Infrared spectrum comparison chart.
Analysis result: organically modified dioctahedral smectite clay with long-chain aliphatic amide/ester modifier.
The infrared spectrum exhibits bands characteristic of a dioctahedral aluminosilicate smectite clay mineral (e.g., Al OH bending at 683 and 913 cm⁻¹, external tetrahedral Si O vibrations near 745 cm⁻¹) superimposed with strong organic absorptions. The organic contribution displays long-chain aliphatic C–H stretches at 2919 and 2850 cm⁻¹, an ester carbonyl at 1740 cm⁻¹, amide I and II bands at 1642 and 1549 cm⁻¹, and aromatic C–H out-of-plane modes at 704 and 722 cm⁻¹. This pattern is most consistent with an organically modified clay, where the organic modifier bears amide and ester (methacrylate/methoxy) functionality, aligning with the moderate library match to a tetradecanamide-like pattern and the Top‑15 consensus of methoxy/methacrylate chemistry