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Substitution of lithogenic with pedogenic soil carbonates in Korean coastal rice paddy under desalinization: Evidences from δ13C
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DOI：10.1016/j.agee.2025.109993.png)
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Abstract
En 中文
• δ13C of soil varied with the content and sources of inorganic C in coastal paddies. • Total inorganic C did not change with salinity but increased with Ca content. • Lithogenic carbonate decreased but pedogenic carbonate increased with desalinization. • Desalinization increased pedogenic carbonate via increased SOC and microbial activity
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