The terrestrial carbon (C) cycle has received increasing interest over the past few decades,
however, there is still a lack of understanding of the fate of newly assimilated C allocated …

Gas exchange between soil and atmosphere represents a major component of global
greenhouse gas fluxes. Chamber methods and micro-meteorological methods are well …

While increasing methane emissions from thawing permafrost are anticipated to be a major
climate feedback, no observational evidence for such an increase has previously been …

To better understand the biotic and abiotic factors that control soil CO2 efflux, we compared
seasonal and diurnal variations in simultaneously measured forest-floor CO2 effluxes and …

Natural source zone depletion (NSZD) has emerged as a practical alternative for restoration
of light non‐aqueous phase liquid (LNAPL) sites that are in the later stages of their …

Carbon stored in soils represents the largest terrestrial carbon pool and factors affecting this
will be vital in the understanding of future atmospheric CO2 concentrations. This book …

Background An acceleration of model-data synthesis activities has leveraged many
terrestrial carbon datasets, but utilization of soil respiration (RS) data has not kept pace …

Widespread recognition of the importance of soil CO 2 efflux as a major source of CO 2 to
the atmosphere has led to active research. A large soil respiration database and recent …

Pressure equilibrium between inside a soil CO2 flux chamber and the surrounding air
outside the chamber must be maintained during a measurement if measured soil CO2 flux …

In the long term, all CO2 produced in the soil must be emitted by the surface and soil CO2
efflux ([Formula: see text]) must correspond to soil respiration (Rsoil). In the short term …