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921.
In this paper, the shear strength with respect to the matric suction of unsaturated soils was studied. For this purpose, unsaturated
triaxial testing procedures were applied to the undisturbed residual soil specimens. An apparatus for performing triaxial
tests was designed and constructed. In the tests, matric suction was controlled by using the axis translation technique, and
pore water volume changes were measured by means of a volume change transducer with 10−8 m3 sensitivity. The test results indicated that the matric suction contributes to the shear strength of unsaturated soil specimens,
and this contribution called suction strength varies non-linearly with respect to the matric suction. The logarithmic model
needing to know the air-entry value and the internal friction angle of a soil specimen for prediction of the suction strength
were presented and compared with the test results. It was found that suction strength values predicted from the proposed model
were in satisfactory agreement with the experimental results. 相似文献
922.
Richard J. Squire Walter Herrmann Daniel Pape D. Ian Chalmers 《Mineralium Deposita》2007,42(5):489-503
The early Palaeozoic Macquarie Arc, southeastern Australia, hosts a variety of major late Ordovician to earliest Silurian
subduction-related deposits (e.g., Cadia East, Ridgeway, Cadia Hill, Cowal and Northparkes). However, there is uncertainty
about whether coeval high-sulfidation epithermal deposits, which occur in intra-oceanic metallogenic belts elsewhere in the
West Pacific, (e.g., Lepanto and Chinkuashih), are also present in the Macquarie Arc. This has led to suggestions that their
absence may be due to the poor preservation potential of deposits that form at relatively shallow crustal levels in ancient
rocks. We present here an interpretation for evolution of the Peak Hill Au–Cu deposit based on the distribution of alteration
facies, sulfur isotope data from several textural forms of pyrite and barite, and an assessment of the regional volcanic and
sedimentary facies architecture. These data show that the Peak Hill deposit displays a distinct sub-vertical zoning with a
pyrophyllite and vuggy-quartz core, that today extends about 350 m east–west and at least 550 m north–south, which grades
out through paragonite+muscovite, kaolinite to a chlorite+epidote alteration zone at the margin. The alteration zoning reflects
both lower temperatures and neutralisation of acid fluids with increasing distance from the core, which represents the conduit
along which hot acidic hydrothermal fluids were channelled. Several temporally overlapping events of silicification, bladed-quartz-pyrite
veining, brecciation and pyrite veining occurred during the last stages of hydrothermal alteration, although most appear to
predate mineralisation. Au–Cu mineralisation was associated with late quartz-pyrite-barite veins, and the highest gold grades
occur mainly in microcrystalline-quartz-altered rocks in the paragonite+muscovite alteration zone, generally within 50 m outward
from the boundary of the pyrophyllite and vuggy-quartz core. Sulfur- and lead-isotope data, and the characteristic zoning
of ore minerals and alteration assemblages support a magmatic source for the hydrothermal fluids. Similarities in many of
the isotopic signatures between Peak Hill and deposits such as Northparkes support generation of the high-sulfidation mineralisation
during the Late Ordovician to earliest Silurian (possibly ca. 440 Ma) metallogenic event. The Late Ordovician to Early Silurian
volcanic and sedimentary facies associations at Peak Hill are consistent with alteration and mineralisation occurring in rocks
deposited in a submarine setting. 相似文献
923.
在煤田测井中,井径的变化对其它测井参数是一种干扰,但利用井径的相对变化值(井径扩大系数),可有效地评估岩石的强度等级和可采煤层顶底板的稳定性。统计鱼卡煤田东部勘探区29个钻孔孔径的变化值,按岩石抗压强度划分原则,将其七煤顶板稳定性划分为5个等级,据此固定了该煤田七煤顶板稳定性分布图。 相似文献
924.
The scope of this paper is to introduce a method for the analysis of rock tunnels reinforced by grouted bolts, based on the
convergence-control approach. The analytical formulations presented in this paper refers to an elasto-plastic behavior of
the rock mass and the latest Hoek and Brown yield criterion (Version 2002). In order to model the reinforced plastic zone,
the equivalent material approach was taken into account such that the apparent strength of the rock mass is improved as a
consequence of the bolting effect. The general design guides and examples presented are intended to facilitate the comprehension
and application of the proposed analytical solution in practice. 相似文献
925.
T. Szwedzicki 《Rock Mechanics and Rock Engineering》2007,40(1):97-104
926.
Effect of brittle fracture on the rheological structure of the lithosphere and its application in the Ordos 总被引:2,自引:0,他引:2
An empirical formula for the fracture strength of the principal rock type in the lithosphere is obtained based on the experimental data from previous studies, in which the effects of the confining pressure, size of the rock sample, temperature, strain rate and the pore pressure are taken into account, the empirical formulae for the effects of them are also presented. By comparing the frictional strength to the fracture strength calculated using the new empirical formula, it is shown that frictional sliding is dominant in the upper crust but brittle fracture is dominant in the lower part of the crust and the lithosphere beneath the crust. Therefore the fracture mechanism must be taken into account in the study of the rheological structure of the lithosphere. The empirical formula for the fracture strength is applied to study the rheological structure of the lithosphere in the Ordos block. Brittle regime in the rheological structure can be divided into two sub-regions, in one of which brittle fracture and in the other frictional sliding are dominant, respectively, unlike previous conventional studies in which frictional sliding is assumed to be the only factor; the magnitude of the rheological strength of the lithosphere calculated by the empirical formula is also lower than that obtained in previous conventional studies. 相似文献
927.
