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Titlebook: Geomechanics and Fluidodynamics; With Applications to Victor N. Nikolaevskiy Book 1996 Springer Science+Business Media Dordrecht 1996 Boreh

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發(fā)表于 2025-3-21 19:42:05 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書(shū)目名稱Geomechanics and Fluidodynamics
副標(biāo)題With Applications to
編輯Victor N. Nikolaevskiy
視頻videohttp://file.papertrans.cn/384/383424/383424.mp4
叢書(shū)名稱Theory and Applications of Transport in Porous Media
圖書(shū)封面Titlebook: Geomechanics and Fluidodynamics; With Applications to Victor N. Nikolaevskiy Book 1996 Springer Science+Business Media Dordrecht 1996 Boreh
描述Geomechanics is the basic science for many engineering fields, including oil and gas recovery, mining, civil engineering, water supply, etc., as well as for many environmental sciences, including earthquake prediction, ecology, landscape dynamics, and explosion works. Historically, the major concepts of geomechanics were founded on the methods of the elasticity theory and the static equilibrium of joints with solid friction. Underground hydrodynamics was developed quite separately and included only simple, conventional ideas of elastic pore-space deformation. Today, the situation is drastically different. Tremendous achievements in numerical computer technique have eliminated many of the routine difficulties of problem solution with respect to selected mathematical models. As the result, major efforts now are applied to sophisticated experimental studies and to new applications of generalized continuum theories. Of course, traditional rheological schemes have been adjusted to be into account the real properties of such geomaterials as soils, rocks and ice. The main changes have been connected with the kinematics of the internal structure of geomaterials that influences their streng
出版日期Book 1996
關(guān)鍵詞Borehole; Moho; Reservoir; geophysics; thermodynamics; terrestrial pollution
版次1
doihttps://doi.org/10.1007/978-94-015-8709-9
isbn_softcover978-90-481-4638-3
isbn_ebook978-94-015-8709-9Series ISSN 0924-6118 Series E-ISSN 2213-6940
issn_series 0924-6118
copyrightSpringer Science+Business Media Dordrecht 1996
The information of publication is updating

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Mechanics of a Saturated Geostratum,as pores and cracks — that is, if fluid channels in a solid matrix, fluid drops and gas bubbles are much less than the average scale of space, which is equal to the linear dimension of an elementary (differential) volume of the medium. It is also assumed that every differential volume has a complete
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Explosions and Seismic Waves in Geostrata, due to the depth of the explosive charge disposal. From mathematical point of view the underground contained explosion is the simplest one [183] because this dynamical motion possesses the spherical symmetry.
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Structure and Rheology of the Lithosphere,ments of loads and deformation have led to the discovery of the rheological laws of geomaterials [160]. In Section 1.3, the basic mathematical model of deformation of dilating rocks is given. The detailed description of the hardening and softening processes is necessary for an adequate computer simu
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Geodynamical Processes,s called the lithosphere. It is more cold and rigid than the others beneath it. Temperature and pressure grow with the depth inside the Earth, and the result is a partial melting of polycrystalline rocks at a depth of . to .. The corresponding layer of the Earth is known as the astenosphere, which i
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Geomechanics and Fluidodynamics978-94-015-8709-9Series ISSN 0924-6118 Series E-ISSN 2213-6940
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