Ammonio-Illite-Smect

Ammonio-Illite-Smect — FTIR1,801 points · 4004000 cm⁻¹
500100015002000250030003500400000.02000.04000.06000.0800Wavenumber (cm⁻¹)Absorbance
Ammonio-Illite-Smect sample photograph, USGS Spectral Library Version 7
Sample photograph — USGS Spectral Library v7

Spectrum Details

Modality
FTIR
Category
mineral
Material Type
Phyllosilicate
Sample ID
GDS87
Collection Locality
Synthetic
Spectral Purity
1b2b3b4_ # 1= 0.2-3, 2= 1.5-6, 3= 6-25, 4= 20-150 microns
Composition / XRD
None # XRF, EPMA, ICP(Trace), WChem
Sample Description
IMAGE_OF_SAMPLE:
XRD Analysis
40 kV - 30 mA, 6.5-9.5 keV File: amilsm87_mdi (smear on quartz plate) References: Deer, Howie and Zussman (1962); Srodon and Eberl (1984); PDF2 #29-1496 Found: Rectorite and/or illite Sought: illite, mascagnite Comment: The pattern consists of broad peaks, some having shoulders or tails extending toward lower d-spacings. The alpha1-alpha2 reflections are not resolved. Both rectorite (29-1495, a 1:1 regularly interstratified dioctahedral mica and dioctahedral smectite) and 1M illite (29-1496) explain most features of the pattern. Neither has a basal reflection exactly in the observed position, 11.0 Angstroms. Weak but sharp and symmetric reflections at 6.10 and 5.45 Angstroms are not identified; in a subsequent bulk mount, the intensity at 5.45 Angstroms was greatly enhanced and that at 6.10 Angstroms greatly reduced. Glycolation of the bulk mount so reduced all intensities that the pattern was useless.
X Units
cm⁻¹
Y Units
Absorbance
Data Points
1,801

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Attribution

USGS Spectral Library Version 7, U.S. Geological Survey

License: Public Domain

DOI: 10.3133/ds1035

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