177,159 research outputs found

    The molecular composition of humus carbon: Recalcitrance and reactivity in soils

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    Soil organic C (SOC) is the largest terrestrial reservoir in the biosphere, accounting for 1500–1770 Pg, as compared to C stocks of vegetation (450– 650 Pg) (IPCC, 2013). Although humus C represents from 60% to 80% of SOC, its dynamics still remain poorly understood after nearly a century of study, due to the multiplicity of factors that affect stabilization of humic matter. Industrial agricultural practices accelerate the decline of humus content in soil, and, consequently, the reduction of soil fertility, biodiversity, and soil structural stability (Fontaine et al., 2007; Reeves, 1997), while enhancing greenhouse gases (GHG) emissions from soil (Smith et al., 2014). Because it is the specific molecular composition of the soil Humeome that significantly affects SOC storage dynamics (Woo et al., 2014), soil basal respiration (Fang et al., 2005), and humus-plant relationships (Canellas and Olivares, 2014), a rigorous identification of the molecular structure of the components of soil humus C is necessary, if any technological control of its content and dynamics can ever be introduced

    State of the art of CPMAS 13C-NMR spectroscopy applied to natural organic matter

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    The structural and conformational characteristics of humic carbon backbones were studied using NMR spectroscopy. Cross-polarized spectroscopy was used to investigate the composition of purified humic substances. High spin rate was obtained by reducing the size of rotors. Protons irradiation eliminated the heteronuclear dipolar interactions. It was found that the NMR signals were reduced due to the mobility of humic material inside the rotors
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