Tolerable versus actual soil erosion rates in Europe |
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| Institution: | 1. Department of Agroecology, Aarhus University, Blichers Allé 20, 8830 Tjele, Denmark;2. Earth & Life Institute, TECLIM, Université catholique de Louvain, Mercator, Place Louis Pasteur 3, 1348 Louvain-la-Neuve, Belgium;3. Department of Bioscience, Aarhus University, Vejlsøvej 25, 8600 Silkeborg, Denmark;1. Université de Liège, Gembloux Agro-Bio Tech, BIOSE, Soil Water Plant Exchanges, Passage des Déportés 2, Gembloux, Belgium;2. Université catholique de Louvain, Environmental Sciences, Earth and Life Institute, Croix du Sud 2 L7.05.02., B-1348 Louvain-la-Neuve, Belgium |
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| Abstract: | Erosion is a major threat to soil resources in Europe, and may impair their ability to deliver a range of ecosystem goods and services. This is reflected by the European Commission's Thematic Strategy for Soil Protection, which recommends an indicator-based approach for monitoring soil erosion. Defined baseline and threshold values are essential for the evaluation of soil monitoring data. Therefore, accurate spatial data on both soil loss and soil genesis are required, especially in the light of predicted changes in climate patterns, notably frequency, seasonal distribution and intensity of precipitation. Rates of soil loss are reported that have been measured, modelled or inferred for most types of soil erosion in a variety of landscapes, by studies across the spectrum of the Earth sciences. Natural rates of soil formation can be used as a basis for setting tolerable soil erosion rates, with soil formation consisting of mineral weathering as well as dust deposition. This paper reviews the concept of tolerable soil erosion and summarises current knowledge on rates of soil formation, which are then compared to rates of soil erosion by known erosion types, for assessment of soil erosion monitoring at the European scale.A modified definition of tolerable soil erosion is proposed as ‘any actual soil erosion rate at which a deterioration or loss of one or more soil functions does not occur,’ actual soil erosion being ‘the total amount of soil lost by all recognised erosion types.’ Even when including dust deposition in soil formation rates, the upper limit of tolerable soil erosion, as equal to soil formation, is ca. 1.4 t ha? 1 yr? 1 while the lower limit is ca. 0.3 t ha? 1 yr? 1, for conditions prevalent in Europe. Scope for spatio-temporal differentiation of tolerable soil erosion rates below this upper limit is suggested by considering (components of) relevant soil functions. Reported rates of actual soil erosion vary much more than those for soil formation. Actual soil erosion rates for tilled, arable land in Europe are, on average, 3 to 40 times greater than the upper limit of tolerable soil erosion, accepting substantial spatio-temporal variation. This paper comprehensively reviews tolerable and actual soil erosion in Europe and highlights the scientific areas where more research is needed for successful implementation of an effective European soil monitoring system. |
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