Assessment of organic carbon in soils: A comparison between the Springer-Klee wet digestion and the dry combustion methods in Mediterranean soils (Southern Italy)

Soil organic carbon (SOC) is the largest carbon pool in the terrestrial biosphere and it is among the most important factors responsible for conservation of soil quality. Automated dry combustion techniques are gradually replacing traditional quantification methods based on wet digestion chemistry. Critical comparison of different methods is fundamental to reevaluate archives of SOC data and accurately assess and model long-term carbon stock variation and should be performed for different soil types and management conditions. Two analytical methods, the Springer–Klee wet digestion and the dry combustion using an automated analyser,were compared for soils typical of a Mediterranean environment in Southern Italy. Soil sampleswere collected from three sites, at two depths. Soils were fine textured (from clay–loam to clay) with total carbonate ranging from 6.6 to 16.7 g 100 g−1. SOC content varied from 6.92 to 28.86 g kg−1 (as average of the two methods), with values and ranges typical of Southern Europe. On average, Springer–Klee method gave slightly higher values and showed greater data variability. This behaviour, in agreement with other studies, can be attributed to the reaction of K2Cr2O7 with other soil constituents and to analytical constraints. Our results suggest high consistency between Springer– Klee and dry combustion techniques and show recoveries close to one both for the whole dataset and for data grouped per experimental site or soil depth. Linear regression equations between the two methods were slightly affected by different soil types (P= 0.0621). The best fitting of the relationship was a linear regression passing through the origin for the whole dataset (R2adj = 0.965; RPD = 3.41). The strong overall agreement observed between the twomethods would enable the direct comparison of newdata setwith those already existing in Southern Italy for soils with similar characteristics.