Biofuels Induced Land Use Change Emissions: The Role of Implemented Land Use Emission Factors

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2.1. Common Approach in Calcualting ILUC Emissions

As noted in the Introduction, two sets of data are required to calculate ILUC emissions from a biofuel pathway: (i) estimated land-use changes due to an increase in consumption/production of the selected biofuel, and (ii) a set of LUEFs for the relevant land-use transitions. In general, regardless of differences across modeling practices, the following stylized formula has been implemented to calculate an ILUC emissions value for a given pathway (Zhao et al. [12]):

I L U C = i , k , r L i , k , r   ×   L U E F i , k , r T × E

In this formula, the index i represents the list of all types of land transitions (e.g., forest to cropland, forest to pasture, etc.), the index k shows spatial resolution (which could represent the national level, agro-ecological level, grid cell, or any other geographical resolution) within each country, and the index r indicates countries. The variables L , L U E F , T, and E are land conversions in hectares, land-use emission factors measured in gCO2e per hectare, amortization time horizon in years, and annual energy produced by the pathway under study measured in megajoules (MJ), respectively. Therefore, an ILUC emissions value estimates emissions in gCO2e/MJ.

Hence, one needs to determine L , L U E F , T, and E in calculating ILUC emissions values. The last two variables of this list are usually predetermined by the accounting system and fuel type, respectively. However, the first two variables are unknown and must be estimated, simulated, or measured. A sizeable expansion in production or consumption of a biofuel pathway that uses agricultural feedstocks (e.g., corn, soybeans, or perennial grasses) could induce land-use changes directly or indirectly at the local, national, and international levels (Hertel et al. [13]. The size, location, and type of land-use changes (i.e., L i , k , r ) could vary based on the characteristics of the pathway under consideration and on many economic and biophysical variables. Unfortunately, land-use changes are not directly observable or measurable. Economic models have been used to estimate land-use changes. In this paper, we use the results of a well-known computable general equilibrium (CGE) model, GTAP-BIO, which has been widely used in this field of research to assess land-use changes for various biofuel pathways.

2.2. Components and Sources of LUEFs

In calculating ILUC emissions values, one needs to determine the variable L U E F i , k , r for the i, k, and r indices, which is not a trivial task. In principle, this variable should capture all types of carbon fluxes associated with each type of land conversion. These fluxes are driven by changes in biological and mineral carbon pools, including soil organic carbon, carbon stock in above- and belowground live biomass, and dead organic matter and litter. Additionally, some carbon accounting frameworks include forgone carbon sequestration, emissions due to biomass burning through land clearing, and non-CO2 emissions associated with the land use, land-use change, and forestry (LULUCF). Because of differences in background data and the included categories of emissions, alternative data sources provide widely varying estimates of L U E F i , k , r for the same land-use transition and location.

Several foundational data sources in this field include the Harmonized World Soil Database (HWSD) [14], IPCC [15,16], Winrock [17], and Woods Hole [18] datasets of carbon in soil and vegetation. Terrestrial-biogeochemical models such as Century [19,20], Daycent [21], TEM [22], and ISAM [23] have also been widely used to estimate the core components of LUEFs. Additional sources for critical background data on terrestrial carbon pools and associated GHG emissions during land-use transitions include individual studies such as Gibbs et al. [24], Saatchi et al. [25], and Batjes [26].

In addition to the required data on soil and vegetation carbon stocks, depending on the case under study, one may need additional information or use certain assumptions to mix and match L i , k , r and L U E F i , k , r variables. One may follow different approaches and assumptions to facilitate this process, which can cause significant variations in the resulting ILUC emissions values. The following three examples represent different approaches that the AEZ-EF and CCLUB models use to match the GTAP-BIO estimated land-use changes with their emission factors. Example 1: The GTAP-BIO model projects conversion of “cropland pasture” (a category of marginal land) to crop production due to biofuel shocks. In an ad hoc manner, the AEZ-EF model assumes that the soil carbon content for this type of land in each AEZ region is half of that of pasture land. On the other hand, the CCLUB model relies on a terrestrial-biogeochemical model (Century) to evaluate carbon content for this type of land by AEZ. Example 2: The AEZ-EF uses some assumptions and extends the original GTAP-BIO land conversions beyond the land conversions that this CGE model provides to match the land conversions with its emissions factors. For instance, the AEZ-EF model includes emission factors for converting forest or pasture to sugarcane. The GTAP-BIO model does not determine these land conversions. However, the AEZ-EF model uses some assumptions and determines these land conversions. The CCLUB model only uses the original GTAP-BIO land conversions. Example 3: The AEZ-EF uses some assumptions and assigns a portion of converted forest to cropland as forest on peat land, while the CCLUB uses more recent data with a different assumed portion of converted forest to cropland as forest on peat land.

Because the results of the GTAP-BIO model are used in this paper, we use two emissions accounting models that have been developed and used to convert the results of this model to ILUC emissions values. These two models are the AEZ-EF and CCLUB. The AEZ-EF model relies on IPCC, FAO, HWSD, and several other data sources to convert the GTAP-BIO results to ILUC emissions. This model follows the IPCC approach of using the differences in the biomass and soil organic carbon (SOC) pools between land-cover types as the emissions (or sequestration) values from land conversion.

In contrast, CCLUB provides users with Century simulated GHG emissions changes in US domestic land conversions to cropland and the option of using either the Winrock or Woods Hole data sources for international land conversions to simulate biomass and SOC changes between land-use categories over a period of time. As mentioned earlier, using the Century model, the CCLUB model also provides some assessments for the emission factors associated with the land category of “cropland pasture”. In conclusion, the AEZ-EF and CCLUB models use different sources of data on carbon pools and follow different assumptions to convert the results of the GTAP-BIO model to ILUC emissions, especially for US domestic land conversions.

