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1.
L. B. Volkomirskaya S. A. Gorbunov S. V. Panfilov A. E. Reznikov 《Planetary and Space Science》1988,36(12):1305-1315
The multicomponent data of the electromagnetic field obtained on the Aureol-3 satellite were studied. On the basis of the application of the multispectral analysis, nonlinear interactions on the harmonics of the proton gyro-frequency were determined. By the power spectra of the low frequency radiation components, the principal regulations of behaviour of the vectors of the wave normal and of the wave distribution function from the frequency and the invariant latitude L were found. It is noted, that at frequencies below the proton gyro-frequency there often arises the second maximum in the form of a wave distribution function, that can be interpreted as a reflected wave. 相似文献
2.
A. I. Miroshnichenko A. P. Sorokin V. A. San’kov A. V. Lukhnev S. V. Ashurkov A. T. Sorokina N. I. Panfilov M. A. Serov S. I. Sherman 《Russian Journal of Pacific Geology》2008,2(1):64-71
The Amur-Zeya geodynamic test ground was set up in 2000 to study recent intracontinental crustal deformations. The velocity field calculations for the period of 2000 to 2003 describe three movements scales. The general level is characterized by the vectors of IGS sites in the eastern part of Asia, the BLAG (Blagoveshchensk) site included. The southeast movement of the IRKT (Irkutsk) site of the stable Siberian Platform is indicative of deformations in the northeastern part of the Amur Plate. Measurement data on the regional near-latitudinal profile Blagoveshchensk-Sutara, which crosses the Nizhnyaya Zeya Basin, demonstrate a southwestward displacement of the Badzhal-Bureya-Lesser Khingan block relative to the North China block. The dynamic effect of the convergent boundary between the Amur and Okhotsk Sea plates is assumed to extend inland also involving the Zeya-Bureya Basin area. The measurements on the local geodynamic test site relate the deformations of buildings and constructions in the Settlement of Konstantinovka to the mobility of basement faults in the southern part of the Nizhnyaya Zeya Basin. Aseismic deformations are determined by slow horizontal tectonic movements in the junction zone of NNE-trending structures of the latter basin and near-latitudinal faults of the Khailar-Xunhei Belt. 相似文献
3.
B. Hagemann M. Rasoulzadeh M. Panfilov L. Ganzer V. Reitenbach 《Computational Geosciences》2016,20(3):595-606
The intermittent production of the renewable energy imposes the necessity to temporarily store it. Large amounts of exceeding electricity can be stored in geological strata in the form of hydrogen. The conversion of hydrogen to electricity and vice versa can be performed in electrolyzers and fuel elements by chemical methods. The nowadays technical solution accepted by the European industry consists of injecting small concentrations of hydrogen in the existing storages of natural gas. The progressive development of this technology will finally lead to the creation of underground storages of pure hydrogen. Due to the low viscosity and low density of hydrogen, it is expected that the problem of an unstable displacement, including viscous fingering and gravity overriding, will be more pronounced. Additionally, the injection of hydrogen in geological strata could encounter chemical reactivity induced by various species of microorganisms that consume hydrogen for their metabolism. One of the products of such reactions is methane, produced from Sabatier reaction between H2 and CO2. Other hydrogenotrophic reactions could be caused by acetogenic archaea, sulfate-reducing bacteria and iron-reducing bacteria. In the present paper, a mathematical model is presented which is capable to reflect the coupled hydrodynamic and bio-chemical processes in UHS. The model has been numerically implemented by using the open source code DuMuX developed by the University of Stuttgart. The obtained bio-chemical version of DuMuX was used to model the evolution of a hypothetical underground storage of hydrogen. We have revealed that the behavior of an underground hydrogen storage is different than that of a natural gas storage. Both, the hydrodynamic and the bio-chemical effects, contribute to the different characteristics. 相似文献
4.
Hydrogen penetration in water through porous medium: application to a radioactive waste storage site
Hydrogen penetration in water through porous medium was analyzed in the paper. A two-phase compositional model approach was
considered. The first part of the work deals with the thermodynamic analysis of the hydrogen–water system. The thermodynamic
model was calibrated using the experimental data of hydrogen solubility in water. The phase densities, viscosities and phase
concentrations were presented in an analytical form. Moreover, the domain of validity of analytical laws—such as Henry’s,
Raoult’s and Kelvin’s laws—for the estimation of phase properties was presented for the analyzed system. The second part deals
with two-phase hydrodynamic behaviors. An analytical solution for the non-compressible flow was constructed. In general case,
the influence of relative permeabilities on the flow regimes was analyzed numerically. The notion pseudo-saturation was introduced
to define phase appearance. Actually, mobile gas created a time displaced front relatively slower than mobile gas flow. Diffusion
becomes really important for low mobile gas case as the penetration accelerates for the large range of saturation. In contrast,
the mass exchange phenomena have a small influence on the flow type. Thus, the regimes of hydrogen penetration in liquid were
shown really sensitive to the relative permeability form. 相似文献
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6.
