Carbon stocks in Swiss agricultural soils predicted by land-use, soil characteristics, and altitude

Effects of agricultural land-use and land-use change on soil organic carbon (SOC) pools play an important role in the mitigation of the global greenhouse effect. To estimate these effects, baseline SOC data for individual regions or countries are needed. The aim of this study was to quantify current SOC stocks in Swiss agricultural soils, to identify meaningful predictors for SOC, and to estimate historical SOC losses. SOC stocks in mineral soils were estimated from combined georeferenced data for land-use, topography, and profile data (n = 544) from Soil Surveys. Mean SOC density in the layer 0-20 cm ranged between 40.6 +/- 8.9 t ha(-1) (+/-95% confidence interval (CI)) for arable land and 50.7 +/- 12.2 t ha(-1) for favourable permanent grassland, and in the layer 0-100 cm front 62.9 +/- 15.2 t ha(-1) for Unfavourable grassland to 117.4 +/- 29.8 t ha(-1) for temporary Grasslands (leys). SOC stocks in organic soils were quantified separately for intact and cultivated peatlands using data from peatland inventories and Current SOC densities calculated from average peat decay rates. Organic soils account for less than 3% of the total area but store about 28% (47.2 +/- 7.3 Mt) of the total SOC stock of 170 +/- 17 Mt. Land-use type, clay content, and altitude (serving as a climate proxy for grassland soils at higher altitudes) were identified as main SOC predictors in mineral soils. Clay content explained up to 44% of the variability in SOC concentrations in the fine earth of arable soils, but was not significantly related to SOC in grassland soils at higher altitudes. SOC concentration under permanent grassland increases linearly with altitude, but because soil depth and stone content limit carbon storage in alpine grassland soils, no relationship was found between altitude and SOC stock. A preliminary estimate suggested that about 16% of the national SOC stock has been lost historically due to peatland cultivation, urbanisation, and deforestation. It seems unlikely that future changes in agricultural practices could compensate for this historical SOC loss in Swiss agricultural soils. (C) 2004 Elsevier B.V. All rights reserved.