Soils and sediments are major reservoirs of organic matter (OM), whose dynamic turnover
has a major impact on carbon cycling and global climate. OM in soils and sediments is …

The organic matter of living plants is the precursor material of the organic matter stored in
terrestrial soil ecosystems. Although a great deal of knowledge exists on the carbon turnover …

Trophic interactions play a vital role in soil functioning and are increasingly considered as
important drivers of the soil microbiome and biogeochemical cycles. In the last decade …

Although the influence of microplastics (MPs) in different soil environments has been
investigated, their effects on the physiochemical properties and chemical speciation of …

The redox activity of Fe-bearing minerals is coupled with the transformation of organic matter
(OM) in redox dynamic environments, but the underlying mechanism remains unclear. In this …

Over the last few years, the question of whether soil carbon sequestration could contribute
significantly to climate change mitigation has been the object of numerous debates. All of …

There is currently an intense debate about the potential for additional organic carbon
storage in soil, the strategies by which it may be accomplished and what the actual benefits …

One‐fourth of the global soil organic carbon (SOC) is stored in the boreal region, where
climate change is predicted to be faster than the global average. Planetary warming is …

Return of biomass-derived biochar (BC) into soil has been considered as one of the carbon
sequestration (CS) methods. It is important to evaluate the long-term biochar CS potential by …

Increasing soil organic carbon (SOC) in agroecosystems enables to address simultaneously
multiple goals such as climate change adaptation and mitigation as well as food security. As …