APLICATION OF FINITE ELEMENT METHOD IN HYDROTHERMAL SYSTEM MODELING

The Finite Element Method (FEM) is one numerical method for finished the problematical of limite condition in diferensial equation. The FEM contents is general domain representation in a simple sub-domain point of view, called as finite element. This method has been applicated in groundwater current...

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Main Author:	CAMAR REMOA (NIM : 10209020)
Format:	Final Project
Language:	Indonesia
Online Access:	https://digilib.itb.ac.id/gdl/view/18194
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Institution:	Institut Teknologi Bandung
Language:	Indonesia

id	id-itb.:18194
spelling	id-itb.:181942017-09-27T11:45:16ZAPLICATION OF FINITE ELEMENT METHOD IN HYDROTHERMAL SYSTEM MODELING CAMAR REMOA (NIM : 10209020), Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/18194 The Finite Element Method (FEM) is one numerical method for finished the problematical of limite condition in diferensial equation. The FEM contents is general domain representation in a simple sub-domain point of view, called as finite element. This method has been applicated in groundwater current modeling and SP (Self Potential) distribution in 2D profile. Validation of SP distribution has been compared to SP values in the field.Result of this modeling is hydrothermal velocity flows about 10-11 - 10-7 m/second and we can see the manifestation formed in Domas Carter. The SP values distribution modeling has been bigger from Domas Crater to Jarian Crater. 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	The Finite Element Method (FEM) is one numerical method for finished the problematical of limite condition in diferensial equation. The FEM contents is general domain representation in a simple sub-domain point of view, called as finite element. This method has been applicated in groundwater current modeling and SP (Self Potential) distribution in 2D profile. Validation of SP distribution has been compared to SP values in the field.Result of this modeling is hydrothermal velocity flows about 10-11 - 10-7 m/second and we can see the manifestation formed in Domas Carter. The SP values distribution modeling has been bigger from Domas Crater to Jarian Crater.
format	Final Project
author	CAMAR REMOA (NIM : 10209020),
spellingShingle	CAMAR REMOA (NIM : 10209020), APLICATION OF FINITE ELEMENT METHOD IN HYDROTHERMAL SYSTEM MODELING
author_facet	CAMAR REMOA (NIM : 10209020),
author_sort	CAMAR REMOA (NIM : 10209020),
title	APLICATION OF FINITE ELEMENT METHOD IN HYDROTHERMAL SYSTEM MODELING
title_short	APLICATION OF FINITE ELEMENT METHOD IN HYDROTHERMAL SYSTEM MODELING
title_full	APLICATION OF FINITE ELEMENT METHOD IN HYDROTHERMAL SYSTEM MODELING
title_fullStr	APLICATION OF FINITE ELEMENT METHOD IN HYDROTHERMAL SYSTEM MODELING
title_full_unstemmed	APLICATION OF FINITE ELEMENT METHOD IN HYDROTHERMAL SYSTEM MODELING
title_sort	aplication of finite element method in hydrothermal system modeling
url	https://digilib.itb.ac.id/gdl/view/18194
_version_	1820745811664830464

APLICATION OF FINITE ELEMENT METHOD IN HYDROTHERMAL SYSTEM MODELING

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