“…The formation of high-molecular-weight HA in soils, predominantly those with more aromatic, recalcitrant, and hydrophobic structures, has been reported to increase aggregate stability, decrease disaggregation effects, and increase microbial growth and CEC (Chaney & Swift, 1986;Piccolo & Mbagwu, 1997;Piccolo & Mbagwu, 1999;Piccolo & Stevenson, 1982;Tan, 2014). The application of exogenous sources of HS, including lignin, to the soil leads to both C accumulation and increased soil fertility (Montiel-Rozas, Panettieri, Madejón, & Madejón, 2015), and there is evidence of increased CEC, water retention capacity and soil aggregation and decreased soil density and resistance to penetration (Aksakal, Sari, & Angin, 2016;Lal, 2006 where the increase in structural recalcitrance could contribute to increased stabilization of humified OM. Conversely, in the case of less intense management systems, including G and AFS, increased HA lability requires enhanced transformation processes such as humification and interaction with the mineral fraction, which also contribute to OM stabilization as previously discussed.…”