Keywords

14.1 Introduction

Latest report given by IPCC (Intergovernmental Panel on Climate Change) reveals the role of humans in aggravating the issue of climate change across the world. For the last 40 years combustion of fossil fuel and industrial activity have contributed more than two-third of GHG (greenhouse gas) concentration into the atmosphere (IPCC 2014). On the other hand, AFOLU (Agriculture, Forestry and Other Land Use) sector has contributed 25% GHG emissions by anthropogenic activity. As a matter of fact, there is gradual rise of energy and associated climate footprint during last few decades. Now various governments across various nations across the globe are trying to reduce the energy emission footprint and climate footprint by reducing GHG emission and switching over to renewable source of energy (Meena and Lal 2018). European Commission has set a target of increasing 20% of renewable source of energy in the overall energy consumption pattern followed by 10% in the transportation sector by 2020 (European Commission Directive 2009; Meena et al. 2018). As per the reports, more than 10% of the energy supply came from renewable sources in 2008 where major share comes from the bioenergy sector (Moomow et al. 2011). In the bioenergy sector, biomass tends to has significant contribution in energy production and use (Allen et al. 2014; Meena et al. 2020a, b). Biomass energy in the form of fuelwood, crop residues and energy crop has taken a significant share across various nations in the globe. Food crops can be used sometimes as energy crops having higher yield followed by lesser agro-inputs (Cherubini et al. 2009). A very interesting fact is that energy generation from energy crops is highly beneficial due to equality of CO2 (carbon dioxide) capture followed by its release. It was observed that GHG emission takes place at various segments of the production process and thus proper agricultural management would help to reduce GHG emission from the concerned sector (Blengini et al. 2011).

The concept of C (carbon) footprint reveals the requirement of formulation of guidelines and standards for specific assessment of GHG emission. C footprint potential is the technique for calculating the potential GHG emission through life cycle analysis expressed as CO2eq. Various tools are used to assess the GHG emission from agricultural products (Colomb et al. 2013). The calculators for CFP (carbon footprint potential) have been divided into three sections which include calculating tools, standard procedures and modeling approach (Denef et al. 2012). Various methods are available which are used to measuring CFP with latest advancement in the form of web based system for calculation of GHG emission during energy crop plantation in cultivation process (Colomb et al. 2013). CFP calculation has been used under diverse cultivation system associated with crop management at the farm level.

The concept of CFP calculators were used by the farming community, agricultural workers and researchers to identify and quantify the GHG emission at local level (Hillier et al. 2009). Overall the CFP calculation while suggesting mitigatory strategies should include the local ecological condition, prevailing agricultural practices and technologies along with various forms of crop management (Brankatschk and Finkbeiner 2015).

Modification or alteration of crop rotation pattern tends to reduce the GHG emission to a considerable extent (Nemecek et al. 2015). However, C footprint potential calculation for crop cultivation practices considers a single growth period for a single crop (Brankatschk and Finkbeiner 2015). As the agroecosystems are complex in nature and therefore, short span analysis does not reveal the clear picture. Most of the calculation ignores several factors such as the cropping pattern, crop interactions between existing and previous crops, time duration of farming activities which may influence the CF (carbon footprint) calculation (Brankatschk and Finkbeiner 2015). The challenges associated with CFP calculation are that it does not include the time schedule of the cultivation practices present in the agricultural production.

It was observed that in agriculture field direct source of GHG is the crop residues as well as different forms of synthetic and organic fertilizer. As per AFOLU of IPCC direct emission should be considered in the form of CO2 and indirect emission in the form of ammoniacal nitrogen for calculating anthropogenic GHG emission (IPCC 2006). Emission of CO2 takes place through liming and urea application. Application of mineral and organic fertilizer adds nitrous oxide (N2O) into the atmosphere from the agroecosystem through nitrogen volatilization along with leaching and agricultural runoff from fertilizer application. Nature and type of fertilizer applied under field condition determine the fate of GHG emission (Bouwman et al. 2002). Application of digestate in the form of organic fertilizer as an alternative for mineral fertilizer tends to reduce GHG emission. However, it was observed that application of digestate leads to higher diesel consumption followed by increase in GHG emission (Gissén et al. 2014).

Further the process of denitrification and nitrification GHG emission takes place from the crop residues. Therefore, such emissions should be included for carbon footprint calculation. It was also revealed that, CH4 (methane), CO2, and N2O emission along with other air pollutants are released into the atmosphere due to fossil fuel combustion practices (IPCC 2006). The fuel amount depends upon various cultivation activities as well as on crop management practices (Sorensen et al. 2014). Changes in land use pattern may alter the soil organic carbon stock leading to emission of CO2. Selection of suitable crop species has got a significant influence over GHG emission. Therefore, type of energy crop used is significant for calculating energy footprint of agroecosystem.

14.2 Energy Footprint of Agroecosystem and Agriculture Sector

The term energy can be simply defined as the capacity to do work. There is a mutual dependency between economy, environment, and energy (Pimentel et al. 1994). Agriculture is intricately interrelated with the energy sector. Agriculture activities are using energy supplies the energy in the form of bioenergy (Alam et al. 2005). During the present era there is continuous growth in science and technology. This growth is also prevalent in the agriculture sector in which the output of agroecosystem is dependent upon the use of energy. Amount of energy consumption is dependent upon amount of agricultural activity, agricultural lands as well as level mechanization involved in the agricultural process. The input output ratio of energy is dependent upon the cropping pattern, soil type, agricultural activity, yield and productivity operations (Ozpinar and Ozpinar 2011). Gradual technological growth has increased more use of energy during cultivation of crop. As a consequence the efficiency of energy use by the agroecosystem is reflecting a declining trend (Mandal et al. 2002). With gradual increase in energy consumption by the agroecosystem it is adversely affecting the environment in the form of depletion of resources followed by contribution to global warming and climate change (Ghorbani et al. 2011; Raj et al. 2020; Banerjee et al. 2020; Jhariya et al. 2019a, 2019b). Changing climatic pattern and perturbances is reducing the yield to a significant level (Lobell and Gourdji 2012).

