BDOM was identified as an important determinant of biochar-mediated Cd binding in soils.
Thermal reorganization shifted BDOM from heterogeneous humic aggregates into phenolic O-coordinating domains.
This reorganization enhances Cd immobilization and limits the transfer from the soil to the biosphere, here ryegrass.
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Comparative analysis of molecular characteristics in BDOM across thermal gradients
Thermal reorganization reshapes BDOM molecular networks and Cd coordination pathways
Structural analysis of BDOM-Cd
Molecular transformations during Cd coordination (A-C)
Molecular and thermodynamic pathways during Cd coordination
Possible transformation pathways of BDOM during Cd chelation and the effect of pyrolysis temperature on BDOM formation.
BDOM immobilizes soil Cd and limits its uptake by ryegrass