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Soil physicochemical and microbial drivers of temperature sensitivity of soil organic matter decomposition under boreal forests

Soil physicochemical and microbial drivers of temperature sensitivity of soil organic matter decomposition under boreal forests

作     者:Beata KLIMEK Marcin CHODAK Matgorzata JAZWA Hamed AZARBAD Maria NIKLINSKA Beata KLIMEK;Marcin CHODAK;Ma(l)tgorzata JA(Z)WA;Hamed AZARBAD;Maria NIKLI(N)SKA

作者机构:Institute of Environmental SciencesFaculty of BiologyJagiellonian UniversityGronostajowa 7Krakow 30-387(Poland) Department of Management and Protection of EnvironmentAGH University of Science and TechnologyMickiewicza 30Krakow 30-059(Poland) Institute of BiologyFaculty of Natural Sciences and TechnologyUniversity of OpoleOleska 22Opole 45-052(Poland) 

出 版 物:《Pedosphere》 (土壤圈(英文版))

年 卷 期:2020年第30卷第4期

页      面:528-534页

核心收录:

学科分类:0818[工学-地质资源与地质工程] 09[农学] 0903[农学-农业资源与环境] 0901[农学-作物学] 090301[农学-土壤学] 

基  金:The research received funding from the European Union Seventh Framework Programme(FP7/2007-2013)under grant agreement No.262693(INTERACT) by Jagiel-lonian University,Poland(subsidy DS/WBiNoZ/INoS/758) 

主  题:CoO2 evolution global warming microbial functional diversity MicroResp^TM Q10 metabolic coefficient 

摘      要:Soil organic matter(SOM)in boreal forests is an important carbon *** aim of this study was to assess and to detect factors controlling the temperature sensitivity of SOM *** were collected from Scots pine,Norway spruce,silver birch,and mixed forests(O horizon)in northern Finland,and their basal respiration rates at five different temperatures(from 4 to 28℃)were *** Q10 values,showing the respiration rate changes with a 10℃ increase,were calculated using a Gaussian function and were based on temperature-dependent *** soil physicochemical parameters were measured,and the functional diversity of the soil microbial communities was assessed using the MicroResp?*** temperature sensitivity of SOM decomposition differed under the studied forest *** forests had the highest temperature sensitivity for SOM decomposition at the low temperature range(0–12℃).Within this temperature range,the Q10 values were positively correlated with the microbial functional diversity index(H’mic)and the soil C-to-P *** suggested that the metabolic abilities of the soil microbial communities and the soil nutrient content were important controls of temperature sensitivity in taiga soils.

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