Abstract
Purpose
There is currently a weak or no link between the indicator scores quantified in life cycle assessment (LCA) and the carrying capacity of the affected ecosystems. Such a link must be established if LCA is to support assessments of environmental sustainability and it may be done by developing carrying capacity-based normalisation references. The purpose of this article is to present a framework for normalisation against carrying capacity-based references and to develop average normalisation references (NR) for Europe and the world for all those midpoint impact categories commonly included in LCA that link to the natural environment area of protection.
Methods
Carrying capacity was in this context defined as the maximum sustained environmental intervention a natural system can withstand without experiencing negative changes in structure or functioning that are difficult or impossible to revert. A literature review was carried out to identify scientifically sound thresholds for each impact category. Carrying capacities were then calculated from these thresholds and expressed in metrics identical to midpoint indicators giving priority to those recommended by ILCD. NR was expressed as the carrying capacity of a reference region divided by its population and thus describes the annual personal share of the carrying capacity.
Results and discussion
The developed references can be applied to indicator results obtained using commonly applied characterisation models in LCIA. The European NR are generally lower than the global NR, mainly due to a relatively high population density in Europe. The NR were compared to conventional normalisation references (NR′) which represent the aggregated interventions for Europe or the world in a recent reference year. For both scales, the aggregated intervention for climate change, photochemical ozone formation and soil quality were found to exceed carrying capacities several times.
Conclusions
The developed carrying capacity-based normalisation references offer relevant supplementary reference information to the currently applied references based on society’s background interventions by supporting an evaluation of the environmental sustainability of product systems on an absolute scale.
Recommendations
Challenges remain with respect to spatial variations to increase the relevance of the normalisation references for impact categories that function at the local or regional scale. The sensitivity of NR to different choices, e.g. threshold value, should be quantified with the aim of understanding and managing uncertainties of NR. For complete coverage of the midpoint impact categories, normalisation references based on sustainability preconditions should be developed for those categories that link to the areas of protection human health and natural resources.
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Notes
Wildlife management, chemistry, medicine, economics, anthropology, engineering and population biology are listed as examples by Sayre (2008).
The concept of resilience may offer a bridge between anthropocentric and eco-centric approaches to environmental management since studies generally show that ecosystems with high genotype diversity and species diversity has a high resilience, meaning in general terms, that they are better at adapting to sudden changes in conditions than ecosystems with lower diversity (Scheffer et al. 2001; Carpenter et al. 2001). The protection of ecosystem structure can therefore be seen both as eco-centric and as being in the enlightened self-interest of man.
Ionizing radiation effects on the natural environment was excluded since the recommended LCIA model was classified as interim by Hauschild et al. (2013).
The reason we could not use the FF of the GWP100 model to make the conversion is that the FF calculates a time integrated increase in radioactive forcing caused by an emission rather than the steady state increase in radioactive forcing or temperature required to convert the two thresholds (1 W/m2 and 2 °C) into carrying capacities according to our definition.
Note that this carrying capacity is much lower than the 2050 goal of 2 tons per capita often mentioned in the climate change debate. The 2 tons per capita target was derived from the RCP2.6 reduction pathway designed to stay below the 2 °C threshold by 2100 (Van Vuuren et al. 2011; IPCC 2013). In the year 2100 of the RCP2.6 reduction pathway CO2 emissions are nearly zero, which is consistent with our low carrying capacity figures for CO2.
We could not use the FF of CFC-11 of the ODP model because it is expressed relative to a reference substance (CFC-11) and not as an absolute steady-state ozone response to changes in emission.
Although the number of daylight hours exceed 8 per day during May–July at all latitudes within Europe, we chose a time frame of 8 h/day for the translation of the time integrated concentration threshold (3 ppm × h AOT40) to a concentration threshold (ppb) to be compatible with the time frame of the recommended indicator of Van Zelm et al. (2008). Had we chosen a longer time frame, e.g. 12 h/day, the concentration threshold would have been only slightly lower (43 ppb instead of 44 ppb) and so would the resulting carrying capacity calculated.
This number is in good agreement with recent conclusions that around 34 % of global terrestrial coverage should be conserved to achieve biodiversity protection goals given patterns and effects of current land conservation (Butchart et al. 2015).
The difference between these two rules is not trivial. Consider the potentially large differences between per capita domestic carrying capacities of Canada and Singapore for the many impact categories related to the availability of land and water as source or sink.
A hysteresis is a phenomenon which causes the exceedance of a threshold to be difficult to revert because the natural system has entered a new stable state characterized by stabilizing feedback mechanisms. In practice, this means that a reduction in environmental intervention of a similar magnitude as the increase in interventions that previously caused the threshold to be exceeded is not sufficient to bring the system back to its original state. Hysteresis has been observed for e.g. the response of shallow lakes to changes in phosphorous loadings (Scheffer 2001).
For instance, increased run-off due to the exceedance of the climate change carrying capacity can lead to a higher loss of reactive nitrogen and phosphorous from fertilizer application, thereby increasing the risk of exceeding carrying capacities for freshwater and marine eutrophication. See Steffen et al. (2015) for elaboration on this topic.
Midpoint is here understood as the point at which the impact pathway of different substances converge (Hauschild et al. 2013). Because this point of convergence varies the impact pathway location of the midpoint varies across impact categories. In comparison the endpoint is consistently located at the of the impact pathway and typically expressed in a metric related to the disappearance of species (Hauschild et al. 2013).
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Acknowledgments
We thank Guus Velders (RIVM), Rosalie van Zelm (Radboud University Nijmegen) and Annie Levasseur (CIRAIG) for assisting with quantifying the carrying capacity for stratospheric ozone depletion, photochemical ozone formation and climate change respectively and Tue Vissing Jensen (DTU) for technical support.
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Bjørn, A., Hauschild, M.Z. Introducing carrying capacity-based normalisation in LCA: framework and development of references at midpoint level. Int J Life Cycle Assess 20, 1005–1018 (2015). https://doi.org/10.1007/s11367-015-0899-2
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DOI: https://doi.org/10.1007/s11367-015-0899-2