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Littérature scientifique sur le sujet « Fluid in the seismogenic process »

Auteur : Grafiati

Publié le 10 mars 2023

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Articles de revues sur le sujet "Fluid in the seismogenic process"

Parry, W. T., et R. L. Bruhn. « Fluid pressure transients on seismogenic normal faults ». Tectonophysics 179, n^o 3-4 (juillet 1990) : 335–44. http://dx.doi.org/10.1016/0040-1951(90)90299-n.

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Liao, Chun-Fu, Strong Wen, Chau-Huei Chen et Ying-Nien Chen. « Exploring the Rheology of a Seismogenic Zone by Applying Seismic Variation ». Applied Sciences 11, n^o 19 (23 septembre 2021) : 8847. http://dx.doi.org/10.3390/app11198847.

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Although the study of spatiotemporal variation of a subsurface velocity structure is a challenging task, it can provide a description of the fault geometry as well as important information on the rheological changes caused by fault rupture. Our main objective is to investigate whether rheological changes of faults can be associated with the seismogenic process before a strong earthquake. For this purpose, a 3D tomographic technique is applied to obtain P- and S-wave velocity structures in central Taiwan using travel time data. The results show that temporal variations in the Vs structure in the source area demonstrate significant spatiotemporal variation before and after the Chi-Chi earthquake. We infer that, before the mainshock, Vs began to decrease (and Vp/Vs increased) at the hanging wall of the Chelungpu fault, which may be induced by the increasing density of microcracks and fluid. However, in the vicinity of the Chi-Chi earthquake’s source area, Vs increased (and Vp/Vs decreased), which may be attributed to the closing of cracks or migration of fluid. The different physical characteristics at the junctional zone may easily generate strong earthquakes. Therefore, seismic velocity changes are found to be associated with a subsurface evolution around the source area in Taiwan. Our findings suggest that monitoring the Vp and Vs (or Vp/Vs) structures in high seismic potential zones is an important ongoing task, which may minimize the damage caused by future large earthquakes.

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Marchesini, Barbara, Paolo Stefano Garofalo, Luca Menegon, Jussi Mattila et Giulio Viola. « Fluid-mediated, brittle–ductile deformation at seismogenic depth – Part 1 : Fluid record and deformation history of fault veins in a nuclear waste repository (Olkiluoto Island, Finland) ». Solid Earth 10, n^o 3 (13 juin 2019) : 809–38. http://dx.doi.org/10.5194/se-10-809-2019.

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Abstract. The dynamic evolution of fault zones at the seismogenic brittle–ductile transition zone (BDTZ) expresses the delicate interplay between numerous physical and chemical processes. Deformation and fluid flow at the BDTZ are closely related and mutually dependent during repeating and transient cycles of frictional and viscous deformation. Despite numerous studies documenting in detail seismogenic faults exhumed from the BDTZ, uncertainties remain as to the exact role of fluids in facilitating broadly coeval brittle and ductile deformation at that structural level. We combine structural analysis, fluid inclusion, and mineral chemistry data from synkinematic and authigenic minerals to reconstruct the temporal variations in fluid pressure (Pf), temperature (T), and bulk composition (X) of the fluids that mediated deformation and steered strain localization along BFZ300, a strike–slip fault originally active at the BDTZ. BFZ300 deforms the Paleoproterozoic migmatitic basement of southwestern Finland and hosts in its core two laterally continuous quartz veins formed by two texturally distinct types of quartz – Qtz I and Qtz II, with Qtz I older than Qtz II. Veins within the damage zone are formed exclusively by Qtz I. Mesostructural and microstructural analysis combined with fluid compositional data indicate recurrent cycles of mutually overprinting brittle and ductile deformation triggered by oscillations of fluid pressure peaking at 210 MPa. Fluid inclusion microthermometry and mineral pair geothermometry indicate that the two documented quartz types precipitated from different fluid batches, with bulk salinities in the 1 wt % NaCleq–5 wt % NaCleq range for Qtz I and in the 6 wt % NaCleq–11 wt % NaCleq range for Qtz II. The temperature of the fluids involved with initial strain localization and later fault reactivation evolved through time from > 350 ∘C during Qtz I precipitation to < 300 ∘C at the time of Qtz II crystallization. The peak fluid pressure estimates constrain pore pressure oscillations between 80 and 210 MPa during the recorded faulting episodes. Our results suggest variability of the physico-chemical conditions of the fluids steering deformation (Pf, T, X), reflecting the ingress and effects of multiple batches of fluid in the fault zone. Initial fluid-mediated embrittlement generated a diffuse network of joints and/or hybrid–shear fractures in the damage zone; subsequent strain localization led to more localized deformation within the fault core. Localization was guided by cyclically increasing fluid pressure and transient embrittlement of a system that was otherwise under overall ductile conditions. Our analysis suggests that fluid overpressure at the BDTZ can play a key role in the initial embrittlement of the deforming rock and steer subsequent strain localization.