To highlight uncertainties and variations in the data on L U E F i , k , r , we first review four existing sets of emission factors for converting forest to cropland and pasture to cropland: AEZ-EF, TEM, Winrock, and Woods Hole. These datasets have been used in calculating ILUC values for various US biofuel pathways over the past 15 years, but are limited by their reliance on outdated data in assessing emission factors. For example, the AEZ-EF model uses the 2006 IPCC guidelines for national greenhouse gas inventories instead of the new guidelines published in 2019. To highlight the potential impacts of using outdated data, we compare changes in the reference values for SOC stocks obtained from the IPCC 2006 and 2019 guidelines.

Finally, we calculate ILUC emissions values for eight aviation biofuel pathways that can be produced in the US by using the estimated land-use changes provided by the GTAP-BIO model and CCLUB carbon accounting model and compare the results with the corresponding values that have been calculated by the Carbon Offsetting and Reduction Scheme for International Aviation (CORSIA) of the International Civil Aviation Organization (ICAO) [12] using the AEZ-EF model. The eight selected SAF pathways are introduced in the next section. In this paper, we calculate ILUC emissions values for the selected pathways using the AEZ-EF and CCLUB models to highlight their differences.

2.3. A Short Review of GTAP-BIO Model and Implemented L for the Examined SAF Pathways

As mentioned above, the AEZ-EF and CCLUB emission calculators were designed to use the estimated land conversions ( L ) obtained from the GTAP-BIO model. Hence, in this paper, we use the estimated land-use changes obtained from this CGE model which has been widely used in assessing ILUC emissions values due to biofuel production and policy. This global CGE model is an advanced version of the standard GTAP model originally developed by Hertel [27]. This global macro model represents consumers and producers and simulates their behaviors in consuming and producing goods and services to determine their demands and supplies, respectively. It also includes government consumption, international trade, and investment. The standard GTAP model traces the production, consumption, and trade of all goods and services produced across the world by country. However, the standard model and its database do not represent biofuels and their by-products explicitly. The GTAP-BIO model and its database remedy this deficiency and explicitly represent supplies and uses of alternative types of biofuels that are commercially produced around the world [13,28,29,30,31,32]. These biofuels include ethanol produced from grains (e.g., corn and wheat) and sugar crops (e.g., sugarcane and sugar beet) and biodiesel produced from soy oil, rapeseed oil, palm oil, and other types of vegetable oils. Note that using oilseeds for biodiesel production generates oilseed meal and converting grains to ethanol generates distiller’s dried grains with solubles (DDGS). These by-products play an important role when assessing the system-wide land-use effects of a biofuel pathway.

In addition, the GTAP-BIO model represents land uses by the agricultural and forestry sectors and traces their changes due to changes in demands for foods and biofuels. The agricultural sectors in this model include crop producers (rice, wheat, coarse grains, soybeans, rapeseed, palm oil, other oilseeds, sugar crops, and other crops) and livestock producers (dairy farms, ruminants, and non-ruminants). The GTAP-BIO model divides the accessible land across three land-cover categories: forest, pasture/grassland, and cropland. It then allocates pasture land across livestock activities and cropland across crop producers. The model takes into account multiple cropping (producing more than one crop per year on the same cropland), allows the return of unused cropland to crop production if needed, and takes into account yield improvement due to higher crop profitability.

An advanced version of GTAP-BIO has been developed to assess potential land-use changes for pioneering biofuels that are not yet produced at the commercial level. In addition to traditional crops, this model also has the capability to simulate the production of dedicated energy crops such as miscanthus, switchgrass, and poplar. Zhao et al. [12] have used this advanced version of the GTAP-BIO model to estimate land-use changes for a wide range of SAF pathways that can be produced across the world. This study applies the estimated land-use changes provided by Zhao et al. [12] for eight SAF pathways that can be produced in the US. These pathways are: (i) jet fuel produced from soy oil using the hydro-processed ester and fatty acid technology (soy oil HEFA); (ii) jet fuel produced from corn using the iso-butanol alcohol technology (corn ATJ); (iii) jet fuel produced from corn ethanol (corn ETJ); (iv) jet fuel produced from miscanthus using the Fischer–Tropsch technology (miscanthus FTJ); (v) jet fuel produced from switchgrass using the Fischer–Tropsch technology (switchgrass FTJ); (vi) jet fuel produced from poplar using the Fischer–Tropsch technology (poplar FTJ); (vii) jet fuel produced from miscanthus using the iso-butanol alcohol technology (miscanthus ATJ); and (viii) jet fuel produced from switchgrass using the iso-butanol alcohol technology (miscanthus ATJ). The technical details regarding these pathways are provided in the CORSIA Supporting Document [33]. More details about the estimated land-use changes for these pathways are provided in Zhao et al. [12]. The estimated land-use changes for the selected SAF pathways were obtained for the given expansions in their fuel supplies as reported in Table 1.
As shown in Table 1, in addition to jet fuel, some SAF pathways produce a conventional biofuel co-product as well. The co-product biofuels could be ethanol or biodiesel that can be used in road transportation. The biofuel co-products of the HEFA and ETJ technologies are biodiesel and diesel/gasoline, respectively. The ATJ technology produces no co-product biofuel. The total energy output for each pathway (including jet fuel and conventional biofuel) is shown in petajoules and also in billion gallons of gasoline equivalent (BGGE) in Table 1. The variable E presented in the denominator of Equation (1) represents the total energy output of each pathway after conversion to megajoules.

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