Relevant bibliographies by topics / Pressure inversion

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Pressure inversion'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Pressure inversion"

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Egger, Joseph, Klaus-Peter Hoinka, and Thomas Spengler. "Inversion of Potential Vorticity Density." Journal of the Atmospheric Sciences 74, no. 3 (2017): 801–7. http://dx.doi.org/10.1175/jas-d-16-0133.1.

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Abstract Inversion of potential vorticity density with absolute vorticity and function η is explored in η coordinates. This density is shown to be the component of absolute vorticity associated with the vertical vector of the covariant basis of η coordinates. This implies that inversion of in η coordinates is a two-dimensional problem in hydrostatic flow. Examples of inversions are presented for (θ is potential temperature) and (p is pressure) with satisfactory results for domains covering the North Pole. The role of the boundary conditions is investigated and piecewise inversions are performe
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Nygård, Tiina, Teresa Valkonen, and Timo Vihma. "Antarctic Low-Tropospheric Humidity Inversions: 10-Yr Climatology." Journal of Climate 26, no. 14 (2013): 5205–19. http://dx.doi.org/10.1175/jcli-d-12-00446.1.

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Abstract Humidity inversions are nearly permanently present in the coastal Antarctic atmosphere. This is shown based on an investigation of statistical characteristics of humidity inversions at 11 Antarctic coastal stations using radiosonde data from the Integrated Global Radiosonde Archive (IGRA) from 2000 to 2009. The humidity inversion occurrence was highest in winter and spring, and high atmospheric pressure and cloud-free conditions generally increased the occurrence. A typical humidity inversion was less than 200 m deep and 0.2 g kg−1 strong, and a typical humidity profile contained seve
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Nygård, T., T. Valkonen, and T. Vihma. "Characteristics of Arctic low-tropospheric humidity inversions based on radio soundings." Atmospheric Chemistry and Physics 14, no. 4 (2014): 1959–71. http://dx.doi.org/10.5194/acp-14-1959-2014.

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Abstract. Humidity inversions have a high potential importance in the Arctic climate system, especially for cloud formation and maintenance, in wide spatial and temporal scales. Here we investigate the climatology and characteristics of humidity inversions in the Arctic, including their spatial and temporal variability, sensitivity to the methodology applied and differences from the Antarctic humidity inversions. The study is based on data of the Integrated Global Radiosonde Archive (IGRA) from 36 Arctic stations between the years 2000 and 2009. The results indicate that humidity inversions ar
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Nygård, T., T. Valkonen, and T. Vihma. "Characteristics of Arctic low-tropospheric humidity inversions based on radio soundings." Atmospheric Chemistry and Physics Discussions 13, no. 8 (2013): 22575–605. http://dx.doi.org/10.5194/acpd-13-22575-2013.

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Abstract. Humidity inversions have a high potential importance in the Arctic climate system, especially for cloud formation and maintenance, in wide spatial and temporal scales. Here we investigate the climatology and characteristics of humidity inversions in the Arctic, including their spatial and temporal variability, sensitivity to the methodology applied and differences from the Antarctic humidity inversions. The study is based on data of the Integrated Global Radiosonde Archive (IGRA) from 36 Arctic stations between the years 2000–2009. The results indicate that humidity inversions are ne
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Nodzu, Masato I., Shin-Ya Ogino, and Jun Matsumoto. "Development and Decay Processes of Dual Inversion Layers in Winter over the Northwest Coast of the South China Sea." Journal of Climate 31, no. 3 (2018): 1245–66. http://dx.doi.org/10.1175/jcli-d-16-0907.1.

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Abstract Inversion layers in the lower troposphere appear centered at two heights, 1.5 and 4 km, over the northwestern coast of the South China Sea in late boreal winter. The mechanisms of these dual inversion layers are investigated with thermal budget and composite analyses of the JRA-55 dataset. The thermal budget analysis classifies inversion layers between the levels of 700 and 600 hPa into two types. One type is related to high pressure moving southward along the eastern edge of the Tibetan Plateau; the arrival of the high coincides with subsidence that warms the 600-hPa level more stron
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Hanson, Jonathan M. "Nonlinear Inversion of Pressure-Transient Data." SPE Formation Evaluation 1, no. 04 (1986): 355–62. http://dx.doi.org/10.2118/12848-pa.

