• Journal of the Korean Ceramic Society
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• v.32 no.6
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• pp.703-709
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• 1995

Octadecylenetrimethylammonium-montmorillonite as an organophilic montmorillonite intercalations complex was formed by cation exchange reaction between Na-montmorillonite and 9-octadecylenetrimethylammonium cation. After drying of this organophilic montmorillonite at $65^{\circ}C$ in high vacuum, the complexes were reacted with various swelling-solutions such as benzene, toluene, o-xylene, pyridine, $\alpha$-picoline, 2-ethyl-pyridine, 2-vinyl-pyridine and styrene, and the corresponding basal spacing obtained were 43.9$\AA$, 54.3$\AA$, 51.7$\AA$, 41.5$\AA$, 42.5$\AA$, 39.9$\AA$, 39.8$\AA$, 44.8$\AA$, respectively.

• Journal of the Korean Ceramic Society
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• v.31 no.3
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• pp.282-290
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• 1994

In this research, the organic salt [RCOOH] Br with long alkyl-chain was synthesized, and the organophilic [RCOOH]-Montmorillonite was formed by cation-exchange-reaction between Na-Montmorillonite and synthesized organic salt [RCOOH] Br. After drying of the organophilic [RCOOH]-Montmorillonite at $65^{\circ}C$ in high vaccum, the experiments for the probability of forming its complexes with various swelling-solutions as dist, water, methanol, ethanol, acetonitrile, propionitrile, butyronitrile, toluene and n-decanol were performed, and the corresponding basal spacings obtained were 17.44$\AA$, 31.86$\AA$, 34.38$\AA$, 30.37$\AA$, 32.39$\AA$, 35.04$\AA$, 14.16$\AA$ and 14.63$\AA$ respectively.

• Journal of the Korean Ceramic Society
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• v.38 no.5
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• pp.431-437
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• 2001

본 연구에서는 양이온 교환반응에 의해 Na-Mont와 R$_{11}$SO$_4$로부터 R$_{11}$SO$_4$-Mont 층간화합물을 합성한 후, 이 R$_{11}$SO$_4$-Mont 층간화합물을 다시 제 4차 유기 양이온인 (Et)$_4$N$^{+}$ 이온 및 (Bu)$_4$N$^{+}$ 이온과 반응시켜 그 거동을 살펴보았다. R$_{11}$SO$_4$-Mont를 (Et)$_4$N$^{+}$이온과 반응시켰을 대보다 (Bu)$_4$N$^{+}$ 이온과 반응시킨 경우에 좀 더 큰 층간거리가 얻어졌다. R$_{11}$SO$_4$-Mont를 (Et)$_4$N$^{+}$이온 및 (Bu)$_4$N$^{+}$과 반응시켜 얻은 층간화합물을 다시 아세토니트릴, 에탄올 및 디옥산과 팽윤반응을 수행한 결과 층간거리가 확장되었으나, 이는 Na-Mont를 R$_{11}$SO$_4$와 48시간 교환 반응시킨 후에 교환용액 하에서 얻은 R$_{11}$SO$_4$-Mont의 층간거리에 불과했다. 원소분석결과, R$_{11}$SO$_4$-Mont와 (Bu)$_4$N$^{+}$를 반응시킬 경우 반응이 반응식 b에 의거 진행되고, (Bu)$_4$N-Mont를 R$_{11}$SO$_4$와 반응시킬 경우에는 반응식 c에 의거 진행됨을 예측할 수 있었다.의거 진행됨을 예측할 수 있었다.

• Journal of the Korean Ceramic Society
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• v.36 no.2
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• pp.151-158
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• 1999

$\varepsilon$-Caprolactame as organic monomer was intercalated in the interlayer space of montmorillonite and polymerized by polymerization reaction so that the inorganic polymer and organic polymer could be combined each other by chemical bonding. The results of X-ray and IR analysis showed that the polymerization reaction of $\varepsilon$-caprolactame between the interlayer spaces has been performed sucessfully. In order to study polymeric reaction product in detail we have isolated the polymerized material from the interlayer space and analyzed it by X-ray diffractometer and IR-Spectrocopy. The comparison of these results with them of the analyses for thee pure polymer which has been synthesized by polymeric reaction of $\varepsilon$-carolactame without montmorillonite showed that the obtained both polymeric materials are the same compounds.

• Proceedings of the Korea Association of Crystal Growth Conference
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• 1996.06b
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• pp.223-237
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• 1996

