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Characterization of humic substances and non-ideal phenanthrene sorption as affected by clay-humic interactions.

机译:受粘土-腐殖质相互作用影响的腐殖质和非理想菲吸附的表征。

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摘要

Humic substances (HS) are major components of soil organic matter (SOM). Advances on characterization of HS and their interaction with minerals can provide a more fundamental understanding of HS functions in soils. The objectives of this research were to investigate potential fractionation of humic acid (HA) upon adsorption on minerals and to determine any variation on structure and sorption properties of humin extracted by different methods. Nuclear magnetic resonance (NMR) spectra, for the first time, provided direct evidence that HA was fractionated during adsorption on mineral surfaces. Aliphatic fractions of HA were preferentially adsorbed while aromatic fractions were more likely to be left in solution. The bound HA fractions had higher sorption linearity (N) and affinity (KOC) for phenanthrene than the source HA. For montmorillonite and kaolinite, the KOC values of adsorbed HA were up to several times higher than that of the source HA as a result of fractionation. Extraction procedures had substantial influences in structure and sorption characteristics of humin. Humin from 0.1 M NaOH exhaustive extraction and 6 M HF/HCl extraction at 60°C had relatively more aliphatic components as compared with 1 M HF extracted humin. The treatment of 6 M HF/HCl at 60°C reduced more than 50% carbohydrate components (50-108 ppm) and enriched amorphous poly(methylene) domains. The NaOH exhaustively extracted humin had the most nonlinear sorption isotherms and the HF extracted humin had the lowest KOC. We concluded that both NaOH and NaOH-HF procedures were appropriate approaches for humin extraction but the extraction with 6 M HF/HCl at 60 °C would be discouraged for use due to structural modifications of humin both chemically and physically. Segmental mobility of HA in solution was also explored by NMR relaxation. Proton spin-lattice relaxation time (T1) of HAs ranged from 0.3 to 0.8 s in d6-DMSO, and from 0.26 to 2.3 s in 0.5 M NaOD at 300 MHz. Proton correlation time of HA in solvents was in an order of 10-10 s. Carbohydrate was identified as the largest and the most immobile components while aliphatic and aromatic fragments were relatively smaller and more mobile in aqueous solution.
机译:腐殖质(HS)是土壤有机质(SOM)的主要成分。 HS的表征及其与矿物质的相互作用的进展可以提供对土壤中HS功能的更基本的了解。这项研究的目的是研究腐殖酸(HA)在矿物上吸附后的潜在分馏作用,并确定通过不同方法提取的腐殖质的结构和吸附特性的任何变化。核磁共振(NMR)光谱首次提供了直接的证据,证明HA在矿物表面吸附过程中被分离了。 HA的脂肪级分优先吸附,而芳族级分更可能留在溶液中。与来源HA相比,结合的HA馏分对菲的吸附线性(N)和亲和力(KOC)高。对于蒙脱石和高岭石,由于分馏,吸附的HA的KOC值比源HA的KOC值高几倍。提取程序对腐殖质的结构和吸附特性有重大影响。与1 M HF提取的腐殖质相比,0.1 M NaOH彻底提取和6 M HF / HCl提取在60°C下的腐殖质具有相对更多的脂肪族成分。在60°C下处理6 M HF / HCl减少了50%以上的碳水化合物成分(50-108 ppm),并富集了无定形的聚(亚甲基)域。用NaOH彻底萃取的人红素具有最大的非线性吸附等温线,而用HF萃取的人红素具有最低的KOC。我们得出的结论是,NaOH和NaOH-HF程序均是提取腐殖质的合适方法,但由于腐殖质的化学和物理结构改变,不建议在60°C下用6 M HF / HCl进行提取。还通过NMR弛豫探索了HA在溶液中的节段迁移率。在d6-DMSO中,HA的质子自旋晶格弛豫时间(T1)在0.3到0.8 s之间,而在300 MHz下在0.5 M NaOD中则在0.26到2.3 s之间。 HA在溶剂中的质子相关时间约为10-10 s。碳水化合物被认为是最大和最不易移动的组分,而脂肪族和芳香族的碎片相对较小,并且在水溶液中更易移动。

著录项

  • 作者

    Wang, Kaijun.;

  • 作者单位

    University of Massachusetts Amherst.;

  • 授予单位 University of Massachusetts Amherst.;
  • 学科 Agriculture Soil Science.; Environmental Sciences.; Geochemistry.
  • 学位 Ph.D.
  • 年度 2005
  • 页码 123 p.
  • 总页数 123
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 土壤学;环境科学基础理论;地质学;
  • 关键词

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