Recently identified post-fire carbon fluxes indicate that, to understand whether global fires
represent a net carbon source or sink, one must consider both terrestrial carbon retention …

Purpose Mountains have unique microclimates and rich plant diversity, resulting in different
patterns and dynamics of soil organic carbon (SOC) across plant communities and …

High-intensity wildfires alter the chemical composition of organic matter, which is expected
to be distinctly different from low-intensity prescribed fires. Herein, we used pyrolysis gas …

Pyrogenic organic matter (PyOM) is a product of incomplete combustion during wildfires and
an important pool of soil organic carbon (SOC). The dynamics of PyOM and SOC in boreal …

In recent years, wildfire frequency and severity has increased in the Arctic tundra regions
due to climate change. Pyrogenic organic matter (PyOM) is a product of incomplete …

Climate change is causing larger wildfires and more extreme precipitation events in many
regions. As these ecological disturbances increasingly coincide, they alter lateral fluxes of …

Charcoal‐rich Technosols on century‐old relict charcoal hearths (RCHs) are the subject of
ongoing research regarding potential legacy effects that result from historic charcoal …

Fire relentlessly modifies the belowground pool of pyrogenic carbon (PyC) in boreal
ecosystems. However, only a few soils offer a consistent record of PyC accumulation. Here …

Fires produce an aromatic particulate residue commonly referred to as pyrogenic carbon
(PyC). Particulate PyC is low density, high porosity, and is predominantly deposited on the …

Pyrogenic carbon (PyC) is produced by the incomplete combustion of vegetation during
wildfires and is a major and persistent pool of the global carbon (C) cycle. However, its …