Some implications of statistical transport theory in rock mechanics     

Adrian E. Scheidegger 《Pure and Applied Geophysics》1966,65(1):160-163

Summary Recently, a new theory of the subsidence of rock masses has been advanced byLitwiniszyn and coworkers, which is based on the notion that the individual rock particles perform random walks. It is shown in the present paper that the final equations of the random walk theory can be justified from general principles of statistical mechanics in which no specific theoretical model of particle behaviour has to be made. The theory appears to account appropriately for subsidence phenomena.The research reported in this paper was supported by the Petroleum Research Fund of the American Chemical Society. Acknowledgment is made to the donors of the Petroleum Research Fund administered by the American Chemical Society for support of this reseach.  相似文献   

Micro-spectroscopic investigations of highly heterogeneous waste repository materials   总被引：1，自引：0，他引：1  

A.M. Scheidegger  D. Grolimund  C.R. Cheeseman  R.D. Rogers 《Journal of Geochemical Exploration》2006,88(1-3):59

Assuring safe disposal and long-term storage of radioactive and toxic wastes corresponds to a primary environmental task of present societies. To improve any technical limitation, a mechanistic understanding of the processes governing the binding of heavy metals and radionuclides is required. In this study, the significance of synchrotron-based X-ray microprobes for elucidating the spatial distribution and the speciation of radionuclides in highly heterogeneous waste repository materials will be outlined. A case study on the uptake process of Co in cementitious engineered barrier materials exposed to microbial degradation will be presented.  相似文献   

The connection of geodynamics with seismicity patterns     

Adrian E. Scheidegger 《Natural Hazards》1988,1(1):5-13

When a study is to be made of seismic risks, the present-day geodynamic conditions are of fundamental importance: Earthquakes do not happen by themselves, they do have a cause. The cause of earthquakes is that the tectonic stresses exceed a critical limit. The build-up of these stresses is conditioned by the geodynamic processes occurring in the region in question. A knowledge of the geodynamics characteristic of a region is therefore fundamental for seismic risk studies. The general methodology for making such a geodynamic study is based on the entire set of manifestations of the plate-tectonic conditions of that region: these include the mechanism of earthquakes, the stresses observed in mines, the orientation of surface joints and even the direction of river valleys. Examples of geodynamic studies and their bearing on seismic risks are shown from various areas of the world, notably from China, India, and Colombia.  相似文献   

The significance of surface joints     

Adrian E. Scheidegger 《Surveys in Geophysics》1985,7(3):259-271

This brief review demonstrates the significance, on a global scale, of joints as shearing surfaces in the neotectonic stress field. Thus, the principal directions of the neotectonic stress field can be determined by a statistical treatment of joint orientation data. These principal stress directions agree with those postulated from plate tectonic theory in every case, on five continents.  相似文献   

Natural Hazard Risk Assessment and Publicity Policy — Anticipating the Unexpected | W.J. Petak and A.A. Atkisson, 1982. Springer Verlag,Berlin, xvi + 489 pp., DM129.-, approx. US$51.60 (hardcover)     

A.E. Scheidegger 《Earth》1984,21(4):304-305

  相似文献   

Compressional angles of isallo stress theory for a circular-cylindrical,spherical and elliptic-cylindrical elastic inhomogeneity in an elastic medium     

Hans Pulpan  Adrian E. Scheidegger 《Pure and Applied Geophysics》1969,76(1):147-152

Summary The compressional angle of isallo stress theory for the case of a cylindrical (circular and elliptic) and spherical subsurface inhomogeneity, assuming that the conjugate fracture surfaces are inclined at a Mohr angle of 30° toward the largest compression, has been calculated. The solution for a spherical and cylindrical inclusion in an infinite medium subject to a uniform stress field (at infinity) were taken as the basis for the stress analysis. The stress angle was then calculated for the mentioned types of inclusions.  相似文献   

Directional permeability of porous media to homogeneous fluids     

Dr. Adrian E. Scheidegger 《Pure and Applied Geophysics》1954,28(1):75-90

Summary Investigations have shown that in groundwater- and oil-bearing strata there are preferential directions of flow that are often maintained over wide areas.Johnson & Hughes (1948, see Ref.) analysed a series of oil well cores by cutting them into small horizontal plugs and they obtained directional permeabilities which they plotted in the form of polar graphs. They were not able to give a physical explanation of this phenomenon. On the other hand, there exists a theory of permeability in which the latter is represented as a symmetric tensor. This theory has been developed byFerrandon (1948, see Ref.), but no experimental substantiation of it seems ever to have been attempted.In the present paper, the author undertakes to compare the two sets of findings. FromFerrandon's theory, the directional permeabilities (denoted byk) corresponding to the experiments ofJohnson & Hughes are calculated and it is shown thatk ^–1/2 if plotted as polar graph, should form an ellipse. The data ofJohnson & Hughes are then are drawn. In this manner, a substantiation of the tensor theory ofFerrandon is obtained.

