• 한국토양환경학회지
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• 제4권1호
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• pp.57-68
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• 1999

흔한 토양구성 광물인 일라이트(illite), 카올린 광물의 일종인 할로이사이트(halloysite), 제올라이트(clinoptilolite), 침철석(goethite)을 흡착제로 사용하여 산성용액 중에 존재하는 중금속원소들의 흡착특성을 비교하여 검토하였다. 금속원소의 흡착반응은 반응시간과 광물종에 따라서 다양한 특성을 보여 준다. 1주 또는 2주 동안 반응한 용액과 초기 용액간에는 존재하는 화학종들의 변화는 거의 없는데, 이는 개개의 원소들의 화학종의 변화를 수반하지 않으면서 처음의 상태와 비슷한 비율로 진행되고 있음을 나타낸다. 모든 광물에서 흡착되어 제거율이 가장 높은 원소는 Fe와 As이며 흡착반응은 광물의 종류와 중금속원소의 종류에 따라서 다양하지만 1시간 내에 대부분 일어난다. 중금속흡착은 전체적으로 보면 할로이사이트가 가장 효과적인 흡착능력을 보여준다. 한편 알칼리원소의 흡착은 수화반경에 의하여 예측되는 경향을 잘 따르지 않는다.

• The Journal of Advanced Prosthodontics
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• 제8권3호
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• pp.167-171
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• 2016

PURPOSE. This study inspects the effect of incorporating halloysite nanotubes (HNTs) into polymethyl methacrylate (PMMA) resin on its flexural strength, hardness, and Young's modulus. MATERIALS AND METHODS. Four groups of acrylic resin powder were prepared. One group without HNTs was used as a control group and the other three groups contained 0.3, 0.6 and 0.9 wt% HNTs. For each one, flexural strength, Young's modulus and hardness values were measured. One-way ANOVA and Tukey's test were used for comparison (P<.05). RESULTS. At lower concentration (0.3 wt%) of HNT, there was a significant increase of hardness values but no significant increase in both flexural strength and Young's modulus values of PMMA resin. In contrast, at higher concentration (0.6 and 0.9 wt%), there was a significant decrease in hardness values but no significant decrease in flexural strength and Young's modulus values compared to those of the control group. CONCLUSION. Addition of lower concentration of halloysite nanotubes to denture base materials could improve some of their mechanical properties. Improving the mechanical properties of acrylic resin base material could increase the patient satisfaction.

• 한국세라믹학회지
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• 제32권6호
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• pp.735-747
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• 1995

The synthesis of clay mineral through the hydrothermal reaction of the anorthite, which is distributed in San Chung-District of Korea and called as the ground rock for halloysite-kaolin, has been investigated. It was observed that this anorthite sample was easily converted into clay mineral with 0.5 wt% HCl solution at a temperature below 20$0^{\circ}C$ under a pressure about 15 atm. The conversion reaction was promoted by adding aluminum chloride under the condition concerned. Aluminum chloride was considered to supply the insufficient aluminum ion during the conversion reaction and to reprepare the acid solution-condition by adding the HCl-component as a by-product. According to the electron micrographs, it was confirmed that fine tubular or needle-shaped halloysite-kaolin minerals with the crystal length shorter than about 1.1${\mu}{\textrm}{m}$ could be obtained by the hydrothermal reaction for 5 days under those conditions.

• 한국세라믹학회지
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• 제14권2호
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• pp.82-87
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• 1977

The material used in this experiment is Ha-Dong kaolin whichis composed of almost crystallographically pure meta-halloysite. It was grinded and passed through 250 mesh and 325 mesh. It was treated with oxalic acids and EDTA which are different in concentration. The samples in conical beaker were kept in laboratory incubator at $25^{\circ}C$ for a certain hours. The treated samples were stirred twice a day. The sample in the conditions as A-7 was kept in an autoclave under the pressure of 3 atmospheric. The samples suspended in each solution were kept for 1.5, 3 and 6 months. The transformation of crystals was detected by X-ray spectrometer, electron microscopy, and infrared spectrometer. The sample through 325 mesh compared with one through 250 mesh was transformed much more. It took for 6 months to transfer from halloysite to kaolinite in EDTA, and 3~4 months under 3 atms in autoclave at the same condition. In oxalic acids it took more than 6 months.

• 한국세라믹학회지
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• 제30권1호
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• pp.41-45
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• 1993

synthesis of artificial kaolinite and the transformation of domestic halloysite have been attempted by means of the hydrothermal treatment. The hydrothermal reaction of the mixtures of gibbsite and amorphous silica was conducted for the synthesis of kaolinite under the pressure of 125MPa at 30$0^{\circ}C$ and especially the seed of kaolinite was added so as to facilitate the synthesis reaction. Domestic pink kaolin of B-grade was hydrothermally treated, in a similar way, for the transformation of crystalline form of it. Boehmite and the artificial kaolinite less than 0.4${\mu}{\textrm}{m}$ could be obtained through the hydrothermal reaction. It could also be found that the majority of hyalloysite was transformed into the plate-type kaolinite through the recrystallization by treating hydrothermally for a long time.

