A Lifetime Perspective on the Chemistry of Soil Organic Matter
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2020, Geochimica et Cosmochimica ActaCitation Excerpt :Other groups such as ammonium and phosphate are also important due to the wide presence of biomolecules in soils (Schnitzer, 1999). The understanding of SOMs experienced a conceptual evolution from polymers (Kononova, 1961; Stevenson, 1994) and macromolecules (Schnitzer, 1999) to supramolecular associations (Piccolo, 2001). The latter has been gradually accepted over the past decades (Sutton and Sposito, 2005).
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2018, Soil and Tillage ResearchCitation Excerpt :Soil organic carbon (SOC) pools, dynamics and storage are affected by conventional (CT) and no-tillage (NT) systems (Angers et al., 1995; Six et al., 1999; Lupwayi et al., 2004; Huggins et al., 2007; Schjønning et al., 2007; Alvarez and Steinbach, 2009; Beyaert and Voroney, 2011). SOC is the carbon stored in soil organic matter (SOM), which refers to the organic fraction of soil that consists of a mixture of plant and animal residues in various stages of decomposition, microbial biomass, and substances made microbiologically or chemically from by-products (Schnitzer, 2000; Weil and Brady, 2016). Lehmann and Kleber (2015) provides empirical evidence that SOM is a continuum of progressively decomposing organic carbon-containing substances but argues against the formation of stable humic substances.
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