• Title/Summary/Keyword: tourmaline

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Mineralogical Study of Sericite in the Daehyun Mine: Formation, Chemistry and Polytype (대현광산 견운모의 생성과정과 화학조성 및 폴리타잎)

  • 이병임;김수진
    • Journal of the Mineralogical Society of Korea
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    • v.11 no.2
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    • pp.69-84
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    • 1998
  • The Daehyun sericite deposit in socheon-myun, Bongwha-gun, Kyungsangbuk-do, Korea, has been formed by the hydrothermal alteration of the Hongjesa granite of Precambrian age, leaving the muscovite granite between ore body and the Hongjesa granite as the wall rock alteration zone. The process of sericitization of granitic rock as well as chemistry and structures of sericites were studied using polarizing microscope, X-ray diffractometer (XRD), electron probe microanalyzer (EPMA) and high resolution transmission electron microscope (HRTEM). There are two genetic types of sericites having different chemistry and structure. The early sericite is of 2M1 polytype and has octahedral composition close to muscovite. It has been formed from the primary muscovite, tourmaline and quartz under a relatively high temperature. The late sericite is of 1M, 2M1 and 3T polytypes and has phengitic composition. It has been formed form feldspar, biotite, muscovite and tourmaline under a relatively low temperature. Chemical analyses show t, the early sericite has less Mg+FeT content and lower Si/AlIV ratio in tetrahedral site than the late sericite.

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Analysis on the water quality improvement effects by Tourmaline (Tourmaline의 수질개선 효과 분석)

  • Soh, Dea-Wha;Park, Jung-Cheul;Jang, Dong-Hoon;Jung, Jo-Young
    • Proceedings of the Korean Institute of Electrical and Electronic Material Engineers Conference
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    • 2003.05d
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    • pp.113-118
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    • 2003
  • 투어멀린(Tourmaline)은 비대칭 쌍극자를 가진 천연 유극성 결정체로 광물 중에서 영구전기분극을 띄고 있는 유일한 물질로써 일명 "전기석"이라고 알려져 있다. 분극에 의한 자체 미약전류(약 $60{\mu}A$)와 함께 음이온 및 원적외선의 발생으로 최근 우리주변에서 건강과 환경을 위한 관심고조의 대상인 육방정계의 압전성 및 초전성을 띄는 붕규산염(주요성분: Mg, Fe, B, Si, Ca)으로, 투어멀린 원석이나 그 복합세라믹체의 면역지수가 ~1000에서 ~400,000 이상인 점을 비롯하여 그 유용성을 이용하려는 새로운 아이디어 신상품들이 계속 개발되고 있다. 뿐만 아니라 물분자를 만나면 수소$(H^+)$와 수산기 $(OH^-)$로 전기분해 하여 친수기와 소수기 부분으로 구분하며, $H^+$$OH^-$는 각각 $H_2O$와 결합하여 활성이 강한 hydronium ion$(H_3O^+)$을 생성하고, 물 속에서 계속 불안정한 상태로 존재하는 수산기는 계면활성 작용이 있는 hydroxyl ion$(H_3O_2^-)$을 형성하여 물을 약 알카리성 (pH~7.4)으로 바꿔주며, 물분자 클러스터 세분화와 미네랄을 용출, 공급하여 이 물이 체내에 흡수되면 살균, 항균성의 면역기능을 갖게 되며, 혈액정화 기능과 자율신경 자극으로 교감신경의 흥분을 억제해 준다. 이와 함께 전기분극을 띈 투어멀린 입자는 다른 물질에 비하여 경이적 수치의 원적외선을 발생하여 강력한 열 효과와 높은 침투력으로 인체의 혈액순환 촉진과 혈전용해 작용을 주어 건강과 활력에 도움을 주는 것으로 확인되어 많은 관심을 끌고 있다. 따라서 유익한 이용가치를 인정받고 있는 천연 투어멀린을 단독 형태나 또는 서로 상승효과를 줄 수 있는 유용한 타 물질과 혼합물을 구성하여 성형 또는 EPD 방법으로 전착한 후 소결 처리하여, 소결체의 특성 분석과 함께 물에 대한 전기 화학적 작용 및 항균 효과를 조사, 확인하여 수질개선 효과를 분석하고 그 응용성을 개발, 확보하였다.

