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Responses in sediment phosphorus and lanthanum concentrations and composition across 10 lakes following applications of lanthanum modified bentonite

机译:镧改性膨润土应用后对10个湖泊沉积物中磷和镧浓度和组成的响应

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摘要

A combined field and laboratory scale study of 10 European lakes treated between 2006 and 2013 with a lanthanum (La) modified bentonite (LMB) to control sediment phosphorus (P) release was conducted. The study followed the responses in sediment characteristics including La and P fractions and binding forms, P adsorption capacity of discrete sediment layers, and pore water P concentrations. Lanthanum phosphate mineral phases were confirmed by solid state P-31 MAS NMR and L-III EXAFS spectroscopy. Rhabdophane (LaPO4 center dot nH(2)O) was the major phase although indications of monazite (LaPO4) formation were also reported, in the earliest treated lake. Molar ratios between La and P in the sediments were generally above 1, demonstrating excess La relative to P. Lanthanum was vertically mixed in the sediment down to a depth of 10 cm for eight of the ten lakes, and recovery of La in excess of 100% of the theoretical aerial load indicated translocation of the LMB towards the deepest areas of the lakes. Lanthanum was generally recovered from bed sediment samples following sequential chemical extraction from the HCI fraction. Soluble reactive P (SRP) release experiments on intact sediment cores indicated conditions of P retention (with the exception of two lakes) by sediments, indicating effective control of sediment P release, i.e. between two and nine years after treatment. (C) 2016 Elsevier Ltd. All rights reserved.
机译:在2006年至2013年之间对10个欧洲湖泊进行了野外和实验室规模的联合研究,这些湖泊使用镧(La)改性膨润土(LMB)处理以控制沉积物磷(P)的释放。该研究跟踪了沉积物特征中的响应,包括La和P分数和结合形式,离散沉积物层对P的吸附能力以及孔隙水中P的浓度。磷酸镧矿物相通过固态P-31 MAS NMR和L-III EXAFS光谱确认。尽管最早的湖泊中也有独居石(LaPO4)形成的迹象,但Rhabdophane(LaPO4中心点nH(2)O)是主要相。沉积物中La和P的摩尔比通常大于1,表明相对于P过量的La。在十个湖泊中的八个中,镧在沉积物中垂直混合至10 cm的深度,而La的回收率超过100理论空载的百分比表示LMB向湖泊最深处转移。从HCI馏分中进行顺序化学萃取后,通常从床沉积物样品中回收镧。在完整的沉积物核心上进行的可溶性反应性P(SRP)释放实验表明,沉积物对P的保留条件(两个湖泊除外),表明了对沉积物P释放的有效控制,即在处理后的2至9年之间。 (C)2016 Elsevier Ltd.保留所有权利。

著录项

  • 来源
    《Water Research》 |2016年第15期|101-110|共10页
  • 作者单位

    Univ Southern Denmark, Dept Phys Chem & Pharm, Campusvej 55, DK-5230 Odense M, Denmark|Univ Southern Denmark, Dept Biol, Campusvej 55, DK-5230 Odense M, Denmark;

    Univ Southern Denmark, Dept Phys Chem & Pharm, Campusvej 55, DK-5230 Odense M, Denmark;

    Wageningen Univ, Dept Environm Sci, Aquat Ecol & Water Qual Management Grp, POB 47, NL-6700 AA Wageningen, Netherlands;

    Ctr Ecol & Hydrol, Penicuik EH26 0QB, Midlothian, Scotland;

    Inst Dr Nowak, Mayenbrook 1, D-28870 Ottersberg, Germany;

    Swedish Univ Agr Sci, Dept Chem & Biotechnol, POB 7015, SE-75007 Uppsala, Sweden;

    Ctr Ecol & Hydrol, Penicuik EH26 0QB, Midlothian, Scotland;

    Univ Southern Denmark, Dept Phys Chem & Pharm, Campusvej 55, DK-5230 Odense M, Denmark;

    Univ Southern Denmark, Dept Biol, Campusvej 55, DK-5230 Odense M, Denmark;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Lake restoration; Dissolved organic carbon (DOC); 31P NMR; Lanthanum; P sequestration; EXAFS; Full scale; Lanthanum modified bentonite;

    机译:湖泊恢复;溶解有机碳(DOC);31P NMR;镧;P螯合;EXAFS;大型;镧改性膨润土;
  • 入库时间 2022-08-17 13:41:49

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