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

被引:61
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
相关论文
共 66 条
[21]   Respiratory quotients and Q10 of soil respiration in sub-alpine Australia reflect influences of vegetation types [J].
Jenkins, Meaghan E. ;
Adams, Mark A. .
SOIL BIOLOGY & BIOCHEMISTRY, 2011, 43 (06) :1266-1274
[22]   Factors controlling soil CO2 effluxes and the effects of rewetting on effluxes in adjacent deciduous, coniferous, and mixed forests in Korea [J].
Kim, Dong-Gill ;
Mu, Shouguo ;
Kang, Sinkyu ;
Lee, Dowon .
SOIL BIOLOGY & BIOCHEMISTRY, 2010, 42 (04) :576-585
[23]   Root and rhizomicrobial respiration: A review of approaches to estimate respiration by autotrophic and heterotrophic organisms in soil [J].
Kuzyakov, Y ;
Larionova, AA .
JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE, 2005, 168 (04) :503-520
[24]   Sources of CO2 efflux from soil and review of partitioning methods [J].
Kuzyakov, Y .
SOIL BIOLOGY & BIOCHEMISTRY, 2006, 38 (03) :425-448
[25]   REVIEW: Time lag between photosynthesis and carbon dioxide efflux from soil: a review of mechanisms and controls [J].
Kuzyakov, Yakov ;
Gavrichkova, Olga .
GLOBAL CHANGE BIOLOGY, 2010, 16 (12) :3386-3406
[26]   Autotrophic and heterotrophic respiration in needle fir and Quercus-dominated stands in a cool-temperate forest, central Korea [J].
Lee, Na-yeon ;
Koo, Jin-Woo ;
Noh, Nam Jin ;
Kim, Joon ;
Son, Yowhan .
JOURNAL OF PLANT RESEARCH, 2010, 123 (04) :485-495
[27]   Global terrestrial carbon storage and uncertainties in its temperature sensitivity examined with a simple model [J].
Lenton, TM ;
Huntingford, C .
GLOBAL CHANGE BIOLOGY, 2003, 9 (10) :1333-1352
[28]   Elevated CO2 and temperature impacts on different components of soil CO2 efflux in Douglas-fir terracosms [J].
Lin, GH ;
Ehleringer, JR ;
Rygiewicz, PT ;
Johnson, MG ;
Tingey, DT .
GLOBAL CHANGE BIOLOGY, 1999, 5 (02) :157-168
[29]   ON THE TEMPERATURE-DEPENDENCE OF SOIL RESPIRATION [J].
LLOYD, J ;
TAYLOR, JA .
FUNCTIONAL ECOLOGY, 1994, 8 (03) :315-323
[30]   Factors Affecting Spatial Variation of Annual Apparent Q10 of Soil Respiration in Two Warm Temperate Forests [J].
Luan, Junwei ;
Liu, Shirong ;
Wang, Jingxin ;
Zhu, Xueling .
PLOS ONE, 2013, 8 (05)