Grasslands store approximately one third of the global terrestrial carbon stocks and can act
as an important soil carbon sink. Recent studies show that plant diversity increases soil …

Global warming has caused changes in temperature and precipitation patterns, and the
subsequent effects on the dynamics of soil respiration (Rs) have had a significant impact on …

Global climate warming may induce a positive feedback through increasing soil carbon (C)
release to the atmosphere. Although warming can affect both C input to and output from soil …

Current consensus on global climate change predicts warming trends with more
pronounced temperature changes in winter than summer in the Northern Hemisphere at …

The ongoing climate change is predicted to induce more weather extremes such as frequent
drought and high‐intensity precipitation events, causing more severe drying‐rewetting …

Grazing exclusion alters grassland soil aggregation, microbiome composition, and
biogeochemical processes. However, the long‐term effects of grazing exclusion on the …

Soil organic carbon (SOC) is heterogeneous and consists of multiple pools differing in
physical and chemical properties. SOC stocks are expected to increase in response to …

Soil organic carbon (SOC) sequestration effectively reduces global CO 2 emissions while
ensuring crop production and sustainable agricultural development. Evaluating the effects of …

Global potent greenhouse gas nitrous oxide (N2O) emissions from soil are accelerating, with
increases in the proportion of reactive nitrogen emitted as N2O, ie, N2O emission factor (EF) …

Anthropogenic nitrogen (N) input has overtaken natural N fixation as the leading source of
reactive N, and can profoundly alter the structure and functions of terrestrial ecosystems. N …