Dissolved
organic matter (DOM) is a major pool of actively cycling
organic carbon in soils, and can be exported to aquatic environments.
The quantity and chemistry of DOM vary with different environmental
factors, such as soil properties and climate. Accordingly, the amount
and composition of DOM in soil and that which is exported to aquatic
systems are likely altered by land-use change, but these aspects have
not been studied with various environmental factors and associated
land-use gradients in detail. To address this, both native and cultivated
soil samples from North and South America were used to extract soil-derived
DOM. DOM samples were isolated and analyzed for total organic carbon
concentration and solution-state nuclear magnetic resonance spectroscopy.
The concentration of dissolved organic carbon (DOC) was significantly
correlated with soil organic carbon concentration (r = 0.869, p < 0.01, n = 14)
and relative soil organic matter degradation state (r = −0.578, p < 0.05, n = 14). Land-use change decreased the controls of environmental factors
on the concentration of DOC but enhanced the correlations between
DOM aromaticity and mean annual precipitation (r =
−0.957, p < 0.01, n =
7) and sand concentration (r = −0.867, p < 0.05, n = 7). This study found that
land-use conversion and environmental conditions alter the quantity
and quality of DOM distinctly and uniquely. Here, we identified the
main factors that regulate the formation of soil DOM and its potential
mobility in soil profiles as well as export to aquatic ecosystems.