Microbes are responsible for cycling carbon (C) through soils, and predicted changes in soil
C stocks under climate change are highly sensitive to shifts in the mechanisms assumed to …

Organic amendments stimulate carbon (C) mineralization by affecting the soil nutrient
content, soil organic carbon (SOC) chemistry, and microbial community structure, especially …

The extent to which long-term application of mineral fertilizers regulates the quantity, quality,
and stability of soil organic matter (SOM) in soil matrices remains unclear. By combining four …

Subsoils contain more than half of soil organic carbon (SOC) and are expected to
experience rapid warming in the coming decades. Yet our understanding of the stability of …

Recent observations document that long-term soil warming in a temperate deciduous forest
leads to significant soil carbon loss, whereas chronic soil nitrogen enrichment leads to …

Both warming and nitrogen (N) addition affect the chemistry and characteristics of soil
organic matter (SOM). However, their interactive impacts on molecular compositions and …

Soil microbial carbon use efficiency (CUE) refers to the efficiency of microorganisms in
converting absorbed carbon into their own biomass carbon. Soil microbial CUE is a key …

Soil organic carbon (SOC) is a key component of the global carbon pool, which is crucial to
the fertility and health of soils and deeply influences global carbon cycling.“Mollisols belts” …

摘要土壤有机碳库是陆地生态系统最大的碳库, 在调控全球碳循环和气候变化中起着重要的作用
. 人为活动所导致的氮, 磷输入和大气氮, 磷沉降提高了陆地生态系统的氮, 磷可利用性 …

Soil fungi are key regulators of forest carbon cycling and their responses to global change
have effects that ripple throughout ecosystems. Global changes are expected to push many …