根际
中观
化学
有机质
土壤有机质
溶解有机碳
稻草
基质(水族馆)
土壤碳
植物
农学
营养物
土壤水分
环境化学
生物
生态学
细菌
有机化学
遗传学
作者
Oyindamola Ibitola Jackson,Richard S. Quilliam,Alistair W. Stott,Helen Grant,Jens‐Arne Subke
出处
期刊:Plant and Soil
[Springer Nature]
日期:2019-05-08
卷期号:440 (1-2): 473-490
被引量:45
标识
DOI:10.1007/s11104-019-04072-3
摘要
Belowground C supply from plant roots may accelerate the decomposition of SOM through the rhizosphere priming effect, but the detailed interaction between substrate quality and rhizosphere C supply is poorly understood. We hypothesize that decomposition of organic matter is enhanced by the combined effect of assimilate C supply to the rhizosphere and substrate amendments. Birch trees (Betula pendula) planted in experimental mesocosms; half of these trees were shaded to reduce the supply of assimilate C to roots and ECM fungi. Either 13C-enriched glucose, straw, fungal necromass or C4 biochar were subsequently added to each mesocosm. CO2 efflux derived from substrates were separated from that derived from native SOM and roots based on the isotopic composition of total respired CO2. The addition of all substrates increased fluxes in both un-shaded and shaded treatments, with greatest total CO2 efflux observed in soils amended with straw. Increases in un-labelled CO2 were observed to be greater in the presence of belowground C supply than in mesocosms with shaded trees. Turnover of SOM is closely linked to belowground C allocation. The biochemical quality and recalcitrance of litter entering the soil C pool is of critical importance to this priming, as is the interaction with rhizosphere-associated decomposition activity.
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