2.1. Agricultural Open Field Biomass Burning in China
Biomass burning is the burning of living and dead vegetation, including anthropogenic burning and natural fires [
8]. Ninety percent of all biomass-burning is thought to be human initiated [
8]. Anthropogenic burning is used in many applications, such as agricultural expansion, weed and residue burning, and harvesting practices. Natural fires include forest and grassland fires, caused by lighting [
8]. Globally, it is estimated that 8700 Tg of dry matter is burnt each year [
7]. China is one of the greatest sources of biomass burning emissions [
14], predominantly due to anthropogenic burning such as post-harvest agricultural open field biomass burning. A previous study has estimated that about 122 Tg of crop residues are burned annually in China [
14]. Since 1997, a series of regulations and laws to prohibit field burning were enacted by the Chinese government [
2]. Farmers were encouraged to return crop residue to agricultural soils as fertilizer. However, despite these prohibitive laws, changes in practice were not widely adopted by farmers. For example, about 43% of crop residue was burned in the field in Suqian according to field investigations from 2001 to 2005 [
21].
In China, crop residue burning accounts for a major part of total biomass burning [
2]. There are several reasons for this. Firstly, China is an agricultural country, and produces large amounts of crop residue every year. Secondly, due to the high cost of straw collection, and limited room for straw storage, open field burning is the most effective option of all treatments. Finally, mechanized harvesting is another reason for crop residue burning in the field [
21,
22]. After mechanized harvesting, the height of the stubble left in the fields is about 30 cm, making sowing difficult. Fragments are scattered throughout the field, making recovery difficult and reducing the potential for reuse as an industrial raw material.
Crop residue burning has an obvious spatial and temporal pattern in China. Based on the daily fire point derived from MODIS from 2002 to 2015, fire peak month and intensity were documented by Zhong et al. [
23]. Most of the burning was observed in Eastern China. Previous studies also demonstrated that the North China Plain, Northeastern China and South China were the most important contributors to crop open burning in fields [
17]. More than 80% of the agricultural burnings were in the agricultural regions, such as Anhui, Jiangsu, Shandong and Henan Provinces [
10]. The temporal pattern of crop open burning is significantly associated with local sowing and harvest timing. In Mainland China, there were two distinct peaks corresponding to the summer and autumn harvest periods, especially in June and October [
10]. The annual percentages of fires that occurred in June and October were 61–86% and 5–14%, respectively, according to active fire products derived from MODIS from 2009 to 2010 [
10]. In the Northern China Plain, over 75% of the annual fires occurred in June, with another smaller peak in early October [
17].
Besides the obvious spatial and temporal patterns, emissions of gaseous pollutants and aerosol particles from biomass burning also have distinct aerosol characteristics. Emissions from biomass burning are known as a source of greenhouse gases such as carbon dioxide, methane, and nitrous oxide. Furthermore, aerosols emitted from biomass burning have high mass concentrations of PM
2.5 (particles smaller than 2.5 μm in diameters), OC (organic carbon), EC (elemental carbon) and K (potassium) [
24]. Reports suggest that approximately 50–70% of the mass of all particle emissions from biomass burning is carbon, with OC and EC accounting for 55% and 8% of fine particle mass, respectively [
25]. Trace inorganic species, mostly dominated by K, Cl (chlorine) and Ca (calcium), account for approximately 10% of the mass of fresh smoke [
25]. In China, the PM mass concentrations tend to be higher in winter, due to the high coal consumption [
26]. The emissions of OC, EC and PM have two peaks, in May to June and October, after the harvesting of crops. Because the two periods are times of important agricultural activities, the increase of biomass burning, fertilizer and other agricultural activities during this time contributes a great amount of OC, EC and PM [
26]. The sensitivity of gaseous pollutants and aerosol particle emissions from biomass burning to air quality was also simulated by Zhong et al. [
27]. Their results suggest that the improvement of provincial-level emissions estimation of primary PM, SO
2 and NO
X should be considered in future studies.
Estimates of the effects of biomass burning on regional haze and air quality are based on emission inventories of agricultural straw burning. The emission inventory was calculated by multiplying the total amount of crop residue burnt by the corresponding emission factors. Methods for establishing an emission inventory include a bottom-up approach and a top-down approach [
22]. The difference between the two approaches is the calculation of amount of crop residue burnt. In the bottom-up approach, the total amount of crop residue burnt was based on statistical data (e.g., product of crop production, residue-to-production ratio, dry matter-to-crop residue ratio, the percentage of dry matter burned in fields, etc.), whereas the top-down approach was based on satellite data. There are also two approaches about satellite data, one is based on the burned area, and the other is based on FRP. However, each of the methods has some limitations. Statistical data acquisition requires more time to analyze the collection of agricultural straw products, burnt fraction and burnt efficiency data, while satellite data perform poorly for small fires, especially for burned-area-based approach. Indoor biofuel burning and open field burning with a smaller area was not detected by satellite. FRP-based approach was developed in the past few years; it can calculate biomass burning emission inventory with higher temporal and spatial resolution, which is more suitable for model users. Nonetheless, the emission inventory is important for estimating the effect of agricultural residue burning on air quality and climate change [
11].