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Wen, Yangmao, Zhuohui Xiao, Ping He, Jianfei Zang, Yang Liu et Caijun Xu. « Source Characteristics of the 2020 Mw 7.4 Oaxaca, Mexico, Earthquake Estimated from GPS, InSAR, and Teleseismic Waveforms ». Seismological Research Letters 92, n^o 3 (3 février 2021) : 1900–1912. http://dx.doi.org/10.1785/0220200313.

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Abstract On 23 June 2020, an Mw 7.4 earthquake struck offshore Oaxaca, Mexico, providing a unique opportunity to understand the seismogenic tectonics of the Mexican subduction zone. In this study, near-field coseismic deformation caused by the event was retrieved from Global Positioning System (GPS) observations and Interferometric Synthetic Aperture Radar (InSAR) measurements. Given static geodetic measurements, high-rate GPS waveforms, and teleseismic waveforms, the fault geometry and rupture process for the 2020 Oaxaca earthquake were robustly determined by nonlinear joint inversions. The main slip was located at a depth of 20–30 km with a peak slip of 3.4 m near the epicenter. The total released moment was 1.70×1020 N·m, corresponding to Mw 7.4. The whole rupture process lasted 14 s, with the dominant rupture slip occurring 5–8 s after initial rupture. The mainshock rupture mostly occurred along the fault strike, covering a size of ∼55 km(along strike)×∼35 km(along dip) and totally overlapping with the 1965 Mw 7.5 rupture zone. We speculate that this 2020 earthquake is a repeat event following that in 1965. Fluid percolation under the slab may be one of the key factors affecting the seismogenic depth in the Oaxaca region.

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Qu, Rui, Yingfeng Ji, Weiling Zhu, Youjia Zhao et Ye Zhu. « Fast and Slow Earthquakes in Alaska : Implications from a Three-Dimensional Thermal Regime and Slab Metamorphism ». Applied Sciences 12, n^o 21 (3 novembre 2022) : 11139. http://dx.doi.org/10.3390/app122111139.

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Fast and slow earthquakes are predominantly generated along faults constituting active plate boundaries. Characterized by repeated devastating earthquakes and frequent slow slip events and tremors, the Alaska megathrust presents a chance to understand the complicated dynamics of a subduction system changing from steep to shallow dips associated with enigmatically abundant fast and slow seismic events. Based on three-dimensional thermal modeling, we find that the downgoing metamorphosed oceanic crust containing bound water releases a large amount of fluid and causes the recurrence of fast and slow earthquakes by elevated pore fluid pressure and hydrofracturing. The seismogenic interface and the slow slip events (SSEs) identified beneath the Upper Cook Inlet coincide well with the slab metamorphic dehydration regions. The observed slow earthquakes with quasi-stable fault slips preferentially occur, accompanied by high dehydration and temperature downdip along the transition zone.

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Liu, Qinqin, Angelo De Santis, Alessandro Piscini, Gianfranco Cianchini, Guido Ventura et Xuhui Shen. « Multi-Parametric Climatological Analysis Reveals the Involvement of Fluids in the Preparation Phase of the 2008 Ms 8.0 Wenchuan and 2013 Ms 7.0 Lushan Earthquakes ». Remote Sensing 12, n^o 10 (22 mai 2020) : 1663. http://dx.doi.org/10.3390/rs12101663.

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A multi-parametric approach was applied to climatological data before the Ms 8.0 2008 Wenchuan and Ms 7.0 2013 Lushan earthquakes (EQs) in order to detect anomalous changes associated to the preparing phase of those large seismic events. A climatological analysis for seismic Precursor Identification (CAPRI) algorithm was used for the detection of anomalies in the time series of four parameters (aerosol optical depth, AOD; skin temperature, SKT; surface latent heat flux, SLHF and total column water vapour, TCWV). Our results show a chain of processes occurred within two months before the EQs: AOD anomalous response is the earliest, followed by SKT, TCWV and SLHF in the EQs. A close spatial relation between the seismogenic Longmenshan fault (LMSF) zone and the extent of the detected anomalies indicates that some changes occurred within the faults before the EQs. The similarity of time sequence of the anomalies between the four parameters may be related to the same process: we interpret the observed anomalies as the consequence of the upraising of gases from a fluid-rich middle/upper crust along pre-existing seismogenic faults, and of their release into the atmosphere. Our multi-parametric analytical approach is able to capture phenomena related to the preparation phase of strong EQs.

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Petrosino, Simona, et Paola Cusano. « Low frequency seismic source investigation in volcanic environment : the Mt. Vesuvius atypical case ». Advances in Geosciences 52 (10 juin 2020) : 29–39. http://dx.doi.org/10.5194/adgeo-52-29-2020.

