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 | |
# Topics | |
DTIC Archive; Vizgirda,Joana; CALIFOR... | |
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