Results 141 to 150 of about 435,541 (193)
Some of the next articles are maybe not open access.
Geothermal Reservoir Modelling
SPE Annual Fall Technical Conference and Exhibition, 1977Abstract This paper describes and partially evaluates an implicit, three-dimensional geothermal reservoir simulation model. The evaluation emphasizes stability or time-step tolerance of the implicit finite-difference formulation.
openaire +1 more source
ORIGIN OF STEAM IN GEOTHERMAL RESERVOIRS
Proceedings of SPE Annual Fall Technical Conference and Exhibition, 1977Abstract In geothermal systems, due to the mechanism of mass and heat transport on the boiling point for depth curve, stable steam-water mixtures can occur only at reservoir pressures less than about 30.6 bars and at temperatures less than about 235 deg. C.
openaire +1 more source
Assessment of Geothermal Potential in the Tbilisi Geothermal Reservoir
2022<p>Taking into account the world-wide energy crisis, the search and rational use of cheap and</p><p>ecologically pollution-free renewable energy sources are extremely important. Among these sources the geothermal energy is of great potentialities.
Nino Kapanadze +4 more
openaire +1 more source
Radon Transect Analysis in Geothermal Reservoirs
SPE California Regional Meeting, 1980ABSTRACT Radon transect experiments have been conducted to study flow and emanation characteristics of geothermal reservoirs. Transect experiments have been carried out at three geothermal reservoirs: 1) The vapor-dominated field at The Geysers, California; 2) the liquid-dominated field at Wairakei, New Zealand; and 3) the liquid ...
Lewis Semprini, Paul Kruger
openaire +1 more source
Numerical Modeling of a Desaturating Geothermal Reservoir
Numerical Heat Transfer, Part B: Fundamentals, 1978Abstract To achieve a better understanding of hot-water geothermal reservoirs, the problem of a hypothetical geothermal aquifer that depletes the fluid saturating its upper regions during production is considered. This depletion leads to the characteristic depressurization and drawdown of the liquid surface observed typically at the Wairakei geothermal
R. N. Home, M. J. O'Sullivan
openaire +1 more source
Geothermal Reservoir Engineering
1987Importance of Geothermal Reservoir Engineering in the Assessment of Geothermal Sources.- Geothermal Energy Assessment.- Reservoir Physics and Conceptual Modelling.- Downhole Measurements in Geothermal Wells.- Transient Pressure Testing in Geothermal Systems.- Two-Phase Flow in Geothermal Wells.- Use of Tracers in the Geothermal Industry Tracer Flow ...
openaire +1 more source
Geothermal Reservoir Simulation
Proceedings, 2013A three-dimensional (3D) numerical model was proposed for natural state simulation of the Las Tres Virgenes (LTV) geothermal system from emplacement and cooling of the heat source. The conceptual model is based on the volcanic history of the field. Chamber volumes were estimated from outcropping geology and eruptive volumes.
openaire +1 more source
Isotope Geochemistry In Geothermal Reservoir Studies.
SPE California Regional Meeting, 1977American Institute of Mining, Metallurgical, and Petroleum Engineers, Inc. Abstract Isotope geochemistry has contributed greatly to our scientific knowledge of geothermal systems. The near identity of deuterium isotopes of thermal waters and local rain waters has shown that geothermal systems are ...
A.H. Truesdell, G.A. Frye
openaire +1 more source
Numerical Modeling Of The Wairakei Geothermal Reservoir
SPE California Regional Meeting, 1977American Institute of Mining, Metallurgical, and Petroleum Engineers, Inc. Abstract In order to achieve a better understanding of the Wairakei geothermal reservoir and of others of similar type, the current investigation considers the problem of a hypothetical geothermal aquifer that depletes the ...
Roland Horne, Michael O'Sullivan
openaire +1 more source
Nonstatic Reservoirs: The Natural State of the Geothermal Reservoir
Journal of Petroleum Technology, 1983Summary Above-hydrostatic-reservoir-pressure gradients are found in many geothermal fields before exploitation. In higher-temperature fields, steam and water also coexist in the upper levels. These factors indicate natural upflow in these reservoirs-i.e. the dynamic state of the fluid.
Ian G. Donaldson +2 more
openaire +1 more source

