Deformation of a poroelastic layer overlying an elastic half‐space due to dip‐slip faulting          下载免费PDF全文

R. C. Verma  S. Rani  S. J. Singh 《国际地质力学数值与分析法杂志》2016,40(3):391-405

An analytical solution of the plane strain problem of the deformation of a homogeneous, isotropic, poroelastic layer of uniform thickness overlying a homogeneous, isotropic, elastic half‐space due to two‐dimensional seismic sources buried in the elastic half‐space has been obtained. The integral expressions for the displacements, stresses and pore pressure have been obtained using the stress function approach by applying suitable boundary conditions at the free surface and the interface. The solution obtained is in the Laplace–Fourier transform domain. The case of a vertical dip‐slip line dislocation for the oceanic crust model of Earth is studied in detail. Schapery's formula is used for the Laplace inversion and the extended Simpson's formula for the Fourier inversion. Diffusion of pore pressure in the layer is studied numerically. Contour maps showing the pore pressure in the poroelastic layer have been plotted. The effect of the compressibility of the solid and fluid constituents on pore pressure has also been studied. Copyright © 2015 John Wiley & Sons, Ltd.  相似文献   

On Coronal Loop Heating by Torsional Alfvén Waves     

U. Narain  P. Agarwal  R.K. Sharma  L. Prasad  B.N. Dwivedi 《Solar physics》2001,199(2):307-315

Heating of coronal loops by linear resonant Alfvén waves, excited by the footpoints motions in the photosphere, has been studied. The analysis of single-layer heating is extended to multilayer heating, in semiempirical treatment. Heating and nonthermal velocities in different layers of loops in X-ray bright points, active regions, and large-scale structures are estimated. The average value of velocity is found to be in agreement with the observations.  相似文献   

Study of drainage pattern through aerial data in Naugarh area of Varanasi district, U.P.   总被引：1，自引：0，他引：1  

C S Agarwal 《Journal of the Indian Society of Remote Sensing》1998,26(4):169-175

Drainage pattern of Naugarh Block of district Varanasi has been mapped. The basin characterestics have been analysed is terms of basin morphology and related parameters. The drainage system of the region is composed of 3 perennial rivers with 7 sub-basins. A total of 1223 streams. of 1st to 6th order exist, out of which 761 are of 1st order and 350 of 2nd order which hold sufficient amount of water duing the peak monsoon period Surface water resources could be enhanced in the region by constructing check dams and creating artificial recharge through effective and management.  相似文献   

Origin of high fluoride in groundwater in the North Gujarat-Cambay region, India   总被引：2，自引：0，他引：2  

S. K. Gupta  R. D. Deshpande  Meetu Agarwal  B. R. Raval 《Hydrogeology Journal》2005,13(4):596-605

This paper reports on the origin of high fluoride in a regional alluvial aquifer system under water stress in the North Gujarat-Cambay (NGC) region in western India. This region is severely affected by endemic fluorosis due to ingestion of groundwater containing excessive fluoride. With an objective to understand factors controlling high fluoride concentration in groundwater of this region, 225 groundwater samples have been analysed for various chemical parameters. Samples were collected from different depth zones tapping shallow dug wells, geothermal springs, hand-pumps and tubewells, including free flowing artesian wells up to 450 m depth from the aquifers in the Quaternary alluvial formation covering most of the study area. No relation was found between fluoride concentration and depth of sampled groundwater. However, certain sub-aquifer zones have been identified within the Cambay Basin where groundwater contains relatively high fluoride concentration. In general, areas of high fluoride overlap areas with high electrical conductivity (EC). On the west flank of the Cambay Basin in the low lying belt linking Little Rann of Kachchh-Nalsarovar-Gulf of Khambhat (LRK-NS-GK), high fluoride and EC in shallow aquifers originate from evaporative enrichment. On the east flank of Cambay Basin, some high fluoride pockets are observed which are probably due to preferential dissolution of high fluoride bearing minerals. On this flank high fluoride is also associated with thermal springs. Within the Cambay Basin, alternating belts of low and high fluoride concentrations are ascribed to groundwater recharge during the past wet and arid climatic phases, respectively. This is based on groundwater radiocarbon age contours of ~20 ka overlapping the high fluoride belt.

