Human activities have more than doubled reactive nitrogen (N) deposited in ecosystems,
perturbing the N cycle and considerably impacting plant, animal, and microbial communities …

Globally increasing nitrogen (N) deposition is recognized as an important regulator of soil
microbial communities. However, how N enrichment affects soil microbial diversity, richness …

Nitrogen (N) availability has been considered as a critical factor for the cycling and storage
of soil organic carbon (SOC), but effects of N enrichment on the SOC pool appear highly …

Little is currently known about how climate modulates the relationship between plant
diversity and soil organic carbon and the mechanisms involved. Yet, this knowledge is of …

Identifying controls on soil organic carbon (SOC) storage, and where SOC is most
vulnerable to loss, are essential to managing soils for both climate change mitigation and …

Phosphorus deposition can stimulate both plant carbon inputs and microbial carbon outputs.
However, how P enrichment affects soil organic carbon (SOC) storage and the underlying …

Atmospheric nitrogen (N) deposition is enriching soils with N across biomes. Soil N
enrichment can increase plant productivity and affect microbial activity, thereby increasing …

Soil moisture drought, as one of the most important drought categories, is determined by
both water supply (eg, precipitation) and demand (eg, potential evapotranspiration). To shed …

Formation of mineral‐associated organic matter (MAOM) supports the accumulation and
stabilization of carbon (C) in soil, and thus, is a key factor in the global C cycle. Little is …

Nitrogen (N) addition can have substantial impacts on both aboveground and belowground
processes such as plant productivity, microbial activity, and soil properties, which in turn …