標題: Titlebook: Chaotic Processes in the Geological Sciences; David A. Yuen Conference proceedings 1992 Springer-Verlag New York, Inc. 1992 applied mathem [打印本頁] 作者: 選民 時間: 2025-3-21 18:21
書目名稱Chaotic Processes in the Geological Sciences影響因子(影響力)
書目名稱Chaotic Processes in the Geological Sciences影響因子(影響力)學科排名
書目名稱Chaotic Processes in the Geological Sciences網(wǎng)絡(luò)公開度
書目名稱Chaotic Processes in the Geological Sciences網(wǎng)絡(luò)公開度學科排名
書目名稱Chaotic Processes in the Geological Sciences被引頻次
書目名稱Chaotic Processes in the Geological Sciences被引頻次學科排名
書目名稱Chaotic Processes in the Geological Sciences年度引用
書目名稱Chaotic Processes in the Geological Sciences年度引用學科排名
書目名稱Chaotic Processes in the Geological Sciences讀者反饋
書目名稱Chaotic Processes in the Geological Sciences讀者反饋學科排名
作者: 顯微鏡 時間: 2025-3-21 21:38 作者: 繁榮地區(qū) 時間: 2025-3-22 03:53
Convection and Chaos,iffering aspects of the motion find their expression in the migration of subduction zones and hot spots, respectively. The analysis of plumes in a single convection cell can be attempted in the framework of Howard’s ‘bubble’ model of convection, using an asymptotic analysis based on a similar method作者: sorbitol 時間: 2025-3-22 07:04
Strongly Chaotic Newtonian and Non-Newtonian Mantle Convection,nts initiated by physicists, may be useful for understanding the dynamics of magma oceans developed in the early stages of terrestrial planets. Results drawn from two-dimensional numerical simulations of base-heated thermal convection for both linear and non-linear rheologies are presented to show b作者: 我沒有命令 時間: 2025-3-22 09:45
Routes to Chaos in the Solid Earth,nvection can be specified and an essential feature is the very large Prandtl number. We examine routes to chaos in two-dimensional thermal convection in a fluid layer heated from below. Twelve, twenty-four and forty-mode expansions are considered. The twelve and forty-mode expansions evolve to chaot作者: angiography 時間: 2025-3-22 15:14 作者: angiography 時間: 2025-3-22 19:09 作者: albuminuria 時間: 2025-3-22 23:48 作者: 頑固 時間: 2025-3-23 03:17 作者: Patrimony 時間: 2025-3-23 08:08
Convection in Porous Media with Thermal and Chemical Buoyancy: A Comparison of Two Models for Solute is made of an effective dispersion coefficient that is taken as a constant scalar. In the second, a velocity-dependent dispersivity term that explicitly considers both molecular and mechanical dispersion is used. The results show that for the particular cases studied (. = 600φ/σ = 1, aspect ratio 作者: 高興去去 時間: 2025-3-23 11:33 作者: 舊石器時代 時間: 2025-3-23 14:59
Theory of the Geodynamo and Core-Mantle Coupling,ity in the lower mantle of the Earth is emphasized. The latter may be responsible for the separation between standing and drifting fields found in the analysis of secular variation. It is even possible in principle to find dynamo action based on lateral variations of conductivity.作者: Infirm 時間: 2025-3-23 19:44
Nonlinear Dynamical Models for Earthquakes and Frictional Sliding, in nature effects associated with classical growth mechanisms for shear fractures. Moreover, friction experiments in the laboratory display a rate dependence through a series of state variables whose physical interpretation is unclear. Of the two nonclassical approaches examined here, the first is 作者: Cuisine 時間: 2025-3-24 00:21 作者: arthroplasty 時間: 2025-3-24 05:34 作者: nonsensical 時間: 2025-3-24 09:25
Bayesian Networks in Decision Support,ity in the lower mantle of the Earth is emphasized. The latter may be responsible for the separation between standing and drifting fields found in the analysis of secular variation. It is even possible in principle to find dynamo action based on lateral variations of conductivity.作者: 可用 時間: 2025-3-24 12:29 作者: Crumple 時間: 2025-3-24 18:07 作者: staging 時間: 2025-3-24 21:01 作者: 一再遛 時間: 2025-3-25 00:49
https://doi.org/10.1007/b105919gineering applications. Recent experiments by the Chicago group (Heslog .., and Casting ..) have shown that at high Rayleigh numbers (Ra) the flow undergoes a transition in its structure from soft turbulence to hard turbulence. In particular, in the central turbulent core the probability distributio作者: Bureaucracy 時間: 2025-3-25 06:45 作者: 善變 時間: 2025-3-25 08:20
https://doi.org/10.1007/b105919iffering aspects of the motion find their expression in the migration of subduction zones and hot spots, respectively. The analysis of plumes in a single convection cell can be attempted in the framework of Howard’s ‘bubble’ model of convection, using an asymptotic analysis based on a similar method作者: 脫離 時間: 2025-3-25 14:52
https://doi.org/10.1007/b105919nts initiated by physicists, may be useful for understanding the dynamics of magma oceans developed in the early stages of terrestrial planets. Results drawn from two-dimensional numerical simulations of base-heated thermal convection for both linear and non-linear rheologies are presented to show b作者: 起皺紋 時間: 2025-3-25 17:31 作者: Collision 時間: 2025-3-25 23:27
https://doi.org/10.1007/b105919op for the divariant Spinel-post Spinel transition is extremely narrow in pressure and that the Clapeyron slope of this transition is near -2.8 .. Extremely high resolution calculations of the nature of convective mixing in a flow in which both this and the Olivine-Spinel transition are present, dem作者: braggadocio 時間: 2025-3-26 00:54
https://doi.org/10.1007/b105919icomponent silicate melt that crystallizes to form a solid whose components differ locally from those of the original melt. This difference in composition can drive strong convective motions in the melt and cause large-scale zonation of minerals..This paper considers a series of general, one-dimensi作者: Confound 時間: 2025-3-26 06:57
A Design Space Exploration Methodologyevelopment and testing of flow models. Lavas contain gas bubbles and hence have two specific properties: compressibility and dilatational viscosity. The effects of dilatational viscosity are only significant for eruptions with high mass flux. On the contrary, compressibility is always important. For作者: arthroscopy 時間: 2025-3-26 10:03 作者: BUMP 時間: 2025-3-26 15:46
Hannu Nurmi,Tommi Meskanen,Antti Pajalae is made of an effective dispersion coefficient that is taken as a constant scalar. In the second, a velocity-dependent dispersivity term that explicitly considers both molecular and mechanical dispersion is used. The results show that for the particular cases studied (. = 600φ/σ = 1, aspect ratio 作者: transdermal 時間: 2025-3-26 18:52 作者: 職業(yè)拳擊手 時間: 2025-3-26 21:49
Bayesian Networks in Decision Support,ity in the lower mantle of the Earth is emphasized. The latter may be responsible for the separation between standing and drifting fields found in the analysis of secular variation. It is even possible in principle to find dynamo action based on lateral variations of conductivity.作者: Palliation 時間: 2025-3-27 03:22 作者: BRAVE 時間: 2025-3-27 09:08 作者: LASH 時間: 2025-3-27 09:59
The IMA Volumes in Mathematics and its Applicationshttp://image.papertrans.cn/c/image/223931.jpg作者: 大量 時間: 2025-3-27 13:36
Conference proceedings 1992ces have many nonlinearities from the nature of the complicated physical laws which give rise to strongly chaotic behavior. Foremost and most visible are earthquakes and volcanic eruptions, more subtle are the time- dependent variations of the Earth‘s magnetic fields and motions of the surface plate作者: 魅力 時間: 2025-3-27 18:49 作者: 枯燥 時間: 2025-3-27 23:25
Convection and Chaos,corresponding Poincaré map should lead to a chaotic distribution of plumes in space and time..For cellular convection, we give a synopsis of the recent scaling theory of the Chicago group. There is a mean flow in the cell, fuelled by thermal plumes which erupt from the boundary layer as they are adv作者: 斜 時間: 2025-3-28 03:47 作者: avarice 時間: 2025-3-28 07:27
Vigorous Motions in Magma Chambers and Lava Lakes,m laboratory experiments using aqueous solutions. The agreement between the two sets of results is shown to be very good. Calculations using the simple, geologically oriented, two- component anorthite-diopside system are presented and their geological interpretation discussed briefly.作者: reception 時間: 2025-3-28 11:55
The Eruption and Spreading of Lava,ints on the evolution of the magma reservoir which feeds them. During flow away from a volcanic vent at the Earth’s surface, compressibility affects the dynamics of spreading, leading to smaller variations of flow thickness and hence to slower rates of advance..Lava eruptions present a puzzle becaus作者: 固定某物 時間: 2025-3-28 15:59 作者: 高歌 時間: 2025-3-28 20:25 作者: bizarre 時間: 2025-3-29 02:01
0940-6573 t visible are earthquakes and volcanic eruptions, more subtle are the time- dependent variations of the Earth‘s magnetic fields and motions of the surface plate978-1-4684-0645-0978-1-4684-0643-6Series ISSN 0940-6573 Series E-ISSN 2198-3224 作者: Optimum 時間: 2025-3-29 05:29 作者: 不能根除 時間: 2025-3-29 09:19 作者: Merited 時間: 2025-3-29 14:44 作者: OMIT 時間: 2025-3-29 17:41
https://doi.org/10.1007/b105919m laboratory experiments using aqueous solutions. The agreement between the two sets of results is shown to be very good. Calculations using the simple, geologically oriented, two- component anorthite-diopside system are presented and their geological interpretation discussed briefly.作者: 貿(mào)易 時間: 2025-3-29 20:27
A Design Space Exploration Methodologyints on the evolution of the magma reservoir which feeds them. During flow away from a volcanic vent at the Earth’s surface, compressibility affects the dynamics of spreading, leading to smaller variations of flow thickness and hence to slower rates of advance..Lava eruptions present a puzzle becaus作者: 散開 時間: 2025-3-30 02:24
Hannu Nurmi,Tommi Meskanen,Antti Pajalaield mixes more quickly. For .ρ = 0.5, chaotic flow characterizes convection for both dispersion models and regions of sharp solute gradients are highly mobile in time and space. The main difference between the two solute dispersion models for .ρ = 0.5 is that the interior of the solute field is les作者: averse 時間: 2025-3-30 07:44 作者: patriarch 時間: 2025-3-30 11:26
