Mycorrhizal contribution to soil respiration in an apple orchard

被引:15
|
作者
Tome, Elisabetta [1 ]
Ventura, Maurizio [1 ]
Folegot, Silvia [1 ,2 ]
Zanotelli, Damiano [1 ]
Montagnani, Leonardo [1 ,3 ]
Mimmo, Tanja [1 ]
Tonon, Giustino [1 ]
Tagliavini, Massimo [1 ]
Scandellari, Francesca [1 ]
机构
[1] Free Univ Bolzano, Fac Sci & Technol, Piazza Univ 5, I-39100 Bolzano, Italy
[2] Univ Birmingham, Sch Geog Earth & Environm Sci, Birmingham B15 2TT, W Midlands, England
[3] Autonomous Prov Bolzano, Forest Serv, Via Brennero 6, I-39100 Bolzano, Italy
关键词
Stable isotopes; Trenching; Fruit trees; Natural abundance; CO2; PHOTOSYNTHETIC ACTIVITY; ARBUSCULAR MYCORRHIZAS; ROOT RESPIRATION; CARBON-DIOXIDE; CO2; FLUX; FUNGI; TEMPERATURE; RHIZOSPHERE; DEPENDENCE; MYCELIUM;
D O I
10.1016/j.apsoil.2016.01.016
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Soil respiration (R-soil) partitioning into its components is pivotal to understand C cycling in ecosystems. Notwithstanding the importance of mycorrhizal fungi in the belowground C cycle, their respiration (R-myc) is poorly studied in agricultural ecosystems. In this study, we applied a modified trenching method and the C-13 natural abundance technique to distinguish R-myc from root respiration (R-root) and from the respiration due to soil organic matter (SOM) degradation (R-som) in an apple orchard (Malus domestica Borkh.) located in Northern Italy. Membranes with different mesh size were used to physically exclude roots or mycorrhizae from soil cores with a different delta C-13 than the orchard average value. The CO2 efflux from soil cores was determined with an infrared gas analyser, and isotopic measurements were performed on the soil-emitted CO2. The different R-soil components were determined both by difference and by the isotopic mass balance. Mycorrhizal contribution to soil respiration (11 +/- 6%) was of similar magnitude to that of roots (12 +/- 4%) while R-som accounted for 73 +/- 3% of R-soil. In presence of apple roots, respiration of SOM and mycorrhizae (Rsom+myc) significantly increased in late summer and autumn, likely because of a priming effect of roots on SOM degradation or to a stimulation of mycorrhizal respiration. Our results suggest that respiration of mycorrhizal fungi can significantly contribute to R-soil, and need to be considered to correctly partition soil respiration. Furthermore, as roots increased Rsom+myc, the root exclusion method for soil respiration partitioning may overestimate R-root. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:165 / 173
页数:9
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