• 한국세라믹학회지
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• 제17권1호
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• pp.13-19
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• 1980

Mineral identifications on halloysite in Hadong-Sancheong area and the halloysite bearing clay ii Yeoju, Yesan and Hampyeong-Muan area are carried out by the method of X-ray diffraction, electron microscopy and DTA. Chemical composition of the above minerals are analyzed by means of X-ray-fluorescence. Refractoriness are also measured by refractoriness tester. A standard diagram for quantitative analysis of halloysite is given.

• 한국광물학회지
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• 제13권3호
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• pp.121-137
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• 2000

공주군 유구 일대의 화강암질편마암은 온대습윤기후의 지형적 영향에 기인한 산성환경 및 양호한 배수조건에서의 풍화작용으로 두께가 8m인 깊은 saprolite층과 50cm 이상의 두꺼운 토양층을 형성하였다. 풍화단면에서는 흑운모/질석혼합층 광물, 삼팔면체, 할로이사이트, 캐올리나이트, 일라이트, 이팔면체질식, 스백타이트, 깁사이트, 침철석 등의 풍화광물이 확인되었다. 흑운모의 변질은 질석화작용이 미약한 반면에 풍화단면 전반에서 고령토화작용이 매우 현저한 풍화양상을 보여주며, 흑운모-흑운모/질석 혼합층 광물-질석, 흑운모-할로이사이트, 캐올리나이트, 깁사이트 및 흑운모-일 라이트의 풍화과정을 나타낸다. 흑운모의 풍화작용으로 생성된 고령토광물은 주로 할로이사이트이며, 고령토화작용으로 방출된 Fe는 변질된 흑운모 주변에서 침철석을 형성한다 사장석은 용해-침전작용으로 관상의 할로이사이트를 형성한다. 할로이사이트의 산출양상은 사장석의 용해유형에 따라 방향성이 강한 할로이사이트 집합체와 매우 구불구불한 할로이사이트 집합체로 나타난다. 모암에서 철을 함유하고 있던 광물은 용해되어 모암광물의 가상을 유지한 채 또는 그 주변에서 침철석을 형성한다. 연구지역 화강암질편마암의 단면은 풍화도가 증가할수록 모암 구성광물이 감소하는 반면에 점토광물의 양이 증가하는 전형적인 풍화 양상을 보여주며, 광물의 풍화작용은 산성환경과 양호한 배수환경과 같은 지역적인 조건에 영향을 받아 복잡하고 다양한 풍화광물을 형성하였다.

• 한국광물학회지
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• 제17권2호
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• pp.157-168
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• 2004

수용액 내 캐올리나이트와 할로이사이트의 표면화학 특성을 전위차 적정 실험과 FITEQL3.2 프로그램을 이용하여 연구하였다. 표면복합반응 모델 중 일정용량 모델을 적용하였으며, 표면을 사면체 자리와 팔면체 자리로 나누어 설정한 2 sites - 3 $pK_{a/s}$ 모델은 캐올리나이트와 할로이사이트의 표면화학 특성을 설명하는데 적합하였다. 두 점토광물 표면은 pH 4 이상에서 음전하를 띄며 pH가 높아질수록 양성자 표면 전하 밀도는 낮아진다. 산성 및 중성 영역에선 Si 사리(≡$SiO^{-}$ )가, 염기성 영역에선 Al 자리(≡$AlO^{-}$)가 양이온을 흡착하는데 중요한 역할을 할 것으로 예상된다. 모델링 결과 캐올리나이트의 경우 $pK_{a2(si)}$ /$^{int}$, p $K_{al(Al) }$ /$^{int}$ /, $pK_{a2}$ $(Al)^{int}$ /는 각각 4.436. 4.564, 및 8.461이며, 할로이사이트의 경우는 각각 7.852, 3.885, 7.084이다. 캐올리나이트의 총 Si 표면자리 농도와 총 Al 표면자리 농도는 0.215와 0.148 mM이며, 할로이사이트의 경우는 0.357과 0.246 mM이다 두 광물 모두 Si 표면자리 밀도 : Al 표면자리 밀도가 1 : 0.69로 비슷하다. 캐올리나이트의 총 표면자리 밀도는 3.774 sites/$nm^2$로 할로이사이트의 2.292 sites/n $m^2$ 값보다 약 1.6배정도 높다.다.

• 산업기술연구
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• 제6권
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• pp.49-55
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• 1986

A rapid and simple test to distinguish halloysite from kaolinite in mineral mixtures has been developed based on differences in the rate and extent of formamide intercalation. The results of quantitative analysis by formamide intercalation reaction GEC contained 90% of kaolin minerals, GEC contained of 86% of halloysite and GYK contained of 59% kaolinite. The extent of formamide intercalation by kaolinite was likely influenced by sample crystallinity.

• 한국세라믹학회지
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• 제15권1호
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• pp.21-27
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• 1978

Hadong Kaolin (Halloysite) was granulated cylindrically and treated with 1N aqueous sodium hydroxide solution for 6-48 hrs at 60-10$0^{\circ}C$. The crystalling structure of surface of the products was studied by X-ray powder diffraction method. The reaction rate of halloysite to sodium A zeolite showed a gradual decrease from surface to inner layer. At the surface layer, the reaction mechanism was observed as first order consecutive reaction as follows: halloysitelongrightarrowamorphous aluminosilicatelongrightarrowsodium A zeolitelongrightarrowhydroxysodalite By applying the above reaction mechanism, the rate constants and activation energies was measured.