• Journal of the Mineralogical Society of Korea
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• 제17권1호
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• pp.23-35
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• 2004

The weathering characteristics of periodically submerged sedimentary rocks in the Sayeon dam, Ulsan was examined by field work, electron probe micro-analysis, X-ray diffraction, and X-ray fluorescence spectrometry. Analysis of fracture zone and exfoliation showed the submerged sedimentary rocks have undergone severe mechanical weathering. Mechanical weathering in the water-rock interface accelerated chemical weathering, such as dissolution and alteration of the most of minerals except for quartz in the weathering zone. The dissolution of carbonates specially calcite, is remarkable creating the cavities, whereas formation of minerals including clay minerals is not active. The sedimentary rocks have been periodically submerged for a certain period of time, and have repeated freezing and thawing. This mechanical weathering favored infiltration, which accelerated mineral dissolution. The high content of easily soluble carbonate of the sedimentary rocks is likely the major cause of intense chemical weathering. The dissolved elements within the infiltrated water interrupted the occurrence of clay and weathering minerals, and expend fractures by infiltrated water accelerated weathering process.

• Journal of the Mineralogical Society of Korea
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• 제14권1호
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• pp.1-11
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• 2001

미국 메사추세츠 북중부에 산출되는 데본기 리틀톤층(Littleton Formation)의 남정석-십자석-석류석대에서 채취한 석류석 반상변정의 화학적 누대구조는 여러 번의 성장 단계를 경험했음을 보여준다. 석류석 반상변정들은 비대칭적이고 불규칙적인 Mn, Mg, Ca의 누대구조를 보인다. 조직대 경계부에서 석류석 성분들은 단면선에 따라 그 형태가 다르게 나타나고, $X_{Mn}$ 과 Fe/(Fe+Mg)비의 역전 누대구조는 석류석내의 내부엽리의 발달과 밀접한 관계를 보여준다. 이런 관찰 사항들은 석류석 누대구조가 석류석을 형성/소모시키는 반응뿐만 아니라, 용해작용과 침전작용과 관련된 기존의 미세구조에 의해 변화되었음을 의미한다. 화학적 그리고 조직적 잘림구조의 관계 그리고 저자가 제안한 석류석 성장모델은 석류석 누대구조가 엽리의 발달 동안 전단 응력대에서 일어나는 선택적 용해작용과 압축 운동대에서 발생하는 침전작용에 의해 조절되었음을 지시한다.

• The Korean Journal of Petroleum Geology
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• 제3권1호
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• pp.16-27
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• 1995

The Early Miocene Temblor Formation forms an important sandstone reservoir at Kettleman North Dome oil field, California. Sandstones are mostly arkosic in composition except deepest sandstones containing much volcanic rock fragments. Arranged in paragenetic sequence prior to feldspar alteration, the Temblor sandstones contain cements of early calcite, dolomite, quartz, albite, mixed-layer ohloriteismectite (C/S) and smectite, and anhydrite. Diagenetic changes associated with feldspar are albitization of plagioclase, late calcite and laumontite cementation and grain replacement, plagioclase dissolution, and kaolinite cementation. Plagioclase albitization and late calcite and laumontite cementation in Temblor sandstones occurred at the time of maximum burial with temperatures up to $130^{\circ}C$. Volcanic plagioclases were selectively albitized. Most diagenetic changes are interpreted to have occurred before the maior uplift which occurred within the last one million years ago. Since then to the time of hydrocarbon emplacement plagioclase dissolution and kaolinite cementation occurred. This reaction occurred in relatively closed system due to the occurrence of kaolinite next to the site of plagioclase dissolution. Unaltered part of volcanic plagioclase and plutonic plagioclase which escaped albitization during maximum burial were preferentially dissolved to make plagioclase porosity. Secondary porosity resulting from dissolution of plagioclase and carbonate and anhydrite cements was mainly produced by formation waters containing organic acids released during atagenesis of organic matter.

• Journal of the Korean Society of Food Science and Nutrition
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• 제14권4호
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• pp.401-408
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• 1985

The yeast cell wall lytic action of the alkaline AL-protease, which was found out of the crude Zymolyase that a kind of yeast cell wall lytic $endo-{\beta}-1$, 3-glucanase produced from Arthrobacter luteus, was investigated with the viable cells of S. sake and it's cell wall preparation. AL-protease on the lysis of the viable yeast cells showed very low activities with the alone, but the lytic activities were highly increased with the combination of AL-protease and Zymolyase. On the stepwise treatment of the viable yeast cells with AL-protease and Zymolyase, the cells were lysed highly only by the course having a treatment with Zymolyase after pretreatment with AL-protease. Thus synergistic action of AL-protease was not observed with any some commercial enzymes, known as a type of alkaline and serine protease such as AL-protease, and was also found to be affected greatly by the culture conditions and species of the yeast tested. AL-protease caused the release of some peptide and a lot of sugar from the cell wall preparation, but could not lysed the cell wall more than 66%. Whereas Zymolyase could lysed the cell walls almost completely with alone. On the basis of these results, the synergistic action of AL-protease on the lysis of S. sake cells is hypothesized that at first AL-protease bind to the yeast cell surface layer consisting of mannan and protein, and then changes their conformation to facilitate the penetration of Zymolyase from the outside to the inside framework layer constituted of alkali insoluble ${\beta}-1,\;3-glucan$.

