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Updated: Sep 16, 2025

Paramagnetic Relaxation Enhancement for Detecting and Characterizing Self-Associations of Intrinsically Disordered Proteins
Published on: September 23, 2021
Paramagnetic Probing of Humic Acid Supramolecular Structure: Iron (III)-Induced Rearrangements Revealed by
Pellegrino Conte1, Calogero Librici1
1Department of Agricultural, Food and Forest Sciences, University of Palermo, Palermo, Italy.
Iron (III) binding to humic acids causes structural changes, rigidifying carboxyl and aromatic parts while leaving aliphatic regions flexible. This reveals how metal ions reorganize soil organic matter at a molecular level.
Area of Science:
- Environmental Chemistry
- Soil Science
- Spectroscopy
Background:
- Humic acids (HAs) are crucial soil organic matter components.
- Metal ion complexation significantly alters HA structure and dynamics.
- Molecular-level understanding of these interactions is limited.
Purpose of the Study:
- To investigate iron (III)-induced structural and dynamic changes in soil-derived humic acids.
- To quantify metal-induced reorganization using NMR relaxation parameters.
Main Methods:
- Solid-state 13C CPMAS NMR spectroscopy was used.
- Cross-polarization time constants (TCH) and proton rotating-frame relaxation times (T1ρ[H]) were measured.
- Analysis focused on Fe/C ratios to determine binding hierarchies and dynamic changes.
Main Results:
- Iron (III) binding induced distinct structural rigidification, strongest in carboxyl groups, followed by aromatic domains.
- Aliphatic carbons showed minimal response, indicating their exclusion from metal coordination.
- T1ρ(H) data confirmed restricted molecular mobility in carboxyl and aromatic regions due to Fe (III).
Conclusions:
- Fe (III) acts as a supramolecular cross-linker, selectively rigidifying humic acid structure via carboxylate and aromatic interactions.
- NMR relaxation parameters (TCH and T1ρ[H]) provide quantitative insights into metal-induced reorganization of soil organic matter.
- This study enhances mechanistic understanding of organo-mineral interactions in soils.
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