The "Heat-Pipe" Effect in Vapor-Dominated Geothermal Systems

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Book Synopsis The "Heat-Pipe" Effect in Vapor-Dominated Geothermal Systems by :

Download or read book The "Heat-Pipe" Effect in Vapor-Dominated Geothermal Systems written by and published by . This book was released on 1977 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt: White, Muffler, and Truesdell (1971) and Truesdell and White (1973) developed a conceptual model of transport in vapor-dominated geothermal zones. The main theme of the model is that coexisting liquid and vapor phases form a counterflowing convection system similar to that observed in a heat pipe (Dunn and Reay, 1976). It is hypothesized that water evaporates from a deep water table, passes upward through the formation, and condenses at an impermeable cap rock, effectively transferring the latent heat of boiling through the formation. The liquid water then percolates downward, completing the cycle. The physics involved in the flow system is illustrated in an analysis of an idealized one-dimensional, homogeneous, 2 km deep vapor-dominated zone which is bounded below by a water table which has a temperature of 236°C. Flow of water and steam in the system is assumed to be described by Darcy's law for unsaturated porous materials. The liquid water potential, defined as the Gibbs free energy per unit volume of water, is used in place of the liquid pressure in the equation for water because flow in a highly unsaturated medium is to be considered. Comparison of figures 2 and 4 illustrates that the liquid saturation in a two-phase convection system can be much higher than that predicted from a static pressure analysis. As a result, the "vapor pressure lowering" effect expected in a static system disappears. The decrease in P{sub V} at the top of figure 4 is caused by temperature decrease; the relative vapor pressure in the dynamic system is above 99%. However, the permeability used in this example is very low. At higher permeabilities the condensing steam drains out of the system much faster, and the saturation approaches the static profile. 5 refs., 4 figs.

The Origin of High-temperature Zones in Vapor-dominated Geothermal Systems

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Book Synopsis The Origin of High-temperature Zones in Vapor-dominated Geothermal Systems by :

Download or read book The Origin of High-temperature Zones in Vapor-dominated Geothermal Systems written by and published by . This book was released on 1991 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt: Vapor-dominated geothermal systems are proposed to originate by downward extension (by the ''heat pipe'' mechanism) into hot dry fractured rock above a large cooling igneous intrusion. High temperature zones found by drilling are shallow parts of the original hot dry rock where the penetration of the vapor reservoir was limited, and hot dry rock may extend under much of these reservoirs. An earlier hot water geothermal system may have formed during an early phase of the heating episode.

Simulation of Steam Transport in Vapor-dominated Geothermal Reservoirs

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ISBN 13 :
Total Pages : 96 pages
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Book Synopsis Simulation of Steam Transport in Vapor-dominated Geothermal Reservoirs by : Geological Survey (U.S.)

Download or read book Simulation of Steam Transport in Vapor-dominated Geothermal Reservoirs written by Geological Survey (U.S.) and published by . This book was released on 1976 with total page 96 pages. Available in PDF, EPUB and Kindle. Book excerpt:

Effects of Capillarity and Vapor Adsorption in the Depletion of Vapor-dominated Geothermal Reservoirs

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Total Pages : 10 pages
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Book Synopsis Effects of Capillarity and Vapor Adsorption in the Depletion of Vapor-dominated Geothermal Reservoirs by :

