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Titlebook: Geothermal Engineering; Fundamentals and App Arnold Watson Book 2013 Springer Science+Business Media New York 2013 Geothermal Drilling.Geot

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樓主: Nonchalant
11#
發(fā)表于 2025-3-23 11:43:47 | 只看該作者
The Discharging Well,sure declines, but some have a periodic flow or even a regular intermittent discharge like a geyser. It is sometimes useful to have a means of predicting the details of the flow during discharge, and numerical discharge prediction methods have been developed. All of these matters are discussed in this Chapter.
12#
發(fā)表于 2025-3-23 15:16:33 | 只看該作者
The Transient Response of Formations to Flow in a Well: Transient Pressure Well Testing,nd the historical development of methods of dealing with real effects such as skin and wellbore storage in single-phase flows is described. The chapter ends by describing the approach to analysing the flow in formations containing two-phase fluid and interference testing.
13#
發(fā)表于 2025-3-23 18:01:29 | 只看該作者
14#
發(fā)表于 2025-3-24 02:04:28 | 只看該作者
15#
發(fā)表于 2025-3-24 03:08:11 | 只看該作者
16#
發(fā)表于 2025-3-24 09:33:41 | 只看該作者
17#
發(fā)表于 2025-3-24 10:52:25 | 只看該作者
18#
發(fā)表于 2025-3-24 15:35:37 | 只看該作者
https://doi.org/10.1007/978-1-4612-4608-4ained, and sensitivity analysis discussed. The role of a geothermal power station in a network is considered next, followed by the need for a more widely based energy analysis. The chapter closes with a discussion of steam sales contracts.
19#
發(fā)表于 2025-3-24 21:01:46 | 只看該作者
Thermodynamics Background and the Properties of Water,r are described, focusing mainly on properties along the saturation line, in particular, formulations produced by the International Association for the Properties of Water and Steam (IAPWS). The chapter ends by examining hydrostatic pressure and the boiling point for depth curve.
20#
發(fā)表于 2025-3-25 02:50:25 | 只看該作者
The Equations Governing Heat and Single-Phase Fluid Flow and Their Simplification for Particular Aprements of equipment designers, are introduced. Natural convection and thermal conduction are briefly introduced. The basis of Darcy’s law is discussed, and the governing equations are reduced to a form suitable for the analysis of the flow in permeable formations in geothermal resources.
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