The soil drying along the increase of warming masks the relation between temperature and soil respiration in an alpine meadow of Northern Tibet
Shen Z. X.; Wang, J. W.; Sun, W.; Li, S. W.; Fu, G.; Zhang, X. Z.; Zhang, Y. J.; Yu, C. Q.; Shi, P. L.; He, Y. T.
2016
关键词soil moisture warming magnitude open top chamber Tibetan Plateau plateau metaanalysis ecosystem
英文摘要A warming experiment with two magnitudes was performed in an alpine meadow of Northern Tibet since late June, 2013. Open top chambers (OTCs) with two top diameters (0.60 m and 1.00 m) were used to increase soil temperature. Soil respiration (R-S) was measured during the growing season in 2013-2014. The OTCs with top diameters of 1.00 m and 0.60 m increased soil temperature by 1.30 and 3.10 degrees C, respectively, during the whole study period, but decreased soil moisture by 0.02 and 0.05 m(3) m(-3), respectively. However, the two patters of OTCs did not affect R-S. These results implied that a higher warming did not result in a higher R-S but a greater soil drying. Therefore, a higher warming may not cause a higher soil respiration, which was most likely due to the fact that a higher warming may result in a greater soil drying.
出处Polish Journal of Ecology
64
1
125-129
收录类别SCI
语种英语
ISSN号1505-2249
内容类型SCI/SSCI论文
源URL[http://ir.igsnrr.ac.cn/handle/311030/43298]  
专题地理科学与资源研究所_历年回溯文献
推荐引用方式
GB/T 7714
Shen Z. X.,Wang, J. W.,Sun, W.,et al. The soil drying along the increase of warming masks the relation between temperature and soil respiration in an alpine meadow of Northern Tibet. 2016.
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