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Haskvitz, Esther M., and William P. Hanten. "Blood Pressure Response to Inversion Traction." Physical Therapy 66, no. 9 (1986): 1361–64. http://dx.doi.org/10.1093/ptj/66.9.1361.

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Su, Xiao Xiang, Y. D. Gu, Guo Qing Ruan, and Xue Jun Ren. "Forefoot Plantar Pressure Distribution Character during Inversion Position." Key Engineering Materials 474-476 (April 2011): 666–68. http://dx.doi.org/10.4028/www.scientific.net/kem.474-476.666.

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This study analyzed the plantar pressure distribution character as the foot position between normal to inversion. Eight healthy male volunteers have participated in the test with the foot position from normal to 20 inversion angles which controlled by wedges. The results of this test showed that the centre of the pressure was clearly transferred from centre to lateral side when the foot position was changed from normal to inversion. In addition, the contact area varied largely between the normal and inversion condition, but changed a little between two inversion loading situations. The finding
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Egger, Joseph, and Klaus-Peter Hoinka. "Potential Temperature and Potential Vorticity Inversion: Complementary Approaches." Journal of the Atmospheric Sciences 67, no. 12 (2010): 4001–16. http://dx.doi.org/10.1175/2010jas3532.1.

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Abstract Given the distribution of one atmospheric variable, that of nearly all others can be derived in balanced flow. In particular, potential vorticity inversion (PVI) selects potential vorticity (PV) to derive pressure, winds, and potential temperature θ. Potential temperature inversion (PTI) starts from available θ fields to derive pressure, winds, and PV. While PVI has been applied extensively, PTI has hardly been used as a research tool although the related technical steps are well known and simpler than those needed in PVI. Two idealized examples of PTI and PVI are compared. The 40-yr
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Wypych, Agnieszka, and Bogdan Bochenek. "Vertical Structure of Moisture Content over Europe." Advances in Meteorology 2018 (July 12, 2018): 1–13. http://dx.doi.org/10.1155/2018/3940503.

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The vertical structure of water vapor content in the atmosphere strongly affects the amount of solar radiation reaching the Earth’s surface and processes associated with the formation of clouds and atmospheric precipitation. The purpose of this study was to assess the vertical differentiation of water vapor over Europe on a seasonal basis and also to evaluate the role of atmospheric circulation in changes therein. Daily values of specific humidity (SHUM) for the time period 1981–2015 were obtained from pressure levels available from ECMWF Era-Interim reanalysis data and used in the study. Eigh
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Dissertations / Theses on the topic "Pressure inversion"

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Ribeiro, Christophe. "Time-lapse seismic inversion for pressure and saturation in clastic reservoirs." Thesis, Heriot-Watt University, 2006. http://hdl.handle.net/10399/189.

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Hodgson, Neil. "Inversion for reservoir pressure change using overburden strain measurements determined from 4D seismic." Thesis, Heriot-Watt University, 2009. http://hdl.handle.net/10399/2320.

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When significant pore pressure changes occur because of production from a hydrocarbon reservoir the rocks both inside and outside of the reservoir deform. This deformation results in traveltime changes between reflection events on timelapse seismic data, because the distance between reflection events is altered and the seismic velocity changes with the strain. These traveltime differences are referred to as time-lapse time shifts. In this thesis, time-lapse time shifts observed in the overburden are used as an input to a linear inversion for reservoir pressure. Measurements from the overburden
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Wilson, Adam. "Theory and methods of frequency-dependent AVO Inversion." Thesis, University of Edinburgh, 2010. http://hdl.handle.net/1842/4740.

