journal article·2020-11

Microaggregation of goethite and illite evaluated by mechanistic modeling

Simon Zech, Stefan Dultz, Georg Guggenberger, Alexander Prechtel, Nadja Ray

Publisher page

Abstract

Abstract Clay minerals and Fe- and Al-oxyhydroxides are considered as the most important materials for the formation of microaggregate building units in soils. The mode of aggregation and the resulting structure and stability are largely determined by their size, aspect ratio (AR), differences in surface charge (SC), and mixing ratio. Here, the impact of these parameters on the formation of microaggregate building units (BUs) was elucidated with a mechanistic model, i.e. using a twophase cellular automaton method, in which prototypes of illite and goethite were implemented. The simulations allowed assessing the formation of particle arrangements during aggregation, moreover building unit diameters, and the number of discrete particles. The contact area between particles was evaluated as a quantitative measure for stability. Homoaggregation of illite under the sole influence of attracting van der Waals forces enabling face-to-face as well as edge-to-face contacts, resulted in compact structures with a small mean diameter and specific surface area. In contrast, electrostatic attraction between negatively charged faces and positively charged edges favored formation of larger card-house structures, where low contact areas indicated the low stability of the resulting BUs. At constant AR, homoaggregation of illite of different particle size led to BUs of different stability, more precisely smaller particle sizes led to more stable BUs. Variation of the AR of illite, while keeping the particle size constant, revealed that most stable BUs arose from illite with smallest AR. Shielding of coarse goethite particles due to attachment of fine illite with negatively charged edges increased the number of discrete fine illite particles not aggregated. Aggregation of illite with positively charged edges was in fundamental difference to results from simulations with negative edges because of electrostatic attraction between illite particles. The simulation setting, without using fitting parameters resulted in an appropriate approximation of laboratory findings. The simulation clearly facilitated the understanding of microaggregate building unit formation and stability by illuminating turnover dynamics and provision of quantitative data.
Source: openaire · Quality: candidate unverified · Source record ↗

Research context

OpenAlex topics: Soil and Unsaturated Flow · Clay minerals and soil interactions · Geotechnical Engineering and Soil Mechanics

SciVX discovery tags are terminology-based. OpenAlex topics are source-provided classifications.

References (33)

Show source-provided references
1. Adsorption of a soil humic acid at the surface of goethite and its competitive interaction with phosphate10.1016/j.geoderma.2006.10.011 ↗
2. Evidence of aggregate hierarchy at micro- to submicron scales in an allophanic andisol10.1016/j.geoderma.2013.10.005 ↗
3. Effects of iron and organic matter on the porosity and structural stability of soil aggregates10.1016/S0167-1987(98)00092-0 ↗
4. Rheological properties of sodium montmorillonite dispersions10.1016/0169-1317(88)90033-6 ↗
5. Surface charge evolution of mineral-organic complexes during pedogenesis in hawaiian basalt10.1016/j.gca.2004.06.005 ↗
6. Microbial diversity affects self-organization of the soil – microbe system with consequences for function10.1098/rsif.2011.0679 ↗
7. Iron (hydr)oxide crystallinity effects on soil aggregation10.2136/sssaj2003.6060 ↗
8. Size and charge constraints in microaggregation: Model experiments with mineral particle size fractions10.1016/j.clay.2019.01.002 ↗
9. Interaction of fe-oxyhydroxide colloidal particles with montmorillonite10.1180/claymin.1995.030.3.03 ↗
10. Shear rheology of hard-sphere, dispersed, and aggregated suspensions, and filler-matrix composites10.1016/j.cis.2011.12.005 ↗
11. Phosphorus-induced mobilization of colloids: model systems and soils10.1111/j.1365-2389.2007.00982.x ↗
12. Johnston · 2002 · 37
13. Impact of organic matter, iron oxides, alumina, silica and drying on mechanical and water stability of artificial soil aggregates. Assessment of new method to study water stability10.1016/j.geoderma.2014.01.020 ↗
14. The role of edge surfaces in flocculation of 2:1 clay minerals10.2136/sssaj1995.03615995005900020023x ↗
15. The ph dependent surface charging and points of zero charge. viii. update10.1016/j.cis.2019.102064 ↗
16. Aggregation in dispersions of hematite and of hematite-akageneite composite containing anionic surfactants10.1080/01932691.2016.1170611 ↗
17. Influence of ph and humic acid on coagulation kinetics of kaolinite: a dynamic light scattering study10.1006/jcis.1998.5440 ↗
18. Chapter 8 – colloid clay science
19. Influence of aspect ratio on barrier properties of polymer-clay nanocomposites10.1103/PhysRevLett.95.088303 ↗
20. Clay mineralogy of soils
21. Aggregate hierarchy in soils10.1071/SR9910815 ↗
22. Lessivage as a major process of soil formation: a revisitation of existing data10.1016/j.geoderma.2011.07.031 ↗
23. Discrete-continuum multiscale model for transport, biomass development and solid restructuring in porous media10.1016/j.advwatres.2017.04.001 ↗
24. Modeling the formation of soil microaggregates10.1016/j.cageo.2019.02.010 ↗
25. Discrete-continuum multiphase model for structure formation in soils including electrostatic effects10.3389/fenvs.2018.00096 ↗
26. Application of a cellular automaton method to model the structure formation in soils under saturated conditions: a mechanistic approach10.3389/fenvs.2019.00170 ↗
27. Aggmodel: a soil organic matter model with measurable pools for use in incubation studies10.1016/j.ecolmodel.2013.04.010 ↗
28. Organic matter and water-stable aggregates in soils10.1111/j.1365-2389.1982.tb01755.x ↗
29. Surface charge heterogeneity of kaolinite in aqueous suspension in comparison with montmorillonite10.1016/j.clay.2006.05.009 ↗
30. Microaggregates in soils10.1002/jpln.201600451 ↗
31. Biological and physical processes that mediate micro-aggregation of clays10.1097/01.ss.0000178206.74040.0c ↗
32. A collection of aspect ratios of common clay minerals determined from conductometric titrations10.1180/claymin.2014.049.3.10 ↗
33. Adsorption of humic acids onto goethite: Effects of molar mass, ph and ionic strength10.1016/j.jcis.2007.05.039 ↗