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DTIC ADA071508: Shock Effects in Carbonates.
by Defense Technical Information Center
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Permanent deformation of very small crystallites of
carbonate minerals, such as those occurring in the
Eniwetok core, has been examined using the following
techniques: (a) Peak broadening of X-ray powder
diffractometer patterns due to decreasing effective grain
size with increasing shock deformation is observed. This
effect is clearly seen in the core material taken from
directly under the Cactus explosion. (b) Angular strain
in calcite single crystals has been observed in Debye-
Scherrer patterns of laboratory shocked samples and
single-crystallities from the Eniwetok core. Tentative
peak shock pressures of approximately 8 kbar at a depth
of approximately 15 m decaying the approximately 3 kbar
at a depth of approximately 30 m are inferred on the
basis of very preliminary data. (c) Shock-induced erasure
of defect spectra, as examined by electron-spin resonance
(ESR) techniques, is observed in carbonate materials,
both shocked in the laboratory and by the Cactus
explosion. This effect is yet 'uncalibrated.' (d) Also
using the ESR techniques, a systematic loss of fine
structure of the resonance of Mn(++) impurities in
calcite is observed with increasing shock pressure, both
in laboratory shocked samples and those in the Cactus
core. (Author)
Date Published: 2017-09-21 06:49:02
Identifier: DTIC_ADA071508
Item Size: 19060976
Language: english
Media Type: texts
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