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pro vyhledávání: '"C Butenuth"'
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Akademický článek
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Publikováno v:
Bulletin of Engineering Geology and the Environment. 69:411-419
This paper describes how simple pycnometric studies using water and a non-polar fluid such as n-heptane, may be used to recognise the presence and indicate the magnitude of chemical “reactions” between mineral surfaces and water. The results of s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3a0bd947044371a2b7572f14c7987e01
https://doi.org/10.1007/s10064-010-0284-0
https://doi.org/10.1007/s10064-010-0284-0
Publikováno v:
Bulletin of Engineering Geology and the Environment. 63:179-189
This paper outlines the need for a description to quantify the natural response of rock to the presence of water. It discusses the change in mass that occurs in a sample exposed to water vapour over time could provide such a description, and the reas
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::02cc73d5d8662278807cce3154befdc0
https://doi.org/10.1007/s10064-004-0241-x
https://doi.org/10.1007/s10064-004-0241-x
Publikováno v:
Géotechnique. 50:315-318
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1c11fc1535e5dabeb78451509691b69b
https://doi.org/10.1680/geot.2000.50.3.315
https://doi.org/10.1680/geot.2000.50.3.315
Publikováno v:
Bulletin of Engineering Geology and the Environment. 57:31-40
The Hoop Tension Test has proved to be a reliable and sensitive test for measuring rock strength in tension. This paper describes experiments using Penrith Sandstone hoops of different sizes, failed under tension by this procedure. The distribution a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bda86e76b482eadd6c6f4029f7ef9ae3
https://doi.org/10.1007/s100640050018
https://doi.org/10.1007/s100640050018
Publikováno v:
Geological Society, London, Engineering Geology Special Publications. 15:185-191
Studies of a weak sandstone which disaggregates in water reveal that particles of colloidal dimensions are released as the sand-sized particles separate. Colloids are the building blocks of gels and their presence suggests that gels (in this case sil
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d12470c0263ae8602103f6df201ecd9c
https://doi.org/10.1144/gsl.eng.1998.015.01.19
https://doi.org/10.1144/gsl.eng.1998.015.01.19
Autor:
C. Butenuth
Publikováno v:
Rock Mechanics and Rock Engineering. 30:65-72
A number of methods exists to fail rock in tension. In general the experimental results obtained by these methods differ, and it is not known how to quantitavely compare them other than by empiricism, even to obtain a value for tensile strength. Thus
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::051a332a59e0a20b7c1691047b4a1694
https://doi.org/10.1007/bf01020114
https://doi.org/10.1007/bf01020114
Publikováno v:
Geological Society, London, Special Publications. 122:107-119
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aaf0a968b1cc2ea534f882a05e5b006e
https://doi.org/10.1144/gsl.sp.1997.122.01.08
https://doi.org/10.1144/gsl.sp.1997.122.01.08
Publikováno v:
Geological Society, London, Special Publications. 122:377-388
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::657f7159cca6ebe5a1dbf0fa5aa96a9a
https://doi.org/10.1144/gsl.sp.1997.122.01.21
https://doi.org/10.1144/gsl.sp.1997.122.01.21