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Amplitude-versus-offset, AVO, approximations allow the estimation of various properties from pre-stack seismic gathers. Recently it has been suggested that fluid mobility is a controlling factor in pore pressure equalisation and can result in anomalous velocity dispersion in the seismic bandwidth. However, current approximations all assume an elastic subsurface and are unable to account for velocity dispersion. I have applied existing methodologies to a real dataset to qualitatively detect and interpret spectral amplitude anomalies. Three areas had AVO and spectral signature consistent with fr
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Cochain, Jérémy. "Numerical and experimental study of misaligned and wavy mechanical face seals operating under pressure pulses and pressure inversions." Thesis, Poitiers, 2018. http://www.theses.fr/2018POIT2271/document.

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Les garnitures mécaniques sont utilisées dans de multiples applications pour réaliser l'étanchéité autour d'arbres en rotation. Ces composants peuvent fonctionner efficacement pendant plusieurs années en conditions stables, mais leur durée de vie est significativement réduite lorsque les conditions varient. L'objectif de ce travail de recherche est de développer et d’utiliser un banc d'essais et code de calcul pour étudier l'impact de pulsations de pression, d’inversions de pression et du chargement dynamique résultant sur les performances de garnitures mécaniques ayant des faces mésalignées e
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Carter, Robert Hansbrough. "Characterizing the Mechanical Properties of Composite Materials Using Tubular Samples." Diss., Virginia Tech, 2001. http://hdl.handle.net/10919/28453.

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Application of composite materials to structures has presented the need for engineering analysis and modeling to understand the failure mechanisms. Unfortunately, composite materials, especially in a tubular geometry, present a situation where it is difficult to generate simple stress states that allow for the characterization of the ply-level properties. The present work focuses on calculating the mechanical characteristics, both on a global and local level, for composite laminate tubes. Global responses to axisymmetric test conditions (axial tension, torsion, and internal pressure) are me
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Cederholm, Alex. "Homogeneous models of anechoic rubber coatings." Doctoral thesis, KTH, Aeronautical and Vehicle Engineering, 2003. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-3611.

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Rocha, Douglas Martins. "Estudo dos efeitos da injeção de água e de gás sobre a redução do gradiente de pressão total no escoamento vertical ascendente de óleos viscosos." Universidade de São Paulo, 2016. http://www.teses.usp.br/teses/disponiveis/18/18147/tde-07062017-155542/.

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A maioria dos poços de petróleo offshore explorados no Brasil utilizam a técnica de elevação artificial de petróleo conhecida como gas-lift. Mais importante, há previsão de uso intensivo dessa técnica nos poços do pré-sal, sob pressões extremas e condições operacionais ainda não compreendidas completamente. O efeito de injetar gás em um escoamento em tubo vertical é o decréscimo do componente gravitacional do gradiente de pressão total. Por outro lado, os óleos pesados (10 < ºAPI < 19) são viscosos e difíceis de escoar. Em certas ocasiões, este tipo de petróleo não é extraído pela falta de tec
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Manivannan, Sivaprasath. "Measuring permeability vs depth in the unlined section of a wellbore using the descent of a fluid column made of two distinct fluids : inversion workflow, laboratory & in-situ tests." Thesis, Université Paris-Saclay (ComUE), 2018. http://www.theses.fr/2018SACLX086/document.

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Dans les puits de production d’eau, de pétrole, de gaz et de chaleur géothermique, ou dans les puits d’accès à un stockage d’hydrocarbures, il est précieux de connaître la perméabilité de la formation ou de sa couverture en fonction de la profondeur, soit pour améliorer le modèle de réservoir, soit pour choisir les zones dans lesquelles procéder à des opérations spéciales.On propose une technique qui consiste à balayer la hauteur du découvert par une interface entre deux liquides de viscosités très contrastées. Le débit total qui pénètre la formation à chaque instant est ainsi une fonction de
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Larson, Ilene L. "The effect of inversion on blood pressure, heart rate, and breathing rate." 1986. http://catalog.hathitrust.org/api/volumes/oclc/15020818.html.

