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dc.contributor.author | Wei X. | |
dc.contributor.author | Razavi B. | |
dc.contributor.author | Hu Y. | |
dc.contributor.author | Xu X. | |
dc.contributor.author | Zhu Z. | |
dc.contributor.author | Liu Y. | |
dc.contributor.author | Kuzyakov Y. | |
dc.contributor.author | Li Y. | |
dc.contributor.author | Wu J. | |
dc.contributor.author | Ge T. | |
dc.date.accessioned | 2020-01-15T21:17:13Z | |
dc.date.available | 2020-01-15T21:17:13Z | |
dc.date.issued | 2019 | |
dc.identifier.issn | 0178-2762 | |
dc.identifier.uri | https://dspace.kpfu.ru/xmlui/handle/net/155529 | |
dc.description.abstract | © 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 root-detritusphere. However, the effect of the C/P ratio of root-detritus on the dynamics and distribution of enzyme activities is little revealed. We hypothesised that P fertilisation would decrease the C/P ratio of root-detritus, therefore affecting the hotspot areas and hot moments of C-acquiring and P-acquiring enzyme activities, as well as their activity ratio (C/P acquisition ratio). Root-detritus of low (59.0) and high (170.8) C/P ratios was produced in P-poor soil with and without P fertilisation, respectively. In situ soil zymography showed that the distribution of C-acquiring enzymes (β-glucosidase and cellobiohydrolase) was more associated with root-detritus than P-acquiring enzymes (acid and alkaline phosphomonoesterase). P fertilisation increased the hotspot areas of C-acquiring enzyme activities over the experiment, without influencing their temporal dynamics. However, its effect on phosphomonoesterase activities depended on the decomposition and delayed the appearance of the highest hotspot areas. P supply met the microbial demand in P-fertilised soil, with high C/P acquisition ratio and constant stoichiometry of microbial biomass C (MBC)/microbial biomass P (MBP). A low C/P acquisition ratio and high MBC/MBP in non-fertilised soil was observed, indicating P limitation for microorganisms. After the 150-day incubation, Olsen P significantly increased in P-fertilised soil (P < 0.05), whereas it decreased in the root-detritusphere of non-fertilised soil. We conclude that the decomposition of root-detritus with a low C/P ratio has potential to improve soil P availability; however, C-P imbalance may increase during the decomposition of root-detritus with a high C/P ratio. | |
dc.relation.ispartofseries | Biology and Fertility of Soils | |
dc.subject | C/P acquisition ratio | |
dc.subject | Hot moments | |
dc.subject | Hotspot areas | |
dc.subject | P fertilisation | |
dc.subject | Root-detritus C/P ratio | |
dc.subject | Root-detritusphere | |
dc.subject | Soil zymography | |
dc.title | C/P stoichiometry of dying rice root defines the spatial distribution and dynamics of enzyme activities in root-detritusphere | |
dc.type | Article | |
dc.relation.ispartofseries-issue | 3 | |
dc.relation.ispartofseries-volume | 55 | |
dc.collection | Публикации сотрудников КФУ | |
dc.relation.startpage | 251 | |
dc.source.id | SCOPUS01782762-2019-55-3-SID85060720664 |