Organic matter coatings of soil minerals affect adsorptive interactions with phenolic and amino acids

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dc.identifier.uri http://dx.doi.org/10.15488/3731
dc.identifier.uri https://www.repo.uni-hannover.de/handle/123456789/3765
dc.contributor.author Gao, J.
dc.contributor.author Jansen, B.
dc.contributor.author Cerli, C.
dc.contributor.author Helmus, R.
dc.contributor.author Mikutta, R.
dc.contributor.author Dultz, S.
dc.contributor.author Guggenberger, G.
dc.contributor.author Vogel, C.
dc.contributor.author Kalbitz, K.
dc.date.accessioned 2018-09-21T12:30:25Z
dc.date.available 2018-09-21T12:30:25Z
dc.date.issued 2018
dc.identifier.citation Gao, J.; Jansen, B.; Cerli, C.; Helmus, R.; Mikutta, R. et al.: Organic matter coatings of soil minerals affect adsorptive interactions with phenolic and amino acids. In: European Journal of Soil Science 69 (2018), Nr. 4, S. 613-624. DOI: https://doi.org/10.1111/ejss.12562
dc.description.abstract Phenolic (PAs) and amino acids (AAs) contribute potentially to the stabilization of organic matter (OM) in soil by forming mineral–organic associations (MOAs). However, little is known about how natural OM coating affects the adsorption of these compounds and their mutual interaction upon adsorption. Therefore, batch adsorption experiments were carried out to study how coatings of minerals with dissolved organic matter (DOM) obtained from forest leaf litter (L-DOM) and from the O horizon (O-DOM) affect the adsorption of phenolic acids (salicylic, syringic, ferulic and vanillic acid) and amino acids (lysine, glutamic acid, leucine and phenylalanine) at pH 6. Moreover, the adsorption of PAs on OM-coated minerals was tested after preconditioning by AAs and vice versa. Adsorption of DOM depended on the mineral (goethite ≫ kaolinite > montmorillonite) and sources of DOM (O-DOM > L-DOM for goethite). Coatings of all minerals with both DOM sources reduced the adsorption of PAs and the acidic glutamic acid but enhanced that of the basic lysine. The adsorption of PAs decreased with increasing OM coating of the minerals. Strong bonds between AAs and OM-coated minerals generally enhanced adsorption of PAs with preconditioning by AAs. This indirectly indicates a multilayer model of MOA. Adsorption of AAs, however, was rarely influenced by preconditioning with PAs. Competition between AAs and PAs generally suppressed the adsorption of AAs on coated minerals, whereas the PAs were hardly affected. These results emphasize that the amount and composition of OM coating must be considered when studying the adsorption of PAs and AAs in soil. Highlights: Adsorption of DOM on minerals followed the order: goethite ≫ kaolinite > montmorillonite. Adsorption of O-DOM (O horizon) on goethite was larger than that of L-DOM (leaf litter). Coatings of DOM reduced adsorption of PAs and acidic AAs and enhanced that of basic AAs. The amount and composition of OM coating affected the adsorption of PAs and AAs. eng
dc.language.iso eng
dc.publisher Hoboken, NJ : Blackwell Publishing Ltd
dc.relation.ispartofseries European Journal of Soil Science 69 (2018), Nr. 4
dc.rights CC BY-NC-ND 4.0 Unported
dc.rights.uri https://creativecommons.org/licenses/by-nc-nd/4.0/
dc.subject adsorption eng
dc.subject amino acid eng
dc.subject coating eng
dc.subject dissolved organic matter eng
dc.subject experimental study eng
dc.subject leaf litter eng
dc.subject phenolic compound eng
dc.subject soil horizon eng
dc.subject soil nutrient eng
dc.subject soil organic matter eng
dc.subject soil stabilization eng
dc.subject.ddc 550 | Geowissenschaften ger
dc.title Organic matter coatings of soil minerals affect adsorptive interactions with phenolic and amino acids
dc.type Article
dc.type Text
dc.relation.issn 13510754
dc.relation.doi https://doi.org/10.1111/ejss.12562
dc.bibliographicCitation.issue 4
dc.bibliographicCitation.volume 69
dc.bibliographicCitation.firstPage 613
dc.bibliographicCitation.lastPage 624
dc.description.version publishedVersion
tib.accessRights frei zug�nglich


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