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Thesis (M.S.)--University of Wisconsin--Madison, 1986.<br>Typescript. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 79-83).
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Bui, Hoa Q. "The Asperity-deformation Model Improvements and Its Applications to Velocity Inversion." 2009. http://hdl.handle.net/1969.1/ETD-TAMU-2009-05-425.

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Quantifying the influence of pressure on the effective elastic rock properties is important for applications in rock physics and reservoir characterization. Here I investigate the relationship between effective pressure and seismic velocities by performing inversion on the laboratory-measured data from a suite of clastic, carbonate and igneous rocks, using different analytic and discrete inversion schemes. I explore the utility of a physical model that models a natural fracture as supported by asperities of varying heights, when an effective pressure deforms the tallest asperities, bringing th
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Books on the topic "Pressure inversion"

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N, Lyons Suzanne, and United States. National Aeronautics and Space Administration., eds. Inversion of crater morphometric data to gain insight on the cratering process. National Aeronautics and Space Administration, 1998.

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Dunlop, Storm. 1. The atmosphere. Oxford University Press, 2017. http://dx.doi.org/10.1093/actrade/9780199571314.003.0001.

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‘The atmosphere’ describes the different layers of the atmosphere and the boundaries between them—troposphere, tropopause, stratosphere, mesopause, mesosphere, ionosphere, and thermosphere—and explains why temperature generally declines with increased altitude: a decrease in pressure causes a parcel of air to expand and cool. The change in temperature with altitude is known as the lapse rate and any decrease or increase in lapse rate is known as an inversion. The inversion at the top of the troposphere is a major feature, always present in the atmosphere. The measuring and charting of atmosphe
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Book chapters on the topic "Pressure inversion"

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Kompanichenko, Vladimir N. "Changeability of Pressure, Temperature, and Concentrations of Components in the Explored Hydrothermal Systems." In Thermodynamic Inversion. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-53512-8_9.

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Masumoto, Kiyoshi, and Mario Valle. "Confidence Intervals of Hydraulic Properties Estimated by Highly Efficient Numerical Inversion with Pressure Change Rate Matching." In Groundwater Updates. Springer Japan, 2000. http://dx.doi.org/10.1007/978-4-431-68442-8_62.

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Ouadfeul, Sid-Ali, and Leila Aliouane. "Pre-drill Pore Pressure Estimation in Shale Gas Reservoirs Using Seismic Genetic Inversion: Application to Barnett Shale (USA)." In On Significant Applications of Geophysical Methods. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01656-2_37.

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Baba, Toshitaka, Phil R. Cummins, Hong Kie Thio, and Hiroaki Tsushima. "Validation and Joint Inversion of Teleseismic Waveforms for Earthquake Source Models Using Deep Ocean Bottom Pressure Records: A Case Study of the 2006 Kuril Megathrust Earthquake." In Tsunami Science Four Years after the 2004 Indian Ocean Tsunami. Birkhäuser Basel, 2009. http://dx.doi.org/10.1007/978-3-0346-0064-4_4.

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Dewey, John M. "The Rankine–Hugoniot Equations: Their Extensions and Inversions Related to Blast Waves." In Shock Wave and High Pressure Phenomena. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-70831-7_2.

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"Pollution of the Atmosphere." In Environmental Toxicology, edited by Sigmund F. Zakrzewski. Oxford University Press, 2002. http://dx.doi.org/10.1093/oso/9780195148114.003.0015.

