22 research outputs found
Bio-energy retains its mitigation potential under elevated CO2
Background
If biofuels are to be a viable substitute for fossil fuels, it is essential that they retain their potential to mitigate climate change under future atmospheric conditions. Elevated atmospheric CO2 concentration [CO2] stimulates plant biomass production; however, the beneficial effects of increased production may be offset by higher energy costs in crop management.
Methodology/Main findings
We maintained full size poplar short rotation coppice (SRC) systems under both current ambient and future elevated [CO2] (550 ppm) and estimated their net energy and greenhouse gas balance. We show that a poplar SRC system is energy efficient and produces more energy than required for coppice management. Even more, elevated [CO2] will increase the net energy production and greenhouse gas balance of a SRC system with 18%. Managing the trees in shorter rotation cycles (i.e. 2 year cycles instead of 3 year cycles) will further enhance the benefits from elevated [CO2] on both the net energy and greenhouse gas balance.
Conclusions/significance
Adapting coppice management to the future atmospheric [CO2] is necessary to fully benefit from the climate mitigation potential of bio-energy systems. Further, a future increase in potential biomass production due to elevated [CO2] outweighs the increased production costs resulting in a northward extension of the area where SRC is greenhouse gas neutral. Currently, the main part of the European terrestrial carbon sink is found in forest biomass and attributed to harvesting less than the annual growth in wood. Because SRC is intensively managed, with a higher turnover in wood production than conventional forest, northward expansion of SRC is likely to erode the European terrestrial carbon sink
The European land and inland water CO2, CO, CH4 and N2O balance between 2001 and 2005
Globally, terrestrial ecosystems have absorbed about 30% of anthropogenic greenhouse gas emissions over the period 2000–2007 and inter-hemispheric gradients indicate that a significant fraction of terrestrial carbon sequestration must be north of the Equator. We present a compilation of the CO2, CO, CH4 and N2O balances of Europe following a dual constraint approach in which (1) a landbased
balance derived mainly from ecosystem carbon inventories and (2) a land-based balance derived from flux measurements
are compared to (3) the atmospheric data-based balance derived from inversions constrained by measurements of atmospheric GHG (greenhouse gas) concentrations.
Good agreement between the GHG balances based on fluxes (1294±545 Tg C in CO2-eq yr−1), inventories (1299±200 Tg C in CO2-eq yr−1) and inversions (1210±405 Tg C in CO2-eq yr−1) increases our confidence that the processes underlying the European GHG budget are well understood and reasonably sampled. However, the uncertainty remains large and largely lacks formal estimates. Given that European net land to atmosphere exchanges are determined by a few dominant fluxes, the uncertainty of these key components needs to be formally estimated before efforts could be made to reduce the overall uncertainty. The net land-to-atmosphere flux is a
net source for CO2, CO, CH4 and N2O, because the anthropogenic emissions by far exceed the biogenic sink strength.
The dual-constraint approach confirmed that the European biogenic sink removes as much as 205±72 Tg C yr−1 from fossil fuel burning from the atmosphere. However, This C is being sequestered in both terrestrial and inland aquatic ecosystems. If the C-cost for ecosystem management is taken into account, the net uptake of ecosystems is estimated to decrease by 45% but still indicates substantial C-sequestration.
However, when the balance is extended from CO2 towards the main GHGs, C-uptake by terrestrial and aquatic ecosystems
is offset by emissions of non-CO2 GHGs. As such, the European ecosystems are unlikely to contribute to mitigating the effects of climate change.JRC.H.2-Air and Climat
High Resolution Maps of Potential Biomass Supply from Marginal Lands around a Biorefinery.
MAGIC project, Deliverable D5.