플라스틱재료의 강도, 인성, 경직성, 탄성 등과 같은 기계적 특성을 개선시켜 주기 위해 kaoline, talc, sand, quartz 등과 같은 규산염을 첨가하여 복합재료를 만들고자 하는 연구가 상당히 활발하다. 이와 같이 다양한 규산염이 복합재료의 강화재 또는 첨가제로 사용되는 반면에, 규산염가운데 공업적으로 이용도가 가장 높은 montmorillonite는 아직도 복합재료의 강화재로 폭 넓게 이용되고 있지 못한 실정이다. 이론적으로 볼 때, 높은 분자량을 지니는 무기고분자 (예; inorganic montmorillonite)와 유기고분자 (organic polymer)를 gkadbk는 실질적인 무기-유기 결합물질의 생성이 가능할 수 있으며, 이에 대한 연구 또한 시도되고 있다. 이렇게 해서 얻게 되는 무기-유기 복합체, 즉 montmorillonite로 강화된 플라스틱 복합재료 bumper를 사용함으로써 접촉 또는 충돌시 충격완화의 효과를 가져 올 수 있어 안정성이 좋아지고, 내파괴성이 높기 때문에 비강화 플라스틱재료보다 더 오래 사용할 수 있으므로 경제성이 좋을 뿐만 아니라, 폐품의 감소로 인해 환경보호에도 일익을 담당할 수 있다. 따라서, 본 연구에서는 이러한 montmorillonite강화 플라스틱 복합체를 얻기 위해 우선 무기-유기 고분자물질의 형성이 가능한가를 조사분석하였다. 이를 위해 먼저 amontmorillonite의 층사이에서 화학반응이 수행될 수 있는 충분한 공간을 얻고자 Na-Montmorillonite 층사이의 Na+-이온을 긴 알킬사슬을 취하는 유기 양이온으로 치환시켜 주었다; 이렇게 해서 얻은 유기양이온-몬트모릴로나이트 층간화합물 (Organic cation-Montmorillonite Intercalations-complex)내에 유기 단분자 (organic monomer)를 추가적으로 삽입시킨 후, montmorilonite의 층내에서 증합반응시켜 고분자화해 줌으로써 무기고분자와 유기고분자가 서로 결합된 무기-유기고분자 결합물질을 형성하고자 하였다. X-선 및 IR-분석결과 층내에서의 유기단분자의 고분자화 반응이 성공적으로 이루어 졌음이 입증되었다.

• The Journal of Engineering Research
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• v.4 no.1
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• pp.109-118
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• 2002

In this research, the cation-exchange-reactions between Na-Montmorillonite and betaine compound, $R_{11}SO_4$, with acid group at the end of alkyl chain were performed under the general condition with dist. water including $CO_2$ and under the different pH-conditions with dist. water without $CO_2$, and their behaviors were observed. As results the exchange reaction under the general condition was perfectly finished after 49 h exchange time, and the basal spacings obtained under the exchange solution and after washing with methanol and drying in high vacuum were 23.6, 17.1 and $15.0\AA$, respectively. The basal spacings obtained under pH-exchange solution after exchange time under different pH-values lied between about 24.7 and $25.6\AA$ independently of the pH-values, and those measured after drying on the air and in high vacuum were about $20.0\AA$ and $13.8~14.4\AA$, respectively.

• Economic and Environmental Geology
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• v.45 no.3
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• pp.317-333
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• 2012

The Yeongweol Group is a Lower Paleozoic mixed carbonate-siliciclastic sequence in the Taebaeksan Basin of Korea, and consists of five lithologic formations: Sambangsan, Machari, Wagok, Mungok, and Yeongheung in ascending order. Sequence stratigraphic interpretation of the group indicates that initial flooding in the Yeongweol area of the Taebaeksan Basin resulted in basal siliciclastic-dominated sequences of the Sambangsan Formation during the Middle Cambrian. The accelerated sea-level rise in the late Middle to early Late Cambrian generated a mixed carbonate-siliciclastic slope or deep ramp sequence of shale, grainstone and breccia intercalations, representing the lower part of the Machari Formation. The continued rise of sea level in the Late Cambrian made substantial accommodation space and activated subtidal carbonate factory, forming carbonate-dominated subtidal platform sequence in the middle and upper parts of the Machari Formation. The overlying Wagok Formation might originally be a ramp carbonate sequence of subtidal ribbon carbonates and marls with conglomerates, deposited during the normal rise of relative sea level in the late Late Cambrian. The formation was affected by unstable dolomitization shortly after the deposition during the relative sea-level fall in the latest Cambrian or earliest Ordovician. Subsequently, it was extensively dolomitized under the deep burial diagenetic condition. During the Early Ordovician (Tremadocian), global transgression (viz. Sauk) was continued, and subtidal ramp deposition was sustained in the Yeongweol platform, forming the Mungok Formation. The formation is overlain by the peritidal carbonates of the Yeongheung Formation, and is stacked by cyclic sedimentation during the Early to Middle Ordovician (Arenigian to Caradocian). The lithologic change from subtidal ramp to peritidal facies is preserved at the uppermost part of the Mungok Formation. The transition between Sauk and Tippecanoe sequences is recognized within the middle part of the Yeongheung Formation as a minimum accommodation zone. The global eustatic fall in the earliest Middle Ordovician and the ensuing rise of relative sea level during the Darrwillian to Caradocian produced broadly-prograding peritidal carbonates of shallowing-upward cyclic successions within the Yeongheung Formation. The reconstructed relative sea-level curve of the Yeongweol platform is very similar to that of the Taebaek platform. This reveals that the Yeongweol platform experienced same tectonic movements with the Taebaek platform, and consequently that both platform sequences might be located in a body or somewhere separately in the margin of the North China platform. The significant differences in lithologic and stratigraphic successions imply that the Yeongweol platform was much far from the Taebaek platform and not associated with the Taebaek platform as a single depositional system. The Yeongweol platform was probably located in relatively open shallow marine environments, whereas the Taebaek platform was a part of the restricted embayments. During the late Paleozoic to early Mesozoic amalgamations of the Korean massifs, the Yeongweol platform was probably pushed against the Taebaek platform by the complex movement, forming fragmented platform sequences of the Taebaeksan Basin.