Phosphorus speciation and colloidal phosphorus responses to short-term cessation of fertilization in a lime concretion black soil
文献类型: 外文期刊
第一作者: Bai, Shanshan
作者: Bai, Shanshan;Tan, Jinfang;Zhang, Zeyuan;Wei, Mi;Jiang, Xiaoqian;Bai, Shanshan;Tan, Jinfang;Wei, Mi;Jiang, Xiaoqian;Bai, Shanshan;Tan, Jinfang;Wei, Mi;Jiang, Xiaoqian;Zhang, Huimin
作者机构:
关键词: Fe/Al oxide nanoparticles; fine colloids; P accumulation; 31P nuclear magnetic resonance; P sequential fractionation; soil acidification
期刊名称:PEDOSPHERE ( 影响因子:5.7; 五年影响因子:5.7 )
ISSN: 1002-0160
年卷期: 2023 年 33 卷 6 期
页码:
收录情况: SCI
摘要: Long-term excessive application of mineral fertilizer has led to soil acidification and phosphorus (P) accumulation, increasing the risk of P loss and environmental pollution, and cessation of fertilization is widely considered as a cost-effective management strategy to relieve this situation; however, how such cessation influences P speciation and concentrations in a bulk soil and colloidal fractions and whether decreasing P concentration might maintain soil fertility remain unclear. In this study, the effects of long-term fertilization (ca. 40 years) and short-term cessation of fertilization (ca. 16 months) on inorganic, organic, and colloidal P in lime concretion black soil were investigated using P sequential fractionation and 31P nuclear magnetic resonance spectroscopy. After long-term fertilization, available P, dicalcium phosphate, iron-bound P, orthophosphate monoesters, and orthophosphate diesters increased significantly, but soil pH decreased by ca. 2.8 units, indicating that long-term fertilization caused soil acidification and P accumulation and changed P speciation markedly. In contrast, short-term fertilization cessation increased soil pH by ca. 0.8 units and slightly reduced available and inorganic P. Available P after fertilization cessation was 22.9-29.8 mg kg-1, which was still sufficient to satisfy crop growth requirements. Additionally, fertilization cessation increased the proportions of fine colloids (100-450 nm, including nontronite and some amorphous iron oxides) and drove a significant release of iron/aluminum oxide nanoparticles (1-100 nm) and associated P with orthophosphate and pyrophosphate species. In summary, short-term fertilization cessation effectively alleviated soil acidification and inorganic P accumulation, while concomitantly maintaining soil P fertility and improving the potential mobilization of P associated with microparticles.
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