Plains ( IGP); Mohal-Kullu and Darjeeling in the Indo-Himalayan Range ( IHR). In addition, Ajmer, located upwind of the IGP in NW-India and Giridih and Bhubaneswar, in the downwind to the IGP has also been chosen. To characterize the sources of the ambient PM10, stable isotope ratios of carbon ( d13CTC) and nitrogen ( d15NTN) for the total carbon ( TC) and total nitrogen ( TN) fractions have been considered. Ancillary chemical parameters, such as organic carbon ( OC), elemental carbon ( EC), and watersoluble ionic components ( WSIC) mass concentrations are also presented in this paper. There was very small variation in the daily average d13CTC ratios (-24.8 to -25.9%) among the sites. Comparison with end-member stable C isotopic signatures of major typical sources suggests that the PM10 at the sites was mainly from fossil fuel and biofuel and biomass combustion. Daily average d15NTN ratios were not observed to vary much between sites either ( 8.3 to 11.0%), and the low d15NTN levels also indicate substantial contributions from biofuel and biomass burning of primarily C3 andC4 plant matter.
机译:对于源识别,在2014年冬季在印度大陆的八个取样位点进行涉及颗粒物质(PM10)的实地运动。采样点包括德里(上IGP),勒克瑙(中间IGP)和加尔各答(下IGP)在印度热链(IGP)中; Mohal-Kullu和Darjeeling在Indo Himalayan范围(IHR)。此外,还选择了在NW-India和Giridih和Bhubaneswar的IGP逆向IGP的AJMER,也被选中了在向IGP的顺风中进行。为了表征环境PM10的来源,已经考虑了总碳(TC)和总氮(TN)级分的稳定同位素比率和氮(D15NTN)和总氮(TN)级分。本文还介绍了辅助化学参数,如有机碳(OC),元素碳(EC)和水溶性离子组分(WSIC)质量浓度。在场地之间的每日平均D13CTC比率(-24.8至-25.9%)存在非常小的变化。与最终成员稳定的C同位素特征的比较主要典型来源表明,该地点的PM10主要来自化石燃料和生物燃料和生物量燃烧。未观察到每日平均D15NTN比率(8.3至11.0%)之间的差异很大,并且低D15NTN水平也表明了从生物燃料和生物量燃烧的大量贡献主要是C3和​​型植物。

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