We shall consider diffusion or single-phase flow in a multiscale porous medium which represents an infinite set of self-similar double-porosity media. At each scale, the medium consists of a highly permeable network of connected channels and low-permeable blocks. The characteristic scale of heterogeneity is ε at the highest level of hierarchy, wherein ε is a small parameter. The ratio between the channel and block permeability at each scale is ε 2. The process analyzed is described using a diffusion equation with an oscillating multiscale diffusion parameter. The macroscale behavior is of interest. The transition to the macroscale is performed by means of the two-scale homogenization procedure. One step of averaging at each level of hierarchy leads to the appearance of the memory terms in the averaged equation. The successive averaging steps lead to progressive memory accumulation, so at each step of averaging, the macroscale model changes its type, and even the result of the second step is unknown a priori. The objective was to determine the macroscopic limit model for the infinite number of scales. By the method of induction, we obtained the macroscale model for an arbitrary number of scales and its limit for the infinite hierarchy. The limit model represents the system of two equations with memory terms. The kernel of the memory operator is the solution of a nonlinear integro-differential equation. Its solution is obtained through Laplace transform. 相似文献
7.
S. M. Korotaev E. O. Kiktenko S. P. Gaidash N. M. Budnev R. R. Mirgazov A. I. Panfilov A. A. Khalezov V. O. Serdyuk V. S. Shneer 《Geomagnetism and Aeronomy》2013,53(6):769-773
Based on the data of deepwater measurements of the electric field’s vertical component in Lake Baikal, the relationship between electric field variations and those in background X-ray solar radiation has been revealed. A high correlation between these variations within periods of more than three months has been discovered. 相似文献
8.
For a high-velocity stable flow through a periodic corrugated channel representing an element of porous medium, we suggest splitting the overall nonlinear macroscopic effects into two kinds of different physical origin: a pure inertia effect produced by the convective term of Navier–Stokes equations and an inertia–viscous cross effect representing a variation of the viscous dissipation due to a streamline deformation by inertia forces. We will show that the inertia–viscous cross effects may be revealed by simulating a periodic flow, whilst the pure inertia effects are produced by the microscale flow nonperiodicity. We will reveal the individual flow law for each nonlinear component and analyze the relative role of both components numerically by using the finite element method applied to the Navier–Stokes equations. Both the pure inertia and the inertia–viscous cross effects are revealed to be exponential prior to quadratic or cubic ones. The influence of the dead volume is analyzed. The inertia–viscous cross phenomena are shown to be negligible when the flow structure is clearly nonperiodic. 相似文献
9.
Convection occurs when two water reservoirs, the overlying and the underlying, are connected by a narrow channel and the fluid in the lower reservoir is heated to the stage of phase transition into steam. The laboratory study of the properties of unstable steam-water convection showed that under favourabieP-T conditions the convection can be the triggering mechanism of seismicity. This type of convection causes a sudden fall of pressure in the lower reservoir and in the connecting channel, the impulsive mechanical disturbances, and cyclicity. The point of initiation of this phenomenon can be located at a depth of 5–7 km from the earth's surface with subsequent propagation of the process of instability to larger and smaller depths. This model of the natural terrestrial conditions can account for the earthquake cyclicity in the same focal zones, the rise of temperature and of the level of ground waters during earthquakes, the enhancement of seismicity while filling the water storage basins, the effect of floating up of hypocenters of aftershocks and the greater intervals between them. 相似文献
10.
S. M. Korotaev S. P. Gaidash V. S. Shneer V. O. Serdyuk N. M. Budnev R. R. Mirgazov V. B. Buzin A. A. Khalezov A. I. Panfilov 《Izvestiya Physics of the Solid Earth》2011,47(2):147-153
The long-term deep-water measurements of the vertical component of the electric field on a surface-lakebed base revealed unexpectedly high interannual changeability in the amplitudes of its variations in periods ranging from a few hours to several months. This changeability almost equally affects the field components caused by the induction in the water flows and, supposedly, by the closing current of the global electric circuit above the rift fault. We present the evidence for the correlation of this effect with the interannual variability in meteorological activity. However, the physical background of this correlation is trivial only for the electric component associated with the induction and still remains unclear for the field component caused by the closing current, which has much higher amplitude. 相似文献