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HAL Id: hal-02601095

https://hal.inrae.fr/hal-02601095

Submitted on 16 May 2020

HAL is a multi-disciplinary open access archive for the deposit and dissemination of sci- entific research documents, whether they are pub- lished or not. The documents may come from teaching and research institutions in France or abroad, or from public or private research centers.

L’archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des établissements d’enseignement et de recherche français ou étrangers, des laboratoires publics ou privés.

Water-stress characterization factors for future oriented LCA

Montserrat Nunez Pineda, S. Pfister, M. Vargas, A. Antón

To cite this version:

Montserrat Nunez Pineda, S. Pfister, M. Vargas, A. Antón. Water-stress characterization factors for future oriented LCA. 24th SETAC Europe meeting, May 2014, Basel, Switzerland. pp.1, 2014.

�hal-02601095�

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Materials & methods

Methodology: Pfister et al. 2009. WSI annual: 0.01 (low stress) to 1 (severe stress)

Regionalisation units: 117 sub-watersheds (Fig 1), compared to 51 watersheds in Pfister et al. 2009 (Fig 2)

Temporal scenarios:

(i)

current situation: current use and availability

(ii)

Short-term future: projections for 2015

(iii)

Mid-term future: projections for 2030

Data sources: Watershed management plans and regional reports on potential effects of climate change

Uncertainty assessment: Latin Hypercube procedure (5,000 runs) with the @Risk software

Conclusions & outlook

Different spatial and temporal resolution results in different CFs. Which is the optimal resolution in connection with the LCI?

Introduction & objectives

Water stress indicators in LCA often rely on information of water use/consumption and water availability in a specific area

These indicators are usually applied to predict impacts of future investments, without considering changed water use patterns and climate change. The latter already affecting regional water availability.

In this context of continuous change, characterisation factors (CFs) should be updated periodically to correctly reflect water stress

Aim: to provide water stress index (WSI) CFs at the sub-watershed scale for three temporal scenarios in Spain

Water-stress characterisation

factors for future oriented LCA

TU248

M. Núñez1,2, S. Pfister3, M. Vargas2, A. Antón2

1 Irstea-UMR ITAP, 361 rue Jean-François Breton BP5095, F-34196 Montpellier, France.

2 IRTA Ctra. Cabrils km 2, 08348 Cabrils, Barcelona, Spain

3 ETH Zurich, Institute for Environmental Engineering, 8093 Zurich, Switzerland [email protected]

Acknowledgements

Decocel Innpacto project, supported by the Spanish Ministry of Economy and Competitiveness and the European Regional Development Funds and Industrial Chair ELSA-PACT, funded by Suez Environment, SCP, BRL, Val d'Orbieu-Uccoar, EVEA, ANR, Irstea, CIRAD/ADEME, EMA, ONEMA, and the region Languedoc-Roussillon Regionalisation units to calculate WSI CFs used in: this study (Fig 1); Pfister et al 2009 (Fig 2)

References

Pfister S, Koehler A, Hellweg S (2009) Assessing the environmental impacts of freshwater consumption in LCA. Environ Sci Technol 43(11):4098–4104

Fig 1)

Fig 2)

Results & discussion

Temporal analysis of the WSI shows a relaxation of water stress over the short-term (Fig 3, 4) followed by a new increase (Fig 5)

Short-term future: increase in water availability. Mid-term future: increase in water use and reduction in water availability Fig 3) WSI current situation Fig 4) WSI short-term future Fig 5) WSI mid-term future

<0.09 0.09- 0.5- >0.91

WSI (m3/m3)

WSI under uncertainty

Mode Median Mean

WSI deterministic

Fig 6

WSI deterministic

Watershed

WSI [-]

Past

(Pfister et al.)

Current situation

Short-term future

Mid-term future

Duero 0.17 (n.a.)

0.19

(0.01-1.00)

0.10

(0.01-1.00)

0.20

(0.01-0.98) Guadiana 0.99

(n.a.)

0.52

(0.01-0.96)

0.53

(0.01-0.96)

0.65

(0.01-0.98)

Tajo 0.53

(n.a.)

0.31

(0.03-1.00)

0.19

(0.02-1.00)

0.25

(0.10-1.00) Guadalquivir 1.00

(n.a.)

0.93

(0.92-1.00)

0.63

(0.17-0.99)

0.72

(0.50-1.00) Ebro 0.26

(n.a.)

0.39

(0.02-1.00)

0.38

(0.03-1.00)

0.55

(0.04-1.00)

Duero Ebro Tajo

Guadiana

Guadalquivir

Table 1: Mean WSIs for the largest watersheds in Spain and four temporal scenarios.

In brackets WSI data range for the internal sub-watersheds

Uncertainty: The WSIs under consideration of uncertainty were higher than the deterministic result for intermediate WSIs (Fig 6)

Comparison to Pfister et al. WSIs: major differences are noticed (Table 1, see legend Figures 3 to 5).

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