Titlebook: Geothermal Reservoir Engineering; Ender Okandan Book 1988 Kluwer Academic Publishers 1988 Reservoir.calculus.geothermal energy.linear opti

FECT

Use of Tracers in the Geothermal Industry-Tracer Flow Equations in Porous MediaInlet-outlet tracer techniques are convenient experimental ways of determining internal characteristics of conti nous flow systems. Basicallys a chemical species is injected into the inlet stream and the monitoring of the concentration-time relationships at the outlet is used to provide information about the internal flow characteristics.

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Reservoir Engineering of Wairakei Geothermal FieldWairakei was the first liquid dominated geothermal field exploited for major power production. As such many decisions were taken on an ad-hoc or experimental basis. In retrospect the choice of Wairakei was fortunate: with extensive shallow high permeability and major recharge it is an easy field to exploit.

Asparagus

An Analysis of Natural State of Kizildere Field, TurkeyK?z?ldere geothermal field is located in Western Anatolia and is the first field under exploitation for electricity generation. High CO. content, relatively low temperature and pressure in the well field are the major causes of decline in the power output until to date.

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978-94-010-8153-5Kluwer Academic Publishers 1988

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https://doi.org/10.1007/978-3-663-09954-3403x10. joules above 20 C for 10 km of crustal depth. This estimate drops to 35x10. joules if we consider 3 km of depth. However only a small portion of this enormous energy is exploitable due to geological, technical and economic constraints.

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施魔法

https://doi.org/10.1007/978-981-19-7111-2is leads to the construction of simple concepts or models of the reservoir. From these one can draw immediate qualitative or quantitative inferences about future behaviour; and lay the basis for more detailed reservoir engineering or modelling exercises.

能量守恒

https://doi.org/10.1007/978-3-642-86616-6nciples of the interpretation techniques can, however, be transferred to low temperature or vapour dominated systems or those with more isotropic porosity with little modification. Background material and basic interpretation methods for measurements are given in references 1,2 and 3.