Partitioning soil respiration in a temperate desert steppe in Inner Mongolia using exponential regression method

2010 ◽  
Vol 42 (12) ◽  
pp. 2339-2341 ◽  
Author(s):  
Fang Bao ◽  
Guangsheng Zhou ◽  
Fengyu Wang ◽  
Xinghua Sui
Keyword(s):  
Soil Respiration ◽  
Inner Mongolia ◽  
Regression Method ◽  
Desert Steppe ◽  
Exponential Regression ◽  
Temperate Desert

Effects of short-term warming and increasing precipitation on soil respiration of desert steppe of Inner Mongolia

2013 ◽  
Vol 36 (10) ◽  
pp. 1043-1053 ◽  
Author(s):  
Tao LIU ◽  
Yong-Xian ZHANG ◽  
Zhen-Zhu XU ◽  
Guang-Sheng ZHOU ◽  
Yan-Hui HOU ◽  
...  
Keyword(s):  
Soil Respiration ◽  
Inner Mongolia ◽  
Desert Steppe ◽  
Short Term ◽  
Increasing Precipitation

Evapotranspiration and crop coefficient for a temperate desert steppe ecosystem using eddy covariance in Inner Mongolia, China

2011 ◽  
Vol 26 (3) ◽  
pp. 379-386 ◽  
Author(s):  
Feng Zhang ◽  
Guangsheng Zhou ◽  
Yu Wang ◽  
Fulin Yang ◽  
Christer Nilsson
Keyword(s):  
Eddy Covariance ◽  
Inner Mongolia ◽  
Crop Coefficient ◽  
Desert Steppe ◽  
Steppe Ecosystem ◽  
Temperate Desert

The aboveground biomass of desert steppe and its spatiotemporal variation in western Inner Mongolia

2013 ◽  
Vol 5 (3) ◽  
pp. 339
Author(s):  
Gao Tian ◽  
Xu Bin ◽  
Yang Xiu-Chun ◽  
Jin Yun-Xiang ◽  
Ma Hai-Long ◽  
...  
Keyword(s):  
Aboveground Biomass ◽  
Inner Mongolia ◽  
Spatiotemporal Variation ◽  
Desert Steppe

Ecological responses of Stipa steppe in Inner Mongolia to experimentally increased temperature and precipitation. 3. Soil respiration

2018 ◽  
Vol 40 (2) ◽  
pp. 153 ◽  
Author(s):  
Xuexia Wang ◽  
Yali Chen ◽  
Yulong Yan ◽  
Zhiqiang Wan ◽  
Ran Chao ◽  
...  
Keyword(s):  
Soil Moisture ◽  
Soil Respiration ◽  
Soil Temperature ◽  
Respiration Rate ◽  
Inner Mongolia ◽  
Growing Season ◽  
Climatic Warming ◽  
Soil Respiration Rate ◽  
Natural Rainfall ◽  
Temperature And Precipitation

The response of soil respiration to simulated climatic warming and increased precipitation was evaluated on the arid–semi-arid Stipa steppe of Inner Mongolia. Soil respiration rate had a single peak during the growing season, reaching a maximum in July under all treatments. Soil temperature, soil moisture and their interaction influenced the soil respiration rate. Relative to the control, warming alone reduced the soil respiration rate by 15.6 ± 7.0%, whereas increased precipitation alone increased the soil respiration rate by 52.6 ± 42.1%. The combination of warming and increased precipitation increased the soil respiration rate by 22.4 ± 11.2%. When temperature was increased, soil respiration rate was more sensitive to soil moisture than to soil temperature, although the reverse applied when precipitation was increased. Under the experimental precipitation (20% above natural rainfall) applied in the experiment, soil moisture was the primary factor limiting soil respiration, but soil temperature may become limiting under higher soil moisture levels.

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