2019
DOI: 10.1016/j.geoderma.2019.07.009
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Ecosystem type effects on the stabilization of organic matter in soils: Combining size fractionation with sequential chemical extractions

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Cited by 29 publications
(25 citation statements)
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“…Our second approach investigated the stabilisation of mineral-associated SOC using sequential chemical extractions at increasing pH, which enhances the solubility of SOC by promoting the desorption of organic matter from mineral surfaces 30,31 . Here, we use extraction strength to represent the energy requirement by microorganisms to access mineral-associated SOC.…”
Section: Methodsmentioning
confidence: 99%
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“…Our second approach investigated the stabilisation of mineral-associated SOC using sequential chemical extractions at increasing pH, which enhances the solubility of SOC by promoting the desorption of organic matter from mineral surfaces 30,31 . Here, we use extraction strength to represent the energy requirement by microorganisms to access mineral-associated SOC.…”
Section: Methodsmentioning
confidence: 99%
“…12 solubilizes ‘resistant SOC’ that is strongly bound to active mineral surfaces and is not solubilized by the previous extractions. Finally, a second NaOH extraction after pre-treatment with 0.1 M sodium dithionite reduces the iron in oxides, hydroxides and sesquioxides, thus solubilizing the organic molecules adsorbed to them 30,31 .…”
Section: Methodsmentioning
confidence: 99%
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“…Nitrogen plays a key role in SOM formation (Billings and Ballantyne 2013) because the C:N ratio of organic matter in the early stages of decomposition is higher than the C:N ratio of the microbial biomass, and microbial decomposers therefore require N from supplemental sources (Hessen et al 2004). Indeed, POM that has undergone little decomposition has a C:N ratio similar to plant material (c. 10-40;Fornara et al 2011;Lavallee et al 2020), which declines as decomposition progresses (Khan et al 2016), resulting in MAOM with a C:N ratio similar to microbial biomass (c. 8-13;Giannetta et al 2019;Lavallee et al 2020). As the transformation of plant material into stabilised SOM requires N, the ability of soils to store C is strongly linked to N availability (Kirkby et al 2013;Paul 2016;Cotrufo et al 2019) and N limitation can reduce the microbial contribution to SOM formation (Khan et al 2016).…”
Section: Introductionmentioning
confidence: 99%
“…In highly weathered tropical soils, SOM stabilisation is often associated with high concentrations of iron (Fe) and aluminium (Al) oxides, which are capable of binding organic compounds into stable organo-mineral complexes (Coward et al 2017). The formation of organo-mineral complexes by Al and Fe oxyhydroxides often involves nitrogenous compounds (Giannetta et al 2019) which suggests that N availability might also play a key role in SOM stabilisation in tropical soils. Although N availability in lowland tropical soils is often high relative to other nutrients, tropical forest nutrient cycles are also characterized as efficient, and a large proportion of the nutrients required for plant growth is recycled in litterfall (Vitousek 1984).…”
Section: Introductionmentioning
confidence: 99%