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International Journal of Environmental & Agriculture Research (IJOEAR) ISSN:[2454-1850] [Vol-2, Issue-4, April- 2016]
Page | 39
Greenhouse Gas Emissions from Rice Fields of Bengaluru Urban
District, India
M. Kumar1
, N. Nandini2
Department of Environmental Science, Bangalore University, Jnana Bharathi campus, Bengaluru, Karnataka, INDIA
Abstract— Anaerobic decomposition of organic material in flooded rice paddy fields produces methane and is considered
one of the most prevalent sources for atmospheric methane. Methane from the rice paddy fields escapes to the atmosphere
primarily by diffusive transport through the rice plants during the growing season. This paper aimed at the inventarisation of
greenhouse gas emissions from the flooded rice paddy fields using Intergovernmental Panel on Climate Change (IPCC)
2006 guidelines - Tier 1 approach for Agriculture, Forestry and Other Land-use sector. The methane emission from rice
paddy fields for the year 1990-1991 was 1.255 Gg or 31.364GgCO2e, while 2012-2013 accounts for 0.269Gg or
6.725GgCO2e. The overall decrease of 21.44% of methane emissions from rice paddy fields was observed during the last two
and half decade. The rice paddy fields are decreased over the years due to rapid expansion of the built-up environment in the
outskirts of the urban area.
Key words: Agriculture, greenhouse gas, methane, flooded paddy fields.
I. INTRODUCTION
Globally rice provides the staple food for over 60% of the world’s population. It has a central role in providing food with
substantial environmental impacts. India is the second largest producer and consumer of rice in the world next to China and
accounts for 21% of the world’s total rice production. Paddy cultivation is an important source of methane emissions (a
potent greenhouse gas), emitted from flooded paddy fields, and the energy needed for pumping water. Methane is the
primary greenhouse gas from flooded paddy fields, so understanding methane production is important for understanding the
overall greenhouse gas burden of rice production. The total methane emissions from a paddy field are determined by methane
production, oxidation and transport (Frenzel et al., 1999). Methanogenesis, methane production, is a microbial process
strictly limited to anaerobicconditions (Ma et al., 2010) and flooding is the key driver of soil anaerobic conditions, so the
flooding regime is critical to methanogenesis (Yan et al., 2005). Although not all rice is grown in flooded conditions,
globally 90% of rice land is at least temporarily flooded (Wassmann et al., 2009).Understanding how these emissions arise,
and potential mitigating steps, this paper is aimed at the science associated with greenhouse gas emissions from the flooded
paddy fields.
II. STUDY AREA AND METHODOLOGY
2.1 Study Area
The present study was carried out in Bengaluru urban district; one of the fastest growing cites in India, with a population of
8.4 million (Census of India, 2011) indicating a development of 2196 sq.km geographical area (DES, 2013); located 920m
above mean sea level, and experiencing a salubrious climate throughout the year with an annual rainfall of about 850-
950mm. Bengaluru is branded as 'Silicon Valley of India' for heralding and spearheading the growth of Information
Technology (IT) based industries in the country. Bengaluru has become a cosmopolitan city attracting people and business
alike, within and across nations (Sudhira et al.,2007). Agricultural lands, open lands and barren lands are converted into
urban settlements. From the past two and half decade, rapid urbanization, land utilization and variability in annual rainfall
leads to conversion of agriculture land into urban settlements which resulted in the decrease of paddy cultivation over the
years.
2.2 Methodology
Greenhouse gas emissions from paddy cultivation and urea fertilization are typically small, often negligible for most urban
regions, so this category needs to be carefully considered. The key greenhouse gases of concern in paddy cultivation and urea
fertilization are methane and carbon dioxide respectively. The greenhouse gas emission inventory was associated with paddy
cultivation and urea fertilization using Intergovernmental Panel on Climate Change (IPCC) guidelines - Tier 1 approach for
Agriculture, Forestry and Other Land-use sector (IPCC, 2006).The annual paddy cultivated area and total quantity of urea
fertilisation data's were collected from Directorate of Economics and Statistics, Government of Karnataka for greenhouse gas
International Journal of Environmental & Agriculture Research (IJOEAR) ISSN:[2454-1850] [Vol-2, Issue-4, April- 2016]
Page | 40
emission (methane and carbon dioxide) inventory. The inventory is based on national emission factors and are carried out for
the financial year (i.e., April - March) 1990-1991, 2000-2001, 2010-2011, 2011-2012 and 2012-2013.
