Soil heterotrophic respiration (SHR) is important for carbon‐climate feedbacks because of its
sensitivity to soil carbon, climatic conditions and nutrient availability. However, available …

Soil heterotrophic respiration (RH) is one of the largest and most uncertain components of
the terrestrial carbon cycle, directly reflecting carbon loss from soils to the atmosphere …

Soil heterotrophic respiration (Rh) refers to the flux of CO2 released from soil to atmosphere
as a result of organic matter decomposition by soil microbes and fauna. As one of the major …

Microbially explicit models may improve understanding and projections of carbon dynamics
in response to future climate change, but their fidelity in simulating global‐scale soil …

Soil respiration (Rs), the soil‐to‐atmosphere CO2 flux produced by microbes and plant
roots, is a critical but uncertain component of the global carbon cycle. Our current …

While heterotrophic respiration (Rh) makes up about a quarter of gross global terrestrial
carbon fluxes, it remains among the least-observed carbon fluxes, particularly outside the …

Soil heterotrophic respiration (RH) represents the carbon losses from the decomposition of
litter detritus and soil organic matter by microorganisms. Despite conflicting findings on the …

Belowground autotrophic respiration (RA) is one of the largest but most highly uncertain
carbon flux components in terrestrial ecosystems. However, RA has not been explored …

Global soils store at least twice as much carbon as Earth's atmosphere,. The global soil-to-
atmosphere (or total soil respiration, RS) carbon dioxide (CO2) flux is increasing,, but the …

Soil respiration (Rs) is a major pathway by which fixed carbon in the biosphere is returned to
the atmosphere, yet there are limits to our ability to predict respiration rates using …