Impact of crop residue burning in Haryana on the air quality of Delhi, India

Pallavi Saxena; Saurabh Sonwani; Ananya Srivastava; Madhavi Jain; Anju Srivastava; Akash Bharti; Deepali Rangra; Nancy Mongia; Shweta Tejan; Shreshtha Bhardwaj

doi:10.1016/j.heliyon.2021.e06973

Impact of crop residue burning in Haryana on the air quality of Delhi, India

Heliyon. 2021 May 7;7(5):e06973. doi: 10.1016/j.heliyon.2021.e06973. eCollection 2021 May.

Authors

Affiliations

¹ Department of Environmental Sciences, Hindu College, University of Delhi, Delhi, India.
² Department of Environmental Studies, Zakir Husain Delhi College, University of Delhi, New Delhi, India.
³ Department of Economics, Hindu College, University of Delhi, Delhi, India.
⁴ School of Environmental Sciences, Jawaharlal Nehru University, New Delhi, India.
⁵ Department of Chemistry, Hindu College, University of Delhi, Delhi, India.
⁶ Department of Mathematics, Hindu College, University of Delhi, Delhi, India.
⁷ Department of Physical Science Chemistry, Hindu College, University of Delhi, Delhi, India.

Abstract

Crop residue burning (CRB) over northern India is a major air quality and human health issue. The present study assesses the impact of PM₁₀, PM_2.5, NO₂ and SO₂, emitted during CRB activities in Haryana on the air quality of Delhi. The transition from pre-burning to burning period, in both rabi and kharif seasons, shows considerable increase in pollutant concentrations. PM₁₀ and PM_2.5 concentrations exceeded NAAQS limits by 2-3 times, while NO₂ and SO₂ stayed within the limits. MODIS fire observations used to estimate CRB fire counts (confidence ≥80%) shows that rabi (burning period) fires in Haryana are ~3 times higher and more intense than in kharif. Furthermore, backward trajectories shows air mass movement from Haryana, Punjab and Pakistan. Thus, pollutants emitted reach Delhi via air masses, deteriorating its air quality. Meteorological conditions influence pollutant concentrations during both seasons. Frequent dust storms in rabi, and Dusshera and Diwali firework celebrations in kharif season exacerbate air pollution. In rabi, PM₁₀ and PM_2.5 have a significant negative association with (relative humidity) RH and positive association with (air temperature) AT. High AT during pre-monsoon, accompanied by low RH, loosens up soil particles and they can easily disperse. Stronger winds in rabi season promote NO₂ and SO₂ dispersion. In kharif, lower AT, higher RH and slower winds exist. Both PM₁₀ and PM_2.5 have a negative association with AT and (wind speed) WS. With lower temperature and slower winds during winter, pollutants are trapped within the boundary layer and are unable to disperse. As expected, NO₂ has a significant negative association with AT in Haryana. However, in case of Delhi, the association is significant but positive, and could be due to the odd-even scheme imposed by the Delhi government. More research is needed to determine the health effects of Haryana's rabi CRB activities on Delhi.

Keywords: Air mass movement; Biomass burning; Kharif; Meteorology; Rabi.