Equation 1: Methane emission from rice cultivation
CH4Rice = A x t x EFi x 10-6
Where:
CH4Rice = Amount CH4 emission from rice cultivation (Gg CH4 yr-1
)
A = Annual harvested area (ha yr-1
)
t = Cultivation period of rice (day)
EFi = Emission factor for harvested area (kg CH4 ha-1
day)
Equation 2: CO2 emissions from Urea fertilization
CO2-C Emission = M x EF x 10-6
Where:
CO2-C Emission = CO2-C emission from Urea fertilization (Gg Cyr-1
)
M = Annual amount of Urea fertilization (tonnes urea yr-1
)
EF = Emission factor [tonnes of C (tonne of urea)-1
]
Equation 3: Greenhouse gas emission to Equivalent Carbon dixode
CO2e = GHG x GWP
Where:
CO2e = Equivalent Carbon dioxide
GHG = Greenhouse gas
GWP = Global warming potential
III. RESULTS AND DISCUSSION
The process of urbanization can involve direct change in land use, as formerly agricultural land becomes incorporated within
built-up areas. Urban areas can shape emissions from agriculture and other land-use change. The urban trends towards
suburbanization that is cities are sprawling and encroaching on land that may previously have been covered with agriculture
field – thereby reducing the cultivation of crops especially paddy. The consumption patterns of increasingly wealthy urban
residents can shape the type of agricultural activities that is taking place. For example, the growing paddy is associated with
emissions of methane which is a potent greenhouse gas.
3.1 Paddy cultivation
Anaerobic decomposition of organic material in the flooded rice fields produce methane, which escapes to the atmosphere
primarily by transport through the rice plants. The annual amount of methane emitted from a given area of rice is a fraction
of the number and duration of crop grown, water regimes before and during cultivation period, and organic and inorganic soil
amendments. Soil type, temperature and rice cultivar also affect methane emission. Table 1 presents the annual paddy
cultivated area in Bengaluru urban district from the year 1990 to 2013.
TABLE 1
ANNUAL PADDY CULTIVATED AREA
Year Paddy harvested area (ha yr-1
)
1990-1991 7317
2000-2001 6974
2010-2011 1895
2011-2012 1688
2012-2013 1569
Source: Directorate of Economics and Statistics, Bengaluru
International Journal of Environmental & Agriculture Research (IJOEAR) ISSN:[2454-1850] [Vol-2, Issue-4, April- 2016]
Page | 41
The methane emission from paddy cultivation for the year 1990-1991 was 1.255 Gg or 31.364Gg CO2e, while 2012-2013
accounts for 0.269Gg or 6.725Gg CO2e (Figure 1&2). The overall decrease of 21.44% of methane emissions was observed
during the last two and half decade. The paddy cultivation area is decreased over the years due to rapid expansion of the
built-up environment in the outskirts of the urban area. The maximum paddy cultivation was observed in the northern and
southern part the Bengaluru urban district; now in these parts the agriculture lands are converted into residential sectors,
commercial sectors and industrial estates. Similarly, Indian Greenhouse Gas Emissions report 2007 revealed that paddy
cultivation emitted 69.87 million tons of CO2eq or 3.27 million tons of methane. The emissions cover all forms of water
management practiced for rice cultivation, namely, irrigated, rainfed, deep water and upland rice.