Download or read book Effects of Capillarity and Vapor Adsorption in the Depletion of Vapor-dominated Geothermal Reservoirs written by and published by . This book was released on 1992 with total page 10 pages. Available in PDF, EPUB and Kindle. Book excerpt: Vapor-dominated geothermal reservoirs in natural (undisturbed) conditions contain water as both vapor and liquid phases. The most compelling evidence for the presence of distributed liquid water is the observation that vapor pressures in these systems are close to saturated vapor pressure for measured reservoir temperatures (White et al., 1971; Truesdell and White, 1973). Analysis of natural heat flow conditions provides additional, indirect evidence for the ubiquitous presence of liquid. From an analysis of the heat pipe process (vapor-liquid counterflow) Preuss (1985) inferred that effective vertical permeability to liquid phase in vapor-dominated reservoirs is approximately 1017 m2, for a heat flux of 1 W/m2. This value appears to be at the high end of matrix permeabilities of unfractured rocks at The Geysers, suggesting that at least the smaller fractures contribute to liquid permeability. For liquid to be mobile in fractures, the rock matrix must be essentially completely liquid-saturated, because otherwise liquid phase would be sucked from the fractures into the matrix by capillary force. Large water saturation in the matrix, well above the irreducible saturation of perhaps 30%, has been shown to be compatible with production of superheated steam (Pruess and Narasimhan, 1982). In response to fluid production the liquid phase will boil, with heat of vaporization supplied by the reservoir rocks. As reservoir temperatures decline reservoir pressures will decline also. For depletion of ''bulk'' liquid, the pressure would decline along the saturated vapor pressure curve, while for liquid held by capillary and adsorptive forces inside porous media, an additional decline will arise from ''vapor pressure lowering''. Capillary pressure and vapor adsorption effects, and associated vapor pressure lowering phenomena, have received considerable attention in the geothermal literature, and also in studies related to geologic disposal of heat generating nuclear wastes, and in the drying of porous materials. Geothermally oriented studies were presented by Chicoine et al. (1977), Hsieh and Ramey (1978, 1981), Herkelrath et al. (1983), and Nghiem and Ramey (1991). Nuclear waste-related work includes papers by Herkelrath and O'Neal (1985), Pollock (1986), Eaton and Bixler (1987), Pruess et al. (1990), Nitao (1990), and Doughty and E'ruess (1991). Applications to industrial drying of porous materials have been discussed by Hamiathy (1969) arid Whitaker (1977). This paper is primarily concerned with evaluating the impact of vapor pressure lowering (VPL) effects on the depletion behavior of vapor-dominated reservoirs. We have examined experimental data on vapor adsorption and capillary pressures in an effort to identify constitutive relationships that would be applicable to the tight matrix rocks of vapor-dominated systems. Numerical simulations have been performed to evaluate the impact of these effects on the depletion of vapor-dominated reservoirs.

The Heat Pipe Effect in a Dual-permeability Porous System

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Total Pages : 242 pages
Book Rating : 4.:/5 (29 download)

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Book Synopsis The Heat Pipe Effect in a Dual-permeability Porous System by : Judith Dianne Jennings

Download or read book The Heat Pipe Effect in a Dual-permeability Porous System written by Judith Dianne Jennings and published by . This book was released on 1984 with total page 242 pages. Available in PDF, EPUB and Kindle. Book excerpt:

Unstable Heat Pipes

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Book Synopsis Unstable Heat Pipes by :

Download or read book Unstable Heat Pipes written by and published by . This book was released on 1987 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt: Heat pipes are an important feature of models of vapor-dominated geothermal reservoirs. Numerical experiments reveal that a vapor-dominated heat pipe is unstable if pressure is controlled at shallow levels. This instability is discussed in physical terms, and some implications for geothermal reservoirs are considered. 9 refs., 10 figs.

Convection in Porous Media

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Publisher : Springer Science & Business Media
ISBN 13 : 9780387290966
Total Pages : 672 pages
Book Rating : 4.2/5 (99 download)

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Book Synopsis Convection in Porous Media by : D.A. Nield

Download or read book Convection in Porous Media written by D.A. Nield and published by Springer Science & Business Media. This book was released on 2006-02-23 with total page 672 pages. Available in PDF, EPUB and Kindle. Book excerpt: Nonprofit organizations are suffering from the continuing economic downturn. Donations are decreasing while demand for services is growing, forcing these organizations to be increasingly efficient and effective with their funds. This book introduces the reader to the basic concepts of project management. It provides approaches and templates to help nonprofit managers quickly implement practices to help them manage their limited resources, both financial and volunteer. The book also provides a tool to help the project team determine which practices are most appropriate. The book explores how social media and other technology tools can be used to assist in the management of time-sensitive projects and shows how project portfolio management can be a tool to assist in communications with boards of directors and other governing entities. The project portfolio is a tool that development office managers can easily implement and adopt to facilitate resource assignment. Finally, the book offers three case studies of nonprofit projects that went awry and shows how project management would have assisted.

Quantitative Model of Vapor Dominated Geothermal Reservoirs as Heat Pipes in Fractured Porous Rock

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Book Synopsis Quantitative Model of Vapor Dominated Geothermal Reservoirs as Heat Pipes in Fractured Porous Rock by :

Download or read book Quantitative Model of Vapor Dominated Geothermal Reservoirs as Heat Pipes in Fractured Porous Rock written by and published by . This book was released on 1985 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt: We present a numerical model of vapor-dominated reservoirs which is based on the well-known conceptual model of White, Muffler, and Truesdell. Computer simulations show that upon heat recharge at the base, a single phase liquid-dominated geothermal reservoir in fractured rock with low matrix permeability will evolve into a two-phase reservoir with B.P.D. (boiling point-for-depth) pressure and temperature profiles. A rather limited discharge event through cracks in the caprock, involving loss of only a few percent of fluids in place, is sufficient to set the system off to evolve a vapor-dominated state. The attributes of this state are discussed, and some features requiring further clarification are identified. 26 refs., 5 figs.

