• Title/Summary/Keyword: 암석학적 분석

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Petrographic Examination of Aggregates for Concrete from Maewhacheon A, B area (ASTM C 295) (콘크리트를 위한 매화천 A, B 지역 골재의 암석기재학적 시험 (ASTM C 295))

  • 정지곤
    • Journal of the Mineralogical Society of Korea
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    • v.14 no.2
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    • pp.85-98
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    • 2001
  • This study deals with the petrographic examination of aggregates(ASTM C 295) which is one of the methods to diagnose the quality of aggregates for concrete artifacts. A number of examinations including size and sieve analysis, test on the coating material, description of the weathering and contamination condition, petrographic description, and qualitative and quantitative analyses on the rocks and minerals potential to alkali-aggregates reactivity are carried out to examine the quality of aggregates. Petrographic description method examined on the fluvial aggregates from Maewhacheon A, B area, Uljin-gun, Kyungnam province shows that weathering grade ranges from F(fresh) to WS(slightly weathered) and coating material and contamination are not in a harmful condition. The weight percentage of the alkali-aggregates reactive minerals or structurally unstable rocks of the aggregates from study area covers 26% and 19% of all aggregates, respectively. So it is necessary to further identify their quality through the chemical(ASTM C 289) and mortar-bar method (ASTM C 227).

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가평지역에서 발견된 철운석에 대한 암석학적, 광물학적 기재 및 예비분류

  • An In-Su;Kim Tae-Gyeong;Choe Byeon-Gak
    • 한국지구과학회:학술대회논문집
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    • 2006.02a
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    • pp.111-115
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    • 2006
  • 최근 경기도 가평지역에서 새로운 철운석이 발견되었으며, 이는 한반도에 낙하(fall) 또는 발견(find)된 운석 중 다섯 번째 기록이다. 가평운석(가칭)은 북위 $37^{\circ}52'08'$, 동경$127^{\circ}27'54'$, 고도 147m 지점에서 발견되었으며, 운석의 분류상 철운석에 속한다. 가평운석의 표면은 지표상에서 풍화를 받은 흔적이 나타나나, 내부는 비드만스태튼 무늬(Widmanstatten pattern)와 같은 철운석의 특징이 잘 보존되어 있다. 가평운석의 암석학적, 광물학적 기재와 분류를 위해 주사전자현미경(Scanning Electron Microscope) 및 전자 현미분석기(electron probe micro-analyzer)를 이용했다. 풍화의 산물인 철산화물이 나타나는 최외각부를 제외하면 가평 운석은 거의 순수한 철-니켈 금속광물(Fe-Ni metal)로 이루어져 있다. 이 중 니켈 함량이 적은 카마사이트(kamacite)가 대부분이며 소량의 태나이트(taenite)가 산출되어 비드만스태튼 무늬를 구성한다. 비드만스태튼 무늬의 특징에 의한 분류에 따르면 가평운석은 중립질 또는 조립질 옥타헤드라이트(octahedrite)에 속한다. 철운석은 화학적으로 열 개 이상의 하부그룹으로 세분되며, 가평운석의 정확한 하부그룹으로의 분류는 친철원소에 대한 미량분석이 추가적으로 필요하다. 가평운석의 냉각률은 $^{\sim}1^{\circ}C/Ma$이하로 나타나며, 이는 가평운석이 천천히 냉각된 비교적 규모가 큰 소행성의 핵에서 유래했음을 지시한다.

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The Study on Weathering Hollows Developed on the Coast of Dapyeong-ri, Sacheon-si (사천시 다평리 해안에서 발달한 풍화혈에 관한 연구)

  • Tak, Hanmyeong
    • Journal of the Korean Geographical Society
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    • v.50 no.5
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    • pp.459-472
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    • 2015
  • Weathering hollows which develop on various rocks are the terrain whose lithological characteristics and formation of the bed rock is under active discussion. The shore in Dapyeong-ri, Sacheon-si has alternation of strata of pelite and sandstone, and the weathering hollows develop on the shore platform and the sea cliff where sandstone is exposed. To analyze the development characteristics of weathering hollows by development of joints, interpenetration of veins and physical and chemical features of the stone, the study conducted a topographic investigation, XRD analysis and an observation using a polarizing microscope. As the result of the investigation and analysis, tafoni and gnamma are spread in the same area and new tafoni is being formed as the existing weathering hollows are destroyed by the expansion and growth of the joint. The vein, which was found to be a quartz vein, may accelerate the development of weathering hollows combining with the joint but may also hamper their growth if the veins are penetrating perpendicularly. It is generally known that weathering hollows develop regardless of the type of rocks, however, the analysis on the lithological features show that the development is limited on the fractured and broken rocks.