Under the conventional system of agriculture tillage is the most important factor as it drives the productivity through effective crop management (Busari et al. 2015). Tillage helps to improve the mechanical structure of soil and thus helps to enhance the crop productivity (Parihar et al. 2016). Such an approach emphasizes more fuel and energy consumption leading to higher emissions of CO2. In comparison to conventional system, zero tillage system of agriculture lesser fuel requirement takes place leading to lesser emission of CO2. It is a good aspect as it is a common fact that CO2 leads to global warming followed by climate change (Hobbs et al. 2008). The yield potential is also higher under rainfed condition in comparison to conventional tillage system (Farooq et al. 2011).

Global consumption of energy for agroecosystem stands to be 5% of the total (IPCC 2014). Higher inputs in the form of agrochemicals application, fuel use, use of farm machineries promote higher energy consumption leading to higher emission of GHGs (Li et al. 2016). In order to analyse the production of agroecosystem from energy analysis perspective all the inputs and outputs of the system need to be converted into energy units (Michos et al. 2017). The situation of energy crisis began from 1970 onwards with limited availability of conventional energy resources (Hulsbergen et al. 2001). Scarcity of proper availability of energy resources requires a proper approach for proper estimation of energy and its consumption in agroecosystem (Kizilaslan 2009). As per the reports of FAO (2019) up to 3% fossil fuel consumption were reflected from the agriculture, forestry and allied sector in the European Union (EU) (Eurostat 2014). If we trace the energy inputs in an agroecosystem, use of fossil fuel, electricity consumption for operation of farm machinery are the principle sources of energy inputs (Michos et al. 2018).

As per the reports the cultivation practices are accompanied by 12% global GHG emission which is estimated to be up to 6.1 GtCO2-eq annually till 2005. In comparison other GHGs such as the CH4 and N2O are emitted as 3.3 GtCO2-eq/year and 2.8 GtCO24 -eq/year, respectively till 2005. In the cultivation sector the anthropogenic emission till 2005 has been evaluated which reveals more than half contribution of N2O and CH4. There is a huge amount of exchange of methane between the land and atmospheric system under agroecosystem but the overall flux seems to be remaining balanced. Globally, agricultural CH4 and N2O emissions have increased up to 17% within a span 15 years which is equivalent to 60 Mt. CO2 -eq/year. Non-Annex-I countries reflected more than 30% increment in GHG emissions till 2005 which has a major contribution to agricultural sector.

Annex-I countries has reflected up to 12% decrease in GHG emission. Therefore, reduction in emission of GHG in the agriculture sector can be done through management of pastureland and improved agronomic practices and restoration of soil quality. Further, under rice cultivation proper water management, land use, agroforestry practices and organic farming practices needs to be done. Technological development may act significantly in mitigating the effect of climate change followed by reduction in GHG emission (Khan et al. 2020a, b).

Modeling approach on long-term basis reveals that non-CO2 crop and livestock management may have significant contribution across worldwide up to 1520 Mt. CO2-eq on annual basis till 2030. However, such modeling approach does not include the process of soil C management. The continuous emissions of various GHGs such as CO2, N2O and CH4, etc. either from fuels or from various agroecosystem practices are estimated by a standard methods adopted from IPCC (2006). Also, IPCC has also developed some coefficients for calculating fertilizers and soils (IPCC 2014). Similarly, the ratio of total utilizable volume of water (m3/year) to the total production quantity (kg/year) is used for calculating water footprints (WF) of varying crops in any agroecosystem (Mekonnen and Hoekstra 2014; ISO 2014). Thus, the calculation of both CF and WF reflects the status of energy footprints that could help producers to minimize their greenhouse gases in economically efficient way. However, the CF of various agroecosystem based food items in the world is depicted in Fig. 14.1 (Chapagain and James 2011). It reflects that livestock based food items contributed in higher CF as compared to vegetables and fruits, respectively. That is why ruminant’s animals produce more GHG (especially CH4) due to faulty manure management in agroecosystem. This hypothesis creates one question in our mind “Is animals based food products contributes in higher CF than fruits and vegetables?” Similarly, water footprints of various food items in the world are also depicted in Fig. 14.2 (Hoekstra and Chapagain 2008; Hoekstra 2013).

Fig. 14.1
figure 1

Carbon footprints of food items in the world (Adopted Chapagain and James 2011)

Fig. 14.2
figure 2

Water footprints of food items in the world (Hoekstra and Chapagain 2008; Hoekstra 2013)

As per the prediction the mitigation potential from the agriculture sector stands to be up to 6000 Mt. CO2-eq annually till 2030. Further, it is assumed that sequestration of C in the soil ecosystem has the mitigation potential about 90%. Further, other non-CO2 gases such as CH4, N2O reflects mitigation up to level of 9% and 2%, respectively. However, there are some challenges and uncertainty in terms of future mitigation measures along with effectiveness of adopted measure for reduction of GHG emission. The level of mitigation is influenced by changing climatic pattern, prevailing socio-economic condition. Economic regulation is an also important factor in terms of abatement of GHG emission. For example, higher C price tend to change the land use pattern and allow feed based mechanism for mitigating climate change. Mitigation strategies and policies needs to be evaluated for cultivation practices, land use and crop management.

GHG emission reduction can be achieved by switching off from use of fossil fuels towards organic supplements in the form agriculture by products in the form of feed stocks which can be used as energy source. As per the reports the climate change mitigation potential from the agriculture sector tends to be up to 1260 Mt. CO2-eq till 2030. Further, additional mitigation of CO2 till 2030 can be achieved through climate smart agriculture practices followed by mitigation potential evaluation in the infrastructure and transportation sector. It was predicted that future GHG emission rates may show an increasing trend in due course of time due to population explosion and changes in consumption pattern. Greater food production to fulfil the needs of the growing population may lead to higher emission of CH4 and N2O due to higher presence of livestock population and greater use of nitrogen (N) fertilizers. To inhibit the further increase of GHG emission till 2030 strategies should be formulated for mitigation purpose in the livestock system and application of N fertilizers. Soil C loss would be a significant aspect in relation to climate change.

