• 한국토양비료학회지
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• 제43권6호
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• pp.837-843
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• 2010

토양광물 종류별 토양의 점토활성도를 구분하기 위하여 우리나라 390개 토양통을 점토광물과 함수산화광물을 기준으로 점토광물 조성이 다른 7개의 토양을 선정하여 토양광물 종류에 따른 점토의 CEC와 비표면적을 비교하였다. 토양 CEC에 대한 점토의 비가 0.7 이상인 토양은 사암을 모재로 Chlorite를 주광물로 하는 토양, 안산암질반암을 모재로 Smectite를 함유한 토양, 화산재를 모재로 Allophane과 Ferrihydrite가 주광물로 이루어진 토양이었으며, 점토활성도 0.3-0.7인 토양은 회장석을 모재로 Kaolin이 주광물 토양, 하성퇴적토를 모재로 Kaolin, Illite, Vermiculite가 혼합된 토양이었다. 또한 점토활성도 0.3이하인 토양은 화강암 및 화강편마암 모재의 Kaolin을 주광물로 Geothite와 Hematite가 함유된 적황색계 토양, 석회암 모재의 Illite와 Vermiculite를 주광물로 Gibbsite, Geothite, Hematite가 함유된 적황색계 토양이었다. 토양의 점토활성도는 점토의 CEC, 점토의 비표면적과 상관이 있어서 점토활성도가 높은 토양에서는 점토의 CEC가 높고 점토의 비표면적이 넓었다. 따라서 토양의 점토활성도는 기존의 점토광물의 정성과 정량분석을 실시하지 않고도 토양의 일반적인 분석을 통하여 토양 중 점토광물의 조성을 추정하고 토양의 물리-화학적 특성을 예측하는데 유용한 기준이 될 것으로 생각된다.

• 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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• 제44권5호
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• pp.160-165
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• 2007

This research studied the most suitable synthesis condition of mineral pigments of black spinel, which have a stable chromogenic characteristic also ata high temperature of $1400^{\circ}C$ (it is not currently producedin the country) to meet not only functionality of ceramics but also an individual's aesthetic. It was synthesized by the plastic synthetic method on the basis of basic formation of $Fe_2O_3,\;Cr_2O_3$, Quartz, Kaolin, CoO, $MnO_2$, and plasticity was made at $1500^{\circ}C,\;1550^{\circ}C,\;1600^{\circ}C,\;1650^{\circ}C$. We researched the most suitable condition of plasticity and composition which make crystallization of spinel system and chromogenic characteristic close to black in every composition. And for the experiment of application to Zirconia, after adding synthesized pigments to Zirconia and plasticizing them, we analyzed their color and property of matters. The most suitable synthesis conditions of mineral pigments of black spinel system require composition of $Fe_2O_3-32.01%,\;Cr_2O_3-30.47%$, Quartz-9.66%, Kaolin-18.53%, CoO-3.71%, $MnO_2-5.62%$ and condition of plasticity kept for 1 h at $1600^{\circ}C$. When we added pigments synthesized in this way to Zirconia with 5 wt% and plasticized them at $1410^{\circ}C$, the result was that the degree of $strength-32.6kgf/mm^2$, absorptance-0.108%, $luminosity-L^*:37.54,\;color-a^*:1.31,\;b^*:2.61$ and their use suited for artificial jewelry or decoration Zirconia goods.

• 한국토양비료학회지
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• 제48권1호
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• pp.1-7
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• 2015

Global population is expected to reach nine billion in 2050 and the total demand for food is expected to increase approximately by 60 percent by 2050 as compared to 2005. Therefore, it is important to increase crop production in order to meet the global demand for food. Slow release fertilizers have been developed and designed in order to improve the efficiency of fertilizers. Mineral-based slow release fertilizers are useful because the minerals have a crystalline structure and are environmentally friendly in a soil. This review focuses on slow release fertilizers based on montmorillonite, zeolite, and layered double hydroxide phases as a host for nutrients, especially N. Urea was successfully stabilized in the interlayer space of montmorillonite by the formation of urea-Mg or Ca complex, $[(Urea)_6Mg\;or\;Ca]^{2+}$ protecting its rapid degradation in soils. Naturally occurring zeolites occluded with ammonium nitrate and potassium nitrate by molten salt treatment could be used as slow release fertilizer because the occlusion process increased the capacity of zeolites to store nutrients in addition to exchangeable cations. Additionally, surface-modified zeolites could also be used as slow release fertilizer because the modified surface showed high affinity for anionic nutrients such as nitrate and phosphate. Moreover, there were attempts to develop and use synthetic layered double hydroxide as a carrier of nitrate because it has positively charged layers which electrostatically bond nitrate anions. Kaolin was also tested by combining with a polymer or through the mechanical-chemical process for slow release of nutrients.

