Abstract
Creep in rock depends on the structure as well as on the stress and temperature. Log time creep is often observed and can be explained on the basis of statistical mechanics. Simple Kelvin behavior can be used as an approximation. The code FLAC is concluded to be useful for predicting creep strain, assuming that the rock obeys the Kelvin law. 22 refs.
Citation Formats
Pusch, R, and Hoekmark, H.
Mechanisms and consequences of creep in the nearfield rock of a KBS-3 repository.
Sweden: N. p.,
1992.
Web.
Pusch, R, & Hoekmark, H.
Mechanisms and consequences of creep in the nearfield rock of a KBS-3 repository.
Sweden.
Pusch, R, and Hoekmark, H.
1992.
"Mechanisms and consequences of creep in the nearfield rock of a KBS-3 repository."
Sweden.
@misc{etde_10138844,
title = {Mechanisms and consequences of creep in the nearfield rock of a KBS-3 repository}
author = {Pusch, R, and Hoekmark, H}
abstractNote = {Creep in rock depends on the structure as well as on the stress and temperature. Log time creep is often observed and can be explained on the basis of statistical mechanics. Simple Kelvin behavior can be used as an approximation. The code FLAC is concluded to be useful for predicting creep strain, assuming that the rock obeys the Kelvin law. 22 refs.}
place = {Sweden}
year = {1992}
month = {Dec}
}
title = {Mechanisms and consequences of creep in the nearfield rock of a KBS-3 repository}
author = {Pusch, R, and Hoekmark, H}
abstractNote = {Creep in rock depends on the structure as well as on the stress and temperature. Log time creep is often observed and can be explained on the basis of statistical mechanics. Simple Kelvin behavior can be used as an approximation. The code FLAC is concluded to be useful for predicting creep strain, assuming that the rock obeys the Kelvin law. 22 refs.}
place = {Sweden}
year = {1992}
month = {Dec}
}