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| Content Provider | Springer Nature Link |
|---|---|
| Author | Sharma, Mukesh Kishore, Shyam Tripathi, S. N. Behera, S. N. |
| Copyright Year | 2007 |
| Abstract | Levels of fine Particulate Matter (PM$_{fine}$), SO$_{2}$ and NO$_{x}$ are interlinked through atmospheric reactions to a large extent. NO$_{x}$, NH$_{3}$, SO$_{2}$, temperature and humidity are the important atmospheric constituents/conditions governing formation of fine particulate sulfates and nitrates. To understand the formation of inorganic secondary particles (nitrates and sulfates) in the atmosphere, a study was undertaken in Kanpur, India. Specifically, the study was designed to measure the atmospheric levels of $$ {\text{NH}}^{{\text{ + }}}_{{\text{4}}} ,\;{\text{Ca}}^{{{\text{2 + }}}} ,\;{\text{Mg}}^{{2 + }} ,\;{\text{Na}}^{{\text{ + }}} ,\;{\text{K}}^{{\text{ + }}} ,\;{\text{NO}}^{{\text{ - }}}_{{\text{3}}} ,\;{\text{SO}}^{{{\text{2 - }}}}_{{\text{4}}} ,\;{\text{CI}}^{{\text{ - }}} ,\;{\text{NH}}_{{\text{3}}} \;{\left( {{\text{gas}}} \right)},\;{\text{HNO}}_{{\text{3}}} \;{\left( {{\text{gas}}} \right)},\;{\text{NO}}_{2} \;{\text{and}}\;{\text{PM}}_{{{\text{10}}}} \;{\left( {{{\text{PM}}_{{2.5}} } \mathord{\left/ {\vphantom {{{\text{PM}}_{{2.5}} } {{\text{PM}}_{{{\text{10}}}} \;{\text{ratio}}}}} \right. -} {{\text{PM}}_{{{\text{10}}}} \;{\text{ratio}}} = 0.74} \right)} $$ covering winter and summer seasons and day and night samplings to capture the diurnal variations. Results showed $$ {\text{NO}}^{{\text{ - }}}_{{\text{3}}} ,\;{\text{SO}}^{{{\text{2 - }}}}_{{\text{4}}} ,\;{\text{NH}}^{{\text{ + }}}_{{\text{4}}} ,\;{\text{K}}^{ + } $$ are found to be significantly high in winter season compared to the summer season. In winter, the molar ratio of $$ {\text{NH}}^{{\text{ + }}}_{{\text{4}}} $$ to $$ {\text{SO}}^{{{\text{2 - }}}}_{{\text{4}}} $$ was found to be greater than 2:1. This higher molar ratio suggests that in addition to (NH$_{4}$)$_{2}$SO$_{4}$, NH$_{4}$NO$_{3}$ will be formed because of excess quantity of $$ {\text{NH}}^{{\text{ + }}}_{{\text{4}}} $$ present. In summer, the molar ratio was less than 2:1 indicating deficit of $$ {\text{NH}}^{{\text{ + }}}_{{\text{4}}} $$ to produce NH$_{4}$NO$_{3}$. The nitrogen conversion ratio (NO$_{2}$ to NO$_{3}$) was found to be nearly 50% in the study area that suggested quick conversion of NO$_{2}$ into nitric acid. As an overall conclusion, this study finds that NH$_{3}$ plays a vital role in the formation of fine inorganic secondary particles particularly so in winter months and there is a need to identify and assess sources of ammonia emissions in India. |
| Starting Page | 1 |
| Ending Page | 17 |
| Page Count | 17 |
| File Format | |
| ISSN | 01677764 |
| Journal | Journal of Atmospheric Chemistry |
| Volume Number | 58 |
| Issue Number | 1 |
| e-ISSN | 15730662 |
| Language | English |
| Publisher | Springer Netherlands |
| Publisher Date | 2007-07-17 |
| Publisher Place | Dordrecht |
| Access Restriction | One Nation One Subscription (ONOS) |
| Subject Keyword | Inorganic secondary particles Ammonia Sulfate Nitrate Water soluble ions India Atmospheric Protection/Air Quality Control/Air Pollution Meteorology/Climatology |
| Content Type | Text |
| Resource Type | Article |
| Subject | Environmental Chemistry Atmospheric Science |
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