The Effect of Thermal Conduction Upon Pressure Drawdown and Buildup in Fissured, Vapor-dominated Geothermal Reservoirs

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Total Pages : 6 pages
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Book Synopsis The Effect of Thermal Conduction Upon Pressure Drawdown and Buildup in Fissured, Vapor-dominated Geothermal Reservoirs by :

Download or read book The Effect of Thermal Conduction Upon Pressure Drawdown and Buildup in Fissured, Vapor-dominated Geothermal Reservoirs written by and published by . This book was released on 1978 with total page 6 pages. Available in PDF, EPUB and Kindle. Book excerpt: An analysis of steam-pressure behavior in a vapor-dominated geothermal reservoir with an immobile vaporizing liquid phase was presented by Moench and Atkinson (1977) at the Third Stanford Workshop on Geothermal Reservoir Engineering, and later expanded by Moench and Atkinson (1978). In that study a finite-difference model was used to demonstrate the effects of phase change in the reservoir upon pressure drawdown and buildup. In this paper that model is modified to incorporate heat transfer from blocks of impermeable rock to thin, highly-permeable, porous fissures. The purpose of this study is to demonstrate the added effect of heat transfer of this type upon the transient pressure response of a vapor-dominated geothermal reservoir.

Modelling Studies of the Evolution of Vapour-Dominated Geothermal Systems

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Book Synopsis Modelling Studies of the Evolution of Vapour-Dominated Geothermal Systems by :

Download or read book Modelling Studies of the Evolution of Vapour-Dominated Geothermal Systems written by and published by . This book was released on 1995 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt: Numerical experiments, based on linear stability results, are invoked to model the evolution of two-phase vapor-dominated zones within geothermal systems. A reservoir model with all boundaries impermeable to fluid flow and a uniform heat flux at the bottom boundary is used. The results obtained show that different steady-states are accessible along different quasi-static paths from the same initial vapor-dominated steady-state. Thus, the realization of a steady-state with a two-phase vapor-dominated zone overlying a single-phase hot water region can indicate that the geothermal system undergoes a process of slow cooling. A steady-state with a two-phase vapor-dominated zone overlying a single-phase vapor region can be formed either as a result of slow heating or as a result of a reduction in permeability. A steady-state with an upper vapor-dominated part and a lower liquid-dominated part can occur if permeability of the system has been gradually increased.

A Quantitative Model of Vapor Dominated Geothermal Reservoirs as Heat Pipes in Fractured Porous Rock

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Book Rating : 4.:/5 (785 download)

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Book Synopsis A Quantitative Model of Vapor Dominated Geothermal Reservoirs as Heat Pipes in Fractured Porous Rock by : K. Pruess

Download or read book A Quantitative Model of Vapor Dominated Geothermal Reservoirs as Heat Pipes in Fractured Porous Rock written by K. Pruess and published by . This book was released on 1985 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt:

Convection in Porous Media

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Publisher : Springer
ISBN 13 : 3319495623
Total Pages : 988 pages
Book Rating : 4.3/5 (194 download)

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Book Synopsis Convection in Porous Media by : Donald A. Nield

Download or read book Convection in Porous Media written by Donald A. Nield and published by Springer. This book was released on 2017-03-15 with total page 988 pages. Available in PDF, EPUB and Kindle. Book excerpt: This updated edition of a widely admired text provides a user-friendly introduction to the field that requires only routine mathematics. The book starts with the elements of fluid mechanics and heat transfer, and covers a wide range of applications from fibrous insulation and catalytic reactors to geological strata, nuclear waste disposal, geothermal reservoirs, and the storage of heat-generating materials. As the standard reference in the field, this book will be essential to researchers and practicing engineers, while remaining an accessible introduction for graduate students and others entering the field. The new edition features 2700 new references covering a number of rapidly expanding fields, including the heat transfer properties of nanofluids and applications involving local thermal non-equilibrium and microfluidic effects.

