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Structural analysis of geothermal decline rate = Analisis struktur kadar penurunan geotermal

The aim of semivariogram modeling is to infer the structure of spatial continuity of the measurements. Practical experiences show that semivariogram modeling is an important step in spatial interpolation. The usual empirical semivariogram is sensitive to extreme data and shows a noised pattern. Some...

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Main Authors: Sutawanir Darwis,, Isnani,, Ali Ashat,
Format: Article
Language:English
Published: Universiti Kebangsaan Malaysia 2007
Online Access:http://journalarticle.ukm.my/103/1/1.pdf
http://journalarticle.ukm.my/103/
http://pkukmweb.ukm.my/~jsm/kandungan.html
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id my-ukm.journal.103
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spelling my-ukm.journal.1032016-12-14T06:26:25Z http://journalarticle.ukm.my/103/ Structural analysis of geothermal decline rate = Analisis struktur kadar penurunan geotermal Sutawanir Darwis, Isnani, Ali Ashat, The aim of semivariogram modeling is to infer the structure of spatial continuity of the measurements. Practical experiences show that semivariogram modeling is an important step in spatial interpolation. The usual empirical semivariogram is sensitive to extreme data and shows a noised pattern. Some robust empirical semivariogram was proposed. This paper reports the application of pairwise relative empirical semivariogram to Kamojang geothermal decline rate. Using the same data, the usual empirical semivariogram and pairwise semivariogram are compared. Comparative study shows that the empirical pairwise relative semivariogram is able to infer the structure of spatial continuity of the process. Universiti Kebangsaan Malaysia 2007-12 Article PeerReviewed application/pdf en http://journalarticle.ukm.my/103/1/1.pdf Sutawanir Darwis, and Isnani, and Ali Ashat, (2007) Structural analysis of geothermal decline rate = Analisis struktur kadar penurunan geotermal. Sains Malaysiana, 36 (2). pp. 207-211. ISSN 0126-6039 http://pkukmweb.ukm.my/~jsm/kandungan.html
institution Universiti Kebangsaan Malaysia
building Perpustakaan Tun Sri Lanang Library
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Kebangsaan Malaysia
content_source UKM Journal Article Repository
url_provider http://journalarticle.ukm.my/
language English
description The aim of semivariogram modeling is to infer the structure of spatial continuity of the measurements. Practical experiences show that semivariogram modeling is an important step in spatial interpolation. The usual empirical semivariogram is sensitive to extreme data and shows a noised pattern. Some robust empirical semivariogram was proposed. This paper reports the application of pairwise relative empirical semivariogram to Kamojang geothermal decline rate. Using the same data, the usual empirical semivariogram and pairwise semivariogram are compared. Comparative study shows that the empirical pairwise relative semivariogram is able to infer the structure of spatial continuity of the process.
format Article
author Sutawanir Darwis,
Isnani,
Ali Ashat,
spellingShingle Sutawanir Darwis,
Isnani,
Ali Ashat,
Structural analysis of geothermal decline rate = Analisis struktur kadar penurunan geotermal
author_facet Sutawanir Darwis,
Isnani,
Ali Ashat,
author_sort Sutawanir Darwis,
title Structural analysis of geothermal decline rate = Analisis struktur kadar penurunan geotermal
title_short Structural analysis of geothermal decline rate = Analisis struktur kadar penurunan geotermal
title_full Structural analysis of geothermal decline rate = Analisis struktur kadar penurunan geotermal
title_fullStr Structural analysis of geothermal decline rate = Analisis struktur kadar penurunan geotermal
title_full_unstemmed Structural analysis of geothermal decline rate = Analisis struktur kadar penurunan geotermal
title_sort structural analysis of geothermal decline rate = analisis struktur kadar penurunan geotermal
publisher Universiti Kebangsaan Malaysia
publishDate 2007
url http://journalarticle.ukm.my/103/1/1.pdf
http://journalarticle.ukm.my/103/
http://pkukmweb.ukm.my/~jsm/kandungan.html
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score 13.211869

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