Combining a land surface model with life cycle assessment for identifying the optimal management of short rotation coppice in Belgium
status: publishe
A systematic review of environmental and economic impacts of smart grids
Smart grids (SGs) have a central role in the development of the global power sector. Cost-benefit analyses and environmental impact assessments are used to support policy on the deployment of SG systems and technologies. However, the conflicting and widely varying estimates of costs, benefits, greenhouse gas (GHG) emission reduction, and energy savings in literature leave policy makers struggling with how to advise regarding SG deployment. Identifying the causes for the wide variation of individual estimates in the literature is crucial if evaluations are to be used in decision-making. This paper (i) summarizes and compares the methodologies used for economic and environmental evaluation of SGs (ii) identifies the sources of variation in estimates across studies, and (iii) point to gap in research on economic and environmental analyses of SG systems. Seventeen studies (nine articles and eight reports published between 2000 and 2015) addressing the economic costs versus benefits, energy efficiency, and GHG emissions of SGs were systematically searched, located, selected, and reviewed. Their methods and data were subsequently extracted and analysed. The results show that no standardized method currently exists for assessing the economic and environmental impacts of SG systems. The costs varied between 0.03 and 1143 M€/yr, while the benefits ranged from 0.04 to 804 M€/yr, suggesting that SG systems do not result in cost savings The primary energy savings ranged from 0.03 to 0.95 MJ/kWh, whereas the GHG emission reduction ranged from 10 to 180 gCO2/kWh, depending on the country grid mix and the system boundary of the SG system considered. The findings demonstrate that although SG systems are energy efficient and reduce GHG emissions, investments in SG systems may not yield any benefits. Standardizing some methodologies and assumptions such as discount rates, time horizon and scrutinizing some key input data will result in more consistent estimates of costs and benefits, GHG emission reduction, and energy savings. © 2016 Elsevier Lt
Greenhouse gas balance of cropland conversion to bioenergy poplar short-rotation coppice
The production of bioenergy in Europe is one of the strategies conceived to
reduce greenhouse gas (GHG) emissions. The suitability of the land use
change from a cropland (REF site) to a short-rotation coppice plantation of
hybrid poplar (SRC site) was investigated by comparing the GHG budgets of
these two systems over 24 months in Viterbo, Italy. This period corresponded
to a single rotation of the SRC site. The REF site was a crop rotation
between grassland and winter wheat, i.e. the same management of the SRC site
before the conversion to short-rotation coppice. Eddy covariance
measurements were carried out to quantify the net ecosystem exchange of
CO<sub>2</sub> (<i>F</i><sub>CO<sub>2</sub></sub>), whereas chambers were used to measure N<sub>2</sub>O and
CH<sub>4</sub> emissions from soil. The measurements began 2 years after the
conversion of arable land to SRC so that an older poplar plantation was
used to estimate the soil organic carbon (SOC) loss due to SRC
establishment and to estimate SOC recovery over time. Emissions from
tractors and from production and transport of agricultural inputs
(<i>F</i><sub>MAN</sub>) were modelled. A GHG emission offset, due to the substitution of natural gas with SRC biomass, was credited to the GHG budget of the SRC site. Emissions generated by the use of biomass (<i>F</i><sub>EXP</sub>) were also
considered. Suitability was finally assessed by comparing the GHG budgets of
the two sites. CO<sub>2</sub> uptake was 3512 ± 224 g CO<sub>2</sub> m<sup>−2</sup>
at the SRC site in 2 years, and 1838 ± 107 g CO<sub>2</sub> m<sup>−2</sup> at
the REF site. <i>F</i><sub>EXP</sub> was equal to 1858 ± 240 g CO<sub>2</sub> m<sup>−2</sup>
at the REF site, thus basically compensating for <i>F</i><sub>CO<sub>2</sub></sub>, while it was
1118 ± 521 g CO<sub>2</sub> m<sup>−2</sup> at the SRC site. The SRC site could
offset 379.7 ± 175.1 g CO<sub>2</sub>eq m<sup>−2</sup> from fossil fuel
displacement. Soil CH<sub>4</sub> and N<sub>2</sub>O fluxes were negligible. <i>F</i><sub>MAN</sub>
made up 2 and 4 % in the GHG budgets of SRC and REF sites
respectively, while the SOC loss was 455 ± 524 g CO<sub>2</sub> m<sup>−2</sup>