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Abstract. We present a detailed analysis of the low frequency seismicity occurred at Mt. Vesuvius in the time range 2003–2018. This kind of seismicity is atypical for the volcano and poorly studied, therefore we characterized it in terms of spectral analysis, waveform cross-correlation, location and polarization properties. The different decay patterns of the spectra, the existence of both earthquake families as well as single events, the relatively wide seismogenic volume inferred from the locations and polarization features, indicate that the events are caused by distinct source mechanisms: slow brittle failure in dry rocks and resonance of fluid-filled cracks. On these basis, we classified the earthquakes as Low Frequency (LF) and Long Period (LP). Despite the differences between the two classes, both the event types are ascribable to the dynamics of the deep hydrothermal reservoir which induces variations of the fluid pore pressure in the medium. The fluid amount involved in the generation process, as well as the physical-chemical properties of the surrounding rocks are the essential factors that control the occurrence of a mechanism rather than the other.

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Hidayat, Wahyu, David P. Sahara, Sri Widiyantoro, Suharsono Suharsono, Ridho Kresna Wattimena, Sari Melati, I. Putu Raditya Ambara Putra, Septian Prahastudhi, Eric Sitorus et Erwin Riyanto. « Testing the Utilization of a Seismic Network Outside the Main Mining Facility Area for Expanding the Microseismic Monitoring Coverage in a Deep Block Caving ». Applied Sciences 12, n^o 14 (19 juillet 2022) : 7265. http://dx.doi.org/10.3390/app12147265.

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In the case of mining in an inclined intrusion using the block caving method, the highest stress is usually concentrated in the seismogenic and abutment zones, especially in the front of the sloping area. In an inclined intrusion of more than 40°, the seismometer network is usually distributed in the facility area where the footwall area is also located. This causes a limitation in microseismic monitoring due to ray coverage. In this study, we conduct a seismometer deployment outside a mining facilities area with borehole seismometers. The study aims to maximize the resolution and minimize the monitoring uncertainty of underground mines. We created two scenarios of seismometer deployment: (i) seismometers are deployed following the intrusion mining level in the mining facility area; and (ii) additional seismometers are deployed in off-facilities areas. Both areas were tested for their raypath responses and sensitivity using the Checkerboard Resolution Test (CRT). The monitoring resolution influenced by the additional borehole seismometers in the off-facilities area can be quantified. The results suggest that the additional seismometers in the off-facilities areas can increase resolution by 30% in the seismogenic and abutment zones.

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Console, Rodolfo, Paola Vannoli et Roberto Carluccio. « Physics-Based Simulation of Sequences with Foreshocks, Aftershocks and Multiple Main Shocks in Italy ». Applied Sciences 12, n^o 4 (16 février 2022) : 2062. http://dx.doi.org/10.3390/app12042062.

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We applied a new version of physics-based earthquake simulator upon a seismogenic model of the Italian seismicity derived from the latest version of the Database of Individual Seismogenic Sources (DISS). We elaborated appropriately for their use within the simulator all fault systems identified in the study area. We obtained synthetic catalogs spanning hundreds of thousands of years. The resulting synthetic seismic catalogs exhibit typical magnitude, space and time features that are comparable to those obtained by real observations. A typical aspect of the observed seismicity is the occurrence of earthquake sequences characterized by multiple main shocks of similar magnitude. Special attention was devoted to verifying whether the simulated catalogs include this notable aspect, by the use of an especially developed computer code. We found that the phenomenon of Coulomb stress transfer from causative to receiving source patches during an earthquake rupture has a critical role in the behavior of seismicity patterns in the simulated catalogs. We applied the simulator to the seismicity of the northern and central Apennines and compared the resulting synthetic catalog with the observed seismicity for the period 1650–2020. The result of this comparison supports the hypothesis that the occurrence of sequences containing multiple mainshocks is not just a casual circumstance.

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Si, Kai, Zhendong Cui, Ruidong Peng, Leilei Zhao et Yan Zhao. « Crack Propagation Process and Seismogenic Mechanisms of Rock Due to the Influence of Freezing and Thawing ». Applied Sciences 11, n^o 20 (15 octobre 2021) : 9601. http://dx.doi.org/10.3390/app11209601.

