Chemical Force Spectroscopy Evidence Supporting the Layer-by-Layer Model of Organic Matter Binding to Iron (oxy)Hydroxide Mineral Surfaces
AuthorsChassé, Alexander W.
Higgins, Steven R.
Parr, Thomas B.
Online Publication Date2015-08-07
Print Publication Date2015-08-18
Permanent link to this recordhttp://hdl.handle.net/10754/597767
MetadataShow full item record
Abstract© 2015 American Chemical Society. The adsorption of dissolved organic matter (DOM) to metal (oxy)hydroxide mineral surfaces is a critical step for C sequestration in soils. Although equilibrium studies have described some of the factors controlling this process, the molecular-scale description of the adsorption process has been more limited. Chemical force spectroscopy revealed differing adhesion strengths of DOM extracted from three soils and a reference peat soil material to an iron (oxy)hydroxide mineral surface. The DOM was characterized using ultrahigh-resolution negative ion mode electrospray ionization Fourier Transform ion cyclotron resonance mass spectrometry. The results indicate that carboxyl-rich aromatic and N-containing aliphatic molecules of DOM are correlated with high adhesion forces. Increasing molecular mass was shown to decrease the adhesion force between the mineral surface and the DOM. Kendrick mass defect analysis suggests that mechanisms involving two carboxyl groups result in the most stable bond to the mineral surface. We conceptualize these results using a layer-by-layer "onion" model of organic matter stabilization on soil mineral surfaces.
CitationChassé AW, Ohno T, Higgins SR, Amirbahman A, Yildirim N, et al. (2015) Chemical Force Spectroscopy Evidence Supporting the Layer-by-Layer Model of Organic Matter Binding to Iron (oxy)Hydroxide Mineral Surfaces. Environ Sci Technol 49: 9733–9741. Available: http://dx.doi.org/10.1021/acs.est.5b01877.
SponsorsA.W.C. and T.O. extend our appreciation to Dr. Leonardo Gutierrez at the University of Illinois at Urbana–Champaign and Dr. Jean Philippe Croue at the King Abdullah University of Science and Technology for discussion and assistance with the preparation of the iron (oxy)hydroxide coated AFM probes. This project was supported by USDA-NIFA-AFRI 2013-67019-21368 and the Maine Agricultural and Forest Experiment Station Hatch Project ME0-H-1-00472-11. This is Maine Agricultural and Forest Experiment Station Journal no. 3432.
PublisherAmerican Chemical Society (ACS)
CollectionsPublications Acknowledging KAUST Support
- Higher Molecular Mass Organic Matter Molecules Compete with Orthophosphate for Adsorption to Iron (Oxy)hydroxide.
- Authors: Chassé AW, Ohno T
- Issue date: 2016 Jul 19
- Molecular-Scale Investigation with ESI-FT-ICR-MS on Fractionation of Dissolved Organic Matter Induced by Adsorption on Iron Oxyhydroxides.
- Authors: Lv J, Zhang S, Wang S, Luo L, Cao D, Christie P
- Issue date: 2016 Mar 1
- Iron plays an important role in molecular fractionation of dissolved organic matter at soil-water interface.
- Authors: Huang Z, Lv J, Cao D, Zhang S
- Issue date: 2019 Jun 20
- Effects of clay minerals, hydroxides, and timing of dissolved organic matter addition on the competitive sorption of copper, nickel, and zinc: A column experiment.
- Authors: Refaey Y, Jansen B, Parsons JR, de Voogt P, Bagnis S, Markus A, El-Shater AH, El-Haddad AA, Kalbitz K
- Issue date: 2017 Feb 1
- Adsorption and Molecular Fractionation of Dissolved Organic Matter on Iron-Bearing Mineral Matrices of Varying Crystallinity.
- Authors: Coward EK, Ohno T, Plante AF
- Issue date: 2018 Feb 6