in 2 years. Overall, the REF site was close to neutrality from a GHG
perspective (156 ± 264 g CO<sub>2</sub>eq m<sup>−2</sup>), while the SRC site was
a net sink of 2202 ± 792 g CO<sub>2</sub>eq m<sup>−2</sup>. In conclusion the
experiment led to a positive evaluation from a GHG viewpoint of the
conversion of cropland to bioenergy SRC
Greenhouse gas balance of cropland conversion to bioenergy poplar short-rotation coppice
The production of bioenergy in Europe is one of the strategies conceived to reduce greenhouse gas (GHG) emissions. The suitability of the land use change from a cropland (REF site) to a short-rotation coppice plantation of hybrid poplar (SRC site) was investigated by comparing the GHG budgets of these two systems over 24 months in Viterbo, Italy. This period corresponded to a single rotation of the SRC site. The REF site was a crop rotation between grassland and winter wheat, i.e. the same management of the SRC site before the conversion to short-rotation coppice. Eddy covariance measurements were carried out to quantify the net ecosystem exchange of CO2 (FCO2/, whereas chambers were used to measure N2O and CH4 emissions from soil. The measurements began 2 years after the conversion of arable land to SRC so that an older poplar plantation was used to estimate the soil organic carbon (SOC) loss due to SRC establishment and to estimate SOC recovery over time. Emissions from tractors and from production and transport of agricultural inputs (FMAN/were modelled. A GHG emission offset, due to the substitution of natural gas with SRC biomass, was credited to the GHG budget of the SRC site. Emissions generated by the use of biomass (FEXP/were also considered. Suitability was finally assessed by comparing the GHG budgets of the two sites. CO2 uptake was 3512±224 g CO2 m-2 at the SRC site in 2 years, and 1838±107 g CO2 m-2 at the REF site. FEXP was equal to 1858±240 g CO2 m-2 at the REF site, thus basically compensating for FCO2 , while it was 1118±521 g CO2 m-2 at the SRC site. The SRC site could offset 379.7±175.1 g CO2eqm-2 from fossil fuel displacement. Soil CH4 and N2O fluxes were negligible. FMAN made up 2 and 4% in the GHG budgets of SRC and REF sites respectively, while the SOC loss was 455±524 g CO2 m-2 in 2 years. Overall, the REF site was close to neutrality from a GHG perspective (156±264 g CO2eqm-2/, while the SRC site was a net sink of 2202±792 g CO2eqm-2. In conclusion the experiment led to a positive evaluation from a GHG viewpoint of the conversion of cropland to bioenergy SRC
Energy performances of intensive and extensive short rotation cropping systems for woody biomass production in the EU
AbstractOne of the strategies to ensure energy security and to mitigate climate change in the European Union (EU) is the establishment and the use of short rotation woody crops (SRWCs) for the production of renewable energy. SRWCs are cultivated in the EU under different management systems. Addressing the energy security problems through SRWCs requires management systems that maximize the net energy yield per unit land area. We assembled and evaluated on-farm data from within the EU, (i) to understand the relationship between the SRWC yields and spatial distribution of precipitation, as well as the relationship between SRWC yield and the planting density, and (ii) to investigate whether extensively managed SRWC systems are more energy efficient than their intensively managed counterparts. We found that SRWC yield ranged from 1.3 to 24tha−1y−1 (mean 9.3±4.2tha−1y−1) across sites. We looked for, but did not find a relationship between yield and annual precipitation as well as between yield and planting density. The energy inputs of extensively managed SRWC systems ranged from 3 to 8GJha−1y−1 whereas the energy ratio (i.e. energy output to energy input ratio) varied from 9 to 29. Although energy inputs (3–16GJha−1y−1) were larger in most cases than those of extensively managed SRWC systems, intensively managed SRWC systems in the EU had higher energy ratios, i.e. between 15 and 62. The low energy ratio of extensively managed SRWC systems reflected their lower biomass yield per unit area. Switching from intensively managed SRWC systems to extensively managed ones thus creates an energy gap, and will require more arable land to be brought into production to compensate for the yield loss. Consequently, extensification is not the most appropriate path to the success of the wide scale deployment of SRWC for bioenergy production in the EU