Christy De Meyer
The information obtained from the microscopic examination, the identification of calcite (= CaCO3), enables us to assign certain reflections in this X-ray diffractogram to this compound.
| diffractogram of the ancient plaster |
ICCD-PDF entry for calcite | |||
|---|---|---|---|---|
| d (Å) | I (%) | d (Å) | I (%) | remarks |
| 4.27 | 28 | from another phase | ||
| 3.86 | 12 | 3.86 | 12 | I and d identical + small FWHM peak form calcite |
| 3.343 | 82 | from another phase | ||
| 3.035 | 100 | 3.035 | 100 | I and d identical + small FWHM peak form calcite |
| 2.845 | 3 | 2.845 | 3 | I and d identical + small FWHM peak form calcite |
| 2.742 | 12 | from another phase | ||
| 2.503 | 2 | from another phase | ||
| 2.495 | 15 | 2.495 | 14 | I (14~15) and d the same + small FWHM peak form calcite + perhaps another small peak(?) |
| 2.458 | 10 | from another phase | ||
| 2.284 | 29 | 2.285 | 15 | d slightly different + I different + broad peak peak form calcite + peak from another compound |
| 2.237 | 4 | from another phase | ||
| 2.128 | 8 | from another phase | ||
| 2.102 | 6 | from another phase | ||
| 2.095 | 18 | 2.095 | 18 | I and d identical + small FWHM peak form calcite |
| 1.980 | 4 | from another phase | ||
| 1.939 | 2 | from another phase | ||
| 1.927 | 5 | 1.927 | 5 | I and d identical + small FWHM peak form calcite |
| 1.913 | 17 | 1.913 | 17 | I and d identical + small FWHM peak form calcite |
| 1.875 | 17 | 1.875 | 17 | I and d identical + small FWHM peak form calcite |
| 1.817 | 15 | from another phase | ||
| 1.700 | 5 | from another phase | ||
| 1.672 | 6 | from another phase | ||
| 1.659 | 2 | from another phase | ||
| 1.626 | 4 | 1.626 | 4 | I and d identical + small FWHM peak form calcite |
| 1.604 | 8 | 1.604 | 8 | I and d identical + small FWHM peak form calcite |
| 1.587 | 2 | 1.587 | 2 | I and d identical + small FWHM peak form calcite |
| 1.541 | 12 | from another phase | ||
| 1.525 | 5 | 1.525 | 5 | I and d identical + small FWHM peak form calcite |
| 1.518 | 4 | 1.518 | 4 | I and d identical + small FWHM peak form calcite |
| 1.510 | 4 | 1.510 | 3 | I (4~3) and d the same + broader FWHM peak form calcite + perhaps another small peak(?) |
A number of peaks have already been identified as coming from
CaCO3. If we look at the remaining unidentified peaks, one can
easily notice a very sharp and intense peak at d=3.343Å. Looking in the
Hanawalt search manual, more specific on pages 14 and 15 (in the 3.39 - 3.32
+/-0.02 range) and keeping in mind the information from electron microprobe
analysis (Ca, Si ans Mg as major heavier elements), we can quickly find the
compound SiO2. How did I found this result?
Firstly, I searched
the Hanawalt manual for compounds with the most intense peak at 3.34Å.
Secondly, I checked the chemical composition (especially keeping an eye on
the compounds which contain Mg, Ca and Si).
Further examination included
the comparison of the other d-values (and their order of intensity).
This
yields SiO2 (5-490) as second phase. I searched the ICCD-PDF entry
for SiO2. As I did for CaCO3, I also indicated peaks of
SiO2 in the pattern of the ancient plaster. (In bold)
| diffractogram of the ancient plaster |
ICCD-PDF entry for calcite and SiO2 | |||
|---|---|---|---|---|
| d (Å) | I (%) | d (Å) | I (%) | remarks |
| 4.27 | 28 | 4.26 | 35, but 29 relative to 82 |
I and d nearly the same + small FWHM peak form SiO2 |
| 3.86 | 12 | 3.86 | 12 | peak form calcite |
| 3.343 | 82 | 3.343 | 100, but here 82 | d the same (I reference) + small FWHM peak form SiO2 |
| 3.035 | 100 | 3.035 | 100 | peak form calcite |
| 2.845 | 3 | 2.845 | 3 | peak form calcite |
| 2.742 | 12 | from another phase | ||
| 2.503 | 2 | from another phase | ||
| 2.495 | 15 | 2.495 | 14 | peak form calcite |
| 2.458 | 10 | 2.458 | 12, but 10 relative to 82 |
I and d the same + small FWHM peak form SiO2 |
| 2.284 | 29 | 2.285 2.282 |
15 12, but 10 relative to 82 |
broad peak peak form calcite + SiO2 |
| 2.237 | 4 | 2.237 | 6, but 5 relative to 82 |
I and d nearly the same + small FWHM peak form SiO2 |
| 2.128 | 8 | 2.128 | 9, but 7 relative to 82 |
I and d nearly the same + small FWHM peak form SiO2 |
| 2.102 | 6 | from another phase | ||
| 2.095 | 18 | 2.095 | 18 | peak form calcite |
| 1.980 | 4 | 1.980 | 6, but 5 relative to 82 |
I and d nearly the same + small FWHM peak form SiO2 |
| 1.939 | 2 | from another phase | ||
| 1.927 | 5 | 1.927 | 5 | peak form calcite |
| 1.913 | 17 | 1.913 | 17 | peak form calcite |
| 1.875 | 17 | 1.875 | 17 | peak form calcite |
| 1.817 | 15 | 1.817 | 17, but 14 relative to 82 |
I and d nearly the same + small FWHM peak form SiO2 There should be a very small reflection at 1.801Å but probably this one is lost in the background |
| 1.700 | 5 | from another phase | ||
| 1.672 | 6 | 1.672 | 7, but 6 relative to 82 |
I and d nearly the same + small FWHM peak form SiO2 |
| 1.659 | 2 | 1.659 | 3, but 2 relative to 82 |
I and d nearly the same + small FWHM peak form SiO2 |
| 1.626 | 4 | 1.626 | 4 | peak form calcite |
| 1.604 | 8 | 1.604 | 8 | peak form calcite |
| 1.587 | 2 | 1.587 | 2 | peak form calcite |
| 1.541 | 12 | 1.541 | 15, but 12 relative to 82 |
I and d nearly the same + small FWHM peak form SiO2 There should be a very small reflection at 1.601Å but probably this one is lost in the background |
| 1.525 | 5 | 1.525 | 5 | peak form calcite |
| 1.518 | 4 | 1.518 | 4 | peak form calcite |
| 1.510 | 4 | 1.510 | 3 | peak form calcite |
There are still some gaps left in the spectrum. The highest peak left in this spectrum lies at an d=2.742Å. Thus, the third phase will not be found on pages 13-16.
