Peltre, Clément2; Bruun, Sander3; Du, Changwen4; Thomsen, Ingrid Kaag6; Jensen, Lars S5
1 Department of Agroecology - Soil Fertility, Department of Agroecology, Science and Technology, Aarhus University2 Department of Plant and Environmental Sciences, Faculty of Science, University of Copenhagen,3 University of Copenhagen4 State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences5 KVL6 Department of Agroecology - Soil Fertility, Department of Agroecology, Science and Technology, Aarhus University
Recent progress in microphone sensitivity has dramatically increased the performance of Fourier transform mid-infrared photoacoustic spectroscopy (FTIR-PAS). This technique offers benefits over reflectance spectroscopy techniques because the level of sample reflectance has little effect on the PAS signal. This also means that it should be advantageous for soil analysis because of its highly opaque nature. However, only a limited number of studies have so far applied FTIR-PAS to soil characterization and investigation is still required into its potential to determine soil organic carbon (SOC) degradability. The objective of this study was to assess the potential of FTIR-PAS for the characterisation of the labile fraction of SOC and more classical soil parameters, such as carbon and clay content, for a range of 36 soils collected from various field experiments in Denmark. Partial least squares (PLS) regressionwas used to correlate the collected FTIR-PAS spectra with the proportion of soil organic carbon mineralised after 238 days of incubation at 15 C and pF 2 (C238d) taken as an indicator of the labile fraction of SOC. Results showed that it is possible to predict total organic carbon content, total nitrogen content and the labile fraction of SOC using FTIR-PAS with an accuracy similar to or better than near infrared (NIR) spectroscopy. FTIR-PAS offered the advantage overNIRof allowing identification of chemical compounds that correlated positively or negatively with the labile fraction of SOC. Spectral bands corresponding to aliphatic, methyl, amide III and polysaccharides compounds were positively correlated with C238d, whereas bands corresponding to aromatics, amines, amides II and carboxylic acids were negatively correlated with C238d. In conclusion, FTIR-PAS has proved to be a powerful tool for characterising soil composition and its labile SOC fraction, offering several benefits over reflectance spectroscopy techniques.
Soil Biology and Biochemistry, 2014, Vol 77, p. 41-50