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Numerical modeling is the basic method to determine the growth process that is happen in the geothermal reservoir. Mathematical modeling with finite difference method one phase in numerical approximation is uses with some physical parameter. Darcy's law, Mass Equilibrium, and Energy Equilibrium...

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Main Author: SAUT H. SINAGA (NIM 10203012), HARRYANTO
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/10555
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:10555
spelling id-itb.:105552017-09-27T11:45:12Z#TITLE_ALTERNATIVE# SAUT H. SINAGA (NIM 10203012), HARRYANTO Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/10555 Numerical modeling is the basic method to determine the growth process that is happen in the geothermal reservoir. Mathematical modeling with finite difference method one phase in numerical approximation is uses with some physical parameter. Darcy's law, Mass Equilibrium, and Energy Equilibrium equation are the basic equation that is used in this paper.<p>Heat source from magma will flow through the fractured zone, whereas this zone has different permeability and porosity characteristic from the other area around the fractured zone, and conduction heat transfer will flow to the neighbor area of the fractured zone.<p>The results in this paper are pressure and enthalpy distribution as a time function at each depth. text
institution Institut Teknologi Bandung
building Institut Teknologi Bandung Library
continent Asia
country Indonesia
Indonesia
content_provider Institut Teknologi Bandung
collection Digital ITB
language Indonesia
description Numerical modeling is the basic method to determine the growth process that is happen in the geothermal reservoir. Mathematical modeling with finite difference method one phase in numerical approximation is uses with some physical parameter. Darcy's law, Mass Equilibrium, and Energy Equilibrium equation are the basic equation that is used in this paper.<p>Heat source from magma will flow through the fractured zone, whereas this zone has different permeability and porosity characteristic from the other area around the fractured zone, and conduction heat transfer will flow to the neighbor area of the fractured zone.<p>The results in this paper are pressure and enthalpy distribution as a time function at each depth.
format Final Project
author SAUT H. SINAGA (NIM 10203012), HARRYANTO
spellingShingle SAUT H. SINAGA (NIM 10203012), HARRYANTO
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author_facet SAUT H. SINAGA (NIM 10203012), HARRYANTO
author_sort SAUT H. SINAGA (NIM 10203012), HARRYANTO
title #TITLE_ALTERNATIVE#
title_short #TITLE_ALTERNATIVE#
title_full #TITLE_ALTERNATIVE#
title_fullStr #TITLE_ALTERNATIVE#
title_full_unstemmed #TITLE_ALTERNATIVE#
title_sort #title_alternative#
url https://digilib.itb.ac.id/gdl/view/10555
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