• 한국건축시공학회:학술대회논문집
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• 한국건축시공학회 2004년도 학술대회지
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• pp.71-76
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• 2004

This paper investigate that the effect of the concrete containing mineral admixtures(pozzolanic materials such as fly-ash, ground granulated blast-furnace slag, silica fume and meta kaolin) on the resistance properties to chloride ion invasion. The purposed testing procedure was applied to the concrete added mineral admixtures for $3\sim4$ replacement ratios under W/B ratios ranged from 0.40 to 0.55. Specimens were immersed in $3.6\%$ NaCl solution for 330 days, and penetration depth, water soluble chloride contents and acid soluble chloride contents were measured in 28, 91, 182 and 330 days. Then, diffusion coefficient were calculated using total chloride contents. As a results. the kinds of mineral admixture and replacement ratios had a great effect on the resistance property of the concrete to chloride ion invasion compared with the plain concrete. And the optimal replacement ratios of mineral admixture had a limitation for each admixtures. The amount of acid soluble chloride ions and water soluble chloride ions were varied with the kinds of mineral admixtures and the penetration depth from the concrete skin. Chloride diffusion coefficient of each concretes decreased with the time elapsed. and the diffusion coefficients of the concrete immersed salt water for 330 days had a establishment with the compressive strength measured before immersing.

• 한국광물학회지
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• 제5권1호
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• pp.22-31
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• 1992

습식체질법, 퇴적법 및 원심분리법을 이용하여 얻어진 산청고령토의 9개 입도분리시료에 대하여 체계적인 X-선 회절 및 주사전자현미분석을 시행한 결과, 각 입도분의 점토광물 조성은 고령토의 원조직과 관련이 있음을 알 수 있었다. 침전작용에 의하여 생성된 10-$\AA$ 형 할로이사이트, 일라이트 및 침철석은 미세입도분에 농집되고 모광물의 가상으로 생성된 버미큘라이트는 굵은 입도분에 농집된다. 침전작용 및 가상으로 생성된 다양한 유형의 캐올리나이트는 넓은 입도 분포를 보이지만 일반적으로 굵은 입도분에 농집된다. 굵은 입도분의 할로이사이트는 고령토 원래의 방상구조의 파편들인 할로이사이트 또는 하로이사이트와 캐올리나이트의 덩어리들로 존재하며 분쇄, 초음파처리 및 화학처리에 의해 분산되지 않은 것들이다. 체계적인 습식입도분리 실험에 의하여 10-${\AA}$형 할로이사이트와 캐올리나이트의 구분도 가능하였다. 버미큘라이트와 캐올리나이트 등의 굵은 광물은 2${\mu}m$ 이하의 점토입도분에서는 검출되지 않는 반면 일라이트 및 침철석은 그 양이 적은 경우 원시료만의 X-선 회절분석에서는 검출되지 않는다. 따라서 고령토의 광물조성을 이해하기 위해서는 체계적인 습식입도분리 실험이 필수적이다.

• 한국결정성장학회지
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• 제15권5호
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• pp.202-207
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• 2005

Kaolin과 규석 및 $Mg(OH)_2$등의 원료로 만들어진 slip을 casting 할 때 slip의 점도가 slip casting 속도와 소결체의 미세조직에 미치는 영향을 보면 slip-casting속도는 slip의 점도가 낮을 경우 감소하였으며 slip의 점도범위는 $3.0\~17.0\;cP$가 적당하였다. Slip의 점도를 조절하면 표면층, 표면 내부층, 중간층, 내면층의 미세조직을 비교적 균일하게 casting 할 수 있다 소성온도 $1350^{\circ}C$에서 시편의 구성광물은 cordierite 결정만으로 되어있었다.