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A common problem in cold regions is the influence of freeze–thaw damage on the stability of rock engineering. Therefore, a series of uniaxial compression tests of sandstone after freeze–thaw treatment was carried out in this study. The purpose was to express the initial damage of rock after freezing and thawing treatment more quantitatively and to study the influence of freeze–thaw damage on the rock crack growth process to provide some reference for the stability evaluation of rock engineering in cold regions. The results showed that the number of freeze–thaw cycles and the lowest freeze–thaw temperature had a significant effect on the rock damage and characteristic stress value, and the number of cycles had a more obvious effect: with an increase in the number of freeze–thaw cycles and a decrease in the freeze–thaw temperature, the initial damage DNT had an increasing trend. In addition, the intrinsic mechanism of the freeze–thaw effect on the rock characteristic stress was explained from the perspective of a meso-mechanical mechanism. From the inversion results of the acoustic emission (AE) moment tensor, it was found that the proportion of tensile cracks gradually increased with the increase in the initial damage of the rock in the stable and unsteady stages of the rock crack propagation.

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Thèses sur le sujet "Fluid in the seismogenic process"

Lawther, Susan E. M. « The effects of fluid flow through faults in granite gneiss exhumed from seismogenic depths ». Thesis, University of Glasgow, 2012. http://theses.gla.ac.uk/3374/.

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Fault zones are ubiquitous structures throughout the Earth’s crust and as a fault evolves it can significantly influence the rheological and hydrological properties of the crust. Fluid flow through fault zones is typically associated with fault-fluid-rock interactions and these interactions can affect the mineralogy, strength and evolution of a fault zone. In this study, field mapping is combined with petro-physical and stable isotopic analyses of the fault rock to evaluate the fault-fluid-rock interactions that occur within different fault zones, and the effects of these reactions on fault zone and fault population evolution. At Passo Moro in the NW Itilian Alps, there are three sets of joints cross-cutting the granite gneiss and numerous faults have formed by reactivation of pre-existing joints. The distribution of faults at Passo Moro is ultimately controlled by the variability of joint density within the host rock and the pre-existing joint distribution also affects the likelihood of whether a fault will grow into a mature fault zone or not. Where the joint density is high, strain is unable to accumulate to significant levels to enable joint reactivation into faults, whereas where joint density is low, fault zones are isolated and thus there are no structures nearby to facilitate fault linkage. At Passo Moro the fault population has evolved in a similar way as that described by Martel (1990) whereby small faults link to form simple faults which connect to form compound fault zones. The Virgin Fault and Spaghetti Fault would be considered as small fault zones and The Ciao Ciao Fault is equivalent to a compound fault zone. All three fault zones have different fault architectures and the small faults have been affected by different fluid-rock reactions compared to the larger fault. The small faults have experienced fault zone strengthening by K-feldspar precipitation, whereas the large fault has been weakened by muscovite precipitation. The different reactions between the fault zones are primarily controlled by the water-rock ratio which in turn is governed by permeability and the volume of fluid that infiltrates the fault zone. The Virgin Fault is considered as a rock-dominated system (K-feldspar-rich) whereas The Ciao Ciao fault is a fluid-dominated system (muscovite-rich). However, stable isotopes from both fault zones record a low water-rock ratio signifying rock-dominated conditions. Therefore the mineralogy of the fault rock is not solely controlled by the permeability defined water-rock ratio. The fluid dominated conditions promoting muscovitization in the Ciao Ciao Fault were probably enabled by an open fluid system and large volumes of fluid flowing through the fault during its lifetime. Stable isotopes indicate that water-rock ratios got lower with time in the Virgin Fault implying a limited open system, whereas muscovitization and stable water-rock ratios in the Ciao Ciao Fault point towards open system behaviour. In the Ciao Ciao Fault quartz precipitation only occurs in the foliated cataclasite within the fault core. Quartz precipitation is typically associated with closed system behaviour and suggests that the foliated cataclasite periodically ceased to be open to fluids and hence experienced cycles of higher and lower permeability. Stable isotopes show that the Virgin Fault records mineral precipitation from a metamorphic-like fluid, but after fault deactivation, the fault periodically transmitted progressively more meteoric-like fluids via a micro-fracture network. The Ciao Ciao Fault records mineral precipitation from a more meteoric-like fluid compared to the Virgin Fault, and flow through micro-fracture networks is dominated by an essentially meteoric fluid. The Ciao Ciao Fault therefore does not preserve evidence of fluids from its early history. This study indicates that the geochemical reactions that occur within a fault are controlled in part by the evolutionary stage of the fault, the fault rock permeability and the volume of fluids that pass through the fault. These results have been used to propose models for how the hydraulic properties and strength of a fault (population) evolve with time. The models produced from this study help advance our understanding of the processes that occur during the timescale of the seismic cycle, and how a population of faults will evolve in terms of mineralogy, strength and fluid flow. Such information will be of use to those involved in mineralization and mining studies, the storage of nuclear waste in crystalline rock, and earthquake prediction studies.

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Langenbruch, Cornelius [Verfasser]. « The Role of Stress Fluctuations in Seismogenic Processes : Fluid injection-induced earthquakes and scale invariance / Cornelius Langenbruch ». Berlin : Freie Universität Berlin, 2014. http://d-nb.info/1054637040/34.

