Limited variation in proportional contributions of auto-and heterotrophic soil respiration, despite large differences in vegetation structure and function in the Low Arctic
Arctic ecosystems contain vast stores of soil carbon (C), yet our understanding of the factors
controlling CO 2 efflux from tundra soils remains poor. Partitioning soil respiration (RS) into …
controlling CO 2 efflux from tundra soils remains poor. Partitioning soil respiration (RS) into …
Forest soil carbon efflux evaluation across China: A new estimate with machine learning
H Sun, B Bond‐Lamberty, T Hu, J Li… - Global …, 2023 - Wiley Online Library
Forest soil respiration (Rs) plays an important role in the carbon balance of terrestrial
ecosystems. China's forest occupies a large part of the world's forest. However, due to the …
ecosystems. China's forest occupies a large part of the world's forest. However, due to the …
Estimation of global soil respiration by accounting for land-use changes derived from remote sensing data
M Adachi, A Ito, S Yonemura, W Takeuchi - Journal of environmental …, 2017 - Elsevier
Soil respiration is one of the largest carbon fluxes from terrestrial ecosystems. Estimating
global soil respiration is difficult because of its high spatiotemporal variability and sensitivity …
global soil respiration is difficult because of its high spatiotemporal variability and sensitivity …
The impact of water content on sources of heterotrophic soil respiration
Heterotrophic respiration (RH) is a major flux of CO2 from forest ecosystems and represents
a large source of uncertainty in estimating net ecosystem productivity (NEP) using regional …
a large source of uncertainty in estimating net ecosystem productivity (NEP) using regional …
Soil heterotrophic respiration is insensitive to changes in soil water content but related to microbial access to organic matter
While most models describing soil organic matter dynamics relate the turnover of soil
organic matter to its chemical structure, there is increasing evidence that microbial …
organic matter to its chemical structure, there is increasing evidence that microbial …
Measurement strategies to account for soil respiration temporal heterogeneity across diverse regions
Soil respiration (Rs) rates fluctuate daily and seasonally; therefore, the timing of
measurements is critical when estimating the daily mean and scaling up to annual Rs rates …
measurements is critical when estimating the daily mean and scaling up to annual Rs rates …
Are ecological gradients in seasonal Q10 of soil respiration explained by climate or by vegetation seasonality?
Soil respiration (SR) is highly sensitive to future climate change, and particularly to global
warming. However, considerable uncertainties remain associated with the temperature …
warming. However, considerable uncertainties remain associated with the temperature …
Historically inconsistent productivity and respiration fluxes in the global terrestrial carbon cycle
The terrestrial carbon cycle is a major source of uncertainty in climate projections. Its
dominant fluxes, gross primary productivity (GPP), and respiration (in particular soil …
dominant fluxes, gross primary productivity (GPP), and respiration (in particular soil …
The responses of soil and rhizosphere respiration to simulated climatic changes vary by season
Responses of soil respiration (Rs) to anthropogenic climate change will affect terrestrial
carbon storage and, thus, feed back to warming. To provide insight into how warming and …
carbon storage and, thus, feed back to warming. To provide insight into how warming and …
Soil microclimates influence annual carbon loss via heterotrophic soil respiration in maize and switchgrass bioenergy cropping systems
Heterotrophic soil respiration (RH) is the primary pathway of carbon (C) loss from litter and
soil organic matter, and thus RH partially determines ecosystem C storage. Because RH is …
soil organic matter, and thus RH partially determines ecosystem C storage. Because RH is …