钙质的
磷
化学
黄腐酸
石灰性土壤
土壤水分
环境化学
细菌
环境科学
有机化学
土壤科学
植物
地质学
生物
腐植酸
古生物学
肥料
作者
Xuewei Wang,Yu Liu,Baowei Hu,Steven A. Wakelin,Guixin Chu
标识
DOI:10.1021/acs.jafc.5c04171
摘要
Organic amendments are widely used to activate soil phosphorus (P) and stimulate phoD-harboring bacteria. However, their effects on P dynamics and the phoD community under soil drying remain unclear. Here, we investigated the effects of fulvic acid on P transformation and the phoD community under soil drying (100 → 60 → 20% water-holding capacity (WHC)). Soil drying accelerated the transformation of labile-P (CaCl2-P, citrate-P, Ca2-P) and moderately labile-P (Ca8-P) to recalcitrant P (occluded-P, Ca10-P), thereby decreasing the integrated P availability index (IPAI) by 49.4–54.1%. FA increased microbial biomass-carbon (MBC), -phosphorus (MBP), and phoD abundance. It also strengthened the phoD community’s network complexity. However, FA’s beneficial effects were attenuated along the soil drying gradient. Overall, the beneficial effect of FA in activating soil P was greatly counteracted by soil drying. Our findings highlight that maintaining optimal moisture (60%WHC) is essential to realize FA’s potential in activating soil P and recruiting phoD bacteria in calcareous soils.
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