Seasonal variation of greenhouse gases emissions from landfill areas
Emissions of CO2, CH4 and N2O were significantly higher at domestic landfill sites than at industrial as shown in Table 4. GHGs emissions also varied significantly among different seasons. The highest emission of CO2, CH4 and N2O was recorded in the monsoon season followed by summer and winter. High moisture content and high temperature favored the higher emission of methane (~ 50.49%) during monsoon as compared to the summer (30.74%) and winter (18.77%) seasons in both the landfill sites. During the monsoon and summer seasons, high temperature promotes the microbial metabolic activity and tends to increase the GHGs emission inside the landfill sites (Henneberger et al. 2015). Emission of N2O during monsoon was estimated at 53% followed by 30.23% in summer and 16.28% in winter season (Table 4). Presence of N2O and large portion of CO2 specify that air was present inside the landfill and there was some aerobic degradation. Aerobic degradation was observed, due to open dumping of MSW without soil cover, in both landfill sites. It might have led to oxidation of considerable fraction of CH4 resulting in lower percentage of CH4. Out of total GHGs emission during all the seasons, only 38% of CH4 was estimated while CO2 and N2O accounted for 61 and 1%, respectively. The sampling location i.e. upper, middle and periphery also significantly influenced the GHGs emission. The highest CO2, CH4 and N2O emission were recorded at central (582.54, 341.85, and 0.19 mg m− 2 h− 1, respectively) followed by middle (513.76, 291.33 and 0.14 mg m− 2 h− 1, respectively) and peripheral (462.77, 254.13 and 0.10 mg m− 2 h− 1, respectively) locations of sampling. Wide variations in greenhouse gases emissions between the sampling locations may be due to the heterogeneous nature of landfill and uneven height and compaction across the landfill areas. Out of the total GHGs emissions, 37.36, 38.53 and 44.19% of CO2, CH4 and N2O emission, respectively was recorded from the central location. The central or upper part of both the landfill sites contained earlier dumped wastes, which significantly affects the emission of GHGs. Whereas lower emission of CO2, CH4 and N2O was observed at peripheral location of both the landfill sites because of lesser moisture waste being filled in the region. On average higher emissions of CO2, CH4 and N2O were recorded from domestic landfill sites (49.54, 29.68 and 0.016 ton ha− 1yr− 1, respectively) than industrial (41.16, 23.37 and 0.010 ton ha− 1yr− 1) as shown in Table 5. Higher emission was recorded during every sampling time at domestic landfill site as compared to industrial. Domestic MSW had high percentage of organic matter and moisture content as shown in. The organic portion of the waste could be responsible for this high GHGs emission, because of the uncontrolled anaerobic and aerobic degradation. Gurijala and Suflita (1993) reported greater CH4 emission at pH 6.8–7.4 and at higher moisture contents in landfill areas. Waste characteristics, disposal method, climatic conditions and age of disposal sites are some important factors, which influenced the wide range of variation in GHGs emission between the domestic and industrial landfill sites. Rinne et al. (2005) stated that the production of N2O may be related with the age of the deposited waste in landfill areas. Soil C: N ratio, total organic carbon, and activity of nitrifiers and denitrifiers (Long et al. 2018) and environmental factors like temperature and oxygen content inside the landfill site determine N2O flux. Here combined effect of available nitrogen and high moisture content resulted in the higher emission of N2O at domestic landfill site.
Table 4
Greenhouse gases emission from two landfill sites
| | CO2 (mg m− 2 h− 1) | CH4 (mg m− 2 h− 1) | N2O (mg m− 2 h− 1) |
Site | Industrial | 469.87B | 266.75B | 0.11B |
Domestic | 565.51A | 338.79A | 0.18A |
SD | 9.11 | 1.12 | 0.01 |
LSD | 39.18 | 4.84 | 0.02 |
Season | Winter | 338.24C | 166.53C | 0.07C |
Summer | 469.43B | 272.77B | 0.13B |
Monsoon | 751.40A | 448.02A | 0.23A |
SD | 9.83 | 1.33 | 0.01 |
LSD | 28.09 | 3.79 | 0.02 |
Location | Peripheral | 462.77C | 254.13C | 0.10C |
Middle | 513.76B | 291.33B | 0.14B |
Central | 582.54A | 341.85A | 0.19A |
SD | 7.93 | 2.54 | 0 |
LSD | 19.79 | 6.34 | 0.01 |
Figures in a column followed by the different superscripts differ significantly at P = 0.05 level of significance. SE(d) means standard error of difference. LSD means least significant difference.