It is a proved fact that agriculture sector potentially contribute significant level of CO2 and other GHGs (Paustian et al. 2004). Therefore, the energy footprint for this particular land use seems to be higher from its various component parts. One of the common pathways of CO2 release is the microbial decomposition of the biomass residue, combustion of plant litter and excess presence of soil organic matter (Janzen 2004). Further, CH4 is produced during organic matter decomposition under lack of oxygen which is a common process known as fermentation adopted by livestock population. In addition CH4 is further emitted from organic manures and very prevalent paddy fields (Mosier et al. 1998). N2O is produced through microbial intervention in the form of N from manures and soils. It is enhanced in the presence of excess N which is present in the soil under moist conditions (Oenema et al. 2005). Therefore, there are diverse source within the agroecosystem for emission of GHGs. As a consequence energy footprint is significantly higher in agriculture than the other forms of land use. Still there is high possibility of mitigation of GHG emission through eco-friendly practices and appropriate scientific explorations.

14.2.1 Analysis of Energy in Agroecosystem

Energy analysis is a process or methodology to convert all the inputs and outputs of agroecosystem into units of energy. Under this process the total amount of energy that flows into and out of the agroecosystem is evaluated and measured (Michos et al. 2018). It is a very important aspect for agroecosystem perspective in order to improve the environmental performance of agroecosystem (Chen et al. 2006). In the crisis of ever increasing population, the agricultural production needs to be improved taking into account of efficient use of energy (Michos et al. 2017). Such methodology reflects ecosystem resilience and energy use efficiency of agroecosystem (Ozkan et al. 2007). The evaluation process varies depending upon the site conditions, time of production followed by materials used (Hulsbergen et al. 2001). This would help to reduce the inputs in agriculture production leading to improvement in the productivity (Kehagias et al. 2015). However, this may impact the economy of the agriculture output and therefore it is the urgent need for formulation of strategies to have a harmony between economy and energy use efficiency for effective management of agroecosystem production (Unakitan and Aydin 2018).

14.3 Climate Footprint in Agroecosystem

Concept of climate footprint has emerged from carbon footprinting that evaluates the whole set of GHG gases to be regulated as per Kyoto Protocol. Climate footprint is much more comprehensive in order to assess the role of human beings towards climate change but is a tedious and more labour intensive methodology. The term climate footprint is usually defined as the sum total of all GHG emission that takes place from a population, activity or system. It is usually calculated in the form of CO2eq. using global warming potential for 100 years.

In the agriculture sector the use of energy is directly associated with global greenhouse emission (GGE). GHGs tend to absorb and release radiation in the form of heat and increased temperature in the atmosphere. The major GHGs are CH4, CO2 and N2O. It was reported that the agriculture activity contributes 22% of GGE emission having deleterious impact on climate. On the other hand cultivation of crops contributes 20% of CO2 emission annually (IPCC 2014). In the EU, GGE approximates up to 470.6 Mt. of CO-eq from the agriculture activities which is one tenth of the total emission of GGE (Eurostat 2014). As per the Paris agreement the emission of GGE should be reduced through reduction in the fossil fuel consumption along with the other sustainable cultivation practices (Bryngelsson et al. 2016). The climate footprint of agricultural produce can be estimated through life cycle analysis of product (Weidema et al. 2008).

14.4 Measuring Energy Footprint Through Life Cycle Assessment Approach

Life cycle assessment (LCA) is an integrated approach to quantify the used energy in any agriculture and farming land use system which calculate both carbon and WF throughout the whole life cycle of plants at farm levels (Michos et al. 2018). Recently, a study has been conducted on LCA application to see environmental benefits through production of jam by fruits based agroforestry system in the region of Peruvian Amazon (Recanati et al. 2018). However, the methodology of LCA is useful to understand the environmental impacts due to prevailing agricultural productions. In this consideration, a research in agriculture system would be modified to explore energy footprints which help in better understanding of environmental impacts. Further, an accepted and valid standardizations are emerged which can be adopted for next part of research for energy footprint in agroecosystem (Roy et al. 2009).

In this context, a flowchart is developed that shows modified LCA methodology to assess energy uses and footprints in agricultural land use systems. In stage 1, quantifying used energy in different agricultural and farming land use system. Exploration and identification of low energy input based species and farming system are also considered under the aims and scope. Calculating energy input-output mechanisms of the prevailing agricultural system are comes under inventory analysis of stage 2. Similarly, stage 3 indicates the impact evaluation that quantifying crops yield effects due to practicing farming system in the regions. Comprises, evaluation and discussion of the findings are comes under stage 4. The last stage 4 indicates the applications of planning for crop replacement, reducing energy inputs and exploring environmental impacts are considered for applications (Fig. 14.3) (Taxidis et al. 2015; Platis et al. 2019).

Fig. 14.3
figure 3

Modified life cycle assessment methodology to assess energy uses and footprints in agricultural land use systems (Modified Taxidis et al. 2015; Platis et al. 2019)

14.5 Pattern of Energy and Climate Footprint of Agroecosystem

Within a span of 15 years (1990–2005), the CH4 and N2O emission reflected a rise of 17%. It appeared that ruminant fermentation; soil emissions followed by biomass burning are the principle sources approximating 88% of the GHGs emission (US-EPA 2006a).

