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 …

Sandy soils are widely distributed across the world. Due to the growing global population
and urbanization, these soils are increasingly used to provide food, feed, fiber, energy, and …

The biogeochemical cycling of soil organic matter (SOM) plays a central role in regulating
soil health, water quality, carbon storage, and greenhouse gas emissions. Thus, many …

There is growing evidence that many nitrogen-and phosphorus-containing organic
compounds in soils have on average a higher affinity for adsorption to mineral surfaces than …

Organo–mineral interactions have been regarded as the primary mechanism for the
stabilization of soil organic carbon (SOC) over decadal to millennial timescales, and the …

Wetlands export large amounts of dissolved organic carbon (DOC) downstream, which is
sensitive to water-table fluctuations (WTFs). While numerous studies have shown that WTFs …

Iron (Fe) oxides are widely recognized to prevent the degradation of organic matter (OM) in
environments, thereby promoting the persistence of organic carbon (OC) in soils. Thus …

Sandy soils cover approximately 900 million ha worldwide particularly in arid and semi-arid
regions. There are extensive areas of sandy soils under cultivation, but the soil fertility is …

It has been shown that reactive soil minerals, specifically iron (III)(oxyhydr) oxides, can trap
organic carbon in soils overlying intact permafrost, and may limit carbon mobilization and …

Coastal wetlands host large and dynamic reservoirs of organic carbon (C) and are also
biogeochemical hotspots for a wide range of Fe (hydr-) oxides with different chemical …