Mechanisms of soil organic carbon (SOC) stabilization have been widely studied due to their
relevance in the global carbon cycle. No‐till (NT) has been frequently adopted to sequester …

Measuring the growth rate of a microorganism is a simple yet profound way to quantify its
effect on the world. The absolute growth rate of a microbial population reflects rates of …

Soil biodiversity (SB) is experiencing significant changes worldwide, yet its responses to
climate and land use changes remain unclear. In light of this, we combined multiple …

Understanding the large-scale pattern of soil microbial carbon use efficiency (CUE) and its
temperature sensitivity (CUET) is critical for understanding soil carbon–climate feedback …

The sensitivity of soil microbial respiration to warming (Q 10) remains a major source of
uncertainty surrounding the projections of soil carbon emissions to the atmosphere as the …

Although our understanding of the effects of microplastics on the dynamics of soil organic
matter (SOM) has considerably advanced in recent years, the fundamental mechanisms …

Nitrification, the oxidation of ammonia to nitrate, is an essential process in the
biogeochemical nitrogen cycle. The first step of nitrification, ammonia oxidation, is performed …

Soils support an immense portion of Earth's biodiversity and maintain multiple ecosystem
functions which are essential for human well-being. Environmental thresholds are known to …

Understanding the determinants of soil carbon mineralization at both the aggregate and
rhizosphere levels is crucial for providing precise feedback on climate change. However, the …

Plant‐and microbially derived carbon (C) are the two major sources of soil organic matter
(SOM), and their ratio impacts SOM composition, accumulation, stability, and turnover. The …