Temperature sensitivity of total soil respiration and its heterotrophic and autotrophic components in six vegetation types of subtropical China

被引:59
|
作者
Yu, Shiqin [1 ,2 ]
Chen, Yuanqi [3 ]
Zhao, Jie [4 ]
Fu, Shenglei [1 ,5 ]
Li, Zhian [1 ]
Xia, Hanping [1 ]
Zhou, Lixia [1 ]
机构
[1] Chinese Acad Sci, Key Lab Vegetat Restorat & Management Degraded Ec, South China Bot Garden, Guangzhou 510650, Guangdong, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Hunan Univ Sci & Technol, Hunan Prov Key Lab Coal Resources Clean Utilizat, Xiangtan 411201, Peoples R China
[4] Chinese Acad Sci, Key Lab Agroecol Proc Subtrop Reg, Inst Subtrop Agr, Changsha 410125, Hunan, Peoples R China
[5] Henan Univ, Coll Environm & Planning, Kaifeng 475004, Peoples R China
基金
中国国家自然科学基金;
关键词
Soil CO2 efflux; Q(10); Vegetation; Heterotrophic respiration; Autotrophic respiration; Soil carbon; TERRESTRIAL CARBON STORAGE; ECOSYSTEM RESPIRATION; FOREST ECOSYSTEMS; ROOT RESPIRATION; CO2; EFFLUX; PLANTATIONS; DEPENDENCE; PATTERNS; PHOTOSYNTHESIS; DECOMPOSITION;
D O I
10.1016/j.scitotenv.2017.06.194
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The temperature sensitivity of soil respiration (Q(10)) is a key parameter for estimating the feedback of soil respiration to global warming. The Q(10) of total soil respiration (R-t) has been reported to have high variability at both local and global scales, and vegetation type is one of the most important drivers. However, little is known about how vegetation types affect the Q(10) of soil heterotrophic (R-h) and autotrophic (R-a) respirations, despite their contrasting roles in soil carbon sequestration and ecosystem carbon cycles. In the present study, five typical plantation forests and a naturally developed shrub and herb land in subtropical China were selected for investigation of soil respiration. Trenching was conducted to separate Rh and Ra in each vegetation type. The results showed that both R-t and R-h were significantly correlated with soil temperature in all vegetation types, whereas Ra was significantly correlated with soil temperature in only four vegetation types. Moreover, on average, soil temperature explained only 15.0% of the variation in Ra in the six vegetation types. These results indicate that soil temperature may be not a primary factor affecting R-a. Therefore, modeling of Ra based on its temperature sensitivity may not always be valid. The Q(10) of Rh was significantly affected by vegetation types, which indicates that the response of the soil carbon pool to climate warming may vary with vegetation type. In contrast, differences in neither the Q(10) of R-t nor that of R-a among these vegetation types were significant. Additionally, variation in the Q(10) of R-t among vegetation types was negatively related to fine root biomass, whereas the Q(10) of R-h was mostly related to total soil nitrogen. However, the Q(10) of R-a was not correlated with any of the environmental variables monitored in this study. These results emphasize the importance of independently studying the temperature sensitivity of R-t and its heterotrophic and autotrophic components. (C) 2017 Elsevier B.V. All rights reserved.
引用
收藏
页码:160 / 167
页数:8
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