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 |
|