As the highest intensity of the third phase in the diffractogram is
resulting from d=2.742Å, I checked pages 30-32 (2.79-2.75 +/-0.1 and 2.74-2.70
+/-0.1). One remark: all of the remaining peaks are broader (FWHM of +/-
0.35).
Firstly, I searched the Hanawalt manual for compounds with the most
intense peak at 2.74Å.
Secondly, I checked the chemical composition (the
compound must contain Mg).
Further examination included the comparison of
the other d-values (and their order of intensity).
This yields
MgCO3 ( 8-479) as third phase. Searching the ICCD-PDF entry and
checking this composition on the pattern of the ancient plaster: (In Italic)
| diffractogram of the ancient plaster |
ICCD-PDF entry for calcite and SiO2 and MgCO2 | |||
|---|---|---|---|---|
| d (Å) | I (%) | d (Å) | I (%) | remarks |
| 4.27 | 28 | 4.26 | 35, but 29 relative to 82 |
peak form SiO2 |
| 3.86 | 12 | 3.86 | 12 | peak form calcite |
| 3.343 | 82 | 3.343 | 100, but here 82 | peak form SiO2 |
| 3.035 | 100 | 3.035 | 100 | peak form calcite |
| 2.845 | 3 | 2.845 | 3 | peak form calcite |
| 2.742 | 12 | 2.742 | 100, but here 12 | d the same (I reference) peak form MgCO3 |
| 2.503 | 2 | 2.503 | 18, but 2 relative to 12 |
I and d nearly the same peak form MgCO3 |
| 2.495 | 15 | 2.495 | 14 | peak form calcite |
| 2.458 | 10 | 2.458 | 12, but 10 relative to 82 |
peak form SiO2 |
| 2.284 | 29 | 2.285 2.282 |
15 12, but 10 relative to 82 |
broad peak peak form calcite + SiO2 |
| 2.237 | 4 | 2.237 | 6, but 5 relative to 82 |
peak form SiO2 |
| 2.128 | 8 | 2.128 | 9, but 7 relative to 82 |
peak form SiO2 |
| 2.102 | 6 | 2.102 | 45, but 5 relative to 12 |
I and d nearly the same peak form MgCO3 There should be a very small reflection at 2.318Å but this one is certainly lost in the background |
| 2.095 | 18 | 2.095 | 18 | peak form calcite |
| 1.980 | 4 | 1.980 | 6, but 5 relative to 82 |
peak form SiO2 |
| 1.939 | 2 | 1.939 | 12, but 1 relative to 12 |
I and d nearly the same peak form MgCO3 |
| 1.927 | 5 | 1.927 | 5 | peak form calcite |
| 1.913 | 17 | 1.913 | 17 | peak form calcite |
| 1.875 | 17 | 1.875 | 17 | peak form calcite |
| 1.817 | 15 | 1.817 | 17, but 14 relative to 82 |
peak form SiO2 |
| 1.700 | 5 | 1.700 | 35, but 4 relative to 12 |
I and d nearly the same peak form MgCO3 There should be a very small reflection at 1.769Å but this one is certainly lost in the background |
| 1.672 | 6 | 1.672 | 7, but 6 relative to 82 |
peak form SiO2 |
| 1.659 | 2 | 1.659 | 3, but 2 relative to 82 |
peak form SiO2 |
| 1.626 | 4 | 1.626 | 4 | peak form calcite |
| 1.604 | 8 | 1.604 | 8 | peak form calcite |
| 1.587 | 2 | 1.587 | 2 | peak form calcite |
| 1.541 | 12 | 1.541 | 15, but 12 relative to 82 |
peak form SiO2 |
| 1.525 | 5 | 1.525 | 5 | peak form calcite |
| 1.518 | 4 | 1.518 | 4 | peak form calcite |
| 1.510 | 4 | 1.510 | 3 | peak form calcite there is a negletable signal from MgCO3 |