2.2. Relationship between Biomass Burning and Regional Haze
Haze is defined as an air clarity phenomenon when visibility is less than 10 km, caused by dry and invisible airborne fine particles according to the criteria prescribed by the China Meteorological Administration [
28]. Biomass burning was the major contributor of local particulate matter, surface ozone, and regional haze [
29]. Under economic development, fossil fuel consumption has also been increasing, and domestic biofuel has been decreasing in rural regions. As a result, the demand of fuel is lower, and more agricultural crop biomass is burned directly in the field [
10]. Agricultural open field crop burning can result in intense local and regional haze and environmental pollution episodes, and can even affect climate change. A previous study documented that crop residue burning was responsible for intensive air pollution during harvest season [
30]. The relationship between biomass burning and regional haze can be deduced from their temporal and spatial pattern and chemical composition over China.
Both biomass burning and regional haze show obvious temporal patterns. In general, aerosol concentrations tend to be higher in winter and lower in summer [
31], with a secondary peak in spring [
31]. Because of the increasing aerosol concentrations, the air quality has been deteriorating and hazy condition has been increasing in the past decades [
26]. Regional haze is more frequent in winter and spring, and less frequent in summer [
32], due to both increasing aerosol emissions from heating and stable atmospheric stratification in winter. However, previous studies indicated that crop burning emits large quantities of particulate matter and gaseous pollutants, and can seriously deteriorate air quality during the harvest season, especially in autumn [
33]. Several active fires were detected in most parts of China during the harvest season [
30], likely due to the common management practice of tilling directly after burning. Notably, in the past few years, October and June are the two months when both biomass burning and regional haze occurred in Northeastern China and Southeastern China, respectively [
10]. In October, large quantities of gaseous pollutants and aerosol particles were emitted into the atmosphere during biomass burning episodes, and the stable atmospheric stratification prevented short term dispersion [
10]; as a result, a regional haze event occurred after the biomass burning period.
Based on the surface visibility observations at meteorological stations in China, four major haze areas are identified: (1) Hua Bei Plain in Northern China, and the Guanzhong Plain; (2) Eastern China with the main body in the Yangtze River Delta area; (3) Southern China with most areas of Guangdong and the Pearl River Delta area; and (4) the Sichuan Basin in Southwestern China [
26]. (Furthermore, Northeastern China has two sub-regions: the major grain producing area mainly in Heilongjiang Province and an old industrial region mainly in Liaoning Province; these could comprise a fifth regional haze area. Northeastern China and the North China Plain are often reported to suffer from heavy regional air pollution during harvest season. Increased crop residue burning is likely to be one of the reasons for an increase in regional haze in Northeastern China. A previous paper documented that Heilongjiang Province (in Northeastern China) was one of three high-density biomass burning regions [
34,
35]. Lower population and a large area of crop land in Heilongjiang Province caused most agricultural biomass to be disposed of by open burning in the field. In summary, the major regional haze distribution is focused in Eastern China, consistent with fire distribution in China.
While temporal and spatial patterns of agricultural burning and regional haze show the same trends, the chemical compositions of particles are another key parameter for estimating the effects of biomass burning on regional haze. Firstly, both biomass burning and regional haze are dominated by fine particles. Approximately 90% of particles emitted from biomass burning are PM
2.5 [
36]. A previous study revealed that atmospheric particles, especially fine particles from wheat straw burning in Northern China Plain, exert considerable influence on Beijing air quality [
37]. Secondly, chemical compositions of particles emitted from agricultural straw burning contained notable amounts of some elements such as K and C. Previous studies have demonstrated that the combustion-derived particles emitted from wheat are enriched in K and Cl, whereas the particles emitted from rice are largely carbonaceous [
38]. Some fraction indicators were selected for assessing the relationship between biomass burning and regional haze. In general, high PM
2.5/PM
10, OC/EC, and K/EC ratios were indices for biomass burning [
9,
24]. High ratios of PM
10/SO
2 and CO/SO
2 showed that air quality was heavily impacted by wheat straw burning, and these ratios can be employed as indicators of the contribution of wheat straw burning to the degradation of Beijing air quality [
37].
Here, we focus on Changchun City as a case study. There are two reasons for choosing Changchun City: (1) it lies in a high-frequency fire region, and suffers from regional haze; and (2) fire locations and PM
2.5 concentrations can be monitored simultaneously. PM
2.5 concentrations, fire points, temperature and precipitation during harvesting season and the regional haze period in Changchun City in 2014 and 2015 are shown in
Figure 1. The PM
2.5 concentrations were downloaded from Air Quality Online Monitoring of China [
39]. There are 10 measurement stations in Changchun for long time online monitoring. The fire points were derived from the NASA Earth Observatory’s Active Fire Data [
40]. In general, harvesting season was from 1 October to 10 November, with biomass burning occurring one week later than harvesting. The PM
2.5 concentrations and fire points presented same temporal pattern both in 2014 and 2015 (
Figure 1).