14.5.1 Future Global Pattern of Energy and Climate Footprint

As per future prediction emission of N2O may rise up to 60% till 2030 due to overuse of chemical fertilizer along with manure production (FAO 2003). Mosier and Kroeze (2000) have mentioned a 50% rise in N2O emission in comparison to the level attained in 1990. With the rising population the demand of food would gradually increase and therefore the emission of GHGs would further increase as per the demand. Therefore, proper management and eco-friendly technologies in the agriculture sector may help to reduce the emission for per unit of food produced.

As per the reports of FAO (2003) the animal husbandry practices would lead a 60% rise of CH4 emission till 2030. This could be managed through alteration in the feeding of ruminants and proper method adapted for manure production. According to USEPA (2006a) the total contribution of CH4 from manure decomposition and bacterial fermentation process would rise up to 21% within a span of 15 years (2005–2020). Further, FAO (2003) estimates a rise of paddy production up to 4.5% and accordingly CH4 emission would rise. The situation could be handled through proper irrigation practice with lesser rise production along with improved rice cultivars that emit less CH4 may serve the purpose to some extend (Wang et al. 1997).

For non-CO2 GHG emission, USEPA (2006a) predicts an increase up to 13% of emission for the last two decades (2000–2020). Similar rate of increase would contribute GHG emission of about 8300 MtCO2–eq up to 2030. Keeping the deforestation rate constant and promoting conservation tillage may cause a reduction of GHG emission to lesser amount across the globe (FAO 2001).

14.5.2 Regional Pattern of Climate and Energy Footprint

In the Middle East, Africa and Sub-Saharan regions have reflected a rise up to 95% of GHG emission within a span of 30% (1990–2020) (US-EPA 2006a). Further work on this aspect reveals that in Sub-Saharan African region the per capita food production has been kept constant or lower down for emission reduction (Scholes and Biggs 2004). This may be low input agriculture or lack of fertility of soil which have reflected such trends (Sanchez 2002).

It is seen that the economy of urban area is gradually increasing with improved lifestyle and infrastructure. Therefore, the diet composition of urban population is shifting towards the livestock products and as a consequence the demand increases. This has secondary consequences of agricultural intensification in South and Central part of Africa with significant rise in GHG emission. Similarly, the GHG emission also increases in Eastern part of Asia from the livestock population. Data of FAOSTAT (2006) reveals the increase of dairy production up to 12th time within a span of 43 years (1961–2004). However, the consumption pattern reflects lesser consumption but the gradual rise of emission would continue for a long span of time. In the South Asian countries the gradual rise of emission is associated with expansion in N fertilizer use for more production to feed the growing population. As an export quantity agricultural products are the base for the Latin America and Caribbean countries who reflected significant changes in land use and its management through forest conversion in to crop land, resulting in to higher GHG emission.

Some regions of Latin American countries have reflected adoption of no-till agricultural practices which approximates 30 Mha areas annually. On the other hand the developed nations such as parts of Europe reflect a steady rising economy through increase in agricultural production. In Russia, the agricultural expansion may take place up to 14%. It was observed that implementation of intensive system of crop management would give 2.5 times higher yields with increased use of N fertilizers. From 1990 onwards the use of N fertilizers showed a declining trend and thus the emission of N2O decreased. With gradual rise in economy the increased application of N fertilizer took place at an unprecedented rate up to pre-1990 levels. US-EPA (2006a) reported a 32% increase in N2O with an average rate of 3.5 MtCO2eq annually for North America and OECD regions. There is a continuous increase in GHG emission from the agricultural sector as reflected from Pacific region of OECD. In most cases the major contributions come from the manure as non-CO2 emissions and N2O from soil. In the region of Oceania there is continuous rise for last 45 years leading to five-fold increase in GHG emission from New Zealand from 1990 onwards. Similar contribution of manure towards GHG emission was also reflected from North American region. In Western Europe the reduction in energy footprint based upon agroecosystem took place through emission reduction by managing inputs along with efficient N use, livestock management by proper feed arrangement laid to reduction in CH4 emission (Paustian et al. 2004; Clemens and Ahlgrimm 2001). However, the result varies from region to region. Agroecosystems tend to hold C as a large reserve in the form of organic matter. It was observed through scientific observation that 50 PgC stored in the soil are released to some extend which can be conserved through suitable management approach (Lal 2004a).

It is seen that methods promoting photosynthetic build up of C and subsequent release through respiration and other abiotic processes tend to increase C reserve and thus converting soil as a large C sink. Researches in this particular aspect have revealed that success in the process lies with the local conditions (Lal 2004a). Contribution of C from vegetal part into the soil can be done by applying agroforestry systems in the agricultural (Albrecht and Kandji 2003). Bioconversion of crop residues in the form of ethanol may help to avoid the GHG emission (Cannell 2003). GHG emission should be avoided or reduced through sustainable agricultural practices (Foley et al. 2005).

Domestic energy consumptions trends are depicted in Table 14.1 which is divisible into commercial and non-commercial sources that shared 58.0 and 42.0%, respectively. Coke contributed 47% of energy consumption followed by coal, LPG and charcoal that shared 29.0, 10.0 and 11.0%, respectively, whereas petrol, diesel and kerosene shared 1% as compared to least contribution (0.09%) by electricity under commercial sources. Similarly, firewood showed highest (62.0%) sources of energy consumption followed by crop residues (37.0%), whereas least (1.0%) contribution from dung cake and biogas, respectively under non-commercial sources for energy consumption in domestic purposes (Ramachandra 2019).

Table 14.1 The trend of domestics energy consumptions in India (Ramachandra 2019)

14.6 Renewable Energy Footprint

Throughout the world there is a continuous swift of energy use pattern as most of the countries are switching over from non-renewable to renewable sources of energy. For example, in United States (US) the use of renewable energy tends to increase up to 35% to be used as electricity. Such events are taking place due to the mega event of climate change. With gradual improved in the living standards through science and technology the energy demand has raised both in developed and developing nation. Further, the dependency on fossil fuels as energy source has lead to release of huge amount of GHGs in the atmosphere giving rise to the mega event of climate change and global warming. Therefore, legal policy framework has been developed to implement more use of renewable source of energy. Among these policies reduction in energy footprint has been aimed through reduced GHG emission (Snape III 2010).

