Journals / Atmospheric Pollution Research / 2016 / Cilt: 7 - Sayı: 5

Spatial variability of concentrations of gaseous pollutants across the National Capital Region of Delhi, India

Pages
808–816
DOI
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AI Summary & Key Takeaways

AI Insight
⚡ TL;DR(Too Long; Didn't Read)

Local NO emissions substantially reduced the urban ozone concentrations asseen by the observed untitrated NO concentrations.

📌 3 Key Takeaways

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Objective & Hypothesis:This study presents a systematic evaluation of a year-long, continuous, real-time measurements ofgaseous pollutants including oxides of nitrogen (NOx ¼ NO þ NO2), carbon monoxide (CO), and ozone(O3) in the National Capital Region (NCR) of Delhi.
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Key Findings & Data:The daily mean concentrations of NOx and CO across NCR of Delhi (average of all seven AMSs) were37.1 ± 11.6 ppb (NO: 18.3 and NO2: 18.8 ppb), and 2.3 ± 0.6 ppm, respectively.
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Conclusion & Impact:Local NO emissions substantially reduced the urban ozone concentrations asseen by the observed untitrated NO concentrations.
🔬Design:Research Article
📍Scope:Comprehensive Sample
⚙️Variables:Domain Parameters

Özet

This study presents a systematic evaluation of a year-long, continuous, real-time measurements ofgaseous pollutants including oxides of nitrogen (NOx ¼ NO þ NO2), carbon monoxide (CO), and ozone(O3) in the National Capital Region (NCR) of Delhi. Data are available from seven air quality monitoringstations (AMS) and meteorological parameters were measured at three meteorological observatories(MO). The daily mean concentrations of NOx and CO across NCR of Delhi (average of all seven AMSs) were37.1 ± 11.6 ppb (NO: 18.3 and NO2: 18.8 ppb), and 2.3 ± 0.6 ppm, respectively. The highest diurnal COconcentrations were observed during midnight (21:00 to 01:00 h LT) due to nocturnal boundary conditions.The daily mean O3 concentration was 37.5 ± 11.0 ppb. The diurnal variations of O3 concentrationswere characterized by the high concentrations during the daytime (07:00 to 17:00 h LT: 43.6 ppb) andlow concentrations during the late evening and early morning hours (18:00 to 06:00 h LT: 31.1 ppb).From 07:00 h onwards, the O3 concentrations start increasing gradually after sunrise coinciding with theincreasing solar radiation. The highest concentrations (51.7 ppb) were observed around 15:00 h.Thereafter, it is decreased. Local sources of gaseous pollutants were identified by analyzing the surfacewind patterns. The annual resultant wind vector were 338 (57%) and 288 (27%) at the Hindon andPalam MOs, respectively. Local NO emissions substantially reduced the urban ozone concentrations asseen by the observed untitrated NO concentrations.

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Cite This Article

TYAGİ, S., TİWARİ, S., MİSHRA, A., HOPKE, P. K., ATTRİ, S., Srivastava, A., Bisht, D. (2016). Spatial variability of concentrations of gaseous pollutants across the National Capital Region of Delhi, India. Atmospheric Pollution Research, Cilt: 7 - Sayı: 5, 808–816. https://ajindex.com/articles/351416

References (5)

  1. Ahammed, Y.N., Reddy, R.R., Gopal, K.R., Narasimhulu, K., Basha, D.B., Reddy, L.S.S., Rao, T.V.R., 2006. Seasonal variation of the surface ozone and its precursor gases during 2001e2003, measured at Anantapur (14.62N), a semi-arid site in India. Atmos. Res. 80, 151e164. Airport Authority of India (AAI). Website: www.aai.aero. (accessed on 15 Jun 2015).
  2. Andreae, M.O., Merlet, P., 2001. Emission of trace gases and aerosols from biomass burning. Glob. Biogeochem. Cycl. 15 (4), 955e966. Awasthi, A., Agarwal, R., Mittal, S.K., Singh, N., Singh, K., Gupta, P.K., 2011. Study of size and mass distribution of particulate matter due to crop residue burning with seasonal variation in rural area of Punjab, India. J. Environ. Monit. 13, 1073e1081. Badarinath, K.V.S., Kharol, S.K., Reddy, R.R., Gopal, K.R., Narasimhulu, K., Reddy, L.S.S., Kumar, K.R., 2009. Black carbon aerosol mass concentration variation in urban and rural environments of India e a case study. Atmos. Sci. Lett. 10, 29e33. Beig, G., Chate, D.M., Ghude, S.D., Mahajan, A.S., Srinivas, R., Ali, K., Sahu, S.K., Parkhi, N., Surendran, D., Trimbake, H.R., 2013. Quantifying the effect of air quality control measures during the 2010
  3. Commonwealth Games at Delhi, India. Atmos. Environ. 80, 455e463. Beig, G., Gunthe, S., Jadhav, D.B., 2007. Simultaneous measurements of ozone and its precursors on a diurnal scale at a semi urban site in India. J. Atmos. Chem. 57 (3), 239e253. http://dx.doi.org/10.1007/s10874-007-9068-8. Centre for Science and Environment (CSE), 2012. Report Published in the Hindu (05.06.2012). http://www.cseindia.org/content/world-environment-daycsewarns-Delhi%E2%80%99s-air-pollution-and-congestion-crisis-will.worsendeca. Census of India, 2011. http://www.censusindia.gov.in/2011-prov-results/data-files/ delhi/2-PDFC-Paper-1-major-trends-44-59.pdf. Central Pollution Control Board(CPCB), 2012. National Ambient Air Quality Status and Trends in India Ministry of Environment and Forests. NAAQMS/35/2011- 2012.
  4. Chatfield, R.B., Delany, A.C., 1990. Convection links biomass burning to increased tropical ozone: however, models will tend to overpredict O3. J. Geophys. Res. 95 (No. D ll), 18,473e18,488. October 20. Chelani, A.B., 2012.
  5. Persistence analysis of extreme CO, NO2 and O3 concentrations in ambient air of Delhi. Atmos. Res. 108, 128e134. Crutzen, P.J., Lawrence, M.J., Poschl, U., 1999. On the background photochemistry of tropospheric ozone. Tellus 51A-B, 123e146. Delhi Statistical Hand Book, 2014. Di