Restructuring of a peat in interaction with multivalent cations: effect of cation type and aging time

PLoS One. 2013 Jun 4;8(6):e65359. doi: 10.1371/journal.pone.0065359. Print 2013.

Abstract

It is assumed to be common knowledge that multivalent cations cross-link soil organic matter (SOM) molecules via cation bridges (CaB). The concept has not been explicitly demonstrated in solid SOM by targeted experiments, yet. Therefore, the requirements for and characteristics of CaB remain unidentified. In this study, a combined experimental and molecular modeling approach was adopted to investigate the interaction of cations on a peat OM from physicochemical perspective. Before treatment with salt solutions of Al(3+), Ca(2+) or Na(+), respectively, the original exchangeable cations were removed using cation exchange resin. Cation treatment was conducted at two different values of pH prior to adjusting pH to 4.1. Cation sorption is slower (>>2 h) than deprotonation of functional groups (<2 h) and was described by a Langmuir model. The maximum uptake increased with pH of cation addition and decreased with increasing cation valency. Sorption coefficients were similar for all cations and at both pH. This contradicts the general expectations for electrostatic interactions, suggesting that not only the interaction chemistry but also spatial distribution of functional groups in OM determines binding of cations in this peat. The reaction of contact angle, matrix rigidity due to water molecule bridges (WaMB) and molecular mobility of water (NMR analysis) suggested that cross-linking via CaB has low relevance in this peat. This unexpected finding is probably due to the low cation exchange capacity, resulting in low abundance of charged functionalities. Molecular modeling demonstrates that large average distances between functionalities (∼3 nm in this peat) cannot be bridged by CaB-WaMB associations. However, aging strongly increased matrix rigidity, suggesting successive increase of WaMB size to connect functionalities and thus increasing degree of cross-linking by CaB-WaMB associations. Results thus demonstrated that the physicochemical structure of OM is decisive for CaB and aging-induced structural reorganisation can enhance cross-link formation.

MeSH terms

  • Cations / chemistry
  • Hydrogen-Ion Concentration
  • Models, Molecular
  • Molecular Conformation
  • Organic Chemicals / chemistry
  • Sodium Hydroxide / chemistry
  • Soil / chemistry*
  • Surface Properties
  • Temperature
  • Time Factors
  • Water / chemistry

Substances

  • Cations
  • Organic Chemicals
  • Soil
  • Water
  • Sodium Hydroxide

Grants and funding

This work was supported by DFG within the priority programme SPP 1315 “Biogeochemical Interfaces in Soil”, projects SCHA849/8 and GE 1676/1 (www.dfg.de). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.