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
For source identification, a field campaign involving simultaneous sampling of particulate matter (PM 10 ) 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...
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creator | Sen, Avirup Karapurkar, Supriya G. Saxena, Mohit Shenoy, Damodar M. Chaterjee, Abhijit Choudhuri, Anil K. Das, Trupti Khan, Altaf H. Kuniyal, Jagdish Chandra Pal, Srimata Singh, Dharam Pal Sharma, Sudhir Kumar Kotnala, Ravindra Kumar Mandal, Tuhin Kumar |
description | For source identification, a field campaign involving simultaneous sampling of particulate matter (PM
10
) 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 PM
10
, stable isotope ratios of carbon (δ
13
C
TC
) and nitrogen (δ
15
N
TN
) 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 water-soluble ionic components (WSIC) mass concentrations are also presented in this paper. There was very small variation in the daily average δ
13
C
TC
ratios (− 24.8 to − 25.9‰) among the sites. Comparison with end-member stable C isotopic signatures of major typical sources suggests that the PM
10
at the sites was mainly from fossil fuel and biofuel and biomass combustion. Daily average δ
15
N
TN
ratios were not observed to vary much between sites either (8.3 to 11.0‰), and the low δ
15
N
TN
levels also indicate substantial contributions from biofuel and biomass burning of primarily C3 andC4 plant matter.
Graphical abstract
Scatter plot of the average (± 1 standard deviation (SD)) δ
13
C
TC
(‰) compared to δ
15
N
TN
(‰) at the sampling sites. |
doi_str_mv | 10.1007/s11356-018-2567-0 |
format | Article |
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10
) 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 PM
10
, stable isotope ratios of carbon (δ
13
C
TC
) and nitrogen (δ
15
N
TN
) 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 water-soluble ionic components (WSIC) mass concentrations are also presented in this paper. There was very small variation in the daily average δ
13
C
TC
ratios (− 24.8 to − 25.9‰) among the sites. Comparison with end-member stable C isotopic signatures of major typical sources suggests that the PM
10
at the sites was mainly from fossil fuel and biofuel and biomass combustion. Daily average δ
15
N
TN
ratios were not observed to vary much between sites either (8.3 to 11.0‰), and the low δ
15
N
TN
levels also indicate substantial contributions from biofuel and biomass burning of primarily C3 andC4 plant matter.
Graphical abstract
Scatter plot of the average (± 1 standard deviation (SD)) δ
13
C
TC
(‰) compared to δ
15
N
TN
(‰) at the sampling sites.</description><identifier>ISSN: 0944-1344</identifier><identifier>EISSN: 1614-7499</identifier><identifier>DOI: 10.1007/s11356-018-2567-0</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Aquatic Pollution ; Atmospheric Protection/Air Quality Control/Air Pollution ; Biodiesel fuels ; Biofuels ; Biomass ; Biomass burning ; Burning ; Carbon ; combustion ; Earth and Environmental Science ; Ecotoxicology ; Environment ; Environmental Chemistry ; Environmental Health ; Environmental science ; Fossil fuels ; India ; Indo-Gangetic Plain ; Isotope ratios ; Isotopes ; Nitrogen ; Organic carbon ; Organic chemistry ; Particulate emissions ; Particulate matter ; particulates ; Research Article ; Sampling ; Stable isotopes ; standard deviation ; total nitrogen ; Waste Water Technology ; Water Management ; Water Pollution Control ; water solubility ; Winter</subject><ispartof>Environmental science and pollution research international, 2018-09, Vol.25 (26), p.26279-26296</ispartof><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2018</rights><rights>Environmental Science and Pollution Research is a copyright of Springer, (2018). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c419t-8c8922112eab044a7fa0b70ff6334c4e80e573527419e054f5aea1f53f6f54ce3</citedby><cites>FETCH-LOGICAL-c419t-8c8922112eab044a7fa0b70ff6334c4e80e573527419e054f5aea1f53f6f54ce3</cites><orcidid>0000-0003-0142-1512</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11356-018-2567-0$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11356-018-2567-0$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Sen, Avirup</creatorcontrib><creatorcontrib>Karapurkar, Supriya G.</creatorcontrib><creatorcontrib>Saxena, Mohit</creatorcontrib><creatorcontrib>Shenoy, Damodar M.</creatorcontrib><creatorcontrib>Chaterjee, Abhijit</creatorcontrib><creatorcontrib>Choudhuri, Anil K.</creatorcontrib><creatorcontrib>Das, Trupti</creatorcontrib><creatorcontrib>Khan, Altaf H.</creatorcontrib><creatorcontrib>Kuniyal, Jagdish Chandra</creatorcontrib><creatorcontrib>Pal, Srimata</creatorcontrib><creatorcontrib>Singh, Dharam Pal</creatorcontrib><creatorcontrib>Sharma, Sudhir Kumar</creatorcontrib><creatorcontrib>Kotnala, Ravindra Kumar</creatorcontrib><creatorcontrib>Mandal, Tuhin Kumar</creatorcontrib><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</title><title>Environmental science and pollution research international</title><addtitle>Environ Sci Pollut Res</addtitle><description>For source identification, a field campaign involving simultaneous sampling of particulate matter (PM
10
) 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 PM
10
, stable isotope ratios of carbon (δ
13
C
TC
) and nitrogen (δ
15
N
TN
) 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 water-soluble ionic components (WSIC) mass concentrations are also presented in this paper. There was very small variation in the daily average δ
13
C
TC
ratios (− 24.8 to − 25.9‰) among the sites. Comparison with end-member stable C isotopic signatures of major typical sources suggests that the PM
10
at the sites was mainly from fossil fuel and biofuel and biomass combustion. Daily average δ
15
N
TN
ratios were not observed to vary much between sites either (8.3 to 11.0‰), and the low δ
15
N
TN
levels also indicate substantial contributions from biofuel and biomass burning of primarily C3 andC4 plant matter.
