Preprints
https://doi.org/10.5194/egusphere-2023-2464
https://doi.org/10.5194/egusphere-2023-2464
10 Nov 2023
 | 10 Nov 2023

Spectroscopic assessment of three ecologically distinct organic carbon fractions of mineral soils

Lewis Walden, Farid Sepanta, and Raphael Viscarra Rossel

Abstract. Soil carbon (C) is heterogeneous and exists in various forms along a decomposition continuum from labile fast-cycling compounds to more persistent forms of C, which can reside in the soil for centuries to millennia. Methods for soil organic C fractionation aim to account for this complexity by separating soil organic C into distinct groups that exhibit similar turnover. Our aims were to (a) fractionate three mineral soils with small C concentrations (<2.5 % C), different textures and mineralogy using a granulometric method to derive the particulate organic C in macroaggregates (POCmac), the particulate organic C in microaggregates (POCmic), and the mineral-associated organic carbon (MAOC), (b) test if mid-infrared (MIR) spectra can discriminate the distinct organic C fractions and characterise the critical organic and mineral functional groups, and c) explore the interactions between the dominant mineral and organic functional groups to elucidate C stabilisation. With a multivariate analyses we found that the MIR spectra use information from mineral and organic frequencies to discriminate the organic C fractions. Closer investigation on specific regions of the MIR spectrum showed that absorptions relating to silicates were more pronounced in the POCmac and POCmic fractions and clay mineral absorptions were stronger in the MAOC fraction. There was little organic C in the POCmic and POCmac fractions, respectively, and their spectra showed mostly mineralogical features. Most of the organic C in the soils was present as MAOC. The stretching vibration of the bonds in the alkyl CH2 molecule was most prominent. However, absorptions from C = C and C = O stretching vibrations, due to alkenes and amides were also present. These molecules are known to form MAOC. We found that the wavenumbers associated with the absorption of alkyl CH2 were positively correlated with the absorption of clay minerals, which may be used to infer the mineral association of organic C. Our results show that MIR spectroscopy can characterise the compositional differences between the C fractions and that the spectra could potentially infer C stabilisation in mineral soils.

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Lewis Walden, Farid Sepanta, and Raphael Viscarra Rossel

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2023-2464', Anonymous Referee #1, 19 Dec 2023
    • AC1: 'Reply on RC1', Lewis Walden, 23 Jan 2024
  • RC2: 'Comment on egusphere-2023-2464', Anonymous Referee #2, 20 Dec 2023
    • AC2: 'Reply on RC2', Lewis Walden, 23 Jan 2024

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2023-2464', Anonymous Referee #1, 19 Dec 2023
    • AC1: 'Reply on RC1', Lewis Walden, 23 Jan 2024
  • RC2: 'Comment on egusphere-2023-2464', Anonymous Referee #2, 20 Dec 2023
    • AC2: 'Reply on RC2', Lewis Walden, 23 Jan 2024
Lewis Walden, Farid Sepanta, and Raphael Viscarra Rossel
Lewis Walden, Farid Sepanta, and Raphael Viscarra Rossel

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Short summary
We characterised the chemical and mineral composition of soil organic carbon fractions with mid-infrared spectroscopy. We identified unique and shared features of the spectra of carbon fractions, and the interactions between their organic and mineral components. These interactions are key to the persistence of C in soils, and we propose that mid-infrared spectroscopy could help to infer stability of soil C.