The Role of Concentration and Solvent Character in the Molecular Organization of Humic Acids

dc.contributor.authorKlučáková, Martinacs
dc.contributor.authorVěžníková, Kateřinacs
dc.coverage.issue1cs
dc.coverage.volume21cs
dc.date.issued2016-10-21cs
dc.description.abstractThe molecular organization of humic acids in different aqueous solutions was studied over a wide concentration range (0.01–10 g/dm3). Solutions of humic acids were prepared in three different media: NaOH, NaCl, and NaOH neutralized by HCl after dissolution of the humic sample. Potentiometry, conductometry, densitometry, and high resolution ultrasound spectrometry were used in order to investigate conformational changes in the humic systems. The molecular organization of humic acids in the studied systems could be divided into three concentration ranges. The rearrangements were observed at concentrations of ~0.02 g/dm3 and ~1 g/dm3. The first “switch-over point” was connected with changes in the hydration shells of humic particles resulting in changes in their elasticity. The compressibility of water in the hydration shells is less than the compressibility of bulk water. The transfer of hydration water into bulk water increased the total compressibility of the solution, reducing the ultrasonic velocity. The aggregation of humic particles and the formation of rigid structures in systems with concentrations higher than 1 g/dm3 was detected.en
dc.description.abstractThe molecular organization of humic acids in different aqueous solutions was studied over a wide concentration range (0.01–10 g/dm3). Solutions of humic acids were prepared in three different media: NaOH, NaCl, and NaOH neutralized by HCl after dissolution of the humic sample. Potentiometry, conductometry, densitometry, and high resolution ultrasound spectrometry were used in order to investigate conformational changes in the humic systems. The molecular organization of humic acids in the studied systems could be divided into three concentration ranges. The rearrangements were observed at concentrations of ~0.02 g/dm3 and ~1 g/dm3. The first “switch-over point” was connected with changes in the hydration shells of humic particles resulting in changes in their elasticity. The compressibility of water in the hydration shells is less than the compressibility of bulk water. The transfer of hydration water into bulk water increased the total compressibility of the solution, reducing the ultrasonic velocity. The aggregation of humic particles and the formation of rigid structures in systems with concentrations higher than 1 g/dm3 was detected.en
dc.formattextcs
dc.format.extent1410-1418cs
dc.format.mimetypeapplication/pdfcs
dc.identifier.citationMOLECULES. 2016, vol. 21, issue 1, p. 1410-1418.en
dc.identifier.doi10.3390/molecules21101410cs
dc.identifier.issn1420-3049cs
dc.identifier.orcid0000-0003-4969-6988cs
dc.identifier.other129206cs
dc.identifier.urihttp://hdl.handle.net/11012/68390
dc.language.isoencs
dc.publisherMDPI AGcs
dc.relation.ispartofMOLECULEScs
dc.relation.urihttp://www.mdpi.com/1420-3049/21/11/1410cs
dc.rightsCreative Commons Attribution 4.0 Internationalcs
dc.rights.accessopenAccesscs
dc.rights.sherpahttp://www.sherpa.ac.uk/romeo/issn/1420-3049/cs
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/cs
dc.subjecthumic aciden
dc.subjectmolecular organizationen
dc.subjectconformationen
dc.subjectaggregationen
dc.subjectultrasound spectrometryen
dc.subjecthumic acid
dc.subjectmolecular organization
dc.subjectconformation
dc.subjectaggregation
dc.subjectultrasound spectrometry
dc.titleThe Role of Concentration and Solvent Character in the Molecular Organization of Humic Acidsen
dc.title.alternativeThe Role of Concentration and Solvent Character in the Molecular Organization of Humic Acidsen
dc.type.driverarticleen
dc.type.statusPeer-revieweden
dc.type.versionpublishedVersionen
sync.item.dbidVAV-129206en
sync.item.dbtypeVAVen
sync.item.insts2025.10.14 14:06:29en
sync.item.modts2025.10.14 09:34:59en
thesis.grantorVysoké učení technické v Brně. Fakulta chemická. CMV - laboratoř biokoloidůcs

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