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| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Satsangi, P Gursumeeran | - |
| dc.contributor.author | Chavan, Suresh P | - |
| dc.contributor.author | Rao, P S P | - |
| dc.contributor.author | Safai, P D | - |
| dc.date.accessioned | 2014-11-28T13:24:43Z | - |
| dc.date.available | 2014-11-28T13:24:43Z | - |
| dc.date.issued | 2014-08 | - |
| dc.identifier.issn | 0975-105X (Online); 0367-8393 (Print) | - |
| dc.identifier.uri | http://hdl.handle.net/123456789/30001 | - |
| dc.description | 284-292 | en_US |
| dc.description.abstract | Particulate matter, PM10 and PM2.5, samples were collected at Sinhagad, a high altitude location, near Pune, India during November 2008 - April 2009. The average concentrations of PM10, PM2.5 and PM10-2.5 at Sinhagad were 35.8, 14.1 and 21.7 µg m-3, respectively. The average ratio of PM2.5/PM10 (0.39) suggested that PM10 at study area is dominated by primary particulate emissions by natural activities. In PM10, anions and cations contributed 33% and 67%, whereas in PM2.5, these were 43% and 57%. In both PM10 and PM2.5, contribution of marine components, viz. Na+, Cl- and Mg2+ were found to be 58% and 49%, respectively reflecting Arabian Sea is the major source of these components. All the ionic components in PM10 showed higher concentration in summer, whereas in PM2.5, secondary particles (SO42-, NO3- and NH4+) showed higher concentration in winter. The order of neutralization factor was found to be Ca2+ > Mg2+ > NH4+ > K+ for PM10; and Ca2+ > NH4+ > Mg2+ > K+ for PM2.5. Source categorization, i.e. marine, crustal and anthropogenic of chemical components of PM has been done. Sea salt and crustal fractions have been calculated by assuming entire Na and Ca from Sea and crust, respectively. The fraction of the chemical component, which remains after deducting the sea and crust fractions, has been considered as of anthropogenic origin. Major contribution observed was from marine sources [PM2.5 (43%) and PM10 (53%)]; followed by crustal sources [PM2.5 (25%) and PM10 (30%)]; and then anthropogenic sources [(PM2.5 (32%) and PM10 (17%)]. | en_US |
| dc.language.iso | en_US | en_US |
| dc.publisher | NISCAIR-CSIR, India | en_US |
| dc.relation.ispartof | 92.60.Sz; 82.33.Tb | en_US |
| dc.rights | CC Attribution-Noncommercial-No Derivative Works 2.5 India | en_US |
| dc.source | IJRSP Vol.43(4-5) [August-October 2014] | en_US |
| dc.subject | Particulate matter | en_US |
| dc.subject | Chemical composition | en_US |
| dc.subject | Air pollution | en_US |
| dc.subject | Aerosol | en_US |
| dc.title | Chemical characterization of particulate matter at Sinhagad, a high altitude station in Pune, India | en_US |
| dc.type | Article | en_US |
| Appears in Collections: | IJRSP Vol.43(4-5) [August-October 2014] | |
Files in This Item:
| File | Description | Size | Format | |
|---|---|---|---|---|
| IJRSP 43(4-5) 284-292.pdf | 695.08 kB | Adobe PDF | View/Open |
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