The Geothermal Resource

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ISBN 13 :
Total Pages : 222 pages
Book Rating : 4.3/5 (91 download)

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Book Synopsis The Geothermal Resource by : Petroleum Information Corporation

Download or read book The Geothermal Resource written by Petroleum Information Corporation and published by . This book was released on 1979 with total page 222 pages. Available in PDF, EPUB and Kindle. Book excerpt:

On Fluid and Heat Transfer in Deep Zones of Vapor-Dominated Geothermal Reservoirs

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Book Synopsis On Fluid and Heat Transfer in Deep Zones of Vapor-Dominated Geothermal Reservoirs by :

Download or read book On Fluid and Heat Transfer in Deep Zones of Vapor-Dominated Geothermal Reservoirs written by and published by . This book was released on 1987 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt: We have presented a preliminary analysis of permeability structure and fluid and heat flow conditions in the deeper horizons of the Larderello geothermal system. Our main observations and findings are: (1) Measurements in deep Larderello wells have indicated formation temperatures near 300 o C at 3000 m depth, and even higher temperatures at greater depth. (2) From an analysis of heat transfer mechanisms we suggest that a transition from vapor-dominated to liquid-dominated conditions must have been present in the natural state of the Larderello geothermal system. No reliable determination of the depth at which this transition occurred has yet been made, but a depth of approximately 2000 m or more appears most likely. (3) From temperature-depth data in two-phase reservoirs it is in principle possible to estimate vertical permeability. (4) For exploited reservoirs such as Larderello, reconstruction of permeability and temperature trends with depth can be made indirectly, using numerical simulation. Our preliminary results indicate that production of high-enthalpy fluids can be explained from two-phase flow effects in a fractured-porous medium. 18 refs., 2 tabs., 7 figs.

Theoretical Analysis of Fluid Flow and Energy Transport in Hydrothermal Systems

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ISBN 13 :
Total Pages : 114 pages
Book Rating : 4.:/5 (6 download)

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Book Synopsis Theoretical Analysis of Fluid Flow and Energy Transport in Hydrothermal Systems by : Charles R. Faust

Download or read book Theoretical Analysis of Fluid Flow and Energy Transport in Hydrothermal Systems written by Charles R. Faust and published by . This book was released on 1977 with total page 114 pages. Available in PDF, EPUB and Kindle. Book excerpt:

Vapor-dominated Hydrothermal Systems Compared with Hot-water Systems

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Total Pages : 53 pages
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Book Synopsis Vapor-dominated Hydrothermal Systems Compared with Hot-water Systems by : Donald Edward White

Download or read book Vapor-dominated Hydrothermal Systems Compared with Hot-water Systems written by Donald Edward White and published by . This book was released on 1970 with total page 53 pages. Available in PDF, EPUB and Kindle. Book excerpt: Vapor-dominated ("dry-steam") geothermal systems are uncommon and poorly understood compared with hot-water systems. Critical physical data on both types were obtained from U.S. Geological Survey research in Yellowstone Park. Vapor-dominated systems require relatively potent heat supplies and low initial permeability. After an early hot-water stage, a system becomes vapor dominated when net discharge starts to exceed recharge. Steam then boils from a declining water table; some steam escapes to the atmosphere, but most condenses below the surface, where its heat of vaporization can be conducted upward. The main vapor-dominated reservoir actually is a two-phase heat-transfer system. Vapor boiled from the deep (brine?) water table flows upward; most liquid condensate flows down to the water table, but some may be swept out with steam in channels of principal upflow. Liquid water favors small pores and channels because of its high surface tension relative to that of steam. Steam is largely excluded from smaller spaces but greatly dominates the larger channels and discharge from wells. With time, permeability of water-recharge channels, initially low, becomes still lower because of deposition of carbonates and CaSO4, which decrease in solubility with temperature. The "lid" on the system consists of argillized rocks and CO2 - saturated condensate. Our model of vapor-dominated systems and the thermodynamic properties of steam provide a good mechanism for separating volatile mercury from all other metals of lower volatility. Mercury is known to be enriched in the vapor of these systems; the zone of condensation that surrounds the uniform reservoir is attractive for precipitating HgS. A more speculative suggestion is that porphyry copper deposits form below the deep water tables hypothesized for the vapor-dominated systems. Some enigmatic characteristics of these copper deposits are consistent with such a relationship, and warrant consideration and testing.

Scientific and Technical Aerospace Reports

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ISBN 13 :
Total Pages : 592 pages
Book Rating : 4.:/5 (319 download)

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Book Synopsis Scientific and Technical Aerospace Reports by :

Download or read book Scientific and Technical Aerospace Reports written by and published by . This book was released on 1992 with total page 592 pages. Available in PDF, EPUB and Kindle. Book excerpt: