標(biāo)題: Titlebook: Geomechanics and Fluidodynamics; With Applications to Victor N. Nikolaevskiy Book 1996 Springer Science+Business Media Dordrecht 1996 Boreh [打印本頁(yè)] 作者: FAD 時(shí)間: 2025-3-21 19:42
書目名稱Geomechanics and Fluidodynamics影響因子(影響力)
書目名稱Geomechanics and Fluidodynamics影響因子(影響力)學(xué)科排名
書目名稱Geomechanics and Fluidodynamics網(wǎng)絡(luò)公開度
書目名稱Geomechanics and Fluidodynamics網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Geomechanics and Fluidodynamics被引頻次
書目名稱Geomechanics and Fluidodynamics被引頻次學(xué)科排名
書目名稱Geomechanics and Fluidodynamics年度引用
書目名稱Geomechanics and Fluidodynamics年度引用學(xué)科排名
書目名稱Geomechanics and Fluidodynamics讀者反饋
書目名稱Geomechanics and Fluidodynamics讀者反饋學(xué)科排名
作者: 有限 時(shí)間: 2025-3-21 21:00
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作者: 切割 時(shí)間: 2025-3-22 00:25 作者: 磨碎 時(shí)間: 2025-3-22 07:57
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.作者: Urea508 時(shí)間: 2025-3-22 09:45
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作者: animated 時(shí)間: 2025-3-22 16:42
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作者: animated 時(shí)間: 2025-3-22 19:00 作者: 兇猛 時(shí)間: 2025-3-22 22:05
Geomechanics and Fluidodynamics978-94-015-8709-9Series ISSN 0924-6118 Series E-ISSN 2213-6940 作者: Camouflage 時(shí)間: 2025-3-23 01:40 作者: Pillory 時(shí)間: 2025-3-23 08:26 作者: 膠狀 時(shí)間: 2025-3-23 13:37
https://doi.org/10.1007/978-3-658-44466-2 symbols (.), (.) correspond to values (1),..., (.); (.) = (1),..., (.), is the component index; C. is the mass concentration of the component . in the phase .. is the saturation of the porous space by the phase . and N. is the mass exchange of the component . between phases; . and .. The number of 作者: Pericarditis 時(shí)間: 2025-3-23 17:47
Neuer Umgang mit digitalen Daten, 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.作者: 美學(xué) 時(shí)間: 2025-3-23 21:59
Sophie Hippmann,Raoul Klingner,Miriam Leisments 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作者: CLEAR 時(shí)間: 2025-3-24 00:43
Digitalisierung & Nachhaltigkeits 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作者: 心痛 時(shí)間: 2025-3-24 02:43
https://doi.org/10.1007/978-3-642-91498-0ith pores and cracks often filled with fluids and gases. Describing such a medium is complicated but it can be simplified if the motions or flow patterns of the geomaterials have length scales, . , that are much larger than the characteristic sizes, . , of individual grains.作者: crutch 時(shí)間: 2025-3-24 09:16
https://doi.org/10.1007/978-3-658-44466-2 symbols (.), (.) correspond to values (1),..., (.); (.) = (1),..., (.), is the component index; C. is the mass concentration of the component . in the phase .. is the saturation of the porous space by the phase . and N. is the mass exchange of the component . between phases; . and .. The number of equations (4.1) is equal to ..作者: Aggressive 時(shí)間: 2025-3-24 13:00 作者: 贊成你 時(shí)間: 2025-3-24 14:56 作者: faculty 時(shí)間: 2025-3-24 21:01 作者: 使絕緣 時(shí)間: 2025-3-25 02:32 作者: 安裝 時(shí)間: 2025-3-25 05:15 作者: 比目魚 時(shí)間: 2025-3-25 08:00 作者: declamation 時(shí)間: 2025-3-25 12:03 作者: MUT 時(shí)間: 2025-3-25 16:56
0924-6118 , 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作者: 伴隨而來(lái) 時(shí)間: 2025-3-25 20:40 作者: Dysplasia 時(shí)間: 2025-3-26 00:42
Book 1996as 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 hydrodyna作者: 軍火 時(shí)間: 2025-3-26 08:14 作者: 肥料 時(shí)間: 2025-3-26 11:25
Sophie Hippmann,Raoul Klingner,Miriam Leisamined. Moreover, additional information on the microstructure of deformed or failed geomaterial is necessary because any internal change results in such hydrological or geophysical properties as permeability, electroconductivity, etc.作者: moribund 時(shí)間: 2025-3-26 15:30 作者: 得罪 時(shí)間: 2025-3-26 16:57 作者: 有限 時(shí)間: 2025-3-26 22:54 作者: fledged 時(shí)間: 2025-3-27 03:06 作者: 痛恨 時(shí)間: 2025-3-27 06:52 作者: 無(wú)彈性 時(shí)間: 2025-3-27 09:42 作者: AGOG 時(shí)間: 2025-3-27 14:00 作者: AMITY 時(shí)間: 2025-3-27 21:10
Roger Barga,Valentine Fontama,Wee Hyong Tokom each other in ways that are both meaningful and measurable. We differ in terms of cognitive ability; aptitude for performing different kinds of mental and physical tasks; temperament; and interests. But somehow, without sufficient examination, we have taken a great collective leap from that commonplace to 978-94-010-5318-1978-94-011-2968-8作者: 微枝末節(jié) 時(shí)間: 2025-3-28 00:21
On Radiocoloring Hierarchically Specified Planar Graphs: ,-completeness and Approximationsproximation algorithm as well as a more efficient asymptotic 10/3-approximation algorithm for RCP on graphs of this class. We note that, the best currently known approximation ratio for the RCP on ordinary (non-hierarchical) planar graphs of general degree is 5?/?3 asymptotically ([., .]).作者: 邊緣 時(shí)間: 2025-3-28 04:17 作者: 遷移 時(shí)間: 2025-3-28 09:52
Dialectical Rationality in History: A Paradigmatic Approach to Karl Marx’s uch more liberal because it assumes “different linguistic games”: not just one language inherent in the empirical natural order. Thus arose the analytical philosophy of history which investigates the morphology of historical writings, different levels of historical knowledge, and the connection with作者: 無(wú)禮回復(fù) 時(shí)間: 2025-3-28 12:58 作者: Seizure 時(shí)間: 2025-3-28 16:15