FIGURE 1: METHANE EMISSION (Gg) FROM PADDY CULTIVATION
FIGURE 2: METHANE EMISSION (Gg CO2e) FROM PADDY CULTIVATION
3.2 Urea as a fertilizer
Addition of urea to soils during fertilization leads to a loss of carbon dioxide that was fixed in the industrial production
process. Urea is converted into ammonia, hydroxyl ion and bicarbonates in the presence of water and urease enzymes.
Similar to the soil reaction following addition of lime, bicarbonates that is formed evolves into carbon dioxide and water.
Table 2 explains about the utilization urea applied in the agriculture fields.
International Journal of Environmental & Agriculture Research (IJOEAR) ISSN:[2454-1850] [Vol-2, Issue-4, April- 2016]
Page | 42
TABLE 2
ANNUAL AMOUNT OF UREA FERTILIZATION
Year Annual amount of Urea Fertilization (tonnes urea yr-1
)
1990-1991 19992.28
2000-2001 16602.73
2010-2011 25823.41
2011-2012 42405.20
2012-2013 32428.35
Source: Directorate of Economics and Statistics, Bengaluru
The carbon dioxide emission from urea fertilization for the year 1990-1991 was 3.998Gg, 2011-2012 was 8.482Gg, while
2012-2013 accounts for 6.486Gg (Figure 3) in Bengaluru urban district. There was increase in the utilization of urea in the
year 2011-2012 because of increased rainfall in that particular year and Government of Karnataka has given subsidy to the
farmers to buy the fertilizers. This in turn increased the yield and production of crops.
FIGURE 3: CARBON DIOXIDE EMISSIONS FROM UREA FERTILIZATION
IV. CONCLUSION
Overall, agriculture sector need to be improved by adopting new technologies based on the availability of water resources.
Methane emissions from the paddy fields can be minimize by changing the water management, but at the expense of
converting flooded paddy field to dry paddy filed. And also, understanding the trade-offs between greenhouse emissions is
important before different methods of rice production are advocated on grounds of climate mitigation. Finally, it is important
to note that greenhouse gas emissions are of great importance they must be put within the wider picture of sustainable
development.
REFERENCES
[1] Census of India. (2011). Karnataka district-wise population - Bengaluru urban. Government of India.
[2] Directorate of Economics and Statistics (DES). (2013). Bangalore Urban District at a glance. Annual report 2012-2013. Government
of Karnataka. 1-232.
[3] Directorate of Economics and Statistics. (1991). Bangalore Urban District at a glance. Annual report 1990-1991. Government of
Karnataka. 1-79.
[4] Directorate of Economics and Statistics. (2001). Bangalore Urban District at a glance. Annual report 2000-2001. Government of
Karnataka. 1-55.
[5] Directorate of Economics and Statistics. (2011). Bangalore Urban District at a glance. Annual report 2010-2011. Government of
Karnataka. 1-220.
International Journal of Environmental & Agriculture Research (IJOEAR) ISSN:[2454-1850] [Vol-2, Issue-4, April- 2016]
Page | 43
[6] Directorate of Economics and Statistics. (2012). Bangalore Urban District at a glance. Annual report 2011-2012. Government of
Karnataka. 1-227.
[7] Frenzel, P., U. Bosse, and P. H. Janssen. (1999). Rice roots and methanogenesis in a paddy soil: ferric iron as an alternative electron
acceptor in the rooted soil. Soil Biology and Biochemistry. 31:421-430.
[8] Ma, K., Q. F. Qiu, and Y. H. Lu. (2010). Microbial mechanism for rice variety control on methaneemission from rice field soil. Global
Change Biology. 16:3085-3095.
[9] Sudhira, H.S., Ramachandra, T.V. and Bala Subrahmanya, M.H. (2007). City profile Bangalore Cities. Cities. 24(5): 379-390.
[10] Wassmann, R., Y. Hosen, and S. K. (2009). Reducing Methane Emissions from Irrigated Rice. IFPRI.