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Fluid Inclusions Trapped in Tourmaline from the Daeyou Pegmatite Deposit, Jangsu-Gun, Jeollabukdo (전북 장수군 대유 페그마타이트광산의 전기석에 포획된 유체포유물)

  • Lee, Ju-Youn;Eom, Young-Bo;Nam, Bok-Hyun;Hwang, Byoung-Hoon;Yang, Kyoung-Hee
    • Journal of the Mineralogical Society of Korea
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    • v.20 no.1 s.51
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    • pp.7-19
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    • 2007
  • Four types of fluid inclusions are trapped within tourmaline from Daeyou pegmatite, Jangsu-Gun, Jeonllabukdo. They range $5{\sim}100\;{\mu}m$ in size and are grouped into I, II, III, and IV based on the phase behavior at the room temperature: (1) Type I inclusions are liquid-rich and NaCl equivalent salinity ranged $0{\sim}12\;wt%$, and the homogenization temperatures (Th) ranged $181{\sim}230^{\circ}C$ with eutectic temperatures (Te) $-54{\sim}-22^{\circ}C$. (2) Type II inclusions are vapor-rich and salinity ranged $3{\sim}8\;wt%$ NaCl, and Th ranged $177{\sim}304^{\circ}C$ also showing Te $-54{\sim}-29^{\circ}C$. (3) Type III inclusions contain a halite daughter mineral with $31{\sim}40\;wt%$ NaCl, Th $230{\sim}328^{\circ}C$. More than 90% of Type III homogenize by halite dissolution and are spatially associated with silicate melt inclusions. (4) Type IV inclusions are $CO_{2}$-bearing containing various daughter minerals such as sylvite and/or halite. The density of $CO_{2}$ system within the Type IV is $0.80{\sim}0.75\;g/cm^{3}$, Th $190{\sim}317^{\circ}C$, and salinity $2{\sim}35\;wt%$ NaCl. Type III fluid inclusions, considered as the earliest fluid, formed from the fluid exsolved from the crystallizing pegmatite. It is suggested that Type II fluid in the central part of tourmaline were exsolved earlier than Type I fluids in the margin indicating salinity fluctuation during the growth of tourmaline. It implies the fluctuation of the pressure since the salinity of fluid exsolved from the crystallizing melt is governed by the pressure. The last fluid was Type IV, which may be derived from the nearby limestone and metasedimentary rocks. It is suggested that Daeyou pegmatite containing muscovite without miarolitic cavities was formed by the partial melting resulted from the regional metamorphism. Subsequently, the exsolving fluids from the crystallizing melt were trapped in tourmaline at high pressure condition. The exsolved fluids contain various components such as $CaCl_{2}\;and\;MgCl_{2}$ as well as NaCl and KCl. The exsolution began at least at $2.7{\sim}5.3\;kbar\;and\;230{\sim}328^{\circ}C$ with the pressure fluctuation.

The single crystal growth of various colored cubic zirconia for jewelry (다양한 색의 보석용 큐빅 지르코니아 단결정 성장)

  • Nam, Kyung-Ju
    • Journal of the Korean Crystal Growth and Crystal Technology
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    • v.17 no.6
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    • pp.272-276
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    • 2007
  • The various colored cubic zirconia single crystals for jewelry were grown by skull melting method of excellent productivity. The cubic zirconia is similar to the character of diamond, which has high refractive index, large dispersion and high hardness. It is possible that the development of new colored cubic zirconia by doping 3d-transition elements or 4f-rare earth elements. The colored cubic zirconia is representative of synthetic gemstone which was grown up by mixing one or over two materials among $Pr_6O_{11},\;TiO_2,\;MnO_2\;and\;Er_2O_3$ as coloring agent. Subsequent heat treatment improves the quality of color and uniformity. This study is aimed the color reappearance of cubic zirconia such as natural peridot, smoky-quartz and red-tourmaline.

