2018
DOI: 10.1016/j.soilbio.2018.08.008
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Increased chemical stability but decreased physical protection of soil organic carbon in response to nutrient amendment in a Tibetan alpine meadow

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Cited by 53 publications
(23 citation statements)
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“…Furthermore, the added N hurt the richness of soil bacteria, which likely reduced SOC mineralization and increased soil C sequestration [28]. Long-term nutrient enrichment might have shifted the mechanisms of C stabilization from physical protection to chemical stabilization via shifting microbial community composition [29]. When M was used as the soil amendment, the application of N was more beneficial for the increase of aromatic C proportion in HAs in Chernozem.…”
Section: Wave Numbers (Cm −1 )mentioning
confidence: 99%
“…Furthermore, the added N hurt the richness of soil bacteria, which likely reduced SOC mineralization and increased soil C sequestration [28]. Long-term nutrient enrichment might have shifted the mechanisms of C stabilization from physical protection to chemical stabilization via shifting microbial community composition [29]. When M was used as the soil amendment, the application of N was more beneficial for the increase of aromatic C proportion in HAs in Chernozem.…”
Section: Wave Numbers (Cm −1 )mentioning
confidence: 99%
“…Verrucomicrobia (5) and Actinobacteria (4) in N30, Bacteroidetes (7) and Fusobacteria (7) in N60, and Spirochaetes (3) and Firmicutes (2) in N90 appeared as the main discriminant clades. Fungal LEfSe indicated that Ascomycota (41,21,18, and 69) and Basidiomycota (15, 7, 8, and 14) were the main discriminant clades, and they displayed sharp changes at the N90 level (Table 5). From these results, we inferred that bacterial groups differed along with fungal groups under SND, thereby suggesting that both bacteria and fungi are sensitive to N levels and that the fungal discriminant clades show an increased response to high N levels.…”
Section: Characteristics Of Microbial Beta-diversity Under Sndmentioning
confidence: 99%
“…Soil microorganisms can be affected by N deposition and features of the soil microhabitat, such as pH [13][14][15], bulk density and water-holding capacity [16,17], particulate size [18,19], and aggregate stability [20,21]. However, alterations in the composition of soil microbial communities due to changes in pH and particle size as a result of N deposition are not well understood despite the importance of microbial communities in the N cycle [15,22,23].…”
Section: Introductionmentioning
confidence: 99%
“…Enzymes rule the biological catabolism of organic and mineral components in the soil. This process is closely related to organic matter, physical properties, and microbial activity and biomass; therefore, it is widely used to assess the quality of the soil, since it indicates changes in microbial activity and the presence of pollutants in the soil [14,20,21].…”
Section: Biological Indicatorsmentioning
confidence: 99%
“…The respiratory coefficient represents the relation between carbon in the microbial biomass and total organic carbon (TOC). This coefficient indicates microbial biomass efficiency in using the available carbon for biosynthesis [21,22].…”
Section: Biological Indicatorsmentioning
confidence: 99%