The renewable energy resource would help in mitigating the event of climate change followed by reduction in emission of GHG. As per the reports US would be requiring more than 65 million acres of land to fulfil the growing demands of electricity and fuel. In order to address the issue of mitigation of climate change use of renewable source of energy such as the biofuels is a suitable alternative. However, the issue of land use stands to be greater in amount for renewable energy in comparison to non-renewable source of energy in the form of fossil fuels. On the other hand the fossil fuel such as the coal extraction leads to environmental degradation in the form of deforestation and biodiversity loss followed by emission of CO2 through coal burning for energy production. Therefore, the non-renewable energy sector reflects two way damages to the whole ecosystem. From this perspective, the renewable energy “footprint” is the most significant approach to regulate the climate change and footprint (US global change research program 2009).

Policy formulation regarding shifting towards renewable source of energy accounts the various sources followed by the individual land footprint of each of the renewable sources. Depending upon the land required for renewable energy harvesting would determine the investment on specific energy resources. However, the major benefit towards switching over to renewable sector would lead to reduction in CO2 emission. Further the environmental consequences that take place through rise in ambient CO2 concentration can be curbed through such approaches. As per the research reports it was found that wind energy may reduce CO2 emissions up to 99% instead of coal and 98% instead of gas. Apparently it is seen that the land investment for renewable energy sources is more than the fossil fuel sources but the net benefit in terms of combating climate change and GHG emission reduction surpasses the increased value of land footprint.

14.6.1 Renewable Energy Footprint to Mitigate Climate Change

Renewable energy sources are becoming a good strategy that helps in reducing energy and footprints and maintain overall environmental sustainability. In this context, some agroecosystem based feedstock’s were used to analyzed for energy values by estimation of feedstock’s and biodiesel yield values which is depicted in Table 14.2 (Salim et al. 2019). From this table, the value of feedstock’s (kg ha−1) and biodiesel yield (kg per kg BDF) are considered highest under Palm (Arecaceae) in the region of Indonesia where least value of biodiesel yield (kg per kg BDF) considered under poultry fat in worldwide, respectively. Thus, these agriculture based feed stocks are considered alternate source of energy consumption rather than fossil fuel consumption which causes unstoppable emission of GHGs into the atmosphere resulting into climate change and global warming phenomenon.

Table 14.2 Energy analysis of biodiesel yield from different feedstock’s biomass in the world

14.7 Reducing Energy and Climate Footprint in Agroecosystem

In the modern times maintaining agricultural production is the key issue to feed the ever increasing human population. Climatic change significantly reduces the productivity of agroecosystem (Schuman et al. 2001; Derner et al. 2006). Therefore, it is the urgent need to reduce the climate footprint through emission reduction in the agriculture practices. Specific policies and strategies need to be formulated to increase the carbon storage in the crop ecosystem and subsequent reduction in CO2 emission. For example, adjusting the livestock strength the emission of non-CO2 gases can be regulated. By increasing the C storage the productivity of the crop ecosystem can be increased. Use of organic amendments in the form of compost, manure, plant litter promotes significant storage of C in soil (Schnabel et al. 2001; Conant et al. 2001). However, application of nitrogen fertilizer creates the opportunity of N2O emission leading to air pollution (Conant et al. 2005). Proper irrigation in grasslands leads to gain in soil C (Conant et al. 2001).

Proper management of nutrient application can mediate emission reduction (Dalal et al. 2003). Further during fertilizer management, proper care should be taken in terms of animal residue management as they add nutrients into the soil (Oenema et al. 2005). Biomass burning contributes significantly towards climate change. For instance, burning of crop residue, stubble mulches after harvesting is an important contributor of CH4 and N2O. Further such activities generate hydrocarbon compounds and nitrogen species which undergo photochemical reactions to produce ozone molecule which is itself a powerful GHG. Further, during burning of the biomass it results into formation of smoke aerosols which alters the climatic condition of the atmosphere (Andreae et al. 2005; Venkataraman et al. 2005). Burning activity causes reduction in the albedo value leading to warming of the earth surface (Beringer et al. 2003). Therefore, reduction in the burning activity may increase the vegetal cover resulting into C sink in biomass and soil (Scholes and van der Merwe 1996). The tree species becomes saturated in terms of C sink up to 50 years but tend to avoid non CO2 gases.

Further, fire suppression techniques may be adopted for mitigating the emission of GHG. It can be achieved through proper management of vegetation by reducing the use as fuel. Strategies can also be oriented in biomass burning at the time of low emission of N2O and CH4 (Korontzi et al. 2003). However, the natural burning process cannot be ignored under climatic influence (Van Wilgen et al. 2004).

Reduction in CO2 emission can be achieved through cultivation of species of grasses that tend to accumulate more C in roots and that ultimately would lead to soil C and further increase in their value. Savannah grassland biome has reflected higher accumulation of C (Conant et al. 2001). As a consequence nations have adopted integrated farming practices involving grass species, livestock and crop cultivation. Concept of zero tillage has also been adopted under integrated system (Machado and Freitas 2004).

Emission reduction of CO2 from crop ecosystem can further achieved through incorporation of legume into the pastureland which add to the soil C pool (Soussana et al. 2004; Jhariya et al. 2018a, b). Due to this, the productivity of the ecosystem increases through biologically added N by replacing synthetic fertilizer (Diekow et al. 2005). Practices oriented towards reducing GHG emission from livestock population of grazing lands through proper livestock management can be achieved (Derner et al. 2006). C storage in croplands can be increased through increasing productivity and through increasing nutrient deficiency which results into higher return of litter followed by soil C storage (Conant et al. 2001). Care should be taken that addition of N fertilizer stimulates the N2O emissions (Conant et al. 2005). Irrigation activity in grassland ecosystem tends to promote soil C increase (Schlesinger 1999). Use of strategies to increase nutrient use by plants can reduce the emission of N2O (Dalal et al. 2003). This strategy is little bit problematic for grassland ecosystem due to nutrient input from the grazing livestock in the form of defecations as well as unequal distribution nutrients in the crop ecosystem (Oenema et al. 2005).