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Tschaikowski, Max. « Fluid aggregations for Markovian process algebra ». Diss., Ludwig-Maximilians-Universität München, 2014. http://nbn-resolving.de/urn:nbn:de:bvb:19-171109.

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Quantitative analysis by means of discrete-state stochastic processes is hindered by the well-known phenomenon of state-space explosion, whereby the size of the state space may have an exponential growth with the number of objects in the model. When the stochastic process underlies a Markovian process algebra model, this problem may be alleviated by suitable notions of behavioural equivalence that induce lumping at the underlying continuous-time Markov chain, establishing an exact relation between a potentially much smaller aggregated chain and the original one. However, in the modelling of massively distributed computer systems, even aggregated chains may be still too large for efficient numerical analysis. Recently this problem has been addressed by fluid techniques, where the Markov chain is approximated by a system of ordinary differential equations (ODEs) whose size does not depend on the number of the objects in the model. The technique has been primarily applied in the case of massively replicated sequential processes with small local state space sizes. This thesis devises two different approaches that broaden the scope of applicability of efficient fluid approximations. Fluid lumpability applies in the case where objects are composites of simple objects, and aggregates the potentially massive, naively constructed ODE system into one whose size is independent from the number of composites in the model. Similarly to quasi and near lumpability, we introduce approximate fluid lumpability that covers ODE systems which can be aggregated after a small perturbation in the parameters. The technique of spatial aggregation, instead, applies to models whose objects perform a random walk on a two-dimensional lattice. Specifically, it is shown that the underlying ODE system, whose size is proportional to the number of the regions, converges to a system of partial differential equations of constant size as the number of regions goes to infinity. This allows for an efficient analysis of large-scale mobile models in continuous space like ad hoc networks and multi-agent systems.

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Yerlett, T. K. « Enthalpies of fluids and fluid mixtures ». Thesis, University of Bristol, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.355339.

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Idris, Muhammad Nuru. « Hydrodynamics and process modelling of fluid catalytic cracking reactors ». Thesis, University of Leeds, 2010. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.531527.

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Palabiyik, Ibrahim. « Investigation of fluid mechanical removal in the cleaning process ». Thesis, University of Birmingham, 2013. http://etheses.bham.ac.uk//id/eprint/4593/.

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The cleaning of pipework from fluids of high viscosity is a significant problem in many food and personal care industries which can cause considerable economic and environmental impact. Three stages are identified in the cleaning of straight pipes; (i) a short core removal stage of product recovery, before water breaks through the filled pipe, (ii) the 1st cleaning stage (film removal stage) when there is a continuous wavy annular film on the wall, and (iii) the 2nd cleaning stage (patch removal stage) in which the material is present as patches on the wall. The product recovery stage is found to influence the overall cleaning process. Conducting product recovery at low temperatures and high flow rates cause the formation of a wavy wall layer which leads to more rapid subsequent removal. A two step CIP protocol is proposed to decrease the environmental impact of cleaning of a viscoelastic material (toothpaste) from pipework. Applying cold water in the 1st cleaning stage and hot water in the 2nd cleaning stage results in 40 % energy saving without affecting the cleaning performance significantly compared to traditional CIP protocols used in plants. Yield stress of deposits is the key effect on the cleaning of deposits. A new dimensionless number is explored. It is physically a ratio of flow energy to the yield stress of a deposit. It has collapsed cleaning time data onto a one curve for different deposits cleaned at different velocities. It can be used to predict cleaning times of deposits or identify the governing cleaning mechanisms in cleaning. It is found that the magnitude of pressure loss in flow can be used to quantify the flow and turbulence effect on cleaning and scale up lab scale data. The results show that although fluid mechanical removal is a complex process, cleaning time of deposits can be predicted by knowing its rheology and fluid mechanical parameters of cleaning fluid.

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Bhattacharya, Sourin. « Fluid Mechanics of Micro Cold Spray Direct Write Process ». Diss., North Dakota State University, 2012. https://hdl.handle.net/10365/26552.

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Cold spray, also known as the gas dynamic spray process, was first discovered in the 1980s while doing high speed two phase wind tunnel experiments. The principle underlying this process is that if a metal particle is accelerated to a velocity above a certain critical velocity, upon impact on a substrate the particle and substrate will undergo rapid plastic deformation and form a ?splat?. This process is currently being used for coatings applications. In this process, metal particles of diameter 5 ?m to 50 ?m are accelerated to a very high velocity (>500 m/s) and are deposited on substrates. Based on principles similar to cold spray process, we have developed a novel direct write process known as the Micro Cold Spray Direct Write (MCS-DW) process. Initial results from our experimental study have shown that conductive patterns of copper, tin and aluminum can be printed on flexible and rigid substrates using this process. The smallest feature size that can be printed using this process is 50 ?m. In order to improve the deposition efficiency of the MCS-DW process, numerical studies were carried out to simulate the flow of aerosol particles through different nozzle geometries. It was found that a convergent capillary nozzle with a linear converging section of length 19 mm and a straight capillary of length 14 mm can be used to accelerate and focus silver particles of diameter 2 ?m. Copper particles of diameter 3 ?m can accelerate to their critical velocity by using a longer straight section of length 30 mm.

