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Phosphorus Buildup and Release Risk Associated with Agricultural Intensification in the Estuarine Sediments of Chaohu Lake Valley, Eastern China

机译:中国东部巢湖流域河口沉积物中与农业集约化有关的磷积累和释放风险

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摘要

Phosphorus (P) accumulation and the risk of P release were studied in the estuarine sediments of the Chaohu Lake Valley in Eastern China. Rapid agricultural intensification has occurred in this area since the 1980s, resulting in the extensive use of phosphate fertilizers. This extensive use of phosphate has affected P processes throughout the valley and resulted in the total phosphorus (TP) contents in the substrates and surface sediments increasing from 374 to 537 mg/kg, on average. Of all the forms of P evaluated in this study, residual P (Res-P) was present at the highest levels and accounted for 19.8-74.0% of the TP. Conversely, the lowest contents were observed for KCl-extracted P (KC1-P), which accounted for only 0.602% of the TP. Additionally, aluminum/iron-bound P (NaOH-Pi), which accounted for 16.0-53.1% of the TP, was an important factor that caused the TP to increase due to long-term P fertilization. However, calcium-bound P (Ca-P) was maintained at a relatively stable level. Furthermore, the degree of P saturation (DPS) and the P-induced lake eutrophication risk index (ERI) were investigated to determine the risk of release of P from the sediments. The average DPS and ERI values were found to range from 3.92-21.4% and from 12.6-33.6%, respectively. These results suggest that almost half of the estuarine sediments posed a potential risk of eutrophication. Moreover, these findings indicate that estuarine sediments that have been enriched with P are likely the sources of P that lead to the formation of algal blooms in Chaohu Lake.
机译:研究了中国东部巢湖流域河口沉积物中的磷(P)积累和磷释放的风险。自1980年代以来,该地区农业集约化迅速发展,导致了磷肥的广泛使用。磷酸盐的广泛使用已影响整个山谷的磷过程,并导致底物和表面沉积物中的总磷(TP)含量平均从374 mg / kg增加到537 mg / kg。在这项研究评估的所有形式的磷中,残留的磷(Res-P)含量最高,占总磷的19.8-74.0%。相反,KCl萃取的磷(KC1-P)的含量最低,仅占TP的0.602%。此外,铝/铁结合的磷(NaOH-Pi)占总磷的16.0-53.1%,是由于长期施磷导致总磷增加的重要因素。但是,钙结合的磷(Ca-P)保持在相对稳定的水平。此外,调查了磷饱和度(DPS)和磷诱导的湖泊富营养化风险指数(ERI),以确定磷从沉积物中释放的风险。发现平均DPS和ERI值分别为3.92-21.4%和12.6-33.6%。这些结果表明,近一半的河口沉积物具有富营养化的潜在风险。此外,这些发现表明,富含磷的河口沉积物很可能是导致巢湖中藻华形成的磷的来源。

著录项

  • 来源
    《Clean》 |2010年第4期|P.336-343|共8页
  • 作者单位

    Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing, P. R. China;

    rnState Key Laboratory on Environmental Aquatic Chemistry, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, P. R. China;

    rnResearch Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing, P. R. China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    agricultural intensification; chaohu lake; estuarine sediments; risk;

    机译:农业集约化;巢湖河口沉积物;风险;

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