[11] Yan, X., K. Yagi, H. Akiyama, and H. Akimoto. (2005). Statistical analysis of the major variables controlling methane emission from
rice fields. Global Change Biology. 11:1131-1141.

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  • 1. International Journal of Environmental & Agriculture Research (IJOEAR) ISSN:[2454-1850] [Vol-2, Issue-4, April- 2016] Page | 39 Greenhouse Gas Emissions from Rice Fields of Bengaluru Urban District, India M. Kumar1 , N. Nandini2 Department of Environmental Science, Bangalore University, Jnana Bharathi campus, Bengaluru, Karnataka, INDIA Abstract— Anaerobic decomposition of organic material in flooded rice paddy fields produces methane and is considered one of the most prevalent sources for atmospheric methane. Methane from the rice paddy fields escapes to the atmosphere primarily by diffusive transport through the rice plants during the growing season. This paper aimed at the inventarisation of greenhouse gas emissions from the flooded rice paddy fields using Intergovernmental Panel on Climate Change (IPCC) 2006 guidelines - Tier 1 approach for Agriculture, Forestry and Other Land-use sector. The methane emission from rice paddy fields for the year 1990-1991 was 1.255 Gg or 31.364GgCO2e, while 2012-2013 accounts for 0.269Gg or 6.725GgCO2e. The overall decrease of 21.44% of methane emissions from rice paddy fields was observed during the last two and half decade. The rice paddy fields are decreased over the years due to rapid expansion of the built-up environment in the outskirts of the urban area. Key words: Agriculture, greenhouse gas, methane, flooded paddy fields. I. INTRODUCTION Globally rice provides the staple food for over 60% of the world’s population. It has a central role in providing food with substantial environmental impacts. India is the second largest producer and consumer of rice in the world next to China and accounts for 21% of the world’s total rice production. Paddy cultivation is an important source of methane emissions (a potent greenhouse gas), emitted from flooded paddy fields, and the energy needed for pumping water. Methane is the primary greenhouse gas from flooded paddy fields, so understanding methane production is important for understanding the overall greenhouse gas burden of rice production. The total methane emissions from a paddy field are determined by methane production, oxidation and transport (Frenzel et al., 1999). Methanogenesis, methane production, is a microbial process strictly limited to anaerobicconditions (Ma et al., 2010) and flooding is the key driver of soil anaerobic conditions, so the flooding regime is critical to methanogenesis (Yan et al., 2005). Although not all rice is grown in flooded conditions, globally 90% of rice land is at least temporarily flooded (Wassmann et al., 2009).Understanding how these emissions arise, and potential mitigating steps, this paper is aimed at the science associated with greenhouse gas emissions from the flooded paddy fields. II. STUDY AREA AND METHODOLOGY 2.1 Study Area The present study was carried out in Bengaluru urban district; one of the fastest growing cites in India, with a population of 8.4 million (Census of India, 2011) indicating a development of 2196 sq.km geographical area (DES, 2013); located 920m above mean sea level, and experiencing a salubrious climate throughout the year with an annual rainfall of about 850- 950mm. Bengaluru is branded as 'Silicon Valley of India' for heralding and spearheading the growth of Information Technology (IT) based industries in the country. Bengaluru has become a cosmopolitan city attracting people and business alike, within and across nations (Sudhira et al.,2007). Agricultural lands, open lands and barren lands are converted into urban settlements. From the past two and half decade, rapid urbanization, land utilization and variability in annual rainfall leads to conversion of agriculture land into urban settlements which resulted in the decrease of paddy cultivation over the years. 2.2 Methodology Greenhouse gas emissions from paddy cultivation and urea fertilization are typically small, often negligible for most urban regions, so this category needs to be carefully considered. The key greenhouse gases of concern in paddy cultivation and urea fertilization are methane and carbon dioxide respectively. The greenhouse gas emission inventory was associated with paddy cultivation and urea fertilization using Intergovernmental Panel on Climate Change (IPCC) guidelines - Tier 1 approach for Agriculture, Forestry and Other Land-use sector (IPCC, 2006).The annual paddy cultivated area and total quantity of urea fertilisation data's were collected from Directorate of Economics and Statistics, Government of Karnataka for greenhouse gas
