Changes in the total carbon (TC), total organic carbon (TOC), total inorganic carbon (TIC), residual oxidizable carbon (ROC), and dissolved organic carbon (DOC) in soil permanently planted with white clover (Trifolium repens) and tall fescue (Festuca arundinacea) as the result of fertilization were quantified. Two nitrogen fertilisers, ammonium sulfate (AS) and urea (U), were separately applied with rice husk biochar carbonized at 700 °C (B) at 5 t ha–1 (B5) and 10 t ha–1 (B10). Adding the biochar to the AS or U resulted in an increase of the TOC, TIC, and ROC of both plants, with the exception of the TIC in ASB5 (white clover) and UB5 and ASB10 (tall fescue). In white clover, TC increased more when the biochar was added, particularly ASB10 and UB10, which also showed the smallest TOC reductions and largest ROC increases. In white clover, UB5 and UB10 resulted in greater DOC losses than when using U alone, likely due to increased microbial activity and mineralization of DOC. Meanwhile, in tall fescue, ASB5 and ASB10 reduced the DOC losses more than AS, likely due to the biochar’s DOC sorptive potential and reduced microbial decomposition. U fertilizer alone resulted in greater percentage changes in TC, TOC, ROC, TIC, and DOC than AS fertilizer in both plants. TC correlated positively with TIC, TOC, ROC, DOC, soil nitrogen, exchangeable calcium, and soil pH. Overall, U applied with 10 t ha–1 biochar improved carbon stabilization in white clover, while AS with biochar reduced DOC losses in tall fescue. The study demonstrates the potential of integrating biochar with nitrogen fertilizers to increase soil carbon retention in two different pasture families.
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