A study on development of spacer fabric air mattress for marine vessels and off shore living room by ILO Convention (국제노동기구협약(ILO)에 의한 선박과 해양시설용 침실의 공기 매트리스의 개발에 관한 연구)

  • Kwon, Ki-Saeng;Nam, Cheol-Woo
    • Proceedings of the Korean Society of Marine Engineers Conference
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    • 2005.06a
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    • pp.700-707
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    • 2005
  • The human being continued the processing of improvement for well being life according to scientific results The other hand, All the seaman life take the rest and sleep in ship's office and living room. In this case, many crew took the pain of back spain or deposit the his fatigue, This will be decrease the productivity owing to crew's back spain or fatigue etc. In this study researched the problem of ship's bed mattress and the principle of Well being air mattress in technical standard etc. Specially decreased some kinds of bacillus, germ and many kinds of bacteria by using of tourmaline which emitted the far red light and negative ion from surface of the mattress. We developed and applied the ship's Well being air mattress to off shore and various kind of ship by International Labour Organization convention 192.

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Properties on Tourmaline Treated-water and it's Disinfection, Suppression Effects of Bacteria Multiplication (투어멀린 처리수의 특성과 세균번식억제 및 살균 작용)

  • Soh, Dea-Wha;Park, Jung-Cheul;Lee, Woo-Sik;Jang, Dong-Hoon
    • Proceedings of the Korean Institute of Electrical and Electronic Material Engineers Conference
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    • 2003.07a
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    • pp.237-242
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    • 2003
  • 투어멀린(Tourmaline)은 비대칭 쌍극자를 가진 유극성 결정체로 광물 중에서 영구적으로 전기분극 특성을 띄고 있는 유일한 물질로써, 일명 "전기석"이라고 알려져 있다. 자체의 미약 전류(약 0,06mA)와 함께 음이온 및 원적외선의 발생으로 최근 우리 주변에서 건강과 환경정화를 위한 관심 대상의 투어멀린은 육방정계의 압전성 및 초전성을 띄는 붕규산염으로, 물분자를 만나면 수소($H^+$)와 수산기($OH^-$)로 분해하여 친수기와 소수기를 구분하여 발생하며, $H^+$$OH^-$는 각각 $H_2O$와 결합하여 활성이 강한 hydronium ion($H_3O^+$)과 계면활성 작용이 있는 hydroxyl ion($H_3O_2^-$)을 생성한다. 물속에서 불안정한 상태로 존재하는 수산기는 hydroxyl (-)ion을 형성하여 약 알카리성($pH{\sim}7.4$)을 띄고, 물의 클러스터(cluster)를 세분화하는 수질개선 기능과 함께 살균, 항균 및 세균번식억제 효과를 갖는 것으로 확인되었다. 따라서 투어멀린 소결체를 활용하여 그 처리수의 특성조사 및 기능개발과 함께 대장균의 번식억제 작용 및 살균작용과 수질개선 기능 등 유용한 결과의 분석으로부터 다양한 응용성을 확보하였다.

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The Efficacy Evaluation of Tourmaline-Ionized Water in Animal Study (투어마린이온활성수의 효능 평가)

  • Yoon, Yang-Suk;Kim, Dong-Heui;Qi, Xu-Feng;Song, Soon-Bong;Jung, Jong-Ho;Joo, Kyung-Bok;Teng, Yung-Chien;Lee, Kyu-Jae
    • Applied Microscopy
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    • v.39 no.4
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    • pp.311-317
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    • 2009
  • This study was performed using animals to confirm the effect of tourmaline-ionized water (TIW) the properties of which were changed by tourmaline energy and electric discharge. In the ICR mice fed high-fat diet, body weight increasing rate of the TIW-treated group (Exp) was generally decreased and moreover exhibited significance at 11th week (P<0.05) compared with the control (Con) group fed distilled water, although water intake of the Exp group was lower than that of the Con group. In the ICR mice with $CCl_4$-induced hepatotoxicity, AST and ALT activities of the Exp group were not significant but showed some decreasing trend, and histological damage of liver was less compared with thatof the Con group. On the study of ethanol-induced hangovers in Sprague-Dawley rat, blood alcohol concentration was significantly decreased (P<0.01), activity of GST, antioxidant enzyme related to the alcohol metabolism, was increased in liver tissue (P<0.05), and AST and ALT show a tendency to be decreasedin the Exp group. These results suggest that drinking TIWhas not only some obesity preventing effect but also an alcohol detoxification effect and liver protecting effect in vivo. It is supposed due to a structural change of water cluster and a property which maintains the changed structure through tourmaline energy and electric discharge. Therefore, TIW has a potentiality to be developed as functional water with several beneficial effects as well as for daily drinking, but further study on the mechanism related with efficacy will be necessary.