  • 2. International Journal of Environmental & Agriculture Research (IJOEAR) ISSN:[2454-1850] [Vol-2, Issue-4, April- 2016] Page | 40 emission (methane and carbon dioxide) inventory. The inventory is based on national emission factors and are carried out for the financial year (i.e., April - March) 1990-1991, 2000-2001, 2010-2011, 2011-2012 and 2012-2013. Equation 1: Methane emission from rice cultivation CH4Rice = A x t x EFi x 10-6 Where: CH4Rice = Amount CH4 emission from rice cultivation (Gg CH4 yr-1 ) A = Annual harvested area (ha yr-1 ) t = Cultivation period of rice (day) EFi = Emission factor for harvested area (kg CH4 ha-1 day) Equation 2: CO2 emissions from Urea fertilization CO2-C Emission = M x EF x 10-6 Where: CO2-C Emission = CO2-C emission from Urea fertilization (Gg Cyr-1 ) M = Annual amount of Urea fertilization (tonnes urea yr-1 ) EF = Emission factor [tonnes of C (tonne of urea)-1 ] Equation 3: Greenhouse gas emission to Equivalent Carbon dixode CO2e = GHG x GWP Where: CO2e = Equivalent Carbon dioxide GHG = Greenhouse gas GWP = Global warming potential III. RESULTS AND DISCUSSION The process of urbanization can involve direct change in land use, as formerly agricultural land becomes incorporated within built-up areas. Urban areas can shape emissions from agriculture and other land-use change. The urban trends towards suburbanization that is cities are sprawling and encroaching on land that may previously have been covered with agriculture field – thereby reducing the cultivation of crops especially paddy. The consumption patterns of increasingly wealthy urban residents can shape the type of agricultural activities that is taking place. For example, the growing paddy is associated with emissions of methane which is a potent greenhouse gas. 3.1 Paddy cultivation Anaerobic decomposition of organic material in the flooded rice fields produce methane, which escapes to the atmosphere primarily by transport through the rice plants. The annual amount of methane emitted from a given area of rice is a fraction of the number and duration of crop grown, water regimes before and during cultivation period, and organic and inorganic soil amendments. Soil type, temperature and rice cultivar also affect methane emission. Table 1 presents the annual paddy cultivated area in Bengaluru urban district from the year 1990 to 2013. TABLE 1 ANNUAL PADDY CULTIVATED AREA Year Paddy harvested area (ha yr-1 ) 1990-1991 7317 2000-2001 6974 2010-2011 1895 2011-2012 1688 2012-2013 1569 Source: Directorate of Economics and Statistics, Bengaluru
  • 3. International Journal of Environmental & Agriculture Research (IJOEAR) ISSN:[2454-1850] [Vol-2, Issue-4, April- 2016] Page | 41 The methane emission from paddy cultivation for the year 1990-1991 was 1.255 Gg or 31.364Gg CO2e, while 2012-2013 accounts for 0.269Gg or 6.725Gg CO2e (Figure 1&2). The overall decrease of 21.44% of methane emissions was observed during the last two and half decade. The paddy cultivation area is decreased over the years due to rapid expansion of the built-up environment in the outskirts of the urban area. The maximum paddy cultivation was observed in the northern and southern part the Bengaluru urban district; now in these parts the agriculture lands are converted into residential sectors, commercial sectors and industrial estates. Similarly, Indian Greenhouse Gas Emissions report 2007 revealed that paddy cultivation emitted 69.87 million tons of CO2eq or 3.27 million tons of methane. The emissions cover all forms of water management practiced for rice cultivation, namely, irrigated, rainfed, deep water and upland rice. FIGURE 1: METHANE EMISSION (Gg) FROM PADDY CULTIVATION FIGURE 2: METHANE EMISSION (Gg CO2e) FROM PADDY CULTIVATION 3.2 Urea as a fertilizer Addition of urea to soils during fertilization leads to a loss of carbon dioxide that was fixed in the industrial production process. Urea is converted into ammonia, hydroxyl ion and bicarbonates in the presence of water and urease enzymes. Similar to the soil reaction following addition of lime, bicarbonates that is formed evolves into carbon dioxide and water. Table 2 explains about the utilization urea applied in the agriculture fields.
