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首页> 外文期刊>Environmental Science & Technology >Linking Phosphorus Sequestration to Carbon Humification in Wetland Soils by ~(31)P and ~(13)C NMR Spectroscopy
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Linking Phosphorus Sequestration to Carbon Humification in Wetland Soils by ~(31)P and ~(13)C NMR Spectroscopy

机译:〜(31)P和〜(13)C NMR光谱法将磷固存与湿地土壤中的碳增湿联系起来

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摘要

Phosphorus sequestration in wetland soils is a prerequisite for long-term maintenance of water quality in downstream aquatic systems, but can be compromised if phosphorus is released following changes in nutrient status or hydrological regimen. The association of phosphorus with relatively refractory natural organic matter (e.g., humic substances) might protect soil phosphorus from such changes. Here we used hydrofluoric acid (HF) pretreatment to remove phosphorus associated with metals or anionic sorption sites, allowing us to isolate a pool of phosphorus associated with the soil organic fraction. Solution ~(31)P and solid state ~(13)C NMR spectra for wetland soils were acquired before and after hydrofluoric acid pretreatment to assess quantitatively and qualitatively the changes in phosphorus and carbon functional groups. Organic phosphorus was largely unaffected by HF treatment in soils dominated by refractory alkyl and aromatic carbon groups, indicating association of organic phosphorus with stable, humified soil organic matter. Conversely, a considerable decrease in organic phosphorus following HF pretreatment was detected in soils where O-alkyl groups represented the major fraction of the soil carbon. These correlations suggest that HF treatment can be used as a method to distinguish phosphorus fractions that are bound to the inorganic soil components from those fractions that are stabilized by incorporation into soil organic matter.
机译:湿地土壤中的磷固存是长期维持下游水生系统水质的前提,但如果养分状况或水文状况发生变化而释放磷,磷的吸收就会受到损害。磷与相对难处理的天然有机物(例如腐殖质)的结合可能会保护土壤磷免于这种变化。在这里,我们使用了氢氟酸(HF)预处理来去除与金属或阴离子吸附位点相关的磷,从而使我们能够分离出与土壤有机部分相关的磷。在氢氟酸预处理之前和之后,获取了湿地土壤的溶液〜(31)P和固态〜(13)C NMR光谱,以定量和定性地评估磷和碳官能团的变化。在难处理的烷基和芳族碳基团为主的土壤中,有机磷在很大程度上不受HF处理的影响,表明有机磷与稳定,增湿的土壤有机质缔合。相反,在以O-烷基为土壤碳主要成分的土壤中,进行HF预处理后,有机磷显着减少。这些相关性表明,HF处理可用作区分结合到无机土壤组分上的磷组分和那些通过掺入土壤有机质而稳定的组分的方法。

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  • 来源
    《Environmental Science & Technology 》 |2012年第9期| p.4775-4782| 共8页
  • 作者单位

    Department of Chemistry & Biochemistry, Florida State University, Tallahassee, Florida 32306-4390, United States;

    Department of Chemistry & Biochemistry, Florida State University, Tallahassee, Florida 32306-4390, United States;

    Smithsonian Tropical Research Institute, Apartado 0843-03092, Balboa, Ancon, Republic of Panama;

    Smithsonian Tropical Research Institute, Apartado 0843-03092, Balboa, Ancon, Republic of Panama;

    Soil and Water Science Department, University of Florida, Gainesville, Florida 32611, United States;

    Department of Chemistry & Biochemistry, Florida State University, Tallahassee, Florida 32306-4390, United States;

  • 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
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