Derivation, by Averaging, of the Equations of Heat, Mass and Momentum Transfer in a Geothermal Reservoir

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Description

The following paper is an abstract of a report under completion at the Lawrence Berkeley Laboratory (Assens, 1977); the main purpose of this report is to (1) provide a mathematical derivation of the equations describing the transfer of heat, mass and momentum in a geothermal brine reservoir (especially when heat or mass sources are present), and (2) help in the choice of the dependent variables best suited for solving these equations numerically. 3 figs., 18 refs., 1 tab.

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268-289

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Assens, Guy E. December 1, 1976.

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Description

The following paper is an abstract of a report under completion at the Lawrence Berkeley Laboratory (Assens, 1977); the main purpose of this report is to (1) provide a mathematical derivation of the equations describing the transfer of heat, mass and momentum in a geothermal brine reservoir (especially when heat or mass sources are present), and (2) help in the choice of the dependent variables best suited for solving these equations numerically. 3 figs., 18 refs., 1 tab.

Physical Description

268-289

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  • Proceedings Second Workshop Geothermal Reservoir Engineering, Stanford University, Stanford, Calif., December 1-3, 1976

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  • Report No.: SGP-TR-20-38
  • Grant Number: E043-326-PA-50
  • Office of Scientific & Technical Information Report Number: 887408
  • Archival Resource Key: ark:/67531/metadc886343

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Office of Scientific & Technical Information Technical Reports

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Creation Date

  • December 1, 1976

Added to The UNT Digital Library

  • Sept. 21, 2016, 2:29 a.m.

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  • Feb. 16, 2017, 7 p.m.

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Assens, Guy E. Derivation, by Averaging, of the Equations of Heat, Mass and Momentum Transfer in a Geothermal Reservoir, article, December 1, 1976; Berkeley, California. (digital.library.unt.edu/ark:/67531/metadc886343/: accessed October 21, 2018), University of North Texas Libraries, Digital Library, digital.library.unt.edu; crediting UNT Libraries Government Documents Department.