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Analysis of Ancient Document and Establishment of Petrological Database for Presumption of Stone Source Area of the Seoul City Wall, Korea (한양도성 석재공급지 추정을 위한 고문헌 분석 및 암석학적 데이터베이스 구축)

  • Jo, Young Hoon;Lee, Chan Hee
    • The Journal of the Petrological Society of Korea
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    • v.24 no.3
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    • pp.193-207
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    • 2015
  • This study analyzed ancient documents and established petrological database through extensive field investigation of provenance sites to presume stone source areas of the Seoul City Wall. By summarizing the ancient documents, the rampart stone was mostly supplied from a stony mountain adjacent to the City Wall in the early Joseon period, whereas the stone was provided from fixed quarry outside the City Wall in the late Joseon period. As a result of the petrological investigation based on quarries recorded in the ancient documents, pinkish granite and leucogranite were distributed as a whole, and the granitoid rocks are similar in mineralogical compositions and geochemical behavior characteristics. However, the pinkish granite with magnetic-series show that the magnetic susceptibility increased from the north slope of Namsan Mountain to Bulamsan Mountain. The leucogranite with ilmenite-series mainly occurred along the boundary between granite and gneiss from Yongmasan Mountain to Inwangsan Mountain. Consequently, the important petrological indicators for presumption of stone source areas are the rock color and the magnetic susceptibility. In addition to the petrological features, the reliability for provenance interpretation should improve considering stone quantities in the quarries, transportation distance and technical skills.

Geochemistry and Petrogenesis of the Badwater Greenstones from Crystal Falls Terrane in Northeastern Wisconsin, U.S.A. (위스콘신주 북동부 지역에 분포하는 Badwater녹암에 대한 지화학적 연구)

  • Wee, Soo-Meen
    • Economic and Environmental Geology
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    • v.29 no.3
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    • pp.281-291
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    • 1996
  • Samples of Badwater greenstones from the Crystal Falls terrane in northeastern Wisconsin have been analyzed for major, trace and rare earth elements. Geochemical characteristics of the rocks provide clues to the petrologic character and paleotectonic environment of basaltic magma generation. They have chemical composition typical of continental tholeiites. The low Mg values and abundances of Ni and Cr indicate that the lavas were extensively fractionated prior to extrusion. The variations of incompatible elements suggest that the rocks were affected by interaction with crustal rocks. The samples least affected by contamination have trace element compositions similar to those of T-type mid-ocean ridge basalts. The parent was modified by crustal contamination process and this process shifted the rock compositions to that of continental tholeiites as the rock evolved. Interpretations of the chemical characteristics of the rocks, based on modem analogs, favor their emplacement in an extensional tectonic regime.

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An Ecological Analysis of Lichens Distributed in Rocks of Coast and Field in U-do by Molecular Technique (분자생물학적 기법에 의한 우도해안과 노지암석에 분포하는 지의류의 생태학적 분석)

  • Gang, Hyeong-Il;Yun, Byeong-Jun;Kim, Seong-Hyeon;Sin, Deok-Ja;Kim, Hyeon-U;Heo, Jae-Seon;Gang, Ui-Seong;O, Gye-Heon;Go, Yeong-Jin
    • Microbiology and Biotechnology Letters
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    • v.32 no.4
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    • pp.334-340
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    • 2004
  • This study was initially performed to obtain fundamental data on lichen distribution depending on environmental condiLichens distributed on coastal rocks atleast 20 m far away from the coast were also investigated. Analyof morphological characteristics and rDNA ITS clones revealed that lichens containing 9 families and 15 genera were distributed in coastal rocks of V-do, while lichens containing 10 families and 14 genera were in field rocks, demonstrating little difference of diversity between both sites. Foliose lichens such as PhaeophysPhyscia, Pyxine belonging to the family Physciaceae were representatives distributed in coastal rocks of V-do, along with Xanthoparmelia belonging to Parmeliaceae, fruticose lichens such as Ramalina to Ramaliand crustose lichen Lecanora to Lecanoraceae. In contrast, foliose lichen Cladonia belonging to the family Cladoniaceae, fruitcose lichen Stereocaulon to Streocaulaceae, and crustose lichen Porpidia to Porpidwere found only on the surface of field rocks. Crustose lichens containing genera Caloplaca, CanDirinaria, Graphis, Rhizocarpon, and Pertusaria were rarely distributed in coastal rocks, and most of them were also found in field rocks.

Estimation of Cerchar abrasivity index based on rock strength and petrological characteristics using linear regression and machine learning (선형회귀분석과 머신러닝을 이용한 암석의 강도 및 암석학적 특징 기반 세르샤 마모지수 추정)

  • Ju-Pyo Hong;Yun Seong Kang;Tae Young Ko
    • Journal of Korean Tunnelling and Underground Space Association
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    • v.26 no.1
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    • pp.39-58
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    • 2024
  • Tunnel Boring Machines (TBM) use multiple disc cutters to excavate tunnels through rock. These cutters wear out due to continuous contact and friction with the rock, leading to decreased cutting efficiency and reduced excavation performance. The rock's abrasivity significantly affects cutter wear, with highly abrasive rocks causing more wear and reducing the cutter's lifespan. The Cerchar Abrasivity Index (CAI) is a key indicator for assessing rock abrasivity, essential for predicting disc cutter life and performance. This study aims to develop a new method for effectively estimating CAI using rock strength, petrological characteristics, linear regression, and machine learning. A database including CAI, uniaxial compressive strength, Brazilian tensile strength, and equivalent quartz content was created, with additional derived variables. Variables for multiple linear regression were selected considering statistical significance and multicollinearity, while machine learning model inputs were chosen based on variable importance. Among the machine learning prediction models, the Gradient Boosting model showed the highest predictive performance. Finally, the predictive performance of the multiple linear regression analysis and the Gradient Boosting model derived in this study were compared with the CAI prediction models of previous studies to validate the results of this research.