Landslide susceptibility mapping using GIS and digital photogrammetric techniques: a case study from Ardesen (NE-Turkey) 总被引:3,自引:3,他引:3
Ardesen is a settlement area which has been significantly damaged by frequent landslides which are caused by severe rainfalls
and result in many casualties. In this study a landslide susceptibility map of Ardesen was prepared using the Analytical Hierarchy
Process (AHP) with the help of Geographical Information Systems (GIS) and Digital Photogrametry Techniques (DPT). A landslide
inventory, lithology–weathering, slope, aspect, land cover, shear strength, distance to the river, stream density and distance
to the road thematics data layers were used to create the map. These layer maps are produced using field, laboratory and office
studies, and by the use of GIS and DPT. The landslide inventory map is also required to determine the relationship between
these maps and landslides using DPT. In the study field in the Hemsindere Formation there are units that have different weathering
classes, and this significantly affects the shear strength of the soil. In this study, shear strength values are calculated
in great detail with field and laboratory studies and an additional layer is evaluated with the help of the stability studies
used to produce the landslide susceptibility map. Finally, an overlay analysis is carried out by evaluating the layers obtained
according to their weight, and the landslide susceptibility map is produced. The study area was classified into five classes
of relative landslide susceptibility, namely, very low, low, moderate, high, and very high. Based on this analysis, the area
and percentage distribution of landslide susceptibility degrees were calculated and it was found that 28% of the region is
under the threat of landslides. Furthermore, the landslide susceptibility map and the landslide inventory map were compared
to determine whether the models produced are compatible with the real situation resulting in compatibility rate of 84%. The
total numbers of dwellings in the study area were determined one by one using aerial photos and it was found that 30% of the
houses, with a total occupancy of approximately 2,300 people, have a high or very high risk of being affected by landslides. 相似文献
928.
Macroseismic effects related to strong ground motion: a study of the South Iceland earthquakes in June 2000 总被引:1,自引:1,他引:1
R. Sigbjörnsson S. Ólafsson J. Th. Snæbjörnsson 《Bulletin of Earthquake Engineering》2007,5(4):591-608
The impact of the June 2000 South Iceland earthquakes has been assessed applying data collected in field surveys and strong-motion
recordings from the Icelandic Strong-Motion Network. The areas within approximately 20 km of the causative faults suffered
considerable damage, including transportation and utility systems as well as buildings, both with regard to structure and
inventories. Ground subsidence and dislocations were significant in the near-fault zone. Aftershocks and permanent displacements
of building foundations resulted in progressive structural damage. By introducing holistic measures derived from the acceleration
data, a fair correlation was achieved between the obtained earthquake intensities and the recorded accelerations. The measures
adopted were square root of the sum of the squares (SRSS) values of peak ground acceleration (PGA) and the trace of the Arias
intensity tensor. It was found that the overall attenuation tended to be more rapid than reflected by common strong-motion
models reported in the literature. There is no simple explanation for this behaviour but it is reasonable to suggest that
it can be partly attributed to the heterogeneous and fractured crust that is characteristic of Icelandic geology. 相似文献
929.
S. Thevanayagam 《地震工程与工程振动(英文版)》2007,6(2):123-134
Mechanical behavior such as stress-strain response, shear strength, resistance to liquefaction, modulus, and shear wave velocity of granular mixes containing coarse and fine grains is dependent on intergrain contact density of the soil. The global void ratio e is a poor index of contact density for such soils. The contact density depends on void ratio, fine grain content (Cv), size disparity between particles, and gradation among other factors. A simple analysis of a two-sized particle system with large size disparity is used to develop an understanding of the effects of Cv, e, and gradation of coarse and fine grained soils in the soil mix on intergrain contact density. An equivalent intergranular void ratio (ec)oq is introduced as a useful intergrain contact density for soils at fines content of less than a threshold value Crth. Beyond this value, an equivalent interfine void ratio (ef)eq is introduced as a primary intergrain contact density index. At higher values of Cv beyond a limiting value of fine grains content CVL, an interfine void ratio ef is introduced as the primary contact density index. Relevant equivalent relative density indices (Drc)eq and (Drf)eq are also presented. Experimental data show that these new indices correlate well with steady state strength, liquefaction resistance, and shear wave velocities of sands, silty sands, sandy silts, and gravelly sand mixes. 相似文献
930.
Most of the available models of monolithic reinforced concrete joints under seismic action focus on estimation of cracking
and ultimate shear strengths. Very few studies have been directed towards developing expressions for the associated joint
deformations at the milestone response points so as to compose a limit-state model for joints that would be compatible with
the emerging framework of deformation based seismic assessment and design methods. This objective is pursued in the present
paper with particular emphasis on monolithic bridge joints. Deformation capacity at yielding and failure of joints is derived
by establishing equilibrium and geometric compatibility of smeared stresses and strains, and satisfying material constitutive
relationships. Expressions and model parameters are calibrated with the database of published bridge joint tests assembled
from International literature, using statistical evaluation. From the mean values of the design parameters simplified equations
for shear strength and ultimate shear strain of bridge joints are proposed. 相似文献