Biomass burning at the onsite level significantly contributes towards climate change. It gives off CH4 and N2O along with hydrocarbon compounds and other nitrogenous emissions. They undergo secondary chemical reactions leading to formation of trophospheric ozone which is considered to be a powerful GHG. Further, biomass burning leads formation of aerosols smoky in nature resulting into warming of the atmosphere or cooling effect (Andreae et al. 2005; Venkataraman et al. 2005). It also reduces the albedo value of the land surface resulting into warming (Beringer et al. 2003). Further, combustion of wood and grassland area can have negative effect as the grassland as savannah occupies 1/8th surface area of the world (Scholes and van der Merwe 1996).

Agroecosystem is an integrated unit from which GHG emission takes place from various sectors. Further, the energy footprint seems to be higher which leads to mega event of climate change, global warming and other forms of environmental pollution. Therefore, the climate footprint also increases which shows deleterious impact over agricultural productivity crop yield, livestock production and other associated products on long-term basis. It was observed that increasing C storage within agro-products may store up to 83 MtC annually during the last four decades. This leads to a tentative removal of CO2 in the range of 3–7 Mt. CO2 from the atmosphere which is very minor amount from mitigation perspective. As per the reports non-CO2 GHGs emission from the farming practices at the global level may reach up to 6116 Mt. CO2-eq annually till 2005 tends to contribute up to 12% of GHGs emission from anthropogenic sources (US-EPA 2006a).

Further, for non-CO2 contribution of GHGs agriculture tends to contribute 47% along with 58% from the anthropogenic source. It was observed that N2O from soil and CH4 from ruminants contributed 38% and 32%, respectively, as non-CO2 emission till 2005 (US-EPA 2006a). The other potential sources include the burning of the biomass, paddy cultivation and activity such as composting, etc. It is seen that CO2 emission from agricultural sector is not evaluated due to incorporation in the process of land use change and forestry practices. According to IPCC (2001) the CO2 inflow and outflow between agroecosystem and atmosphere varies significantly. According to the estimates given by US-EPA (2006b) net emission of CO2 from agricultural soil tends to be in minute quantity (1%) when compared to the anthropogenic sources. The non-Annex-I countries have contributed 74% of GHG emission from the agricultural sector till 2005. In these countries N2O appeared to be the main output as GHGs from the agricultural sector. In case of Caribbean and Latin American countries the fermentation process seems to be the dominant source of GHG emission (US-EPA 2006a). This is dependent upon the large number of livestock population present in the area which represents up to 1/4th of the world population of livestocks (FAO 2003).

GHG emissions from rice production along with biomass burning were found to contribute more than 90% of the emission of the globe. It was observed that CH4 emission takes place from paddy cultivation in various parts of Asian sub-continents where it is the staple food crops. Further, biomass burning taking place in Africa and Latin American countries contributes up to 74% of the emission. Further, manure should be properly managed in order to reduce the emission from both developing and developed countries (US-EPA 2006a). However, the inflow and outflow balance in agroecosystem in relation to CO2 emission is unpredictable and may vary case to case basis. As per the reports of US-EPA (2006b) some nations reported net emission while others reported net removal of CO2.

Considering the energy and climate footprint of agroecosystem it is very important to mitigate them in order to address the issue of climate change and global warming. Moreover, sectors specific approach is required in order to reduce the GHG emission and thus the energy and climate footprint. Firstly, the management of cropland needs to be done properly in order to reduce net GHG emission. In this approach agronomic practices that lead to higher yield along with higher C storage in the soil need to be implemented (Follett 2001). Typical examples include crop rotation, cultivation of perennial crops, lesser of fallow land, etc. would serve the purpose (Freibauer et al. 2004). In general addition of N fertilizer is deleterious in nature but under nutrient deficient conditions adding nutrients may promote C storage in soil. However, proper care should be taken about the N2O emission from N fertilizer and CO2 from synthetic fertilizers (Gregorich et al. 2005).

Nature based cropping system could be highly fruitful in reducing agrochemical inputs along with GHG emission (Paustian et al. 2004). Crop rotation in terms of plantation of leguminous crops may be a fruitful strategy for N2O emission reduction (Rochette and Janzen 2005). Another approach includes provision of vegetative cover between successive crops or rows of plantation may also prove fruitful for reducing emission which builds up soil C and helps to mobilize the unused N in the soil (Freibauer et al. 2004).

It was observed that the synthetic fertilizer applied as nutrient source is not properly utilized by the crops (Galloway 2003). The excess N leads to emission of N2O (McSwiney and Robertson 2005). Increasing the efficiency for proper N utilization may lead to lesser GHG emission. Volatilization of N and its subsequent release if properly managed becomes very effective for reduction of N2O emission. Various methods have been attempted by several workers to increase the N use efficiency of crops. In this context, precision farming, use of slow release fertilizer, inhibition of nitrification are found to be fruitful to reduce N loss. Therefore, N becomes more accessible to plant roots and thus fulfils the plant requirement and emission reduction takes place (Monteny et al. 2006).

In the process of tillage management, shifting towards no-tillage or reduce tillage may prove to be fruitful in reducing GHG emission. This has now being widely adopted by various countries across the globe (Cerri et al. 2004). Further, higher tillage or maximum tillage leads to disintegration of soil particles leading to higher rate of decomposition and erosion which contributes significantly towards C loss (Madari et al. 2005). The application of no-tillage may give good results but the results are controversial both in terms of C gain or reducing N2O emission (Helgason et al. 2005). The results vary in terms of N2O emission on area-to-area basis along with prevailing climatic conditions. Cropping system based on retaining crop residues increases soil C storage and becomes the base materials for formation of soil organic matter. Therefore, burning of stable mulches needs to be avoided (Cerri et al. 2004).

