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Composition, particle size, charge and colloidal stability of pH-fractionated humic acids

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216305%3A26310%2F15%3APU113810" target="_blank" >RIV/00216305:26310/15:PU113810 - isvavai.cz</a>

  • Result on the web

    <a href="http://link.springer.com/article/10.1007/s11368-015-1142-2?wt_mc=email.event.1.SEM.ArticleAuthorAssignedToIssue" target="_blank" >http://link.springer.com/article/10.1007/s11368-015-1142-2?wt_mc=email.event.1.SEM.ArticleAuthorAssignedToIssue</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1007/s11368-015-1142-2" target="_blank" >10.1007/s11368-015-1142-2</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Composition, particle size, charge and colloidal stability of pH-fractionated humic acids

  • Original language description

    Purpose: The purpose of this study was to divide humic acids into several fractions by means of their dissolving in buffers with different pH values and to characterize obtained humic fractions with respect to their composition, structure, particle size and charge. Relation-ships between determined characteristics of fractionated humic acids and pH values of used buffer solutions and the method of fractionation was investigated. Materials and methods: Humic acids were fractionated by means of two different methods: the subsequent dissolution in buffers adjusted to different pH and the sequential dissolution in buffers with increasing pH values. Composition, structure and properties of the obtained humic fractions were studied using elemental analysis, FT-IR spectroscopy, UV/VIS spectroscopy and light scattering methods. Results and discussion: As expected, fractions obtained by subsequent dissolution were more heterogeneous than those prepared by sequential extraction. Fractions obtained at lower pH values contained higher amounts of aromatic and carboxylic groups, while those extracted at higher pH values were rich in aliphatic and/or peptide groups. Fractions extracted close to neutral pH region had some specific properties. Functional groups dissociated in a range of pH values depending on the chemical structure of the molecules. Weaker carboxylic groups could dissociate in less acidic solutions and more aromatic fractions could be dissolved. Conformational changes and deaggregation process differed with the fractionation procedure and concentration of studied solutions. A bimodal distribution of particle sizes and higher values of polydispersity were obtained for some for less concentrated solutions of humic fractions. Conclusions: Obtained humic fractions behave as anionic heterogeneous ligands with many carboxylic and phenolic groups of different strength, and present polyfunctional and polyelectrostatic effects due to different functional sites and net charge

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10403 - Physical chemistry

Result continuities

  • Project

    <a href="/en/project/LO1211" target="_blank" >LO1211: Materials Research Centre at FCH BUT- Sustainability and Development</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2015

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Journal of Soils and Sediments

  • ISSN

    1439-0108

  • e-ISSN

    1614-7480

  • Volume of the periodical

    15

  • Issue of the periodical within the volume

    9

  • Country of publishing house

    DE - GERMANY

  • Number of pages

    9

  • Pages from-to

    1900-1908

  • UT code for WoS article

    000359938600006

  • EID of the result in the Scopus database

    2-s2.0-84939472257