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Nitrogen (N) addition can alter soil organic carbon (SOC) storage, but its effects on functionally distinct SOC fractions remain unclear in global grasslands. Using a meta-analysis of 237 paired observations from 41 studies across global grasslands, we assessed the responses of particulate organic carbon (POC) and mineral-associated organic carbon (MAOC) to N addition and explored their potential drivers. N addition significantly increased the POC and MAOC pools by 8.20% and 5.50%, respectively, and increased the POC:SOC ratio by 13.07%. POC showed a larger response to N addition than MAOC, suggesting that particulate and mineral-associated carbon pools differ in their sensitivity to N addition. The response of POC to N addition was significantly negatively correlated with the responses of soil pH and microbial biomass carbon (MBC), whereas the response of MAOC to N addition was significantly positively correlated only with the response of soil pH. Overall, our findings suggest that N addition reshapes SOC fraction composition by increasing the POC:SOC ratio in global grasslands. These results highlight the importance of considering both fraction-specific responses and their associated drivers when predicting soil carbon dynamics under increasing N deposition.
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Li et al. (2026) studied this question.
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