• Proceedings of the Korean Society of Applied Pharmacology
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• 한국응용약물학회 1993년도 제2회 신약개발 연구발표회 초록집
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• pp.125-125
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• 1993

Saikosaponin은 한방에서 중요하게 사용되고 있는 시호의 항염증작용 성분으로서 주로 염증의 후기 단계에 작용하고 있다. 그러나 현재 시호는 생약자체로만 사용되고 성분이 약물로서 개발되지 못하고 있다. 그것은 Saikosaponin의 용해성이 극히 저조하여 제제화하기 힘든 때문이다. 연자는 시호 Saponin의 용해성을 증가시킬 목적으로 시호 Saponin의 하나인 saikosaponin-a를 Pyridine 중에서 succinic anhydride와 반응시켜 6"-hemisuccinyl saikosaponin-a를 얻고 이를 THF에 용해한 후 KOH와 반응시킨 후 다량의 THF를 추가하여 hemisuccinyl esler의 potassium염을 합성하였다. 이 화합물의 용해도를 원래의 Saponin과 비교시험하였다.

• Journal of the Korean Geotechnical Society
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• 제27권12호
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• pp.17-25
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• 2011

A fabric of soil media may change due to certain factors such as dissolution of soluble particles, desiccation, and cementation. The fabric changes affect the mechanical behavior of soils. The purpose of this study is to investigate the effects of geo-material dissolution on shear strength. Experiments and numerical simulations are carried out by using a conventional direct shear and the discrete element method. The dissolution specimens are prepared with different volumetric salt fraction in sand soils. The dissolution of the specimens is implemented by saturating the salt-sand mixtures at different confining stresses in the experimental study or reducing the sizes of soluble particles in the numerical simulations. Experimental results show that the angle of shearing resistance decreases with the increase in the soluble particle content and the shearing behavior changes from dilative to contractive behavior. The numerical simulations exhibit that macro-behavior matches well with the experimental results. From the microscopic point of view, the particle dissolution produces a new fabric with the increase of local void, the reduction of contact number, the increase of shear contact forces, and the anisotropy of contact force chains compared with the initial fabric. The shearing behavior of the mixture after the particle dissolution is attributed to the above micro-behavior changes. This study demonstrates that the reduction of shearing resistance of geo-material dissolution should be considered during the design and construction of the foundation and earth-structures.

• Journal of Energy Engineering
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• 제9권1호
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• pp.41-46
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• 2000

인류가 발생시키는 이산화탄소를 액화시켜 해양에 저장 또는 용해시키는 방법이 지구온나화 현상을 완화시키는 기술로 알려져있으며, 이 방법을 발전시키기위해서는 심해에 분사된 이산화탄소 액적의 용해거동을 정확히 예측하여야한다. 본 연구에서 중층심해 1000m와 1500m 깊이에 분사된 액체 이산화탄소 액적의 용해거동을 계산한 결과, 해저 약 4500m 깊이에서 이산화탄소의 밀도와 용해도가 가장 크게 변하였고, 분사된 이산화탄소는 초기 액적 지름이 각각 0.010m 그리고 0.015m 이하일 때 500m 이하의 깊이에서 완전히 용해되었다. 그리고 해수와 액체 이산화탄소의 접촉면에 생성되는 하이드레이트막이 이산환탄소 용해에 장애물로 작용한다는 것을 확인하였다.

• Journal of the Korean Chemical Society
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• 제34권4호
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• pp.325-330
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• 1990

The solubilities of caffeine in supercritical ammonia were measured at various temperatures and pressures to represent the relationship between the solubility and the density of ammonia at desired temperature and pressure by means of a simple equation. Using the equation, the interaction virial coefficient between ammonia and caffeine has been determined to give the parameters of Lennard-Jones potential function for the system. Furthermore, there are comparisons and discussions of the interaction virial coefficients and Lennard-Jones potential functions determined by the same techniques from the solubility data of naphthalene in supercritical ammonia and of caffeine and naphthalene in supercritical carbon dioxide from existing data sources others.

• Journal of the Speleological Society of Korea
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• 제50호
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• pp.11-16
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• 1997

우리나라의 석회동굴 속에서는 수많은 종류의 동굴미지형과 지물들이 발견되고 있다. 물론 이들의 동굴미지형과 지물들은 그 모두가 석회동굴 속에서 이루어지고 있기 때문에 포괄적으로는 동굴생성물 또는 2차생성물이라고 총칭하기도 한다. 그러나 이들 동굴생성물들 중에는 종유관, 종유석, 석순같이 퇴적작용으로 이루어지는 생성물과 이와는 달리 지하수의 수식작용과 용해작용으로 이루어지는 동굴생성물 즉 동굴미지형 지물들을 따로 구분하여 취급하고자 한다.(중략)

• Journal of the Speleological Society of Korea
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• 제10권11호
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• pp.32-36
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• 1985

석회암처럼 탄산을 내포하고 물에 용해되는 암석으로 형성된 지방에선 유수가 적은 탓에 골짜기가 잘 발달되지 않고 그 대신 여러 가지 특유한 지형이 발달한다. 이 현상을 총칭하여 카르스트(Karst)라고 한다. 따라서 그 곳에서 이루어지는 윤회를 카르스트 윤회라고 한다. 그 곳에 작용하는 영력은 용해에 의하기 때문에 용식이라고 부른다. (중략)