Characteristic comparison analysis of the green tourmalines from Myanmar and other deposits (미얀마와 타산지 녹색 투어말린의 특성비교 분석)

  • Kim, Kyung-Jin;Chung, Chae-Min;Ahn, Yong-Kil
    • Journal of the Korea Academia-Industrial cooperation Society
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    • v.15 no.1
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    • pp.39-46
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    • 2014
  • The green tourmalines from Kayah state, Myanmar were investigated by WD X-ray fluorescence, UV-vis, and mid-infrared spectroscopy for comparison to tourmalines of other deposits. The group of tourmaline was calculated and classified by chemical analysis. The samples belonged to the Calcic group and Uvite. The green tourmalines showed a strong absorption band at 415 and 611 nm. The presence of $V^{3+}$ ions is responsible for these absorption bands. Combination of the stretching and bending mode by the vibration between cationic and hydroxyl units (metal-OH) are observed in the 4600 ~ 4200 $cm^{-1}$.

The Study of Age Determination Using Stepwise Dissolution Technique (단계적 용해에 의한 연대측정법 연구)

  • 박계헌
    • The Journal of the Petrological Society of Korea
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    • v.10 no.3
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    • pp.133-147
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    • 2001
  • Recently developing method of age determination using stepwise dissolution technique to expand the applicability of absolute age determination significantly is evaluated whether it is applicable to the Korean samples. The materials selected for the study are uranium-bearing black slates from Changni Formation of Ogcheon metamorphic belt, tourmaline separated from Naedeongni granite of Yeongnam massif, garnet and ilmenite separated from ilmenite-bearing anorthositic rock of Yeongnam massif, scheelites from Ogbang mine, and magnetite separated from Gyemyeongsan Formation of Ogcheon metamorphic belt. For the stepwise dissolution, various acid steps with different normalities and different durations were applied to leach the samples. The leachate from each step was analyzed to determine the Pb isotopic composition and concentrations of Pb and U using thermal ionization mass spectrometer. The black slates from the Changni Formation and the tourmaline from the Naedeongni granite reveal significant variation of Pb isotopic composition, which reveals the potential of such stepwise dissolution technique as a dating method. The behaviors of uranium and lead during the each stage of step leaching are different, which seem to reflect the differences in positions within the crystal lattices depending upon mineral species.

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Mineralogy of Nodules in the Milyang Pyrophyllite Deposit, Gyeongsangnamdo, South Korea (밀양 납석광상에서 산출되는 단괴의 광물조성)

  • Moon, Hi-Soo;Lee, Kangwon;Song, Yungoo
    • Economic and Environmental Geology
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    • v.26 no.4
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    • pp.455-464
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    • 1993
  • Some nodules occur in the Milyang pyrophyllite deposit which are hydrothermal alteration products by Late Cretaceous andesitic tuff. These nodules are divided into two types on the basis of mineral assemblages; diaspore and pyrophyllite nodules. The diaspore nodules consist mainly of diaspore, kaolinite, pyrophyllite and pyrite with a small amounts of wavellite and tourmaline. They are light purplish grey in color, ellipsoid in shape and range 1 cm to 15 cm in size. A small or large diffuse band exists in some nodules. The platy coarse-grained diaspore is intergrown with the fine-aggregated kaolinite in the central part of the nodule. It appears that the grain size become fine from center to margin. The pyrophyllite nodules, which have the same shape with diaspore nodules, consist dominantly of pyrophyllite accompanied by small amounts of quartz, kaolinite, svanbergite, wavellite, tourmaline and apatite. Chemical compositions of alteration zones and nodules show that the wall rock alteration involved mainly the removal of large quantities of silica and alkalies and small quantities of Ca, Mg and Fe. The sharp increase in the Al content of the nodules is the result of residual concentration of alumina by the leaching of the mobile components. The pyrophyllite nodules were formed in the fluid saturated with quartz as ${\mu}_{HK_{-1}}$ and ${\mu}_{H_{2}O}$ increase. Under this condition, the pyrophyllite-kaolinite-quartz assemblage was stable. Diaspores formed from pyrophyllites in the fluid undersaturated with quartz as ${\mu}_{H_{2}O}$ increases (decreasing temperature). Under this condition, diaspore-pyrophyllite-kaolinite assemblage become stable. The formation temperature of the nodules on the basis of mineral assemblage is estimated as $275{\sim}340^{\circ}C$.

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