Using the static opaque chamber method, the soil respiration rates (SR) were measured through the continuous experiments in situ in semiarid Stipa grandis steppe in Xilin River Basin of Inner Mongolia, China from June 2001 to June 2003, in parallel, the difference between the SR and the ecosystem respiration rates (TER) were compared. The results indicated that the seasonal variations of the SR and TER were obvious with higher emissions in growing season and a relatively low efflux level in non-growing season, furthermore, the negative effluxes were found in the observation site in winter; the annual CO<inf>2</inf> efflux of total ecosystem ranged from 160.5 gC/(m<sup>2</sup>·a) to 162.8 gC/(m<sup>2</sup>·a) and that of soil ran...
The seasonal dynamics of soil respiration in steppe (S. bungeana), desert shrub (A. ordosica), and s...
Eddy covariance technique was used to measure carbon flux during two growing seasons in 2003 and 200...
This study compared carbon dioxide (CO<sub>2</sub>) fluxes over three grassland ecosyste...
Using the static opaque chamber method, the soil respiration rates (SR) were measured through the co...
Soil respiration is a key component of the global terrestrial ecosystem carbon cycle. The static opa...
Based on the static opaque chamber method, the respiration rates of soil microbial respiration, soil...
Aims Soil CO2 emission from steppes is affected by soil properties and vegetation in different succe...
Fixed field experimental studies are carried out on daily variations of the undisturbed community an...
Chinese grasslands have undergone great changes in land use in recent decades. Approximately 18.2% o...
Most soil respiration measurements are conducted during the growing season. In tundra and boreal for...
Chinese grasslands have undergone great changes in land use in recent decades. Approximately 18.2% o...
There are variations in soil respiration across vegetation types; however, it is unclear which facto...
A two consecutive years' field experiment was carried out on four types of semiarid grassland along ...
Significant CO2 fluxes from snow-covered soils occur in cold biomes. However, little is known about ...
Significant CO2 fluxes from snow-covered soils occur in cold biomes. However, little is known about...
The seasonal dynamics of soil respiration in steppe (S. bungeana), desert shrub (A. ordosica), and s...
Eddy covariance technique was used to measure carbon flux during two growing seasons in 2003 and 200...
This study compared carbon dioxide (CO<sub>2</sub>) fluxes over three grassland ecosyste...
Using the static opaque chamber method, the soil respiration rates (SR) were measured through the co...
Soil respiration is a key component of the global terrestrial ecosystem carbon cycle. The static opa...
Based on the static opaque chamber method, the respiration rates of soil microbial respiration, soil...
Aims Soil CO2 emission from steppes is affected by soil properties and vegetation in different succe...
Fixed field experimental studies are carried out on daily variations of the undisturbed community an...
Chinese grasslands have undergone great changes in land use in recent decades. Approximately 18.2% o...
Most soil respiration measurements are conducted during the growing season. In tundra and boreal for...
Chinese grasslands have undergone great changes in land use in recent decades. Approximately 18.2% o...
There are variations in soil respiration across vegetation types; however, it is unclear which facto...
A two consecutive years' field experiment was carried out on four types of semiarid grassland along ...
Significant CO2 fluxes from snow-covered soils occur in cold biomes. However, little is known about ...
Significant CO2 fluxes from snow-covered soils occur in cold biomes. However, little is known about...
The seasonal dynamics of soil respiration in steppe (S. bungeana), desert shrub (A. ordosica), and s...
Eddy covariance technique was used to measure carbon flux during two growing seasons in 2003 and 200...
This study compared carbon dioxide (CO<sub>2</sub>) fluxes over three grassland ecosyste...