The response of soil organic matter (OM) decomposition to increasing temperature is a
critical aspect of ecosystem responses to global change. The impacts of climate warming on …

The last two decades have seen significant advances in understanding the cycling of carbon
and nutrients in ecosystems characterized by seasonal snow cover. This paper reviews and …

土壤呼吸是陆地生态系统碳循环的重要环节之一, 其对温度升高的敏感程度在很大程度上决定着
全球气候变化与碳循环之间的反馈关系. 为了深刻理解地下生态过程对气候变化的响应和适应 …

Soil microbial communities mediate the decomposition of soil organic matter (SOM). The
amount of carbon (C) that is respired leaves the soil as CO2 (soil respiration) and causes …

Soil total nitrogen (STN) and soil total phosphorus (STP), which vary spatially at different
scales, play important roles in both agriculture and in the natural environment, especially …

Climate warming is one of the most serious threats to soil biodiversity and ecosystem
stability. Straw return has been extensively recommended as an environmentally friendly …

Many serious ecosystem consequences of climate change will take decades or even
centuries to emerge. Long‐term ecological responses to global change are strongly …

The impact of climate change on the stability of soil organic carbon (SOC) remains a major
source of uncertainty in predicting future changes in atmospheric CO2 levels. One unsettled …

Biochar produced from pyrolysis of biomass is a candidate with great potential for climate
change mitigation by carbon sequestration and reduction of greenhouse gases (GHG) …

The rhizosphere is the most dynamic hotspot of microbial activity in the soil. Despite these
dynamics, the spatial pattern of many rhizosphere properties may remain stable because …