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The earth’s atmosphere consists of 78% (by volume) of N2; 21% O2; about 0.033% CO2; trace amounts of noble gases, NOx, and CH3; and variable amounts of water vapor. At sea level, the amount of water vapor may vary from 0.5 g per kg of air in polar regions to more then 20 g per kg in the tropics. The standard atmosphere is a theoretical set of data that serves as a reference point for calculation of atmospheric changes due to the weather. The values are calculated for sea level conditions and correspond to a pressure of 760 mm of mercury (92.29 in., 1013.25 mbar), an air density of 1.22 kg/m3, and a temperature of 15°C (59 °F). The composition of the air within the troposphere, which is the lowest layer of the atmosphere, does not change with altitude; however, the pressure and temperature decrease with altitude. The relationship between altitude and pressure in the standard atmosphere is shown in Figure 10.1, and the relationship between altitude and temperature is shown in Figure 10.2. The rate of decrease of temperature with altitude (6.49 °C per km) is referred to as the ‘‘standard lapse rate’’. This rate is a strictly theoretical average value because the actual lapse rate varies depending on the weather. Because the air density is proportional to the pressure and inversely proportional to the temperature, it changes at the same rate as the pressure does. The atmosphere is divided into troposphere, stratosphere, mesosphere, and ionosphere. As shown in this figure, the division is based on temperature inversions that occur at the higher altitudes; the altitudes of these inversions vary with the season and with the geographic latitude. Although the general shape of the curves remains the same for all latitudes, the altitudes of the inversions are higher over the equator and lower over the poles; the curves presented in Figure 10.3 refer to middle latitudes. The boundary areas at each temperature inversion are called tropopause, stratopause, and mesopause, respectively. Pollution of the atmosphere is generally the least appreciated of all environmental issues.
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Hilton, Andrew. "Pericardial effusion and cardiac tamponade." In Oxford Textbook of Advanced Critical Care Echocardiography, edited by Anthony McLean, Stephen Huang, and Andrew Hilton. Oxford University Press, 2020. http://dx.doi.org/10.1093/med/9780198749288.003.0012.

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Cardiac tamponade results from an increase in pericardial pressure that is sufficient to impede cardiac filling, resulting in high venous filling pressures, low cardiac output, and end-organ hypoperfusion. Most often this is due to the accumulation of a pericardial effusion though there are other possible causes. Patients usually present with features of cardiogenic shock, though some may initially be normotensive or hypertensive. Echocardiography can diagnose the presence of pericardial disease, especially pericardial effusion. Any associated haemodynamic sequelae can often be inferred by static and dynamic two-dimensional echocardiographic and Doppler measured intracardiac flow velocity abnormalities. These include atrial and ventricular wall inversion or collapse, and increased respiratory phasic flow velocities in tricuspid and mitral inflow. The concepts of transmural pressure, pericardial restraint, interventricular dependence, and cardiorespiratory interactions underpin the understanding and limitations of these echocardiographic findings. However, the impact of positive pressure ventilation remains problematic with respect to the interpretation of Doppler-derived intracardiac flow velocity variation. Echocardiography can also identify conditions that may confound the interpretation of accepted echocardiographic criteria (e.g. right ventricular hypertrophy, hypovolaemia, isolated chamber compression after cardiac surgery) and diagnose conditions that may mimic or exaggerate tamponade pathophysiology such as large compressive pleural effusion. Finally, echocardiographic criteria can aid stratification of the risk of tamponade in patients with pericardial effusion, and if necessary, guide percutaneous pericardiocentesis.
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Whiteman, C. David. "Diurnal Mountain Winds." In Mountain Meteorology. Oxford University Press, 2000. http://dx.doi.org/10.1093/oso/9780195132717.003.0019.

