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Phosphorus adsorption and release characteristics of surface sediments in Dianchi Lake, China

机译:滇池表层沉积物对磷的吸附和释放特征

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摘要

Phosphorus adsorption and release characteristics of surface sediments from Dianchi Lake were investigated through indoor simulation experiments. Kinetics and thermodynamics of adsorption and release of phosphorus in sediments were studied, and the influence of different phosphorus fractions on adsorption and release was analysed. Results show that the total phosphorus content in the sediments ranged from 843.96 to 8144.44 mg kg(-1), which was 2-8 times as much as those in other lakes in China (e.g. Erhai Lake and Taihu Lake). The average values of different phosphorus forms in the sediment samples were ranked in the order of organic P (OP), calcium-bound P (Ca-P), metal oxide-bound P (Al-P), residual P (Res-P), Fe-bound P (Fe-P) and weakly absorbed P(NH4Cl-P). Compared with the case of other lakes in China, the sedimentary phosphorus adsorption capacity of Dianchi Lake was at a higher level, but its maximal release rate and release capacity were low, indicating a relatively low release risk. By comparing the equilibrium phosphate concentration in the sediments and the soluble reactive phosphorus in the overlying water, the risks of phosphorus release from sediments in Caohai, Lake Central and Southern Waihai were found to be relatively low in the short term, but were high in Northern Waihai. The release behaviour of sedimentary phosphorus in Dianchi Lake was mainly determined by NH4Cl-P, Fe-P and Al-P, among which NH4Cl-P and Fe-P served a greater function. Therefore, the contents of different fractions of phosphorus and their distribution characterization should be considered when characterizing the adsorption and release status of lake sedimentary phosphorus.
机译:通过室内模拟实验研究了滇池表层沉积物对磷的吸附和释放特征。研究了沉积物中磷的吸附和释放的动力学和热力学,分析了不同磷组分对磷的吸附和释放的影响。结果表明,沉积物中的总磷含量为843.96至8144.44 mg kg(-1),是中国其他湖泊(如Er海和太湖)的2-8倍。沉积物样品中不同磷形态的平均值按有机磷(OP),钙结合磷(Ca-P),金属氧化物结合磷(Al-P),残留磷(Res-P ),Fe结合的P(Fe-P)和弱吸收的P(NH4Cl-P)。与中国其他湖泊相比,滇池的沉积物对磷的吸附能力较高,但最大释放速率和释放能力较低,表明释放风险相对较低。通过比较沉积物中的平衡磷酸盐浓度和上覆水中的可溶性活性磷,在短期内草海,中部湖和南部外海的沉积物释放磷的风险相对较低,而在北部则较高外海滇池沉积物中磷的释放行为主要由NH4Cl-P,Fe-P和Al-P决定,其中NH4Cl-P和Fe-P发挥更大的作用。因此,在表征湖泊沉积磷的吸附和释放状态时,应考虑磷的不同含量及其分布特征。

著录项

  • 来源
    《Environmental earth sciences》 |2015年第5期|3689-3700|共12页
  • 作者单位

    Kunming Inst Environm Sci, Kunming 650032, Yunnan, Peoples R China;

    Kunming Inst Environm Sci, Kunming 650032, Yunnan, Peoples R China;

    Kunming Inst Environm Sci, Kunming 650032, Yunnan, Peoples R China;

    Beijing Normal Univ, Coll Water Sci, Beijing 100875, Peoples R China|Kunming Inst Environm Sci, Kunming 650032, Yunnan, Peoples R China;

    Chinese Res Inst Environm Sci, Beijing 100012, Peoples R China;

    Chinese Res Inst Environm Sci, Beijing 100012, Peoples R China;

    Kunming Inst Environm Sci, Kunming 650032, Yunnan, Peoples R China;

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

    Dianchi Lake; Surface sediment; Phosphorus adsorption; Phosphorus release;

    机译:滇池;地表沉积物;磷吸附;磷释放;
  • 入库时间 2022-08-18 03:30:59

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