Irrigation is a crucial factor in agriculture sector as it regulates the production and yields. It was observed that irrigation of agroecosystem at higher level tend to increase the emission of CO2. On the other hand the use of fuels may also lead to emission of GHG, hydrocarbons and other air pollutant into the atmosphere. However, proper irrigation may increase the yield as well as C storage from the biomass of the crops (Lal 2004a). Further, proper drainage under humid climate increases the soil C and productivity along with reduced N2O emission (Monteny et al. 2006). Cultivation practices such a wetland rice system may be used for reducing CH4 emission (Khalil and Shearer 2006). This is due to the fact that varieties of rice offer important mitigatory approach of CH4 emission reduction (Akiyama et al. 2005). Under off season for paddy cultivation CH4 emission is reduced through sustainable water management in the form of sprinkler or drip irrigation and avoiding water logging (Xu et al. 2003). The two fold process of increasing soil organic C in one hand and proper composting of the organic residues can help to reduce CH4 emission as well as paddy productivity (Pan et al. 2006).

Conversion of crop land into land cover changes in the form of wind breaks, shelter belts could be fruitful to promote C storage. It was observed that the conversion of cropland to grassland helps to accumulate sufficient soil C (Lal 2004b).

Pasture land management is another important aspect in order to reduce GHG emission. Research studies reveal that grazing time and intensity influences the rate of C storage in soil (Conant et al. 2005). Increasing the deficiency of nutrients increases the litter deposition and further decomposition to add to soil C pool (Conant et al. 2001). Irrigation in grassland may increase soil C storage (Conant et al. 2001).

14.8 Role of Agroecosystem Towards Reducing Climate Change and Environmental

14.8.1 Sustainability in the Context Climate and Energy Footprint

Agrotechnology is an important aspect from the perspective of climate change. Under this process the ability of the green plant to absorb CO2 and its further sequestration to soil in the form of biomass can be exploited for a C neutral environment (IPCC 2018).The level of C sequestration may increase on the basis of time span. However, research data reveals that agriculture practices are the significant contributor of GHGs through anthropogenic means (IPCC 2018). Agricultural area expansion through deforestation and grassland destruction are the potential anthropogenic activity increasing the C footprint of the agriculture production. Other potential process includes emission of methane from paddy fields, release of N2O from degradation of unused N fertilizer and ruminant fermentation process. Reports of IPCC reveal that more than 30% of GHG emission results from cultivation practice and altered land use. In the food processing steps, if transportation and consumption of a product is considered then the emission of GHGs goes up to 40%. Therefore, agriculture is the main issue that needs to be addressed in order to mitigate the climate change through GHG emission reduction.

It was observed that the values of climate footprint vary significantly depending upon the cultivation process. As a consequence farming at small scale depending on indigenous inputs is much more eco-friendly than the industrialized fertilizer based intensive cultivation practice. Further, small-scale production for domestic consumption is far more fruitful in comparison marketing based agriculture production in terms of mitigating climate change. Soil management on the basis of climatic condition could be a good option to reduce both the energy and climate footprint and address environmental sustainability of the agroecosystem.

The cultivable land should be kept under vegetal cover and we should move towards zero tillage agriculture practice. This would help in buildup of soil C pool and hence fertility of soil. Some strategies such decomposition of stubble mulches within the soil, implementation of agroforestry systems may help to regain the sustainability of the agroecosystem. For emission reduction and associated reduction of climate and energy foot print concept such as organic farming, biofertilizer technology, use of biopesticides instead of energy intensive synthetic fertilizer and other agrochemical use can be implemented in order to reduce the energy input and output from the agroecosystem. The energy crisis situation has led to the pathway of renewable energy resources along with efficient use of energies. In order to achieve that regenerative practices in agriculture, waste reduction, sequestering more C in the soil followed by emission reduction from the agro-based food products are required. Shifting towards renewable forms of energy can mitigate up to 55% of GHGs emissions.

Circular economy can be effectively utilized for emission reduction up to 49% of GHGs and may thus reduce half of the emission till 2050. Emissions from the AFOLU shared 24% of overall GHGs emission. Production of food is an important component of AFLOU which harbours diverse form of activities and therefore approximates up to 8.4 billion tonnes CO2e to be emitted till 2050. It is seen that 60% of emission is associated with the food production system. As for instance production of beef leads to release of more methane than release of CH4 from paddy cultivation. High tillage operation leads to release of soil C in to atmosphere, use of nitrogenous fertilizer for crop production leads to release of N2O. The amount of food wasted in the life cycle of a product has a significant contribution in emission. Circular economy approach would be highly fruitful in reducing C emission by acting as an integrated unit in the form of sequestering C in soil, reducing C emission, degrading the waste followed by natural system regeneration. According to one estimate if the organic matter level in soil is increased up to 3% it may reduce 1 trillion tonnes CO2eq of C emission. Practices such as the composting can do well good in this aspect. Further the composting process leads to release of CO2 which has a lesser global warming potential than CH4. Further use of compost may also reduce the use of synthetic chemical fertilizer which may reduce the emission of N2O. This would lead to reduce the climate and energy footprint considerably.

Regenerative agriculture is the process that aims towards adopting eco-friendly technology, maintaining soil health and crop biodiversity. Improving C sequestration for a particular area on the basis of soil, topography, prevailing land use practices such as integration of tree crops within the pasture land, cropping perennial crops which add more C to the soil and other modes of eco-friendly agrotechnologies would serve the purpose. Controlled grazing can do world good in reducing emission. Strategies include rotation of feed stock, rotation of livestock population, maintain the density of the livestock population may provide an annual emission reduction of about 1.4 billion tonnes CO2eq. till 2050. Using the concept of regenerative cropland concept by adopting zero tillage activity, intercropping practices, use of organic amendments may lead to higher C sequestration in the soil may benefit up to 2.5 billion tonnes CO2eq.

