THE STRESS STATE OF THE GEOPHYSICAL MEDIUM UNDER SPACE-TIME DISPERSION OF PULSED LOADINGS

dc.contributor.author	Vladimirov V.A.
dc.contributor.author	Mykulyak S.V.
dc.date.accessioned	2021-03-02T07:46:16Z
dc.date.available	2021-03-02T07:46:16Z
dc.date.issued	2001
dc.identifier	https://elibrary.ru/item.asp?id=27818009
dc.identifier.citation	Geophysical Journal, 2001, 20, 1, 49-68
dc.identifier.issn	0275-9128
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/26056
dc.description.abstract	A closed set of simultaneous equations, which takes into account the relaxation properties of a medium with an internal structure, has been developed. Research was conducted on methods to control the stress state of a rock salt massif upon interaction with explosion waves. It was established that the optimum increase in dilatancy is reached when the time delay between triggering of the charges is 40-60 % of the action time of the excess pressure, and the spacing between them equals 15 charge radii. Studies were conducted on the effect of the relaxation time and of the "frozen" and equilibrium ratio of sonic velocities on the stress state caused by pulse loads.
dc.title	THE STRESS STATE OF THE GEOPHYSICAL MEDIUM UNDER SPACE-TIME DISPERSION OF PULSED LOADINGS
dc.type	Статья

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