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Resumen Este artículo reporta sobre el origen de altas concentraciones de flúor en un sistema regional de acuíferos bajo presión hídrica en la región del norte de Gujarat-Cambay (NGC) del occidente de India. Esta región está afectada severamente por fluorosis endémica debido a la ingestión de agua subterránea que contiene exceso de flúor. Se tomaron 225 muestras de agua subterránea las cuales fueron analizadas por varios parámetros químicos con el objetivo de entender los factores que controlan las elevadas concentraciones de flúor en esta región. Las muestras se colectaron a diferentes profundidades en pozos someros, manantiales geotermales, pozos con bombas de mano, y pozos entubados incluyendo pozos artesianos de flujo libre de hasta 450 m de profundidad emplazados en los acuíferos de la formación aluvial Cuaternaria que cubre la mayor parte del área de estudio. No se encontró ninguna relación entre la concentración de flúor y la profundidad de las muestras de agua subterránea. Sin embargo, se identificaron dentro de la cuenca Cambay algunas zonas sub-acuíferas donde el agua subterránea contiene concentraciones relativamente altas de flúor. En general, las áreas con elevada concentración de flúor están sobrepuestas a áreas de alta conductividad eléctrica (CE). Sobre el flanco occidental de la cuenca Cambay, en la faja baja que une Little Rann con Kachchh-Nalsarovar-Golfo de Khamhat (LRK-NS-GK), las altas concentraciones de flúor y altas CE en acuíferos someros se derivan de enriquecimiento por evaporitas. Sobre el flanco oriental de la cuenca Cambay se observaron algunos cuerpos con alta concentración de flúor los cuales se deben probablemente a la disolución preferencial de minerales con alto contenido de flúor. En este flanco el alto contenido de flúor también se asocia con manantiales termales. Dentro de la cuenca Cambay existen fajas alternantes, con concentraciones altas y bajas de flúor, las cuales se atribuyen a recarga de agua subterránea durante las fases climáticas pasadas, húmedas y áridas, respectivamente. Este planteamiento se basa en contornos de edades de ~20 ka de radiocarbono que están sobrepuestos a la faja alta en flúor.

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Résumé Cet article étudie lorigine des teneurs élevées en Fluorure dans un système aquifère alluvial régional, soumis à un stress hydrique dans le Nord Gujarat–région Cambay (NGC) à lOuest de lInde. Cette région est sévèrement affectée par une fluorose endémique, due à lingestion deau souterraine très riche en fluor. Avec pour objectif de comprendre les paramètres contrôlant les fortes teneurs en fluor, 225 échantillons deau souterraine ont été analysés sur différents paramètres. Les échantillons ont été pris à différentes profondeurs : puits de surface, sources géothermiques, pompes à main, forages artésiens jaillissant dont la profondeur avoisine les 450 m dans les formations alluviales quaternaire recouvrant la plus grande partie de la région étudiée. Il ny a pas de relation entre la profondeur et les teneurs en fluorure. Néanmoins, certaines zones sub-aquifères ont été identifiées dans le Basin de Cambay où leau souterraine présentait des concentrations relativement élevées en fluorure. En général les zones de hautes concentrations en fluorure recouvrent les zones à fortes conductivité électrique (abréviation en anglais: EC). Sur le flanc Ouest du bassin de Cambay dans le mince lit reliant Little Ran de Kachchh-Nalsarovar au golfe de Khambhat (LRK-NS-GK), les fortes teneurs en fluorure et les EC dans la nappe phréatique proviennent de lenrichissement par les évaporites. Sur le flanc Est du bassin, des poches de teneurs élevées en fluorures ont été observées, probablement dues à des dissolutions préférentielles de minéraux fluorés. Sur ce flanc des teneurs sont également associées à la présence de sources géothermales. Dans le bassin de Cambay, les alternances de couches lits à fortes teneurs et de lits à faibles teneurs sont expliquées par la recharge durant les périodes climatiques humides et les périodes climatiques plus sèches. Ceci est corroboré par les datations au radiocarbone (environ 20.000 an) au dessus du lit riche en fluorure.

