• Journal of Conservation Science
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• v.37 no.5
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• pp.525-535
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• 2021

This study identified material properties through scientific analysis on Jikgeumdan(satin with gold threads) from Donggungbi-Wonsam and the gold threads used in the embroidery. The Donggungbi-Wonsam's base of gold threads were estimated to have used mulberry fiber's Korean paper(Hanji) because non-wood-based fibers were observed. The X-ray spectrometer showed that the Tongsuseulan of Donggungbi-Wonsam was a flat gold thread of pure gold and Jikgeumdan of flat silver thread of its Saekdong and Hansam. High sulfur levels were detected in the flat silver thread, which appeared to have formed silver sulfide by either manufacturing process using sulfur or conservation environment. he dragon insignia's embroidery is also described as two types twisted gold threads; pure gold and alloying-gold and silver. while dragon insignia's border line is decorated with a twisted gold thread of pure gold. In particular, it was investigated that adhesives such as an animal glue, a protein-based compound by gas chromatography mass spectrometry. Additionally, XRF and Raman spectroscopy analysis on the mixture substances between the metal surface and the base paper of gold threads identified talc and quartz in the gold threads and Seokganju(hematite) in the flat silver threads.

• Korean Journal of Heritage: History & Science
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• v.45 no.1
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• pp.102-121
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• 2012

The purpose of this study is to verify homoteneity of soil and earthenwares and identify firing temperature of earthenwares excavated from Yeoncheon Hapsuri: two earthenwares of the New Stone Age(YCP-1, YCP-2); two of the Bronze Age(YCP-3, YCP-4); and four of the Three States Age(YCP-4~8). The comparative analysis of soil (YCRM) and the earthenwares displays that soil geochemical patterns were similar to YCP-1, YCP-3, YCP-5, YCP-6, YCP-7 and YCP-8. On the other hand, YCP-2 and YCP-4 did not show the similarity to the one of soil because they had been enriched with MgO by contained talc and chlorite. Based on the absorption rate, specific gravity, structural characteristics and XRD analysis, firing temperature has been estimated: for YCP-7 and YCP-8 was $870^{\circ}C$ or over; for YCP-2 and YCP-4 $800^{\circ}C$ or below; and for YCP-1, YCP-3, YCP-5 and YCP-6 between 800 and $870^{\circ}C$. Mineralogical analysis displays that the geochemical pattern of the soil is coincide with the one around Yeoncheon Hapsuri site, which also shows similarity to the one of earthenwares. Such result persuades that the excavated earthenwares were produced with the soils within the precinct of the archaeological sites.

• Journal of the Mineralogical Society of Korea
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• v.8 no.1
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• pp.29-36
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• 1995

연옥은 구성광물의 조직, 결합양상 및 화학조성 등에 의해 일반적인 투각섬석과 구분되며, 색, 경도 및 인성 등에 의해 등급과 가치가 달라진다. 본 연구에서는 춘천산 연옥을 대상으로 연옥의 물리적 특성(조직, 경도 및 인성) 등의 연구가 수행되었다. 춘천산 연옥은 구성광물인 투각섬석의 조직, 입도 및 공생광물(불순물)의 특성에 따라 세 가지 유형(유형 I, 유형 II, 유형 III)으로 구분된다. 유형 I은 치밀한 극미립의 초미정질(<5$\mu\textrm{m}$) 투감섬석의 치밀한 집합체로서 구성되며, 유형 II와 유형 III은 미정질(10~30$\mu\textrm{m}$) 및 세립 (>50$\mu\textrm{m}$)의 투각섬석 집합체로서 투휘석, 활석, 녹니석 및 사문석 등이 미량으로 함유된다.연옥을 구성하는 세 유형의 투각섬석의 화학조성은 Fe, Al 성분이 유형 III에서 가장 높은 함량(1.07~1.88wt.% FeO, 1.3~2.59wt.% Al2O3)을 나타내며, 유형 II(0.22~0.37wt.% FeO, 0.66~0.77wt.% Al2O3), 유형 I (0.20~0.24wt.% FeO, 0.05~0.12wt.% Al2O3)의 순으로 감소함을 보이고, SiO2 성분은 유형 I (59.13~59.67 wt.%), 유형 II(58.02~59.40wt.%), 유형 III (57.34~58.63 wt.%)순으로 함량이 낮아짐을 알 수 있다.연옥의 미경도(VHN=311~659)와 파괴인성치(2.38$\times$105~5.62$\times$105 dyne.cm-3/2)는 유형 I, 유형 II, 유형 III의 순으로 낮아진다. 이러한 결과는 조직 및 집합구조의 특성과 밀접한 관계를 갖고 있음을 반영한다.

