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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

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dc.contributor.author Sen, A.
dc.contributor.author Karapurkar, S.G.
dc.contributor.author Saxena, M.
dc.contributor.author Shenoy, D.M.
dc.contributor.author Chaterjee, A.
dc.contributor.author Choudhuri, A.K.
dc.contributor.author Das, T.
dc.contributor.author Khan, A.H.
dc.contributor.author Kuniyal, J.C.
dc.contributor.author Pal, S.
dc.contributor.author Singh, D.P.
dc.contributor.author Sharma, S.K.
dc.contributor.author Kotnala, R.K.
dc.contributor.author Mandal, T.K.
dc.date.accessioned 2018-12-17T10:34:04Z
dc.date.available 2018-12-17T10:34:04Z
dc.date.issued 2018
dc.identifier.citation Environmental Science And Pollution Research, 25(26), 2018: 26279-26296
dc.identifier.issn 0944-1344
dc.identifier.uri http://ore.immt.res.in/handle/2018/2401
dc.description Indian Statistical Institute; HRDG, CSIR; CSIR-IMMT; Environment, and Sustainability Department of CSIR-IMMT
dc.description.abstract 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.
dc.language en
dc.publisher Springer
dc.relation.isreferencedby SCI
dc.rights Copyright [2018]. All efforts have been made to respect the copyright to the best of our knowledge. Inadvertent omissions, if brought to our notice, stand for correction and withdrawal of document from this repository.
dc.subject Interdisciplinary Sciences
dc.title 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
dc.type Journal Article
dc.affiliation.author CSIR-National Physical Laboratory, New Delhi 110012, India


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