With the increase of nitrogen (N) input in vadose zones-groundwater systems, N
contamination in groundwater has become a global environmental and geological issue that …

Microbial residual carbon (MRC) plays an important role in maintaining soil carbon stability
and is therefore a focus of soil organic carbon (SOC) estimation. However, the global pattern …

Warming is known to reduce soil carbon (C) stocks by promoting microbial respiration, which
is associated with the decomposition of microbial residue carbon (MRC). However, the …

Microbial necromass plays an essential role in soil organic carbon (SOC) accumulation.
Nevertheless, how microbial necromass carbon (C) concentrations and their contributions to …

Microbial necromass carbon (MNC) is an important contributor to soil organic carbon. The
influence of lithology on MNC remains unclear. MNC is often regarded as a stable, uniform …

Microbial necromass carbon (MNC) and glomalin-related soil protein (GRSP) are stable
microbe-derived sources of carbon (C) in soils. MNC constitutes a considerable portion of …

Soil physical and biogeochemical processes are key to regulate the soil microbial
necromass (SMN) patterns. Increasing evidence showed that the SMN contributes to the …

Soil microbial communities play a crucial role in the accumulation and stabilization of soil
organic carbon (SOC) through complex processes involving plant residue transformation …

The rhizosphere is a typical soil microbial hotspot, however, not a homogeneous entity. Due
to root functional differentiation, different root functional modules (ie, absorptive roots and …

摘要采用黄土丘陵区多年生C3 草本植物长芒草为对象, 模拟“枯落物⁃ 土壤” 转换界面,
进行了为期512 d 的室内分解试验, 对枯落物分解过程中界面土层微生物残体和土壤碳组分动态 …