• Geomechanics and Engineering
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• 제33권1호
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• pp.113-120
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• 2023

Coastal and offshore structures such as ports and offshore wind farms will often need to be built on fine-grained sediments. Geotechnical properties associated with sediment compressibility are key parameters for marine construction designs especially on soft grounds, which involve clay-mineral dominated fines that can consolidate and settle significantly in response to engineered and environmental loads. We conduct liquid limit tests and 1D consolidation tests with fine-grained soils (silica silt, mica, kaolin and bentonite) and biogenic soils (diatom). The pore fluids for the liquid limit tests include deionized water and a series of brines with NaCl salt concentrations of 0.001 m, 0.01 m, 0.1 m, 0.6 m and 2.0 m, and the pore fluids for the consolidation tests deionized water, 0.01 m, 0.6 m, 2 m. The salt concentrations help the liquid limits of kaolin and bentonite decrease, but those of diatom slightly increase. The silica silt and mica show minimal changes in liquid limit due to salt concentrations. Accordingly, compression indices of soils follow the trend of the liquid limit as the liquid limit determined the initial void ratio of the consolidation test. Diatoms are more likely to be broken than clastic sediments during to loading, and diatom-rich sediment is therefore generally more compressible than clastic-rich sediment.

• 한국세라믹학회지
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• 제32권7호
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• pp.777-782
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• 1995

The scale up production test for the hydrothermal synthesis of clay mineral from the anorthite, which is distributed in San Chung-District of Korea and called as the ground rock for halloysite-kaolin, has been investigated by using the gaitator type reactor. The automatic control system has been developed and applied for the more effective producibility and the reduction in the defect of this intermittent batch processing property, and finally for the feasibility of this system in actual use. It was observed that this agitator type reactor can reduce the synthesis reaction tme from 5 days to 3 days, only with the condition of 20rpm. The automatic control system could regulate the vessel temperature and pressure precisely at an optimum condition during the treatment. Therefore, from these test results the application-possibility for this system was found to be feasible in actual use.

• Spatial Information Research
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• 제14권1호
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• pp.129-150
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• 2006

본 연구에서는 GIS 및 확률 기법을 이용하여 광상의 위치와 지질, 지화학 및 지구물리 자료들 간의 상관관계를 분석하고, 광상부존가능도(Mineral potential map) 작성 및 검증을 수행하였다. 연구지역은 1:25만 강릉도폭지역 a이며, 구축된 데이터베이스 자료는 1:25만 광상분포도, 지화학도, 지질도, 부우게 중력이상도, 자력이상도이다. 본 연구에 사용된 광상은 퇴적기원의 비금속광상(고령토, 도석, 규석, 운모, 연옥, 석회석, 납석)이다. 원소별 지화학도 작성은 채취된 각 시료 3,595개의 원소별 분석치를 이용하여 IDW 보간법으로 만들었다. 구축된 지화학도는 Al, Alkalinity, As, Ba, Ca, Cd, Co, Cr, Cu, Fe, K, Li, Mg, Mn, Mo, Na, Ni, Pb, Si, Sr, V, W, Zn, $Cl^-,\;F^-,\;{NO_2}^-,\;{NO_3}^-,\;{PO_4}^{3-},\;{SO_4}^{2-}$, pH, Eh 및 Conductivity로 총 32개이다. 이러한 광상과 관련 요인들 간의 상관관계는 확률기법인 weight of evidence를 적용하여 계산하였고, 이를 바탕으로 광상부존가능도를 작성하였다. 광상부존가능도는 wieght of evidence의 W+와 W- 값을 GIS 중첩분석에 적용하여 작성하였다. 계산된 광상부존가능지수는 기존 광상부존가능성을 정량적으로 설명하고 표현하며 검증할 수 있는 값이다. 각 기법을 이용하여 작성한 광상부존가능도의 검증결과는 85.66%의 정확도를 나타내었다.