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Broggio, Jorge A. (Jorge Antonio) 1975. « Fluid damping with elastic medium in 3-D printing process ». Thesis, Massachusetts Institute of Technology, 1998. http://hdl.handle.net/1721.1/9569.

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Moses, Brooks. « Simulation of multiphase fluid flows using a spatial filtering process / ». May be available electronically:, 2007. http://proquest.umi.com/login?COPT=REJTPTU1MTUmSU5UPTAmVkVSPTI=&clientId=12498.

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Tao, Zhengsu. « Characteristics of the transparent fluid assisted in-process measurement method / ». View Abstract or Full-Text, 2003. http://library.ust.hk/cgi/db/thesis.pl?MECH%202003%20TAO.

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Thesis (Ph. D.)--Hong Kong University of Science and Technology, 2003.
Includes bibliographical references (leaves 106-114). Also available in electronic version. Access restricted to campus users.

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Livres sur le sujet "Fluid in the seismogenic process"

Laine, Jouko. Calculation of process response with matrices. Lappeenranta : Lappeenranta University of Technology, 1985.

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Oliemans, R. V. A., dir. Computational Fluid Dynamics for the Petrochemical Process Industry. Dordrecht : Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-011-3632-7.

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A, Oliemans R. V., dir. Computational fluid dynamics for the petrochemical process industry. Dordrecht : Kluwer Academic Publishers, 1991.

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W, Bernard John, dir. Computer control strategies for the fluid process industries. Research Triangle Park, N.C : Instrument Society of America, 1990.

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Oliemans, R. V. A. Computational Fluid Dynamics for the Petrochemical Process Industry. Dordrecht : Springer Netherlands, 1991.

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Whitehouse, Adrian Paul. Heat transfer fluid in an industrial process refrigeration system. Birmingham : University of Birmingham, 1991.

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International Symposium on Advances in Fluid Cracking Catalysts. (7th). Fluid catalytic cracking VII : Materials, methods and process innovations. Amsterdam : Elsevier, 2007.

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Joint Japan-Poland Symposium on Mining and Experimental Seismology (1999 Kyoto, Japan). Seismogenic process monitoring : Proceedings of a Joint Japan-Poland Symposium on Mining and Experimental Seismology, Kyoto, Japan, November 1999. Lisse [Netherlands] : Balkema, 2002.

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Hickin, Edward J. Channel migration at river bends : Theory, process, and engineering applications. Burnaby, B.C : Simon Fraser University, 1985.

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Łukasz, Grabowski. The mixture formation process in the gas fuelled engine. Lublin : Politechnika Lubelska, 2010.

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Chapitres de livres sur le sujet "Fluid in the seismogenic process"

Kreutzer, Michiel T., et Axel Günther. « Fluid-Fluid and Fluid-Solid Mass Transfer ». Dans Micro Process Engineering, 303–22. Weinheim, Germany : Wiley-VCH Verlag GmbH & Co. KGaA, 2013. http://dx.doi.org/10.1002/9783527631445.ch11.

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Aki, Keiiti. « Scale-dependence in Earthquake Processes and Seismogenic Structures ». Dans Microscopic and Macroscopic Simulation : Towards Predictive Modelling of the Earthquake Process, 2249–58. Basel : Birkhäuser Basel, 2000. http://dx.doi.org/10.1007/978-3-0348-7695-7_23.

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Wilhelm, Luther R., Dwayne A. Suter et and Gerald H. Brusewitz. « Fluid Flow ». Dans Food & ; Process Engineering Technology, 65–110. St. Joseph, MI : American Society of Agricultural and Biological Engineers, 2004. http://dx.doi.org/10.13031/2013.17552.

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Cui, Yan, et Xiaoling Ge. « Computer Stimulation of Air-Flowed Smashing Process ». Dans Fluid Machinery and Fluid Mechanics, 363–65. Berlin, Heidelberg : Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-540-89749-1_57.

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Carlo, Debra L., Thorne Lay, Charles J. Ammon et Jiajun Zhang. « Rupture Process of the 1995 Antofagasta Subduction Earthquake (M w = 8.1) ». Dans Seismogenic and Tsunamigenic Processes in Shallow Subduction Zones, 677–708. Basel : Birkhäuser Basel, 1999. http://dx.doi.org/10.1007/978-3-0348-8679-6_13.

