HUBUNGAN ANTARA KOMPOSISI MINERAL, SIFAT FISIK, REGANGANMENGEMBANG DAN KUAT GESER PADA BATULEMPUNG, FORMASI SUBANG:STUDI KASUS DI DAERAH CISAMPIH, KEC. DAWUAN, KAB. SUBANG,JAWA BARAT

The objective of this study is to conduct detail assessment of swelling behavior of Subang Formation claystones at the Cisampih area of Dawuan, Subang Regency, West Java. Field observations were conducted to have a better understanding on swelling behavior of the claystones and its impacts. Me...

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Main Author: Endah Utami, Tri
Format: Theses
Language:Indonesia
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Online Access:https://digilib.itb.ac.id/gdl/view/77078
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:77078
spelling id-itb.:770782023-08-22T09:45:49ZHUBUNGAN ANTARA KOMPOSISI MINERAL, SIFAT FISIK, REGANGANMENGEMBANG DAN KUAT GESER PADA BATULEMPUNG, FORMASI SUBANG:STUDI KASUS DI DAERAH CISAMPIH, KEC. DAWUAN, KAB. SUBANG,JAWA BARAT Endah Utami, Tri Geologi, hidrologi & meteorologi Indonesia Theses claystones, Subang Formation, swelling strains, anisotropy, shear strength INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/77078 The objective of this study is to conduct detail assessment of swelling behavior of Subang Formation claystones at the Cisampih area of Dawuan, Subang Regency, West Java. Field observations were conducted to have a better understanding on swelling behavior of the claystones and its impacts. Meanwhile, laboratory tests were carried out to analyze mineralogical composition, physical properties, swelling strains, and shear strength of claystones. The results from XRD and SEM analyses have shown the composition of plagioclase, quartz, montmorillonite, Illite and kaolinite, in claystones with different percentage. Porosity and water content were tend to increase in weathered claystones than in fresh claystones, however unit weight was tend to decrease. Atterberg limits analyses showed that all claystones can be categorized as CH (clay high plasticity). Owing to the surface (< 3 m) and more weathered condition of claystones; volume change due to swelling process tend to decrease. The swelling strains were significantly influenced by the ratio of (montmorillonite + Illite)/kaolinite, and the ratio of clay minerals/non-clay, also the number of montmorillonite + Illite. Swelling strains in the vertical direction were most likely to be higher than in the horizontal direction, therefore it can be inferred that swelling strains of the claystones are anisotropy. The highest volumetic can be identified on sample 6 (15.28 %), followed by 5 (8.23 %), 4 (7.54 %), 3 (3.5 %), 2 (2.49 %) and sample 1 (1.52 %). Result of direct shear tests clearly showed that shear strength were decrease due to swelling strain, with the decrease values of shear strength were ranging from 45 % to 57 %. 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
topic Geologi, hidrologi & meteorologi
spellingShingle Geologi, hidrologi & meteorologi
Endah Utami, Tri
HUBUNGAN ANTARA KOMPOSISI MINERAL, SIFAT FISIK, REGANGANMENGEMBANG DAN KUAT GESER PADA BATULEMPUNG, FORMASI SUBANG:STUDI KASUS DI DAERAH CISAMPIH, KEC. DAWUAN, KAB. SUBANG,JAWA BARAT
description The objective of this study is to conduct detail assessment of swelling behavior of Subang Formation claystones at the Cisampih area of Dawuan, Subang Regency, West Java. Field observations were conducted to have a better understanding on swelling behavior of the claystones and its impacts. Meanwhile, laboratory tests were carried out to analyze mineralogical composition, physical properties, swelling strains, and shear strength of claystones. The results from XRD and SEM analyses have shown the composition of plagioclase, quartz, montmorillonite, Illite and kaolinite, in claystones with different percentage. Porosity and water content were tend to increase in weathered claystones than in fresh claystones, however unit weight was tend to decrease. Atterberg limits analyses showed that all claystones can be categorized as CH (clay high plasticity). Owing to the surface (< 3 m) and more weathered condition of claystones; volume change due to swelling process tend to decrease. The swelling strains were significantly influenced by the ratio of (montmorillonite + Illite)/kaolinite, and the ratio of clay minerals/non-clay, also the number of montmorillonite + Illite. Swelling strains in the vertical direction were most likely to be higher than in the horizontal direction, therefore it can be inferred that swelling strains of the claystones are anisotropy. The highest volumetic can be identified on sample 6 (15.28 %), followed by 5 (8.23 %), 4 (7.54 %), 3 (3.5 %), 2 (2.49 %) and sample 1 (1.52 %). Result of direct shear tests clearly showed that shear strength were decrease due to swelling strain, with the decrease values of shear strength were ranging from 45 % to 57 %.
format Theses
author Endah Utami, Tri
author_facet Endah Utami, Tri
author_sort Endah Utami, Tri
title HUBUNGAN ANTARA KOMPOSISI MINERAL, SIFAT FISIK, REGANGANMENGEMBANG DAN KUAT GESER PADA BATULEMPUNG, FORMASI SUBANG:STUDI KASUS DI DAERAH CISAMPIH, KEC. DAWUAN, KAB. SUBANG,JAWA BARAT
title_short HUBUNGAN ANTARA KOMPOSISI MINERAL, SIFAT FISIK, REGANGANMENGEMBANG DAN KUAT GESER PADA BATULEMPUNG, FORMASI SUBANG:STUDI KASUS DI DAERAH CISAMPIH, KEC. DAWUAN, KAB. SUBANG,JAWA BARAT
title_full HUBUNGAN ANTARA KOMPOSISI MINERAL, SIFAT FISIK, REGANGANMENGEMBANG DAN KUAT GESER PADA BATULEMPUNG, FORMASI SUBANG:STUDI KASUS DI DAERAH CISAMPIH, KEC. DAWUAN, KAB. SUBANG,JAWA BARAT
title_fullStr HUBUNGAN ANTARA KOMPOSISI MINERAL, SIFAT FISIK, REGANGANMENGEMBANG DAN KUAT GESER PADA BATULEMPUNG, FORMASI SUBANG:STUDI KASUS DI DAERAH CISAMPIH, KEC. DAWUAN, KAB. SUBANG,JAWA BARAT
title_full_unstemmed HUBUNGAN ANTARA KOMPOSISI MINERAL, SIFAT FISIK, REGANGANMENGEMBANG DAN KUAT GESER PADA BATULEMPUNG, FORMASI SUBANG:STUDI KASUS DI DAERAH CISAMPIH, KEC. DAWUAN, KAB. SUBANG,JAWA BARAT
title_sort hubungan antara komposisi mineral, sifat fisik, reganganmengembang dan kuat geser pada batulempung, formasi subang:studi kasus di daerah cisampih, kec. dawuan, kab. subang,jawa barat
url https://digilib.itb.ac.id/gdl/view/77078
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