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Artificial neural network to translate offshore satellite wave data to coastal locations     

Ruchi Kalra  M.C. Deo  Raj Kumar  Vijay K. Agarwal 《Ocean Engineering》2005,32(16):1917-1932

Owing to the spatial averaging involved in satellite sensing, use of observations so collected is often restricted to offshore regions. This paper discusses a technique to obtain significant wave heights at a specified coastal site from their values gathered by a satellite at deeper offshore locations. The technique is based on the approach of Artificial Neural Network (ANN) of Radial Basis Function (RBF) and Feed-forward Back-propagation (FFBP) type. The satellite-sensed data of significant wave height; average wave period and the wind speed were given as input to the network in order to obtain significant wave heights at a coastal site situated along the west coast of India. Qualitative as well as quantitative comparison of the network output with target observations showed usefulness of the selected networks in such an application vis-à-vis simpler techniques like statistical regression. The basic FFBP network predicted the higher waves more correctly although such a network was less attractive from the point of overall accuracy. Unlike satellite observations collection of buoy data is costly and hence, it is generally resorted to fewer locations and for a smaller period of time. As shown in this study the network can be trained with samples of buoy data and can be further used for routine wave forecasting at coastal locations based on more permanent flow of satellite observations.  相似文献   

Delineation of potential sites for water harvesting structures using remote sensing and GIS   总被引：6，自引：0，他引：6  

M. Girish Kumar  A. K. Agarwal  Rameshwar Bali 《Journal of the Indian Society of Remote Sensing》2008,36(4):323-334

Availability of groundwater varies spatially and temporally depending upon the terrain. The scarcity of water affects the environmental and developmental activities of an area. Construction of small water harvesting structures across streams/watersheds is gaining momentum in recent years. In the present study, potential sites for construction of rainwater harvesting structures in the Bakhar watershed of Mirzapur District, Uttar Pradesh, India have been identified by using remote sensing and GIS techniques. Various thematic maps such as Landuse/Landcover, geomorphology and lineaments, etc. were prepared using remote sensing. These layers along with geology and drainage were integrated using GIS techniques to derive suitable water harvesting sites. Each theme was assigned a weightage depending on its influence on ground water recharge (for example weightages 20,18,15,25,25 and 0 were assigned to geomorphology, landuse, geology, lineament, drainage and road and villages respectively). Each class or unit in the map was assigned a knowledge based ranking of one to four depending on its significance in storage and transmittance of groundwater, and these values were multiplied with layer weightage to form score. The average score for excellent region is greater than 200, for good 121 to 200, for moderate 81 to 121 and the other polygon having value less than 80 (excluding zero) were assigned to poor category. The final map showing different categories of suitability sites for water harvesting structures such as Check dams, Contour bunding, Recharge pits, Wells and Contour trenching have been suggested.  相似文献   

Estimation of model parameter of Sumatra earthquake using empirical Green’s function technique and generation of hypothetical earthquake scenario for Andaman Island, India     

A. Joshi  Pushpa Kumari  Sushil Kumar  M. L. Sharma  A. K. Ghosh  M. K. Agarwal  A. Ravikiran 《Natural Hazards》2012,62(3):1081-1108

Empirical Green??s function (EGF) technique is considered to be most effective technique for simulation of ground motions due to a finite earthquake source. In the present paper, this technique has been used to simulate ground motion due to a great earthquake. The coastal region of Sumatra Island has been visited by a great earthquake on December 26, 2004. This earthquake has been recorded at several broadband stations including a nearest broadband station PSI in Indonesia. The shear wave contributions in both horizontal components have been simulated at PSI station using EGF technique. The comparison of simulated and observed waveform has been made for various possibilities of rupture parameters in terms of root mean square error. The final rupture model supports rupture velocity of 3.0?km/s with nucleation point supporting northward propagating rupture that coincide with high-slip asperity defined by Sorensen et al. (Bull Seism Soc Am 97:S139?CS151, 2007). The final modeling parameters have been used to simulate record at MDRS station in coastal state of Tamilnadu, India. In an attempt to model a scenario of great earthquake in the Andaman Island, a hypothetical rupture plane is modeled in this region. The event occurred on August 10, 2008 of magnitude 6.2 (M _w ) recorded on strong motion array at Port Blair has been used as EGF to simulate records due to the hypothetical great earthquake. Possibilities of earthquake due to the oblique strike-slip and thrust mechanism have been modeled in the present paper. Several possibilities of nucleation point for both cases has been considered, and it is seen that variation of peak ground acceleration at Port Blair station for strike-slip and thrust mechanism is 126?C738 gals and 647?C2,571 gals, respectively, which indicate high seismic hazard potential of Andaman Island.  相似文献   