  • 4. International Journal of Environmental & Agriculture Research (IJOEAR) ISSN:[2454-1850] [Vol-2, Issue-4, April- 2016] Page | 42 TABLE 2 ANNUAL AMOUNT OF UREA FERTILIZATION Year Annual amount of Urea Fertilization (tonnes urea yr-1 ) 1990-1991 19992.28 2000-2001 16602.73 2010-2011 25823.41 2011-2012 42405.20 2012-2013 32428.35 Source: Directorate of Economics and Statistics, Bengaluru The carbon dioxide emission from urea fertilization for the year 1990-1991 was 3.998Gg, 2011-2012 was 8.482Gg, while 2012-2013 accounts for 6.486Gg (Figure 3) in Bengaluru urban district. There was increase in the utilization of urea in the year 2011-2012 because of increased rainfall in that particular year and Government of Karnataka has given subsidy to the farmers to buy the fertilizers. This in turn increased the yield and production of crops. FIGURE 3: CARBON DIOXIDE EMISSIONS FROM UREA FERTILIZATION IV. CONCLUSION Overall, agriculture sector need to be improved by adopting new technologies based on the availability of water resources. Methane emissions from the paddy fields can be minimize by changing the water management, but at the expense of converting flooded paddy field to dry paddy filed. And also, understanding the trade-offs between greenhouse emissions is important before different methods of rice production are advocated on grounds of climate mitigation. Finally, it is important to note that greenhouse gas emissions are of great importance they must be put within the wider picture of sustainable development. REFERENCES [1] Census of India. (2011). Karnataka district-wise population - Bengaluru urban. Government of India. [2] Directorate of Economics and Statistics (DES). (2013). Bangalore Urban District at a glance. Annual report 2012-2013. Government of Karnataka. 1-232. [3] Directorate of Economics and Statistics. (1991). Bangalore Urban District at a glance. Annual report 1990-1991. Government of Karnataka. 1-79. [4] Directorate of Economics and Statistics. (2001). Bangalore Urban District at a glance. Annual report 2000-2001. Government of Karnataka. 1-55. [5] Directorate of Economics and Statistics. (2011). Bangalore Urban District at a glance. Annual report 2010-2011. Government of Karnataka. 1-220.
  • 5. International Journal of Environmental & Agriculture Research (IJOEAR) ISSN:[2454-1850] [Vol-2, Issue-4, April- 2016] Page | 43 [6] Directorate of Economics and Statistics. (2012). Bangalore Urban District at a glance. Annual report 2011-2012. Government of Karnataka. 1-227. [7] Frenzel, P., U. Bosse, and P. H. Janssen. (1999). Rice roots and methanogenesis in a paddy soil: ferric iron as an alternative electron acceptor in the rooted soil. Soil Biology and Biochemistry. 31:421-430. [8] Ma, K., Q. F. Qiu, and Y. H. Lu. (2010). Microbial mechanism for rice variety control on methaneemission from rice field soil. Global Change Biology. 16:3085-3095. [9] Sudhira, H.S., Ramachandra, T.V. and Bala Subrahmanya, M.H. (2007). City profile Bangalore Cities. Cities. 24(5): 379-390. [10] Wassmann, R., Y. Hosen, and S. K. (2009). Reducing Methane Emissions from Irrigated Rice. IFPRI. [11] Yan, X., K. Yagi, H. Akiyama, and H. Akimoto. (2005). Statistical analysis of the major variables controlling methane emission from rice fields. Global Change Biology. 11:1131-1141.