Declassified UFO / UAP Document
EXAMENS EN D.E.R. (Enquête 81/01)
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AI-Generated Summary
A 1981 university laboratory report comparing soil samples from a 'crown' to reference soil. The crown samples contained unique non-magnetic black particles and monocrystalline structures not present in the reference soil, which remained unchanged after heating to 1000°C.
This document, dated October 12, 1981, is a laboratory report from the University's Microscopy and Structure of Materials department (ERA301) regarding the analysis of samples provided by an individual identified as 'M. V' on April 22, 1981. The investigation, titled 'Enquête 81/01', involved a comparative study between a 'reference soil' and samples taken from a 'crown' (couronne). The laboratory preparation involved diluting the materials in water, ultrasonic dispersion, and examination via electron microscopy at 80KV. The reference soil was found to be polycrystalline, composed of barium-calcium carbonate, calcium peroxide octahydrate, and iron oxide. The samples from the 'crown' contained black, brilliant, non-magnetic particles that were distinct from the reference soil. Diffraction analysis of the crown samples revealed a higher concentration of calcium peroxide octahydrate and the presence of monocrystalline structures, which were entirely absent in the reference soil. The researchers attempted to replicate the crown sample's structure by heating the reference soil to 1000°C in a vacuum, but no transformation into a monocrystalline state was observed. The report includes photographic plates (clichés) documenting the diffraction patterns of the samples.
Il est à remarquer que nous n'avons pas rencontré de monocristaux dans les échantillons de la terre de référence.
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Official Assessment
The analysis compared soil samples from a 'crown' against reference soil. The crown samples contained black, brilliant, non-magnetic particles. Diffraction analysis showed the reference soil was polycrystalline, containing BaCa(CO3)2, Ca(O2)8H2O, and Fe3O4. The crown samples showed an increased concentration of Ca(O2)8H2O and the presence of monocrystalline components not found in the reference soil. Heating the reference soil to 1000°C did not produce the monocrystalline structure observed in the crown samples.
Key Persons
- M. VProvider of samples