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Composition of dissolved organic matter controls interactions with La and Al ions: Implications for phosphorus immobilization in eutrophic lakes

机译:溶解有机物的成分控制着与La和Al离子的相互作用:对富营养化湖泊中磷的固定化的意义

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摘要

Applications of aluminium (Al) salt or lanthanum (La) modified bentonite (LMB) have become popular methodologies for immobilizing phosphorus (P) in eutrophic lakes. The presence of humic substances, has been shown to inhibit this form of treatment due to the complexation with La/Al. However, the effects of other dissolved organic matter (DOM), especially that derived from phytoplankton (the dominant source in eutrophic lakes) are unknown. In this study, the interaction with La/Al of Suwannee River Standard Humic Acid Standard II (SRHA) and algae-derived DOM (ADOM) were investigated and compared. Differed to SRHA which was dominated by polyphenol-like component (76.8%, C1-SRHA), majority in ADOM were protein-like substance, including 41.9% tryptophan-like component (C2-ADOM) and 21.0% tyrosine-like component (C3-ADOM). Two reactions of complexation and coprecipitation were observed between SRHA/ADOM and La/Al. Complexation dominated at low metal inputs less than 10 mu M and coprecipitation was the main reaction at higher metal inputs. For ADOM, the tryptophan-like component (C2-ADOM) was the important component to react with metal. The reaction rate for C2-ADOM with La were about two-third of that for C1-SRHA, indicating that the influence of C2-ADOM was significant during the P immobilization by La/Al-based treatment in eutrophic lakes. The P removal data in the presence of ADOM confirmed the significant inhibition of ADOM. In addition, based on the composition of coprecipitates and relatively biodegradable character of tryptophan-like substances (C-ADOM), the coprecipitation of ADOM was assumed to reduce the stability of precipitated Pin eutrophic lakes. The release of P from the potential biodegradation of the coprecipitates and thus the possible decline of the performance of P immobilization by La/Al-based treatments is an important work in the future. (C) 2019 Elsevier Ltd. All rights reserved.
机译:铝(Al)盐或镧(La)改性膨润土(LMB)的应用已成为在富营养化湖泊中固定磷(P)的流行方法。由于与La / Al络合,腐殖质的存在已显示出抑制这种处理方式的作用。但是,其他溶解性有机物(DOM)的影响,特别是浮游植物(富营养化湖泊的主要来源)所产生的影响尚不清楚。在这项研究中,调查和比较了Suwannee河标准腐殖酸标准II(SRHA)和藻类衍生的DOM(ADOM)与La / Al的相互作用。与以多酚样成分(76.8%,C1-SRHA)为主的SRHA不同,ADOM中的大部分为蛋白质样物质,其中色氨酸样成分(C2-ADOM)为41.9%,酪氨酸样成分(C3为21.0%)。 -ADOM)。在SRHA / ADOM和La / Al之间观察到两个络合和共沉淀反应。低金属输入量小于10μM时,络合反应占主导,而高金属输入量时,共沉淀是主要反应。对于ADOM,色氨酸样组分(C2-ADOM)是与金属反应的重要组分。 C2-ADOM与La的反应速率约为C1-SRHA的三分之二,表明在富营养化湖泊中,通过La / Al基处理将P固定化过程中,C2-ADOM的影响非常显着。在ADOM存在下的P去除数据证实了ADOM的显着抑制。另外,基于共沉淀物的组成和色氨酸样物质(C-ADOM)的相对可生物降解的特性,假定ADOM的共沉淀会降低沉淀的Pin富营养化湖泊的稳定性。从共沉淀物中潜在的生物降解过程中释放出P,从而可能导致La / Al基处理对P固定化性能的降低,这是将来的一项重要工作。 (C)2019 Elsevier Ltd.保留所有权利。

著录项

  • 来源
    《Environmental Pollution》 |2019年第5期|36-47|共12页
  • 作者单位

    Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing 210008, Jiangsu, Peoples R China;

    Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing 210008, Jiangsu, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China;

    Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing 210008, Jiangsu, Peoples R China;

    Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing 210008, Jiangsu, Peoples R China;

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

    Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing 210008, Jiangsu, Peoples R China;

    Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing 210008, Jiangsu, Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Dissolved organic matter; Interaction; La; Al; EEM-PARAFAC; Phosphorus immobilization;

    机译:溶解有机物;相互作用;La;Al;EEM-PARAFAC;固磷;
  • 入库时间 2022-08-18 04:24:17

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