• Economic and Environmental Geology
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• v.24 no.4
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• pp.363-378
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• 1991

Field and microscopic evidence, XRD,EPMA and chemical data suggest that parent rock of talc ore deposits of Yesan district was originated from ultramafic igneous rock. Parent rock can be divided into serpentinized dunite, serpentinized peridotite, metagabbro, amphibolite and hornblende schist. The ore deposits are highly sheared, and show many evidences of hydrothermal alteration and metamorphism at the greenschist and albite-epidote amphibolite facies. The process of steatitization is variable depending upon the composition, and the degree of alteration and metamorphism of the parent rocks. Steatitization can be divided into two processes with or without serpentinization. The parent rocks with serpentinization are serpentinized dunite, serpentinized peridotite and metagabbro, showing the following alteration process; olivine ${\rightarrow}$ serpentine${\rightarrow}$ talc. The rocks without serpentinization are amphibolite and hornblende schist showing the following sequence; hornblende${\rightarrow}$ chlorite${\rightarrow}$ talc. Formation of talc deposits is summarized as following six stages; I) Intrusion of ultramafic rocks, 2) autometamorphism, 3) metamorphism at greenschist and albite-epidote-amphibolite facies, 4) brittle deformation, 5) hydrothermal alteration, 6) purification of low-grade talc by late dyke intrusion.

• Herbal Formula Science
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• v.12 no.1
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• pp.225-246
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• 2004

Objectives: This study has been done to compare the Talcum's composition before and after using processing method and to clarify its quality and naming through the historical herbal books. Methods: I studied the Talcum and processed Talcum by physical and chemical method which contain microscopic analysis, X-ray diffraction analysis, thermal analysis, XRF, ICP, etc, to compare the compositions and its characters. Results: Talcum is a magnesium hydroxidfe(($Mg_3[Si_4O_{10}][OH]_2$)). Talcum contains a main ingredients of MgO 29.03-30.40%(31.70%), $SiO_2$ $62.00{\sim}62.40%(63.50%)$, $H_2O$ $4.40{\sim}4.85%(4.80%)$ and small ingredients, also. Conclusion: A radio-element contents of U, Th contain less than average contents of the lithosphere's U 1.8ppm, Th 7.2ppm. There are two sorts of Talcum which are a northern Talcum(solid Talcu) and southern Talcum(soft Talcum). A northern natural products of Talcum(solid Talcum) are used mostly in korea and china.

• Journal of the Mineralogical Society of Korea
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• v.8 no.2
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• pp.57-72
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• 1995

춘천 지역 선캠브리아기의 구봉산층군 내의 백운석질 대리암에는 광역변성작용의 산물로서 조립질의 투각섬석이 주된 규산염 광물상을 이루며 산출된다. 이들은 배태 층준과 원암의 조성에 따라 두 가지 유형으로 구분된다. : (1) 투각섬석(흑회색)+방해석+백운석+활석, (2)투각섬석(백색)+금운모+백운석+방해석+K-장석, 백색의 투각섬석이 흑회색형보다 상대적으로 높은 Al과 알칼리 함유도를 보이지만, 전반적으로 모두 Mg-단종에 가까운 화학 조성을 갖는다. 투각섬석들이 격자 구조상의 결함 구조를 갖지 않는데 비해서, 금운모는 1M 구조형을 이루고 저면 격자 간격상에 녹니석 단위의 빈번한 개재에 의한 격자상의 구조적 결함이 흔히 관찰된다.방해석-백운석 지온계에 대한 연구와 TWEEQU 프로그램을 이용한 상평형도 작성을 통해서, 투각섬석들은 500~$600^{\circ}C$의 온도 범위, 8kb 정도의 압력 및 Xco2=0.2~0.5 조건에서 생성된 것으로 해석하였다. 이 지역의 투각섬석은 위와 같은 조건에서 지속적으로 평형 상태가 유지되고 상안정도가 증대되므로서, (1) 투휘석을 수반하지 않고, (2) 격자 구조상의 결합을 갖지 않는, (3) 자형의 큰 결정을 이루게 된 것으로 해석된다.