---

Zusammenfassung Untersuchungen der Permeabilität von Grundwasser und Erdöl führenden Gesteinsschichten haben gezeigt, dass dieselbe in vielen Fällen richtungsabhängig ist. Hierbei bleibt die Richtung extremaler Permeabilität oft über weite Gebiete konstant.Johnson & Hughes untersuchten eine Reihe von Bohrkernen von Oelquellen auf Richtungsabhängigkeit der Permeabilität. Hierzu schnitten sie aus denselben kleine, waagrechte Stücke, bestimmten deren Permeabilität und stellten das Ergebnis ihrer Messungen in der Form von Permeabilitätspolardiagrammen dar. Sie waren nicht im Stande, eine theoretische Erklärung der erhaltenen Kurven zu geben. Auf der anderen Seite existiert eine Theorie der Permeabilität, wobei die letztere als symmetrischer Tensor behandelt wird. Diese Theorie wurde vonFerrandon vorgeschlagen; es scheint aber, dass keine experimentelle Bestätigung davon je versucht worden ist.In der vorliegenden Arbeit vergleicht der Verfasser die zwei Typen von Untersuchungen. Nach derFerrandon'schen Theorie wird die «gerichtete» Permeabilität (mitk bezeichnet), die den Experimenten vonJohnson & Hughes entspricht, berechnet. Es wird gezeigt, dassk ^–1/2, als Polardiagramm dargestellt, die Gestalt einer Ellipse haben sollte. Die Resultate vonJohnson & Hughes werden dann in die Form vonk ^–1/2 umgerechnet und als entsprechende Polardiagramme dargestellt. In dieser Weise wird eine experimentelle Bestätigung der Tensortheorie vonFerrandon erhalten.

---

---

Published by Permission of Imperial Oil Limited, Calgary, Alberta (Canada).  相似文献   

Book reviews     

L. Müller  P. Egger  G. E. A. H.  P. Duffaut  W. Kaiser  A. E. Scheidegger 《Rock Mechanics and Rock Engineering》1972,4(2):130-134

  相似文献   

Eastern Pacific spreading rate fluctuation and its relation to Pacific area volcanic episodes   总被引：1，自引：0，他引：1  

David K. Rea  K.F. Scheidegger   《Journal of Volcanology and Geothermal Research》1979,5(1-2)

Sea-floor spreading rates from four locations along the Nazca-Pacific plate boundary and one along the Juan de Fuca-Pacific plate boundary show variations over the past 2.4 m.y., with decreasing rates prior to the Jaramillo to Olduvai time interval (0.92–1.73 m.y. ago) and increasing rates since then. Other Pacific area volcanic phenomena in mid-plate and convergent-boundary settings also show minima about 1.3–1.5 m.y. ago and a maximum at present and another maximum about 5 m.y. ago: extrusion rates along the Hawaiian Ridge; volcanic episodes associated with calc-alkalic provinces of western Oregon and Central America; temporal variations in the SiO₂ content of Aleutian ash layers; and the number of deep-sea ash layers. These phenomena may fluctuate in response to changing spreading rates. During times of more rapid spreading increased shear and melting along lithospheric boundaries may occasion increased volcanic activity, whereas during times of less rapid spreading volcanic activity may be less intense.  相似文献   

On directional permeability     

A. E. Scheidegger 《Pure and Applied Geophysics》1956,33(1):111-113

Summary ?Directional Permeability? of anisotropic porous media to homogeneous fluids can be defined in two fashions: Firstly, by cutting a pencil shaped piece out of the porous medium and measuring its permability, secondly, by referringDarcy’s law to that component of the seepage velocity which is parallel to the pressure gradient. It is shown that, although these two definitions are not identical, the difference between them is so small that it can usually be neglected. Dr.A. E. Scheidegger, Dominion Observatory,Ottawa (Canada).  相似文献