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完整後設資料紀錄
DC 欄位 | 值 | 語言 |
---|---|---|
dc.contributor.advisor | 陳正宏 | |
dc.contributor.author | Wuh-Terng Lim | en |
dc.contributor.author | 林武滕 | zh_TW |
dc.date.accessioned | 2021-06-15T16:47:52Z | - |
dc.date.available | 2016-08-12 | |
dc.date.copyright | 2015-08-12 | |
dc.date.issued | 2015 | |
dc.date.submitted | 2015-08-09 | |
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dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/53157 | - |
dc.description.abstract | 馬來西亞半島所在的巽他(Sunda)板塊是處於澳洲大陸板塊與歐亞大陸板塊交界處。本研究利用水化學和氣體地球化學來討論溫泉水的來源和來源模式。在馬來西亞半島這個無火山地區上就發現了超過60個溫泉,而本研究取其中的十八處溫泉進行採樣。溫泉的測量例如pH值,溫度和導電度都在現地分析。所選溫泉的溫度介於40.1°C 到88.7°C,pH值也在6.6到9.1之間。溫泉的導電度從最小的200 µs/cm 到 最大的43000 µs/cm不等。利用罐頂空間進行一般溶解氣體如氮氣,甲烷和二氧化碳的分析。三端源圖顯示大多樣品都富集氮氣,只有少數樣品含有二氧化碳的成分;水氡是由可攜帶的RAD7氡氣分析儀器作現地測量。馬來西亞半島溫泉的水氡值介於200 Bq/m3和111866 Bq/m3 之間。水氡分析結果顯示馬來西亞半島溫泉的來源和深埋地底的花崗岩體有關;另外取樣品封存於高真空的玻璃瓶中,進行氦同位素比值、氦氖比值研究。氦同位素比值分析結果發現,馬來西亞半島溫泉大多小於0.1Ra而大於0.02Ra(Ra為大氣中3He/4He的比值),說明氦氣屬於地殼來源和上部地函來源的混合;氫氧同位素和陰陽離子的分析結果把馬來西亞半島的溫泉來源分成了天水來源和天水混合海水來源。另外,本研究認為馬來西亞半島溫泉的加熱源來自於冷卻中的花崗岩體和富含鈾釷元素的花崗岩體不斷放射性衰變之下產生的熱量。 | zh_TW |
dc.description.abstract | Peninsular Malaysia is located on Sunda Plate which is situated between two major boundaries of tectonic plates, the Australian Plate and the Eurasian Plate. Over sixty thermal springs had been reported in Peninsular Malaysia, a non-volcanic country. In this study, eighteen spring samples have been analysed, from which the piper plot and meteoric water line is constructed. Moreover, helium isotopic analyses, dissolved gas analyses and radon activity analyses are also carried out in order to investigate the origin and sources of thermal springs in Peninsular Malaysia. The surface temperature of selected thermal springs ranges from 40.1°C to 88.7°C, the pH values range from 6.6 to 9.1, and the conductivity varies between 200 µs/cm and 43000 µs/cm. The radon activity analyses had been carried out by using RAD7 Radon Detector. Result shows that the radon value of selected thermal springs in Peninsular Malaysia fluctuates within highest value of 111,866 Bq/cm3 and lowest value of 200 Bq/cm3. As for the dissolved gas in thermal springs, nitrogen is the major component and argon, carbon dioxide and oxygen are minor constituents. Isotopic composition of hydrogen (D/H) and oxygen (18O/16O) mostly fall along the local meteoric water line, indicating that the meteoric water is the major fluid source for thermal springs. Meanwhile, the helium isotopic ratios of most samples (except HS 12) show consistently low values, less than 0.1 Ra (Ra is the 3He/4He ratio of the air). It implies that crust component is the major helium gas source for thermal springs, except sample of HS 12 which may involve upper mantle component. | en |
