Qualitative Study on the Observations of Emissions, Transport, and the Influence of Climatic Factors from Sugarcane Burning: A South African Perspective

• Published in: International journal of environmental research and public health 2021-07, Vol.18 (14), p.7672
• Main Authors: Shikwambana, Lerato, Ncipha, Xolile, Sangeetha, Sivakumar Kandasami, Sivakumar, Venkataraman, Mhangara, Paidamwoyo
• Format: Article
• Language: English
• Subjects: Aerosols; Atmosphere; Biomass; Black carbon; Burning; Carbon dioxide; Climate change; Climatic conditions; Data assimilation; Datasets; Emissions; Greenhouse gases; Plantations; Pollutants; Pollution load; Qualitative research; Spatial distribution; Sugar industry; Sugarcane; Sulfur; Sulfur dioxide; Trace gases; Vertical distribution; Wind speed
• ISSN: 1660-4601; 1661-7827; 1660-4601
• DOI: 10.3390/ijerph18147672

There are two methods of harvesting sugarcane—manual or mechanical. Manual harvesting requires the burning of the standing sugarcane crop. Burning of the crop results in the emission of aerosols and harmful trace gases into the atmosphere. This work makes use of a long-term dataset (1980–2019) to study (1) the atmospheric spatial and vertical distribution of pollutants; (2) the spatial distribution and temporal change of biomass emissions; and (3) the impact/influence of climatic factors on temporal change in atmospheric pollutant loading and biomass emissions over the Mpumalanga and KwaZulu Natal provinces in South Africa, where sugarcane farming is rife. Black carbon (BC) and sulfur dioxide (SO2) are two dominant pollutants in the JJA and SON seasons due to sugarcane burning. Overall, there was an increasing trend in the emissions of BC, SO2, and carbon dioxide (CO2) from 1980 to 2019. Climatic conditions, such as warm temperature, high wind speed, dry conditions in the JJA, and SON season, favor the intensity and spread of the fire, which is controlled. The emitted pollutants are transported to neighboring countries and can travel over the Atlantic Ocean, as far as ~6600 km from the source site.