STUDY OF GEOCHEMICAL CHARACTERISTICS OF ADVANCED ARGILLIC ALTERATION ROCKS IN EPITHERMAL HIGH SULPHIDATION GOLD DEPOSITS

Acid rock drainage (ARD) is a water drainage or water seepage caused by mining <br /> <br /> activity process that exposing the rock and characterized by high acidity or the low <br /> <br /> pH value (Gautama, 2014). Mining activity can be done in many type of deposits, <...

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Main Author: DELILA IMANI SUMANTRI (NIM : 12114092), ALIFIANTY
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/25373
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:25373
spelling id-itb.:253732018-07-02T08:55:25ZSTUDY OF GEOCHEMICAL CHARACTERISTICS OF ADVANCED ARGILLIC ALTERATION ROCKS IN EPITHERMAL HIGH SULPHIDATION GOLD DEPOSITS DELILA IMANI SUMANTRI (NIM : 12114092), ALIFIANTY Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/25373 Acid rock drainage (ARD) is a water drainage or water seepage caused by mining <br /> <br /> activity process that exposing the rock and characterized by high acidity or the low <br /> <br /> pH value (Gautama, 2014). Mining activity can be done in many type of deposits, <br /> <br /> such as epithermal high sulphidation deposits that have some alteration zone, there <br /> <br /> are silicic, advanced argillic, argillic, and prophyllitic. Advanced argillic <br /> <br /> alteration zone contains native sulphur, and pyrite minerals which are sulphide <br /> <br /> minerals that forming acid rock drainage. The objective of this study was to do the <br /> <br /> prevention, handling and management of acid rock drainage by predicting the <br /> <br /> potential of acid rock drainage formation and predicting the leachate water quality <br /> <br /> of advanced argillic alteration rock samples. <br /> <br /> Based on the tests, there are two classifications for geochemical characteristics of <br /> <br /> rocks : 3 samples of PAF-LC (Potential Acid Forming-Low Capacity) as rocks that <br /> <br /> potentially produce acid rock drainage with weak acidity and 3 samples of PAFHC <br /> <br /> (Potential Acid Forming-High Capacity) as a rock that potentially produces <br /> <br /> acid rock drainage with strong acidity. Leachate water from all samples needs to <br /> <br /> be processed first because the pH of the water is lower than the pH range allowed <br /> <br /> on the quality standard in the Kepmen LH No. 202 Th. 2004 that was 6-9. In <br /> <br /> addition, the dissolved metal content also increases as TDS increases as pH <br /> <br /> decrease, this allows the dissolved metal content to exceed the maximum limit of <br /> <br /> quality standards. Encapsulation methods are needed to minimize rock exposure <br /> <br /> and prevent the formation of acidic conditions capable of dissolving metals. 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 Acid rock drainage (ARD) is a water drainage or water seepage caused by mining <br /> <br /> activity process that exposing the rock and characterized by high acidity or the low <br /> <br /> pH value (Gautama, 2014). Mining activity can be done in many type of deposits, <br /> <br /> such as epithermal high sulphidation deposits that have some alteration zone, there <br /> <br /> are silicic, advanced argillic, argillic, and prophyllitic. Advanced argillic <br /> <br /> alteration zone contains native sulphur, and pyrite minerals which are sulphide <br /> <br /> minerals that forming acid rock drainage. The objective of this study was to do the <br /> <br /> prevention, handling and management of acid rock drainage by predicting the <br /> <br /> potential of acid rock drainage formation and predicting the leachate water quality <br /> <br /> of advanced argillic alteration rock samples. <br /> <br /> Based on the tests, there are two classifications for geochemical characteristics of <br /> <br /> rocks : 3 samples of PAF-LC (Potential Acid Forming-Low Capacity) as rocks that <br /> <br /> potentially produce acid rock drainage with weak acidity and 3 samples of PAFHC <br /> <br /> (Potential Acid Forming-High Capacity) as a rock that potentially produces <br /> <br /> acid rock drainage with strong acidity. Leachate water from all samples needs to <br /> <br /> be processed first because the pH of the water is lower than the pH range allowed <br /> <br /> on the quality standard in the Kepmen LH No. 202 Th. 2004 that was 6-9. In <br /> <br /> addition, the dissolved metal content also increases as TDS increases as pH <br /> <br /> decrease, this allows the dissolved metal content to exceed the maximum limit of <br /> <br /> quality standards. Encapsulation methods are needed to minimize rock exposure <br /> <br /> and prevent the formation of acidic conditions capable of dissolving metals.
format Final Project
author DELILA IMANI SUMANTRI (NIM : 12114092), ALIFIANTY
spellingShingle DELILA IMANI SUMANTRI (NIM : 12114092), ALIFIANTY
STUDY OF GEOCHEMICAL CHARACTERISTICS OF ADVANCED ARGILLIC ALTERATION ROCKS IN EPITHERMAL HIGH SULPHIDATION GOLD DEPOSITS
author_facet DELILA IMANI SUMANTRI (NIM : 12114092), ALIFIANTY
author_sort DELILA IMANI SUMANTRI (NIM : 12114092), ALIFIANTY
title STUDY OF GEOCHEMICAL CHARACTERISTICS OF ADVANCED ARGILLIC ALTERATION ROCKS IN EPITHERMAL HIGH SULPHIDATION GOLD DEPOSITS
title_short STUDY OF GEOCHEMICAL CHARACTERISTICS OF ADVANCED ARGILLIC ALTERATION ROCKS IN EPITHERMAL HIGH SULPHIDATION GOLD DEPOSITS
title_full STUDY OF GEOCHEMICAL CHARACTERISTICS OF ADVANCED ARGILLIC ALTERATION ROCKS IN EPITHERMAL HIGH SULPHIDATION GOLD DEPOSITS
title_fullStr STUDY OF GEOCHEMICAL CHARACTERISTICS OF ADVANCED ARGILLIC ALTERATION ROCKS IN EPITHERMAL HIGH SULPHIDATION GOLD DEPOSITS
title_full_unstemmed STUDY OF GEOCHEMICAL CHARACTERISTICS OF ADVANCED ARGILLIC ALTERATION ROCKS IN EPITHERMAL HIGH SULPHIDATION GOLD DEPOSITS
title_sort study of geochemical characteristics of advanced argillic alteration rocks in epithermal high sulphidation gold deposits
url https://digilib.itb.ac.id/gdl/view/25373
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