Figure 1 shows a high PM
2.5 concentration during biomass burning. The PM
2.5 concentration peak in 2015 was later than that in 2014, due to the later harvesting and biomass burning in 2015. PM
2.5 concentrations and fire points were lower in 2015 compared with 2014, because of serious prohibition of biomass burning and collection of agricultural residue by the local government in 2015. Nevertheless, a strong peak occurred on 9 November, because most agricultural residue was abandoned in the fields waiting for collection, while weather reports predicted heavy snow on the night of 9 November. If the agricultural residues were not burned before the heavy snow, they would have remained in the field until next spring, thereby delay sowing. Consequently, most farmers burned the residue before 9 November in order to dispose of the residue in time, resulting the emission of large quantities of particulate matter and pollutant gases into the atmosphere in one day. This triggered a regional haze event. Besides biomass burning emission, the weather conditions (temperature and precipitation) between 2014 and 2015 were the same. It suggested that dramatically biomass burning contributed the regional haze in Changchun city. If a prescribed burning had been conducted, and the crop residue was burned over a longer time period instead of on one or two days, there would have been no PM
2.5 concentration peak.
Despite the qualitative understanding of biomass burning and regional haze, the determination of key parameters needed for estimating the effects of biomass burning on regional haze is not straightforward. Generally, methods to determine the impact of biomass burning on air quality and visibility include [
41]: (1) emission inventories; (2) air quality monitoring instruments to measure smoke concentrations in near-real-time; and (3) filter-based monitoring techniques and receptor-oriented methods that quantify burning smoke contribution to air pollution based on the chemical characteristics of smoke particles or their spatial/temporal variability [
41]. Emissions from biomass burning vary depending on fuel type and moisture content, combustion phase, wind conditions, and other meteorological conditions. In addition, biomass-burning aerosols can evolve rapidly as they disperse, so it is difficult to relate agricultural straw burning to the regional haze. A key issue is finding solutions to deal with large quantities of agricultural straw, in order to reduce the effect of agricultural burning on regional haze.
2.3. Solutions for Agricultural Straw
Although agricultural open field burning was prohibited by the government, the effectiveness of this ban is limited and new solutions should be implemented. Since agricultural straw is very useful, there are some suitable solutions, as follows:
- (1)
Electricity generation: Electricity generated by biomass generally offers a favorable price, high efficiency and low emissions, but often has unfavorably high land and water usage. Sixty-two countries produce electricity from biomass [
42]. In China, the maximum power generation potential of agricultural biomass resources is 70,465.35 MW, and the preferred development areas include Heilongjiang, Henan, Shandong and Jilin provinces [
43]. In fact, electricity has been generated in Jilin Provence using this method since 2015.
- (2)
Animal feed supply [
44]: Besides cellulose, straw contains hemicellulose and lignin which are palatable to ruminants such as cows.
- (3)
Bio-ethanol production: Rice straw can be used in bio-ethanol production, bringing additional income and allowing sustainable utilization [
45].
- (4)
Returning straw to the field: This solution is an important soil management practice to improve soil fertility. For example higher soil organic carbon, nitrogen, and phosphorus contents were observed following straw-returning than under normal tillage.
These solutions are rarely adopted in China because large volumes of agricultural straw are hard to collect in a short term after harvest, yet timely removal after the harvest is critical to avoiding missing the sowing season. Furthermore, much room is needed for agricultural straw storage before further processing. Therefore, open field burning is widely used as an inexpensive means of disposal in most parts of China.
Here we propose that prescribed open burning would be a more suitable solution in China. Prescribed burning is the process of planning and applying fire to a predetermined area, under specific environmental conditions, to achieve a desired outcome [
46]. It has been used widely in grassland and forest ecosystem as fuel management tool by reducing the intensity, size and damage of wildfire [
46]. There are several reasons for this: (1) prescribed burning has been used widely in grassland and forest ecosystem as a fuel management tool by reducing the intensity, size and damage of wildfire [
47,
48]; and (2) prescribed burning is an inexpensive and efficient means to clean agricultural straw. However, compared with common open field burning, execution of prescribed burning should consider conditions including wind speed, diffusion of gaseous pollutants and particle matter, air quality, and rainfall forecasts. A lower wind speed would be better than a higher wind speed, to allow control of the area being burned. Atmospheric conditions should be favorable for diffusion, for example before periods of cold air. Prescribed burning should be prohibited during fog or temperature inversion conditions. Background air quality should also be considered. Prescribed burning should be conducted during good or moderate air quality and prohibited during poor or hazardous air quality. Rainfall after the prescribed burning would help reduce particle emissions. Clearly, prescribed burning should be carried out far away from residential areas, shrub land and highways. Heavy smoke from agricultural straw burning should have no effect on highway or airline visibility. Finally, prescribed burning of agricultural straw should be managed by both farmers and governments: farmers carry out the prescribed burning, and the government provides information about when and where agricultural straw should be burned.