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Verheggen, T. M. M. « Stability analysis of fluid-fluid interfaces ». Dans Computational Fluid Dynamics for the Petrochemical Process Industry, 119–30. Dordrecht : Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-011-3632-7_6.

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Dutta, Sujay Kumar. « Fluid Dynamics ». Dans Fundamental of Transport Phenomena and Metallurgical Process Modeling, 1–46. Singapore : Springer Nature Singapore, 2022. http://dx.doi.org/10.1007/978-981-19-2156-8_1.

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Chaves, Iván Darío Gil, Javier Ricardo Guevara López, José Luis García Zapata, Alexander Leguizamón Robayo et Gerardo Rodríguez Niño. « Fluid Handling Equipment ». Dans Process Analysis and Simulation in Chemical Engineering, 103–37. Cham : Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-14812-0_3.

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Ghasem, Nayef. « Computational Fluid Dynamics ». Dans Modeling and Simulation of Chemical Process Systems, 155–221. Boca Raton, FL : CRC Press/Taylor & Francis Group, 2018. : CRC Press, 2018. http://dx.doi.org/10.1201/b22487-4.

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Bussler, Christoph. « Process Inheritance ». Dans Notes on Numerical Fluid Mechanics and Multidisciplinary Design, 701–5. Cham : Springer International Publishing, 2002. http://dx.doi.org/10.1007/3-540-47961-9_49.

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Actes de conférences sur le sujet "Fluid in the seismogenic process"

Hui, Gang, Shengnan Chen et Fei Gu. « Coupled Poroelastic Modeling to Characterize the 4.18-Magnitude Earthquake Due to Hydraulic Fracturing in the East Shale Basin of Western Canada ». Dans SPE Reservoir Simulation Conference. SPE, 2021. http://dx.doi.org/10.2118/203921-ms.

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Abstract Recently, the elevated levels of seismicity activities in Western Canada have been demonstrated to be linked to hydraulic fracturing operations that developed unconventional resources. The underlying triggering mechanisms of hydraulic fracturing-induced seismicity are still uncertain. The interactions of well stimulation and geology-geomechanical-hydrological features need to be investigated comprehensively. The linear poroelasticity theory was utilized to guide coupled poroelastic modeling and to quantify the physical process during hydraulic fracturing. The integrated analysis is first conducted to characterize the mechanical features and fluid flow behavior. The finite-element simulation is then conducted by coupling Darcy's law and solid mechanics to quantify the perturbation of pore pressure and poroelastic stress in the seismogenic fault zone. Finally, the Mohr-coulomb failure criterion is utilized to determine the spatial-temporal faults activation and reveal the trigger mechanisms of induced earthquakes. The mitigation strategy was proposed accordingly to reduce the potential seismic hazards near this region. A case study of ML 4.18 earthquake in the East Shale Basin was utilized to demonstrate the applicability of the coupled modeling and numerical simulation. Results showed that one inferred fault cut through the Duvernay formation with the strike of NE20°. The fracture half-length of two wells owns an average value of 124 m. The brittleness index deriving from the velocity logging data was estimated to be a relatively higher value in the Duvernay formation, indicating a geomechanical bias of stimulated formation for the fault activation. The coupled poroelastic simulation was conducted, showing that the hydrologic connection between seismogenic faults and stimulated well was established by the end of the 38th stage completion for the east horizontal well. The simulated coulomb failure stress surrounding the fault reached a maximum of 4.15 MPa, exceeding the critical value to cause the fault slip. Hence the poroelastic effects on the inferred fault were responsible for the fault activation and triggered the subsequent ML 4.18 earthquake. It is essential to optimize the stimulation site selection near the existing faults to reduce risks of future seismic hazards near the East Shale Basin.

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Shapiro, S. A., C. Dinske et C. Langenbruch. « Quantification of fluid-induced microseismic activity using seismogenic index ». Dans Third Passive Seismic Workshop - Actively Passive 2011. Netherlands : EAGE Publications BV, 2011. http://dx.doi.org/10.3997/2214-4609.20145316.

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Fagereng, Ake, Johann F. A. Diener, Francesca Meneghini et C. Harris. « FLUID RELEASE AND DEFORMATION AT, AND BEYOND, THE BASE OF THE MEGATHRUST SEISMOGENIC ZONE ». Dans GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-297790.

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Hartman, Sean, Scott R. Paterson et Gregory J. Holk. « FAULT VALVE AND SUCTION PUMP FLUID FLOW MECHANISMS AT THE SEISMOGENIC BASE OF A DYING ARC ». Dans 112th Annual GSA Cordilleran Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016cd-274159.

