Journal of Arid Land
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Journal of Arid Land  2017, Vol. 9 Issue (4): 568-579    DOI: 10.1007/s40333-017-0060-0
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Diurnal dynamics of soil respiration and the influencing factors for three land-cover types in the hinterland of the Taklimakan Desert, China
YANG Fan1,2*, ALI Mamtimin1,2, ZHENG Xinqian3, HE Qing1,2, YANG Xinghua1,2, HUO Wen1,2, LIANG Fengchao4, WANG Shaoming5
1 Institute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, China;
2 Taklimakan Desert Atmosphere and Environment Observation Experiment Station, Tazhong 841000, China;
3 Xinjiang Agro-Meteorological Observatory, Urumqi 830002, China;
4 Xinjiang Climate Center, Urumqi 830002, China;
5 Forestry Bureau of Bailongjiang, Lanzhou 730050, China
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Abstract Knowledge of soil respiration and the influencing factors in desert ecosystems is essential to understanding carbon dynamics and responses of biotic and abiotic processes in soils to climate change. In this study, soil respiration rate (Rs) for three land-cover types (shifting sandy land, sandy land with straw checkerboard barriers, and shelter forest land) in the hinterland of the Taklimakan Desert was measured in May 2015 using an automated soil CO2 flux system. The effects of soil temperature (Ts) and soil water content (Ws) on Rs were also analyzed. The results showed that Rs values in shifting sandy land, sandy land with straw checkerboard barriers, and shelter forest land were all low and exhibited obvious diurnal fluctuations. The establishment of straw checkerboard barriers in sandy land had no significant effect on Rs, while the establishment of shelterbelts significantly increased Rs. Shifting sandy land and sandy land with straw checkerboard barriers were carbon sinks at night and early morning and were carbon sources in the daytime, while shelter forest land always acted as a carbon source during the whole day. The synergistic effect of Ts and Ws could better explain the diurnal dynamics in Rs than single factor. In shifting sandy land and sandy land with straw checkerboard barriers, Ws was identified as a limiting factor influencing the diurnal dynamics of Rs. Furthermore, a relatively strong hysteresis loop existed between Rs and Ts. In contrast, in shelter forest land, Rs was significantly influenced by Ts, and a relatively weaker hysteresis loop existed between Rs and Ws.
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Articles by authors
YANG Fan
ALI Mamtimin
ZHENG Xinqian
HE Qing
YANG Xinghua
HUO Wen
LIANG Fengchao
WANG Shaoming
Key wordssoil respiration   soil temperature   soil water content   hysteresis effect   Taklimakan Desert     
Received: 2016-06-05; Published: 2017-05-09
Fund:

This study was funded by the National Natural Science Foundation of China (41175140) and the National Department of Public Benefit (Meteorology) Research Foundation (GYHY201306066).

Corresponding Authors: YANG Fan   
 E-mail: yangfan309@yeah.net
Cite this article:   
YANG Fan,ALI Mamtimin,ZHENG Xinqian et al. Diurnal dynamics of soil respiration and the influencing factors for three land-cover types in the hinterland of the Taklimakan Desert, China[J]. Journal of Arid Land, 2017, 9(4): 568-579.
 
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