PUBLIC SPECTRUM SEARCH
none
Free public result — the submitted spectrum with its top library candidates, not an AI identification.
SPECTRUM & LIBRARY MATCHES
Submitted spectrum and top library candidates
Top 15 library matches
| # | Reference | CAS | Similarity |
|---|---|---|---|
| 1 | none | 0-00-0 | - |
| 2 | none | 0-00-0 | - |
| 3 | none | 0-00-0 | - |
| 4 | none | 7803-57-8 | - |
| 5 | none | 124-40-3 | - |
| 6 | none | 124-40-3 | - |
| 7 | none | 124-40-3 | - |
| 8 | none | 16828-11-8 | - |
| 9 | none | 109-96-6 | - |
| 10 | none | 109-96-6 | - |
| 11 | none | 7784-26-1 | - |
| 12 | none | 2978-58-7 | - |
| 13 | none | 2978-58-7 | - |
| 14 | none | 27761-27-9 | - |
| 15 | none | 124-02-7 | - |
Discussion
Comments and follow-up evidence
Use this area to continue the interpretation, ask questions, or add extra verification evidence.
The large and flat peaks around 1630 and 3300 indicate the presence of water, while the absorption peaks at 3547 and 3652 suggest that the sample may be similiar to hydrous minerals more closely[1].The fingerprint region cannot be precisely matched to a specific mineral, appearing to be predominantly composed of metal hydroxides.
en&2[1]Balan, Etienne, et al. "Surface modes in the infrared spectrum of hydrous minerals: the OH stretching modes of bayerite." Physics and Chemistry of Minerals 35 (2008): 279-285.