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Dinske, Carsten, et Serge Shapiro. « Performance test of the Seismogenic index model for forecasting magnitude distributions of fluid-injection-induced seismicity ». Dans SEG Technical Program Expanded Abstracts 2016. Society of Exploration Geophysicists, 2016. http://dx.doi.org/10.1190/segam2016-13958126.1.

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Shapiro, S., et C. Dinske. « Fault Cohesion, Stress Drop and Seismogenic Index of Seismicity Induced by Long-Term Fluid Productions or Injections ». Dans 82nd EAGE Annual Conference & Exhibition. European Association of Geoscientists & Engineers, 2020. http://dx.doi.org/10.3997/2214-4609.202010286.

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« A process for industry certification of physical simulation codes ». Dans Fluid Dynamics Conference. Reston, Virigina : American Institute of Aeronautics and Astronautics, 1994. http://dx.doi.org/10.2514/6.1994-2235.

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Faehnle, Oliver W., et Hedser H. van Brug. « Fluid jet polishing : removal process analysis ». Dans Optical Systems Design and Production, sous la direction de Roland Geyl et Jonathan Maxwell. SPIE, 1999. http://dx.doi.org/10.1117/12.360189.

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Dvorak, Todd, Linda Malone et Robert Hoekstra. « Statistical Process Control and Design of Experiment Process Improvement Methods for the Powertrain Laboratory ». Dans SAE Powertrain & Fluid Systems Conference & Exhibition. 400 Commonwealth Drive, Warrendale, PA, United States : SAE International, 2003. http://dx.doi.org/10.4271/2003-01-3208.

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Araya, Guillermo G. « Shedding Light into the Quasi-Laminarization Process ». Dans 46th AIAA Fluid Dynamics Conference. Reston, Virginia : American Institute of Aeronautics and Astronautics, 2016. http://dx.doi.org/10.2514/6.2016-3188.

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Rapports d'organisations sur le sujet "Fluid in the seismogenic process"

Carter, S. D., D. N. Taulbee, T. L. Robl et J. C. Hower. The development of an integrated multistage fluid bed retorting process. [Kentort II process]. Office of Scientific and Technical Information (OSTI), août 1992. http://dx.doi.org/10.2172/6869068.

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Carter, S., A. Vego, D. Taulbee et J. Stehn. The development of an integrated multistage fluid bed retorting process. [KENTORT II process--50-lb/hr]. Office of Scientific and Technical Information (OSTI), janvier 1992. http://dx.doi.org/10.2172/5092907.

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Carter, S., J. Stehn, A. Vego et D. Taulbee. The development of an integrated multistage fluid bed retorting process. [Kentort II process--50-lb/hr]. Office of Scientific and Technical Information (OSTI), mai 1992. http://dx.doi.org/10.2172/7310245.

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Fernando, H. J. Laboratory Simulation of Fluid Dynamical Process Related to Winter Arctic Leads. Fort Belvoir, VA : Defense Technical Information Center, septembre 1991. http://dx.doi.org/10.21236/ada252266.

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Oh, C. H. Alternate fluid to improve energy efficiency of supercritical water oxidation process. Office of Scientific and Technical Information (OSTI), mars 1996. http://dx.doi.org/10.2172/236239.

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Panicker, Nithin, Rajneesh Chaudhary, Marco Delchini, Vivek Rao et Prashant Jain. Computational Fluid Dynamics Simulations to Support Efficiency Improvements in Aluminum Smelting Process. Office of Scientific and Technical Information (OSTI), décembre 2021. http://dx.doi.org/10.2172/1844874.

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Carter, S., J. Stehn et A. Vego. The development of an integrated multistage fluid bed retorting process. Quarterly report, October--December 1993. Office of Scientific and Technical Information (OSTI), février 1994. http://dx.doi.org/10.2172/10165383.

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Jain, Prashant, Min-Tsung Kao, Vivek Rao, Emilian Popov, Duy Thien Nguyen, Jamie Wilson, Vittorio Badalassi et Dave Pointer. Computational Fluid Dynamics Modeling to Simulate a Combined Reforming Process for Syngas and Hydrogen Production. Office of Scientific and Technical Information (OSTI), novembre 2021. http://dx.doi.org/10.2172/1838964.

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Tse, P., et G. Vandegrift. Development of supercritical fluid chromatography for analysis of TRUEX process solvents. [N,N-diisobutylcarbamoylmethylphosphine oxide (CMPO)]. Office of Scientific and Technical Information (OSTI), août 1989. http://dx.doi.org/10.2172/5534908.

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Carter, S. D., D. N. Taulbee, J. L. Stehn, A. Vego et T. L. Robl. The development of an integrated multistaged fluid-bed retorting process. Final report, September 1990--August 1994. Office of Scientific and Technical Information (OSTI), février 1995. http://dx.doi.org/10.2172/206399.

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