2018
DOI: 10.1016/j.scitotenv.2017.12.293
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Biochemical stabilization of soil organic matter in straw-amended, anaerobic and aerobic soils

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Cited by 45 publications
(28 citation statements)
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“…Accumulation of nonpolar organic coatings and development of SWR on sand-based growing media can be mitigated by wetting agents (Cisar et al, 2000;Kostka, 2000). Most wetting agents are nonionic surfactants, which have amphiphilic structures consisting of polar hydrophilic heads and nonpolar hydrophobic tails.…”
mentioning
confidence: 99%
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“…Accumulation of nonpolar organic coatings and development of SWR on sand-based growing media can be mitigated by wetting agents (Cisar et al, 2000;Kostka, 2000). Most wetting agents are nonionic surfactants, which have amphiphilic structures consisting of polar hydrophilic heads and nonpolar hydrophobic tails.…”
mentioning
confidence: 99%
“…Most wetting agents are nonionic surfactants, which have amphiphilic structures consisting of polar hydrophilic heads and nonpolar hydrophobic tails. Due to the high affinity among nonpolar structures, once wetting agents are watered in through irrigation/precipitation, these amphiphilic surfactants attach their nonpolar tails onto nonpolar hydrophobic surfaces, and subsequently increase the overall soil wettability by facing the polar heads toward the by-passing water (Cisar et al, 2000;Dekker et al, 2005;Kostka, 2000). Addition of wetting agents can hence reduce the surface tension of water from 73 to 32 mN m -1 or lower depending on the wetting agent selected and rate used, ultimately facilitating spontaneous wetting and water infiltration into hydrophobic sand (Song et al, 2014a).…”
mentioning
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%
“…Six et al (2000) and Garcia-Franco et al (2015) reported that O-alkyl C groups (such as carbohydrates) in SOC play a critical role in the formation of POM. As an effective indicator of soil quality, POM is closely linked to aggregation and its decomposition can enhance soil microbial activity and consequently the production of transient binding agents (Chen et al 2018). Soil microorganisms also play an important role in the formation of soil aggregates and the C sequestration, and their effects are mainly in the following two aspects.…”
Section: Introductionmentioning
confidence: 99%