14.9 Conclusion

Agroecosystem is a key component which needs to monitor in terms of its energy and climate footprint. Addressing sustainability on the issue of footprint is the biggest challenge of the present century. Both the climate and energy footprint address the issue of GHGs emission from various sectors of agriculture. It is crucial from combating climate change perspective. The livestock population and its associated grazing land as a major component of agroecosystem have proven to be the significant source in GHG emission. Both the sectors of crop production and livestock management involving the agroecosystem has reflected significant energy use, emission of GHG leading to gradual increase in the energy and climate footprint value. Research and development techniques have highlighted various methods and techniques to be implemented at the farm level in order to reduce the emission of GHG from its various spheres. This would help to reduce the energy and climate footprint of the agroecosystem and would help to achieve the environmental sustainability of the agroecosystem.

14.10 Research and Development and Future Perspectives towards Energy and Climate Footprint for Environmental Sustainability

Research and development activities are required for reducing climate and energy footprint in order to move towards a greener future for agroecosystem. Adoption of zero emission machineries and farm equipment, optimization of the feed material of the livestock population for lesser fermented emission of GHG (Sass 2003; Harmsen 2019), expansion of anaerobic manuring, improve livestock production efficiencies (FAOSTAT 2019), reduced application of N fertilizer in the developing world, optimum fertilizer application in paddy cultivation (Bell et al. 2010), proper processing of feed grain for lesser fermentation and lesser release of CH4 (Forsgren et al. 2019), nitrification process inhibition on pasture land (Munoz and Llanos 2012) could provide significant result in emission reduction.

Conversion of fuel based equipment to zero emission through manual methods would be highly fruitful in terms of energy saving and emission reduction. Policies regarding proper development of zero emission equipment would help to reduce the emission. Therefore, research and development activities need to be aimed in the aforesaid direction (Munoz and Llanos 2012). Scientific research should be focused on breeding programmes of animal husbandry towards reducing ruminant fermentation process. Researches reveal that 20% of CH4 emission from the livestock comes from the germline (Bell et al. 2010). From US perspective genetically modified products may reduce the methane load up to 11 kgs per cow. Fertilizer amendments in the form of ammonium sulphate and gypsum can reduces the activity of methanogenic bacteria present in paddy field followed by CH4 emission reduction.

Another important research area towards reducing emission reduction is through proper monitoring and evaluation of livestock health which may aid towards emission reduction through optimum fermentation and proper manure management. Animal feed optimization through higher fat diet is another important aspect of reducing the fermentation process. Fat tend to reduce the fermentation of organic matter and improve its further digestibility along with inhibiting methanogenic bacteria to perform their activity in the rumen of the ruminant animals. The dry matter percentage of fat is increased up to 3% in the cattle feed. As a consequence of that CH4 emission reduces up to 4% (IRP and UNEP 2018). Reports have further revealed that cattle feed material such as propionate precursors reduce the cattle fermentation without affecting the growth of the animals. It also mentioned that 13% reduction in fermentation rate along with 2.5% productivity increase has led to 15% reduction in CO2 emission (Ellen MacArthur Foundation 2017).

Improved management of the flooding during paddy cultivation through alternate wetting and drying method has shown to reduce emission reduction to considerable level. Capture of CH4 through anaerobic digestion to reduce GHG emission can be done through the system of hog manure approach. Different types of anaerobic digestors are available for production of biogas which can be used for electricity generation and thus they reduce the GHG emission. Processes such as mechanical flaking improve the grain digestion. This reduces the particle size for greater level of microbial decomposition and thus it can reduce the potential GHG emission. Research studies have shown that such approaches may reduce enteric fermentation up to 15% followed by improved productivity up to 5%. Transplantation of rice seedlings for sowing purpose may be modified through direct dry seeding method. Under this method the field needs not to be flooded for a month thus inhibiting the methanogens for producing and emitting CH4. Such approaches can reduce emission of CH4 up to 45% on per hectare basis. Increasing the production efficiency of livestock population through hormones, and other forms of biomolecular applications in the form of various growth promoting substances that is alternative to antibiotics may reduce the GHG emission lead to 15% CO2 emission reduction (Material Economics 2018).

Use of substances that inhibit nitrification process in pasture land tend to reduce N2O emission (Favier et al. 2018). Zero or low tillage activity tends to conserve soil organic matter which reduces the fuel consumption by the farm machinery up to 75% followed by reduction in the denitrification process and N2O emission up to 18% (UNEP and IEA 2017). Researches at field level has further revealed that use of slow release fertilizer tend to reduce 20% of N2O emission. Such fertilizers fulfil the demand of nutrients required by the crop plants when they require it for growth and development process. In this way they reduce lesser nitrogen loss into the environment (Ellen MacArthur Foundation 2017).

Use of new innovative technologies may also prove good for emission reduction and reducing the footprints of agroecosystem. Simultaneously it would also address the issue of environmental sustainability from future perspective. One such method is the precision agriculture which applies the fertilizer as per the requirement of the crop on per unit area basis through geographical information system and remote sensing based tools. Such approaches tend to reduce the use of excess chemical fertilizer which tends to emission reduction (Zhang et al. 2013). Use of CH4 inhibitors in the feed material has led to 30% reduction in the enteric fermentation. Therefore, future researches should be aimed towards screening of cattle breeds that produces less CH4 after their feeding (Hristov et al. 2015). Future research and various forms of advance technologies (such as gene editing) could play significant part in emission reduction and thus reducing the climate and energy footprint. Improved farming strategies in the form of conversion of anaerobic system of paddy cultivation to anaerobic system may lead to reduction in CH4 emission.