Effects of density, temperature and velocity gradients on inertial Alfven wave in cusp region     

P. Agarwal  P. Varma  M.S. Tiwari 《Planetary and Space Science》2011,59(13):1516-1523

The kinetic approach is used to evaluate the dispersion relation and growth/damping rate of inertial Alfven wave (IAW) with density, temperature and velocity gradients in an inhomogeneous plasma. The effects of gradient terms are studied for both the regions k_⊥ρ_i<1 and k_⊥ρ_i>1, where k_⊥ is the perpendicular wave number and ρ_i is the ion gyroradius. The relevance of theoretical results so obtained is predicted in accordance to the FAST observations in the cusp region. The results are interpreted for the space plasma parameters appropriate to the cusp region. This study elucidates a possible scenario to account for the particle acceleration and the wave dissipation in inhomogeneous plasmas. This model is also able to explain many features observed in plasma sheet boundary layer as well as to evaluate the dispersion relation, growth/damping rate and growth/damping length of inertial Alfven wave. It is found that density, temperature and velocity gradients control the wave frequency and effectively enhance the growth rate of inertial Alfven wave.  相似文献   

Incorporating irregular nonlinear waves in coupled simulation and reliability studies of offshore wind turbines     

Puneet Agarwal  Lance Manuel 《Applied Ocean Research》2011,33(3):215-227

Design of an offshore wind turbine requires estimation of loads on its rotor, tower and supporting structure. These loads are obtained by time-domain simulations of the coupled aero-servo-hydro-elastic model of the wind turbine. Accuracy of predicted loads depends on assumptions made in the simulation models employed, both for the turbine and for the input wind and wave conditions. Currently, waves are simulated using a linear irregular wave theory that is not appropriate for nonlinear waves, which are even more pronounced in shallow water depths where wind farms are typically sited. The present study investigates the use of irregular nonlinear (second-order) waves for estimating loads on the support structure (monopile) of an offshore wind turbine. We present the theory for the irregular nonlinear model and incorporate it in the commonly used wind turbine simulation software, FAST, which had been developed by National Renewable Energy Laboratory (NREL), but which had the modeling capability only for irregular linear waves. We use an efficient algorithm for computation of nonlinear wave elevation and kinematics, so that a large number of time-domain simulations, which are required for prediction of long-term loads using statistical extrapolation, can easily be performed. To illustrate the influence of the alternative wave models, we compute loads at the base of the monopile of the NREL 5MW baseline wind turbine model using linear and nonlinear irregular wave models. We show that for a given environmental condition (i.e., the mean wind speed and the significant wave height), extreme loads are larger when computed using the nonlinear wave model. We finally compute long-term loads, which are required for a design load case according to the International Electrotechnical Commission guidelines, using the inverse first-order reliability method. We discuss a convergence criteria that may be used to predict accurate 20-year loads and discuss wind versus wave dominance in the load prediction. We show that 20-year long-term loads can be significantly higher when the nonlinear wave model is used.  相似文献   

Interplanetary turbulences causing unusual anisotropic wave trains in cosmic rays     

Rajesh K. Mishra  Rekha Agarwal Mishra 《Astroparticle Physics》2007,26(6):387-397

The various observed harmonics of the cosmic ray variation may be understood on a unified basis if the free space cosmic ray anisotropy is non-sinusoidal in form. The major objective of this paper is to study the first three harmonics of high amplitude wave trains of cosmic ray intensity over the period 1991–1994 for Deep River Neutron Monitoring Station. The main characteristic of these events is that the high amplitude wave trains shows a maximum intensity of diurnal component in a direction earlier than 1800 Hr/co-rotational direction. It is noticed that these events are not caused either by the high-speed solar wind streams or by the sources on the Sun responsible for producing these streams such as polar coronal holes. The direction of semi-diurnal anisotropy shows negative correlation with Bz. The occurrence of high amplitude events is dominant for the positive polarity of Bz component of IMF. The diurnal amplitude of these events shows a negative and the time of maximum shows a weak correlation with disturbance storm time index Dst. The direction of tri-diurnal anisotropy of these events is found to significantly correlate with geomagnetic activity index Ap.  相似文献