Carbon inputs regulate the temperature sensitivity of soil respiration in temperate forests

Litter and root activities may alter the temperature sensitivity (Q 10 ) of soil respiration. However, existing studies have not provided a comprehensive understanding of the effects of litter and root carbon inputs on the Q10 of soil respiration in different seasons. In this study, we used the tren...

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Published inJournal of arid land Vol. 14; no. 9; pp. 1055 - 1068
Main Authors Liu, Yulin, Li, Jiwei, Hai, Xuying, Wu, Jianzhao, Dong, Lingbo, Pan, Yingjie, Shangguan, Zhouping, Wang, Kaibo, Deng, Lei
Format Journal Article
LanguageEnglish
Published Heidelberg Science Press 01.09.2022
Springer Nature B.V
Institute of Soil and Water Conservation,Northwest Agriculture and Forestry University,Yangling 712100,China%State Key Laboratory of Loess and Quaternary Geology,Institute of Earth Environment,Chinese Academy of Sciences,Xi'an 710075,China
University of Chinese Academy of Sciences,Beijing 100049,China%Institute of Soil and Water Conservation,Northwest Agriculture and Forestry University,Yangling 712100,China%State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau,Institute of Soil and Water Conservation,Chinese Academy of Sciences and Ministry of Water Resources,Yangling 712100,China
University of Chinese Academy of Sciences,Beijing 100049,China
State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau,Institute of Soil and Water Conservation,Chinese Academy of Sciences and Ministry of Water Resources,Yangling 712100,China
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Summary:Litter and root activities may alter the temperature sensitivity (Q 10 ) of soil respiration. However, existing studies have not provided a comprehensive understanding of the effects of litter and root carbon inputs on the Q10 of soil respiration in different seasons. In this study, we used the trench method under in situ conditions to measure the total soil respiration (R total ), litter-removed soil respiration (R no-litter ), root-removed soil respiration (R no-root ), and the decomposition of soil organic matter (i.e., both litter and root removal; R SOM ) in different seasons of pioneer ( Populus davidiana Dode) and climax ( Quercus liaotungensis Mary) forests on the Loess Plateau, China. Soil temperature, soil moisture, litter biomass, fine root biomass, litter carbon, and root carbon were analyzed to obtain the drive mechanism of the Q 10 of soil respiration in the two forests. The results showed that the Q 10 of soil respiration exhibited seasonality, and the Q 10 of soil respiration was higher in summer. The litter enhanced the Q 10 of soil respiration considerably more than the root did. Soil temperature, soil moisture, fine root biomass, and litter carbon were the main factors used to predict the Q 10 of different soil respiration components. These findings indicated that factors affecting the Q 10 of soil respiration highly depended on soil temperature and soil moisture as well as related litter and root traits in the two forests, which can improve our understanding of soil carbon—climate feedback in global warming. The results of this study can provide reference for exploring soil respiration under temperate forest restoration.
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ISSN:1674-6767
2194-7783
DOI:10.1007/s40333-022-0102-0