• Herbal Formula Science
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• v.16 no.2
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• pp.31-45
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• 2008

This report describes 54 prescriptions related to the use of Talcum mainly blended prescriptions in Dongeuibogam. The following conclusion were reached through investigations on the prescriptions that use Talcum as a key ingredient. Prescriptions that Talcum was taken as a monarch drug are utilized for 22 therapeutic purposes. In particular, 35.2% of prescriptions appear in the chapter of urine, 7.4% of those appear in the chapter of heat. Prescriptions that utilize Talcum as the main ingredient are used in the treatment of uric disease, gonorrhea, heat disease, febrile disease, and they are also used for treating 16 different types of diseases. Talcum is used in pathogenic factors such as heat, wind with heat, and used in pathology related to the fever of small intestine and bladder. The dosage of Talcum is 3jeon(about 11.25g) to 2.5pun(about 0.94g), however 1jeon(about 3.75g) has been taken the most for clinical application. Ikwonsan is the most useful base prescription which use the Talcum as the main ingredient.

• Journal of Korea Technical Association of The Pulp and Paper Industry
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• v.29 no.4
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• pp.45-52
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• 1997

This study was carried out to investigate the adsorption characteristics of cationic starches onto BKP, BCTMP and talc. Concentration of the unadsorbed cationic starch contained in the supernatant of the pulp or talc slurries was determined using a spectoscopy method and the adsorption isotherm of cationc starch was constructed. When the equilibrium concentration of the cationic starch was low, almost complete adsorption of the starch onto BKP and BCTMP was observed. This indicates that electrostatic attraction is the main driving force for the adsorption of cationc starches onto pulps. BCTMP adsorbed greater amount of cationic starches than BKP since it contained more anionc functional groups on its surface. The adsorption amount of the cationic starch increased as the cationicity of the starches decreased. Surface charge density of the pulp and starch adsorption increased as the pH of the pulp slurry increased. Adsorption amount of the cationic starch onto talc was lower than that onto the pulp due to its low charge density and hydrophobic surface property.

• Economic and Environmental Geology
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• v.33 no.4
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• pp.261-271
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• 2000

In order to evaluate the environmental impact of U anormaly in the drainage system around the Shinbo talc mine area, U contents, their distribution patterns, bioaccumulation and a-radioactivity in stream water, stream sediments and aquatic organisms were investigated. The U contents of stream water attenuated with increasing distance from the mine area. The same attenuation pattern is shown in stream sediments from mine to 0.75 km downstream, although these contain highly enriched U contents (24~83 mg/kg) comparing with the international average concentration of surface soils (0.79~11 mg/kg). However, U content increases abruptly in sediment at 1.5 km downstream, probably due to detrital migration and rediposition of U enriched sediments. Futhermore, enriched U in downstream sediments occur in high proportions of carbonate and Fe-Mn oxide bounded forms, which show high potential of a secondary pollution source. For aquatic organisms, bio accumulation degree of U are in the order: aquatic larvae>black snail>mountain frog>crawfish. Cultured trout by the U enrich groundwater (387 ${\mu}g$/l) shows U accumulation in the part of branchia (CRs 5.25) and bones (CRs 11.2) but not in flesh (CRs 0.03). Total a-radioactivity have been measured in the level as 0.47 nCi/l for groundwater, 2.94~18 nCi/kg${\cdot}$DW for organisms and 93~328 nCi/kg${\cdot}$DW for sediments.

• Journal of Korea Foundry Society
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• v.14 no.1
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• pp.45-51
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• 1994

The possibility of using bulk talc as molding material was reviewed and tested with the measurement of thermal properties and computer simulations. The measured thermal conductivity and heat diffusivity($k{\rho}c$) of talc were $2.4W/m^{\circ}C$ and $6.6{\times}10^6J^2/m^4^{\circ}C^2s$, respectively. Thermal properties of talc could be ranked between those of sand mold and iron mold. Talc transforms into cristobalite and enstatite at $910^{\circ}C$, During the transformation volume and structure change, cracks appear on the surface and distortion occurs. Therefore talc can be used for molding material below $910^{\circ}C$ if carefully treated. Computer simulation was carried out to test whether talc insert could promote directional solidification in sand mold and iron mold. In sand mold, it was possible to achieve directional solidification of thin plate casting with the length to thickness ratio of 15, if both iron insert and talc insert were used. In iron mold, it was possible to achieve directional solidification only with talc insert.