Graphical abstract
Scatter plot of the average (± 1 standard deviation (SD)) δ
13
C
TC
(‰) compared to δ
15
N
TN
(‰) at the sampling sites.</description><subject>Aquatic Pollution</subject><subject>Atmospheric Protection/Air Quality Control/Air Pollution</subject><subject>Biodiesel fuels</subject><subject>Biofuels</subject><subject>Biomass</subject><subject>Biomass burning</subject><subject>Burning</subject><subject>Carbon</subject><subject>combustion</subject><subject>Earth and Environmental Science</subject><subject>Ecotoxicology</subject><subject>Environment</subject><subject>Environmental Chemistry</subject><subject>Environmental Health</subject><subject>Environmental science</subject><subject>Fossil fuels</subject><subject>India</subject><subject>Indo-Gangetic Plain</subject><subject>Isotope ratios</subject><subject>Isotopes</subject><subject>Nitrogen</subject><subject>Organic carbon</subject><subject>Organic chemistry</subject><subject>Particulate emissions</subject><subject>Particulate matter</subject><subject>particulates</subject><subject>Research Article</subject><subject>Sampling</subject><subject>Stable isotopes</subject><subject>standard deviation</subject><subject>total nitrogen</subject><subject>Waste Water Technology</subject><subject>Water Management</subject><subject>Water Pollution Control</subject><subject>water solubility</subject><subject>Winter</subject><issn>0944-1344</issn><issn>1614-7499</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNqFkV1rFDEUhoMouFZ_gHcBb1ow9SSTj5lLKXZ3ocWlrdchm02GLLPJmMxa-ov8m2a6giCIV-fmeV7OOS9C7ylcUgD1qVDaCEmAtoQJqQi8QAsqKSeKd91LtICOc0Ibzl-jN6XsARh0TC3Qz_vJbAeHrcnbFLGJOxzDlFPvIg4lTWkMFtt0GFMJU6hE8nhzSwGnHy7jddwlsjSxd1PFNoMJseDz9XJz8RGb3T6FGGKPs-urWZ7Dn41VOJjBPJmI72a3Gqu7C7w75pk2-DHEqYYzoLzudRhN6ONb9Mqbobh3v-cZ-nb95eFqRW6-LtdXn2-I5bSbSGvbjjFKmTNb4Nwob2CrwHvZNNxy14ITqhFMVdqB4F4YZ6gXjZdecOuaM3R-yh1z-n50ZdKHUKwbBhNdOhZds2XHWhDs_yhIyZUUXFT0w1_oPh1zrIfMFBdKsY5Xip4om1Mp2Xk95vqp_KQp6LllfWpZ15b13LKG6rCTU8b5ey7_Sf639AuL4KhE</recordid><startdate>20180901</startdate><enddate>20180901</enddate><creator>Sen, Avirup</creator><creator>Karapurkar, Supriya G.</creator><creator>Saxena, Mohit</creator><creator>Shenoy, Damodar M.</creator><creator>Chaterjee, Abhijit</creator><creator>Choudhuri, Anil K.</creator><creator>Das, Trupti</creator><creator>Khan, Altaf H.</creator><creator>Kuniyal, Jagdish Chandra</creator><creator>Pal, Srimata</creator><creator>Singh, Dharam Pal</creator><creator>Sharma, Sudhir Kumar</creator><creator>Kotnala, Ravindra Kumar</creator><creator>Mandal, Tuhin Kumar</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature 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carbon and nitrogen isotopic composition of PM10 over Indo-Gangetic Plains (IGP), adjoining regions and Indo-Himalayan Range (IHR) during a winter 2014 campaign</title><author>Sen, Avirup ; Karapurkar, Supriya G. ; Saxena, Mohit ; Shenoy, Damodar M. ; Chaterjee, Abhijit ; Choudhuri, Anil K. ; Das, Trupti ; Khan, Altaf H. ; Kuniyal, Jagdish Chandra ; Pal, Srimata ; Singh, Dharam Pal ; Sharma, Sudhir Kumar ; Kotnala, Ravindra Kumar ; Mandal, Tuhin Kumar</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c419t-8c8922112eab044a7fa0b70ff6334c4e80e573527419e054f5aea1f53f6f54ce3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>Aquatic Pollution</topic><topic>Atmospheric Protection/Air Quality Control/Air Pollution</topic><topic>Biodiesel fuels</topic><topic>Biofuels</topic><topic>Biomass</topic><topic>Biomass burning</topic><topic>Burning</topic><topic>Carbon</topic><topic>combustion</topic><topic>Earth and Environmental Science</topic><topic>Ecotoxicology</topic><topic>Environment</topic><topic>Environmental Chemistry</topic><topic>Environmental Health</topic><topic>Environmental science</topic><topic>Fossil fuels</topic><topic>India</topic><topic>Indo-Gangetic