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Diurnal mountain winds develop over complex topography of all scales, from small hills to large mountain massifs and are characterized by a reversal of wind direction twice per day. As a rule, winds flow upslope, up-valley, and from the plain to the mountain massif during daytime. During nighttime, they flow downslope, down-valley, and from the mountain massif to the plain. Diurnal mountain winds are strongest when skies are clear and winds aloft are weak. Diurnal mountain winds are produced by horizontal temperature differences that develop daily in complex terrain. The resulting horizontal pressure differences cause winds near the surface of the earth to blow from areas with lower temperatures and higher pressures toward areas with higher temperatures and lower pressures. The circulations are closed by return, or compensatory, flows higher in the atmosphere. Four wind systems comprise the mountain wind system, which carries air into a mountain massif at low levels during daytime and out of a mountain massif during nighttime. The slope wind system (upslope winds and downslope winds) is driven by horizontal temperature contrasts between the air over the valley sidewalls and the air over the center of the valley. The along-valley wind system (up-valley winds and down-valley winds) is driven by horizontal temperature contrasts along a valley’s axis or between the air in a valley and the air over the adjacent plain. The cross-valley wind system results from horizontal temperature differences between the air over one valley sidewall and the air over the opposing sidewall, producing winds that blow perpendicular to the valley axis and toward the more strongly heated sidewall. The mountain-plain wind system results from horizontal temperature differences between the air over a mountain massif and the air over the surrounding plains, producing large-scale winds that blow up or down the outer slopes of a mountain massif. The mountain-plain circulation and its upper level return flow are not confined by the topography but are carried over deep layers of the atmosphere above the mountain slopes. Because diurnal mountain winds are driven by horizontal temperature differences, the regular evolution of the winds in a given valley is closely tied to the thermal structure of the atmospheric boundary layer within the valley, which is characterized by a diurnal cycle of buildup and breakdown of a temperature inversion.
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Anderson, Greg M., and David A. Crerar. "Applications to Simple Systems." In Thermodynamics in Geochemistry. Oxford University Press, 1993. http://dx.doi.org/10.1093/oso/9780195064643.003.0012.

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Thus far we have developed just about all the thermodynamic concepts required by Earth scientists with the exception of those needed to deal with solutions. Since all naturally occurring substances are solutions of one kind or another (although some can usefully be treated as pure substances), this is quite an important limitation, and we will proceed to discuss the treatment of solutions in Chapter 10. However, a great deal can be done with the thermodynamics of pure systems, and in this chapter we discuss a couple of applications of the concepts so far developed which are of particular interest to Earth scientists—the thermal effects associated with adiabatic volume changes, and the T-P phase diagrams of pure minerals. All systems experience a change in volume in response to changes in pressure. We have discussed this mostly from the point of view of the work accomplished by isobaric volume changes in Chapter 4, but it is even more informative to consider the temperature changes accompanying volume changes. The best way to do this is to consider only cases uncomplicated by heat entering or leaving the system, i.e., adiabatic processes. Such processes, although yet another "hypothetical limiting case," serve as useful end-members in considering actual processes in real systems. The most familiar everyday example is the hand-held bicycle pump, which most cyclists at least know gets quite warm during pumping (compressing air). This process, while not strictly adiabatic (bicycle pumps are not well insulated) is sufficient to show that volume changes can be associated with temperature changes, and it is not difficult to see in this case why—a great deal of energy in the form of work is being added to the gas, and some of it is being used to warm the gas. It seems reasonable to suppose, too, that by reversing the process—suddenly expanding the gas—it would experience a temperature decrease. This much may seem intuitively reasonable, perhaps even obvious. What is not so obvious is the fact, first investigated by Joule and Thompson in 1853, that some substances do not warm but cool during compression, and that in fact all substances have a range of conditions where they warm on expansion and another where they cool on expansion. When the expansions are at constant enthalpy, these two ranges are separated by the Joule-Thompson inversion curve.
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Rees, Elliott, and George Kirov. "The Role of Copy Number Variation in Psychiatric Disorders." In Psychiatric Genetics. Oxford University Press, 2018. http://dx.doi.org/10.1093/med/9780190221973.003.0006.

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Copy number variants (CNVs) are deletions, duplications, inversions, or translocations of large DNA segments. They can play a significant role in human disease. Thirteen CNVs have received strong statistical support for involvement in schizophrenia. They are all rare in cases (&lt;1%), much rarer among controls, and have high odds ratios (ORs) for causing disease. The same CNVs also increase risk for autism spectrum disorders, developmental delay, and medical/physical comorbidities. The penetrance of these CNVs for any disorder is relatively high, ranging from 10% for 15q11.2 deletions to nearly 100% for deletions at 22q11.2. Strong selection pressure operates against carriers of these CNVs. Most of these are formed by non-allelic homologous recombination (NAHR), which leads to high mutation rates, thus maintaining the rates of these CNVs in the general population, despite the strong selection forces.
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Conference papers on the topic "Pressure inversion"

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Hu, Jinqiu, Laibin Zhang, Ronghan Wang, and Qingchun Ma. "Fire Accident Inversion Method Base on STAMP and Topological Network for LNG Depot." In ASME 2018 Pressure Vessels and Piping Conference. American Society of Mechanical Engineers, 2018. http://dx.doi.org/10.1115/pvp2018-85113.

