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C/P stoichiometry of dying rice root defines the spatial distribution and dynamics of enzyme activities in root-detritusphere

Wei X.; Razavi B.; Hu Y.; Xu X.; Zhu Z.; Liu Y.; Kuzyakov Y.; Li Y.; Wu J.; Ge T. (2019)

© 2019, Springer-Verlag GmbH Germany, part of Springer Nature. As the primary microbial substrate after shoot cutting, the element stoichiometry of root-detritus (dying or dead roots) influences the enzyme activity in ...
Divergent mineralization of hydrophilic and hydrophobic organic substrates and their priming effect in soils depending on their preferential utilization by bacteria and fungi

Deng S.; Zheng X.; Chen X.; Zheng S.; He X.; Ge T.; Kuzyakov Y.; Wu J.; Su Y.; Hu Y. (2021)

Hydrophilic and hydrophobic organic compounds extracted from 13C-labelled maize residues were incubated with soils to evaluate their mineralization and priming effect (PE) caused by their utilization by microbial groups. ...
Forest conversion to plantations: A meta-analysis of consequences for soil and microbial properties and functions

Wang Y.; Chen L.; Xiang W.; Ouyang S.; Zhang T.; Zhang X.; Zeng Y.; Hu Y.; Luo G.; Kuzyakov Y. (2021)

Primary or secondary forests around the world are increasingly being converted into plantations. Soil microorganisms are critical for all biogeochemical processes in ecosystems, but the effects of forest conversion on ...
Priming alters soil carbon dynamics during forest succession

Qiao N.; Wang J.; Xu X.; Shen Y.; Long X.; Hu Y.; Schaefer D.; Li S.; Wang H.; Kuzyakov Y. (2019)

© 2019, Springer-Verlag GmbH Germany, part of Springer Nature. The mechanisms underlying soil organic carbon (C) dynamics during forest succession remain challenged because amount, quality, and composition of C inputs ...
Weaker priming and mineralisation of low molecular weight organic substances in paddy than in upland soil

Qiu H.; Zheng X.; Ge T.; Dorodnikov M.; Chen X.; Hu Y.; Kuzyakov Y.; Wu J.; Su Y.; Zhang Z. (2017)

© 2017 Elsevier Masson SAS Although soil organic matter (SOM) and microbial biomass pools in flooded paddy soils are generally larger than they are in upland soils, the processes (i.e., slower mineralisation, other types ...

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