Plain</topic><topic>Isotope ratios</topic><topic>Isotopes</topic><topic>Nitrogen</topic><topic>Organic carbon</topic><topic>Organic chemistry</topic><topic>Particulate emissions</topic><topic>Particulate matter</topic><topic>particulates</topic><topic>Research Article</topic><topic>Sampling</topic><topic>Stable isotopes</topic><topic>standard deviation</topic><topic>total nitrogen</topic><topic>Waste Water Technology</topic><topic>Water Management</topic><topic>Water Pollution Control</topic><topic>water solubility</topic><topic>Winter</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Sen, 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international</jtitle><stitle>Environ Sci Pollut Res</stitle><date>2018-09-01</date><risdate>2018</risdate><volume>25</volume><issue>26</issue><spage>26279</spage><epage>26296</epage><pages>26279-26296</pages><issn>0944-1344</issn><eissn>1614-7499</eissn><abstract>For source identification, a field campaign involving simultaneous sampling of particulate matter (PM
10
) 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 PM
10
, stable isotope ratios of carbon (δ
13
C
TC
) and nitrogen (δ
15
N
TN
) 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 water-soluble ionic components (WSIC) mass concentrations are also presented in this paper. There was very small variation in the daily average δ
13
C
TC
ratios (− 24.8 to − 25.9‰) among the sites. Comparison with end-member stable C isotopic signatures of major typical sources suggests that the PM
10
at the sites was mainly from fossil fuel and biofuel and biomass combustion. Daily average δ
15
N
TN
ratios were not observed to vary much between sites either (8.3 to 11.0‰), and the low δ
15
N
TN
levels also indicate substantial contributions from biofuel and biomass burning of primarily C3 andC4 plant matter.
Graphical abstract
Scatter plot of the average (± 1 standard deviation (SD)) δ
13
C
TC
(‰) compared to δ
15
N
TN
(‰) at the sampling sites.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s11356-018-2567-0</doi><tpages>18</tpages><orcidid>https://orcid.org/0000-0003-0142-1512</orcidid></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0944-1344 |
ispartof | Environmental science and pollution research international, 2018-09, Vol.25 (26), p.26279-26296 |
issn | 0944-1344 1614-7499 |
language | eng |
recordid | cdi_proquest_miscellaneous_2116928052 |
source | SpringerLink Journals - AutoHoldings |
subjects | Aquatic Pollution Atmospheric Protection/Air Quality Control/Air Pollution Biodiesel fuels Biofuels Biomass Biomass burning Burning Carbon combustion Earth and Environmental Science Ecotoxicology Environment Environmental Chemistry Environmental Health Environmental science Fossil fuels India Indo-Gangetic Plain Isotope ratios Isotopes Nitrogen Organic carbon Organic chemistry Particulate emissions Particulate matter particulates Research Article Sampling Stable isotopes standard deviation total nitrogen Waste Water Technology Water Management Water Pollution Control water solubility Winter |
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 |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-28T19%3A54%3A08IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Stable%20carbon%20and%20nitrogen%20isotopic%20composition%20of%20PM10%20over%20Indo-Gangetic%20Plains%20(IGP),%20adjoining%20regions%20and%20Indo-Himalayan%20Range%20(IHR)%20during%20a%20winter%202014%20campaign&rft.jtitle=Environmental%20science%20and%20pollution%20research%20international&rft.au=Sen,%20Avirup&rft.date=2018-09-01&rft.volume=25&rft.issue=26&rft.spage=26279&rft.epage=26296&rft.pages=26279-26296&rft.issn=0944-1344&rft.eissn=1614-7499&rft_id=info:doi/10.1007/s11356-018-2567-0&rft_dat=%3Cproquest_cross%3E2116928052%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2064577294&rft_id=info:pmid/&rfr_iscdi=true |