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Natural Gas is becoming an important energy source option and the capacity of the world to produce it is surging. Natural gas is usually liquefied for shipping and storage. Fire and explosion are among the most dangerous accidents in facilities at LNG Depot; especially pool fire is the most frequent incidents. At the same time the chain of accidents may lead to extremely severe consequences. In order to avoid such calamity a detail study on accident inversion technology is required to save human lives and prohibit the destruction of LNG Depot. In this thesis a topological network based fire ac
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Zhou, Changxi, and Gerard T. Schuster. "Elastic waveform inversion of pressure field data." In SEG Technical Program Expanded Abstracts 1995. Society of Exploration Geophysicists, 1995. http://dx.doi.org/10.1190/1.1887387.

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Tinivella, U., J. M. Carcione, and H. B. Helle. "Estimation of pore pressure by AVO inversion." In SEG Technical Program Expanded Abstracts 2001. Society of Exploration Geophysicists, 2001. http://dx.doi.org/10.1190/1.1816580.

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Gulrajani, Sunil N., Mark G. Mack, and Jack Elbel. "Pressure History Inversion for Interpretation of Fracture Treatments." In SPE Annual Technical Conference and Exhibition. Society of Petroleum Engineers, 1996. http://dx.doi.org/10.2118/36439-ms.

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Booth, R. J. S., K. L. Morton, M. Onur, and F. J. Kuchuk. "Grid-based Inversion of Pressure Transient Test Data." In 12th European Conference on the Mathematics of Oil Recovery. EAGE Publications BV, 2010. http://dx.doi.org/10.3997/2214-4609.20144985.

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Fang*, Liu, Liu Zhibin, Wang Zhihong, Jiao Zhenhua, and Chen Jianjun. "Application of geostatistics inversion in formation pressure prediction." In SPG/SEG 2016 International Geophysical Conference, Beijing, China, 20-22 April 2016. Society of Exploration Geophysicists and Society of Petroleum Geophysicists, 2016. http://dx.doi.org/10.1190/igcbeijing2016-203.

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Rozhenkov, E. A., D. A. Danko, A. V. Shubin, and V. I. Ryzhkov. "Pore Pressure Prediction Based on Seismic Amplitude Inversion." In Geomodel 2021. European Association of Geoscientists & Engineers, 2021. http://dx.doi.org/10.3997/2214-4609.202157125.

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Debec, P. "Rock Physics Model Inversion for Pore Pressure Prediction in Clastic Reservoirs." In First EAGE Workshop on Pore Pressure Prediction. EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201700066.

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9

R. Soleymani, Hamid, SeyedMohsen SeyedAli, and Mohammad A. Riahi. "Pore Pressure Prediction Using Seismic Inversion and Velocity Analysis." In GEO 2010. European Association of Geoscientists & Engineers, 2010. http://dx.doi.org/10.3997/2214-4609-pdb.248.348.

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10

Lang, Xiaozheng, and Dario Grana. "Bayesian pressure-saturation inversion of time-lapse seismic data." In SEG Technical Program Expanded Abstracts 2018. Society of Exploration Geophysicists, 2018. http://dx.doi.org/10.1190/segam2018-2996356.1.

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Reports on the topic "Pressure inversion"

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Sun, Alexander. Pressure-Based Inversion and Data Assimilation System (PIDAS) for CO2 Leakage Detection. Office of Scientific and Technical Information (OSTI), 2018. http://dx.doi.org/10.2172/1494374.

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