Over 70% of soil organic carbon (SOC) is stored at a depth greater than 20 cm belowground.
A portion of this deep SOC actively cycles on annual to decadal timescales and is sensitive …

Rhizospheric organisms have a unique manner of existence since many factors can
influence the shape of the microbiome. As we all know, harnessing the interaction between …

Climate change is progressing and is already visible to the naked eye around the world.
Hydrological events associated with climate change, ie floods and droughts, have reached …

Salinization is one of the most serious land degradation problems facing world. Salinity
results in poor plant growth and low soil microbial activity due to osmotic stress and toxic …

Altered precipitation patterns resulting from climate change will have particularly significant
consequences in water‐limited ecosystems, such as arid to semi‐arid ecosystems, where …

Decreased precipitation significantly suppressed the nutrient provisioning, microbial growth
efficiency, LOM decomposition, and thus, the averaging multifunctionality by 42.6%(p< …

Biochar and chemical fertilizer have been widely used in agriculture. Most studies have
proved that they not only alter soil nutrient content, but also have an impact on soil microbial …

Given that soil water availability is the major limitation on plant growth in desert steppes,
uncovering the connections between belowground and aboveground communities under …

As a primary limiting factor in arid and semiarid regions, precipitation strongly influences soil
microbial properties. However, the patterns and mechanisms of soil microbial responses to …

Changing precipitation regimes could have profound influences on carbon (C) cycle in the
biosphere. However, how soil C release from terrestrial ecosystems responds to changing …