dc.description.provenance | Made available in DSpace on 2021-06-15T16:47:52Z (GMT). No. of bitstreams: 1 ntu-104-R02224218-1.pdf: 7041661 bytes, checksum: a4794a7ab448304fff521767aebe3762 (MD5) Previous issue date: 2015 | en |
dc.description.tableofcontents | 誌謝 ii
Abstract iii 摘要 iv Chapter 1 Introduction 1 1.1 Thermal Spring 1 1.2 Dissolved Gas in Spring Water 2 1.3 Origin and Source of Thermal Spring in Peninsular Malaysia 3 Chapter 2 Study Area 4 2.1 General Geology of Peninsular Malaysia 4 2.2 Langkawi Island 7 2.3 Drainage 10 2.4 Mega-landforms of Peninsular Malaysia 12 Chapter 3 Procedures and Sampling Locations 14 3.1 Introduction 14 3.2 Procedures 17 3.3 Sampling Locations 19 Chapter 4 Laboratory Analyses 22 4.1 Gas Geochemistry Analyses 22 4.1.1 Helium Isotope Analyses 22 4.1.2 Application of Helium Isotope 24 4.1.3 Mass Spectrometer 26 4.1.4 Helium Purification 27 4.1.5 Instrument Errors and Calibration 31 4.1.6 Radon Activity Analyses 32 4.1.7 RAD 7 Radon Detector 34 4.1.8 Experiment Procedure 35 4.1.9 Gas Chromatography (GC) 37 4.2 Hydrochemistry Analyses 40 4.2.1 Oxygen and Hydrogen Isotope 40 4.2.2 Liquid Water Isotope Analyzer (LWIA) 42 4.2.3 Dissolved Ion Analyses 43 4.2.4 Concentration of Dissolved Gas Calculation 44 Chapter 5 Results 45 5.1 Gas Geochemistry 45 5.1.1 Concentration of Dissolved Gas Calculation 45 5.1.2 Radon Activity analyses 48 5.1.3 Helium Isotope Analyses 49 5.2 Hydrochemistry 52 5.2.1 Oxygen and Hydrogen Isotope 52 5.2.2 Anion and Cation Analyses 53 Chapter 6 Discussion 55 6.1 Gas Geochemistry 55 6.1.1 Distribution and Origin of Dissolved Radon 55 6.1.2 Helium Isotope Investigation 60 6.2 Hydrochemistry 65 6.2.1 Oxygen and Hydrogen Isotope 65 6.2.2 Anions and Cations Discussion 68 6.3 Thermal water in Peninsular Malaysia 72 6.3.1 Type I Thermal Water 72 6.3.2 Type II Thermal Water 73 6.4 Flow Pattern of Thermal Spring in Peninsular Malaysia 74 6.5 Origin of Thermal water in Peninsular Malaysia 76 6.5.1 Meteoric Water Origin of Thermal Spring 76 6.5.2 Meteoric-Seawater Mixing Origin of Thermal Spring 81 Chapter 7 Conclusion 87 Reference 89 Appendix 97 | |
dc.language.iso | en | |
dc.title | 馬來西亞半島溫泉水中溶解氣和水化學之研究 | zh_TW |
dc.title | Gas Compositions and Hydrochemistry of Thermal Springs in Peninsular Malaysia | en |
dc.type | Thesis | |
dc.date.schoolyear | 103-2 | |
dc.description.degree | 碩士 | |
dc.contributor.oralexamcommittee | 劉聰桂,呂學諭,陳文福 | |
dc.subject.keyword | 馬來西亞半島,溫泉,水氡,溶解氣體成分,同位素比值, | zh_TW |
dc.subject.keyword | Peninsular Malaysia,Thermal springs,Dissolved gas composition,Water radon,Isotopic composition, | en |
dc.relation.page | 99 | |
dc.rights.note | 有償授權 | |
dc.date.accepted | 2015-08-10 | |
dc.contributor.author-college | 理學院 | zh_TW |
dc.contributor.author-dept | 地質科學研究所 | zh_TW |
顯示於系所單位: | 地質科學系 |
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