Regulation of priming effect by soil organic matter stability over a broad geographic scale on the Tibetan Plateau. Our results show that SOM stability characterized by
chemical recalcitrance and physico-
chemical Global pattern of organic carbon pools in forest soils) and
chemical (labile vs.
recalcitrant SOC) pools in upper 10 cm mineral soils, as well as SOC stock in the O
Zeolites: A Theoretical and Practical Approach with Uses in (Bio)Chemical Processes possible the formation of typical
chemical bonds that are the fingerprint of any zeolitic structure (O
Organic matter chemistry and bacterial community structure regulate decomposition processes in post-fire forest soilsLing L.,
Fu Y.,
Jeewani P.H.,
Tang C.,
Pan S.,
Reid B.J.,
Gunina A.,
Li Y.,
Li Y.,
Cai Y.,
Kuzyakov Y.,
Li Y.,
Su W.-Q.,
Singh B.P.,
Luo Y.,
Xu J. chemical composition (13C NMR), and associated bacterial community structure (16S rRNA gene sequencing
Accumulation of organic compounds in paddy soils after biochar application is controlled by iron hydroxides accumulation after biochar amendment is not solely dependent on the
chemical recalcitrance of biochar, but also
5300-Year-old soil carbon is less primed than young soil organic matter of
chemical recalcitrance and physical protection of soil organic matter (SOM), we showed that leaf litter
Reactive High-Valent Iron Intermediates in Enhancing Treatment of Water by Ferrate) and oxygen-atom transfer (OAT) to oxidize
recalcitrant pollutants are presented. The common constituents
Conversion of cropland to natural vegetation boosts microbial and enzyme activities in soil (0–5 cm) were compared with
chemical functional groups of plant litter identified by 13C NMR spectra
Liquid hot water as sustainable biomass pretreatment technique for bioenergy production: A review among the research community for the production of biofuels and value-added
chemicals. However, biomass