Affiliation: | 1. UMR ECOSYS, Université Paris-Saclay, INRAE, AgroParisTech, 91120 Palaiseau, France;2. Soils and Substrates Group, Institute Land-Nature-Environment, University of Applied Science of Western Switzerland Hepia, route de Presinge 150, 1254 Jussy, Geneva, Switzerland Contribution: Conceptualization, Investigation, Writing - review & editing;3. UMR ECOSYS, Université Paris-Saclay, INRAE, AgroParisTech, 91120 Palaiseau, France Contribution: Conceptualization, Investigation, Writing - review & editing, Formal analysis;4. UMR ECOSYS, Université Paris-Saclay, INRAE, AgroParisTech, 91120 Palaiseau, France Agence de l'environnement et de la maîtrise de l'energie (ADEME), 49000 Angers, France Contribution: Conceptualization, Investigation, Writing - review & editing;5. UMR ECOSYS, Université Paris-Saclay, INRAE, AgroParisTech, 91120 Palaiseau, France Contribution: Conceptualization, Investigation, Writing - review & editing;6. Saint Loup Research Institute, La Grande Romelière, 7 rue des chênes, 79600 Saint Loup Lamairé, France Contribution: Conceptualization, Investigation, Writing - review & editing |
Abstract: | Over the last decade, the ecosystem services (ESs) framework has been increasingly used to support mapping and assessment studies for sustainable land management purposes. Previous analysis of practical applications has revealed the significance of the spatial scale at which input data are obtained. This issue is particularly problematic with soil data that are often unavailable or available only at coarse scales or resolutions in various part of the world. In this context, four soil-based ecosystem services, namely biomass provision, water provision, global climate regulation, and water quality regulation, are assessed using three conventional soil maps at the 1:1,000,000, 1:250,000 and 1:50,000 scales. The resulting individual and joint ES maps are then compared to examine the effects of changing the spatial scale of soil data on the ES levels and spatial patterns. ES levels are finally aggregated to landforms, land use, or administrative levels in order to try to identify the determinants of the sensitivity of ES levels to change in the scale of input soil data. Whereas the three soil maps turn out to be equally useful whenever ESs levels averaged over the whole 100 km2 territory are needed, the maps at the 1:1,000,000 and 1:250,000 induced biases in the assessment of ESs levels over spatial units smaller than 100 and 10 km2, respectively. The simplification of the diversity and spatial distribution of soils at the two coarsest scales indeed resulted in local differences in ES levels ranging from several 10 to several 100%. Identification of the optimal representation of soil diversity and distribution to obtain a reliable representation of ESs spatial distribution is not straightforward. The ESs sensitivity to scale effect is indeed context-specific, variable among individual ESs, and not directly or simply linked with the soil typological diversity represented in soil maps. Forested and natural lands in the study area appear particularly sensitive to soil data scales as they occupy marginal soils showing very specific ESs signatures. |