Table 5
Total (overall) emission of GHGs from both landfill sites as well as from MSWC
Landfill emission | CO2 (ton ha− 1yr− 1) | CH4 (ton ha− 1yr− 1) | N2O (ton ha− 1yr− 1) | * kg CO2eq ton− 1 ha− 1yr− 1 |
Industrial | 41.16 | 23.37 | 0.010 | 628.39 |
Domestic | 49.54 | 29.68 | 0.016 | 796.31 |
MSWC emission | | | | |
Industrial | 17.65 | 9.59 | 0.004 | 258.59 |
Domestic | 20.39 | 11.26 | 0.006 | 303.678 |
* GWP over 100 years for CH4 & N2O were taken from IPCC 4th Assessment Report (AR4), 2007 |
Gases emission during compost formation
Composting is an eco-friendly method for organic waste management and the final product can be used as an amendment and soil conditioner in agriculture sector. During composting of MSW, emission of all three studied gases (i.e. CO2, CH4 and N2O) was higher for domestic than industrial sites. The concentration of CO2 was significantly higher in the case of domestic (i.e. 312.55, 226.75, 202.92 and 188.73 mg m− 2 h− 1 ) at 15, 30, 45 and 60 days of composting, respectively than for industrial MSWC (291.47, 200.9, 162.3 and 151.05 mg m− 2 h− 1, respectively). A similar trend was observed for CH4 emission with values being 184.23, 125.32, 106.62 and 97.8 mg m− 2 h− 1 at 15, 30, 45 and 60 days of composting, respectively for domestic and 146.27, 115.55, 92.8 and 83.22 mg m− 2 h− 1 for industrial MSW compost. N2O emission also showed significantly higher values in domestic MSW at all sampling stages than industrial MSWC. N2O emissions at 15, 30, 45 and 60 days of composting for domestic MSW were 0.05, 0.05, 0.08 and 0.08 mg m− 2 h− 1, respectively in comparison to 0.03, 0.04 0.06 and 0.07 mg m− 2 h− 1, respectively for industrial MSWC. Decreasing trends were observed for CO2 and CH4 emissions from 15 to 30, 45 and 60 days of composting as shown in Fig. 2A and Fig. 2B, but the opposite trend was observed for N2O as shown in Fig. 2C. Presence of sulphur and rice straw hastened the degradation process and higher temperature led to higher oxygen demand. This leads to anaerobic spots within the compost piles and favored the higher emissions of CH4 and CO2. MSW (control) showed least emission during initial sampling possibly due to late entry in thermophilic phase. However, N2O emission showed opposite trend, lesser emission observed at 15 days sampling stage as compared to other later sampling stages. It was mainly due to the fact that higher temperature reduces the N2O emissions (Amlinger et al. 2008). At the time of 30, 45 and 60 days of sampling, an overall reduction was noticed in CO2 and CH4 emission. Least emission of CO2 and CH4 was recorded during 60 days of sampling which indicated the stability of end product or maturation of compost. During later sampling stages, higher emissions of CO2 and CH4 were observed for MSW treatment followed by MSW + G and further by MSW + ES, whereas least being recorded in MSW + G + ES + RS. Conversely during 30 days sampling, control (MSW) entered into the thermophilic phase and resultant high temperature and lower C:N ratio led to higher emissions in MSW treatment. However, presence of sulphur and rice straw in MSW + G + ES + RS seemed to have facilitated the least emission of CO2 and CH4. Because sulphur reduces the pH of compost and had a negative impact on methanogens activity and rice straw increased the C:N ratio as well as enhanced the aeration within the compost piles. N2O showed an increment during 30, 45 and 60 days of sampling stages as the compost was entering to the maturation/cooling phase. Earlier Amlinger et al. (2008) also observed higher concentration of CH4 along with NH3 during initial stage of composting and higher concentration of N2O during cooling phase. Many factors such as temperature, particle size, C:N ratio, pH, moisture along with some additives such as sulphur, straw and phosphorus play an important role in the biochemistry of compost degradation process. Sommer and Moller (2000) investigated the effect of straw addition in pig manure and observed that there was less emission of CH4 and N2O in straw amended low density piles as compared to high density piles (without straw). Whitehead (1995) recorded that higher C: N ratio reduced the mineralization and FYM decomposition, which leads to less emission. Hence, the addition of organic and inorganic additives for composting of MSW need to be thoroughly evaluated and promoted to minimize the global warming impact and enhance the agronomic value of compost (Awasthi et al. 2017). Overall higher emission of CO2, CH4 and N2O was recorded in domestic MSWC formation (20.39, 11.26 and 0.006 ton ha− 1yr− 1, respectively) than in industrial MSWC (17.65, 9.59 and .004 ton ha− 1yr− 1, respectively).
Entire emission of GHGs was incorporated in terms of CO2 equivalent, as CH4 and N2O have a GWP 21 and 298 times that of CO2 over 100 year (IPCC 2007). Significantly lower GWP was recorded during composting of MSW (258.59 and 303.678 kg CO2eq ton− 1 ha− 1yr− 1in industrial and domestic MSW, respectively) than that of landfill sites (628.39 and 796.31 kg CO2eq ton− 1 ha− 1yr− 1, 1in industrial and domestic MSW, respectively). In present study, approximately 43, 41 and 46% reduction was recorded in CO2, CH4 and N2O, respectively, for industrial MSWC than the emission from industrial landfill site. While 41, 38 and 36% reduction in CO2, CH4 and N2O respectively, was observed for domestic MSWC than the emission from domestic landfill site. The total GHGs (CO2, CH4 and N2O) emission, due to composting of MSW, was reduced by 42.27 and 39.95% in industrial and domestic, respectively as compared to the emission recorded at respective city MSW landfill sites. Industrial MSW compost showed considerable higher reduction in GHGs emissions than the domestic compost. This might be due to fact that domestic waste had higher percentage of moisture content and organic material than industrial. High water content in MSW reduces the air space and facilitates the gases emission. Babel and Vilaysouk (2015) also found similar results in offsetting of GHGs emission during composting. They have reported approximately 41% lower CH4 and N2O emission from composting than landfill. Hubbe et al. (2010) also reported that composting is an effective method of decreasing emission of GHGs and subsequently minimization of global warming.
In present study, operating and management cost was not included in the calculation of GHGs emission during composting process because the factors involved, like transportation, salaries and prices with respect to sales, are site specific.