2020
DOI: 10.1016/j.geoderma.2020.114449
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Amino acids and amino sugars as molecular indicators of the origins and alterations of organic matter in buried tephra layers

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Cited by 5 publications
(2 citation statements)
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“…The high contribution of plant residues to SOC might be the reason for the strong decline in SOC with increasing years of peanut monoculture. Plant residues are most likely more easily mineralized by soil microorganisms than microbial residues (Hobara et al., 2020; Khan et al., 2016).…”
Section: Discussionmentioning
confidence: 99%
“…The high contribution of plant residues to SOC might be the reason for the strong decline in SOC with increasing years of peanut monoculture. Plant residues are most likely more easily mineralized by soil microorganisms than microbial residues (Hobara et al., 2020; Khan et al., 2016).…”
Section: Discussionmentioning
confidence: 99%
“…The distribution of fine roots (<2mm in diameter) in deep soil may be influenced by the existence of buried humic soil. Buried humic soil is often formed by lava flows, volcanic deposits, weathered loess and floods covering surface humic soil (Chaopricha and Marin-Spíotta 2014) and is relatively rich in soil organic matter for deep soil (Hobara et al 2020). Humic volcanic soils possess distinctive properties derived from organic matter, such as high water retention, low bulk density (Takahashi and Dahlgren 2016), and high cation exchange capacity derived from organic matter (Suzuki et al 2005, Kaneko 2015), as compared with other soil types, which can facilitate or accelerate root growth.…”
Section: Introductionmentioning
confidence: 99%