生物炭
足迹
磷
化学
预订
环境科学
农学
热解
废物管理
生物
工程类
计算机科学
地质学
计算机网络
古生物学
有机化学
作者
Hongyan Nan,Fan Yang,Chongqing Wang,Xiaoyun Xu,Hao Qiu,Xinde Cao,Ling Zhao
标识
DOI:10.1021/acs.jafc.3c05970
摘要
Two phosphorus (P)-rich biowastes, sewage sludge (SS) and bone dreg (BD), were selected to clarify P footprints among biowaste, biochar, soil, and plants by introducing a novel "3R" concept model. Results showed that pyrolysis resulted in P transformation from an unstable-organic amorphous phase to a stable-inorganic crystalline phase with a P retention rate of 70–90% in biochar (P reservation). In soil, SSBC released more P in acid red soil and alkaline yellow soil than BDBC, while the opposite result appeared in neutral paddy soil. The P released from SSBC formed AlPO4 by combining with Al in soil, whereas P from BDBC transformed into Ca5(PO4)3F(or Cl) in conjunction with Ca in the soil (P replenishment). Various plants exhibited an uptake of approximately 2–6 times more P from biochar-amended soil than from the original soil (P reception). This study can guide the application of biochar in various soil–plant systems for effective nutrient reclamation.
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