Molecular origin of stress softening in elastomer-based nanocomposites via in situ elongational nuclear magnetic resonance spectroscopy
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Le résumé fourni par la source
Understanding the molecular origin of stress softening in silica-reinforced polydimethylsiloxane remains a challenge. Here, we apply in situ elongational nuclear magnetic resonance (NMR) spectroscopy to selectively probe the polymer matrix under deformation. This allows us to address two key questions: how silica nanoparticles influence microscopic polymer deformation and the critical contribution of the interfacial layer to stress softening. By exploiting differences in chain dynamics, we selectively detect protons in the polymer network strands between topological constraints and the interfacial layer. Combining in situ NMR with numerical modeling based on the nonaffine tube model helps us decouple contributions of network strand deformation and orientation to the magnetic resonance signal. We show that nanoparticles significantly influence network deformation via strand reorientation at small strains. However, the strain-independent interfacial fraction indicates a minor role for the interfacial layer in stress softening during quasistatic loading-reloading tests. Stress softening in silica-filled polydimethylsiloxane poses challenges in understanding polymer matrix deformation. Here, the in situ elongational NMR spectroscopy and numerical modeling show that nanoparticle fillers significantly affect polymer network deformation, while the interfacial layer has minimal impact.
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Le contrôle bibliographique ouvert
DOI retrouvé dans Crossref DOI retrouvé ; titre concordant.
- Titre Crossref
- Molecular origin of stress softening in elastomer-based nanocomposites via in situ elongational nuclear magnetic resonance spectroscopy
- Date Crossref
- 19/08/2025
- Éditeur
- Springer Science and Business Media LLC
- Type
- journal-article
Ce recoupement confirme des métadonnées liées au DOI. Il ne confirme ni la méthode ni les conclusions de l’étude, et il ne compte pas comme une seconde source scientifique indépendante.
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